[From the U.S. Government Printing Office, www.gpo.gov]




     z;.\ United States                     In cooperation with
       AN Department of                     South Carolina Agricultural      Soil Survey of
          Agriculture                       Experiment Station and
                                            South Carolina Land Resources
          Soil                              Conservation Commission          Dorchester County
          Conservation
          Service                                                            South               Carolina



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             How To Use This Soil Survey

             General Soil Map

             The general soil map, which is the color map preceding the detailed soil maps, shows the survey area
             divided into groups of associated soils called general soil map units. This map is useful in planning the
             use and management of large areas.

             To find information about your area of interest, locate that area on the map, identify the name of the
             map unit in the area on the color-coded map legend, then refer to the section General Soil Map Units
             for a general description of the soils in your area.

             Detailed Soil Maps

             The detailed soil maps follow the general soil map. These maps can
             be useful in planning the use and management of small areas.


                                                                                            Kok( mo
             To find information about
             your area of interest,
                                                               4

             locate that area on the
                                                            13
             Index to Map Sheets,
             which precedes the soil                     13                                    MAP SHEET
                                             4VI
             maps. Note the number of              11 7.-j- 1-6 4.9
             the map sheet, and turn to                  INDEX TO MAP SHEETS
             that sheet.



                                                                                                   WaF
             Locate your area of                                                        F,     BaC
             interest on the map                                      N                                  AsB
                                                                                       C
             sheet. Note the map unit                                                B@a
                                                                                                              C
             symbols that are in that
             area. Turn to the Index
             to Map Units (see Con-                                                       AREA OF INTEREST
                                                                                  NOTE: Map unit symbols in a soil
             tents), which lists the map                                          survey may consist only of numbers or
             units by symbol and                                                  letters, or they may be a combination
             name and shows the                                                   of numbers and letters.
                                                                                                 c@







             page where each map                  MAP SHEET
             unit is described.


             The Summary of Tables shows which table has data on a specific land use for each detailed soil map
             unit. See Contents for sections of this publication that may address your specific needs.






















                                    This soil survey is a publication of the National Cooperative Soil Survey, a
                                  joint effort of the United States Department of Agriculture and other federal
                                  agencies, state agencies including the Agricultural Experiment Stations, and
                                  local agencies. The Soil Conservation Service has leadership for the federal
                                  part of the National Cooperative Soil Survey.
                                    Major fieldwork for this soil survey was completed in 1985. Soil names and
                                  descriptions were approved in 1985. Unless otherwise indicated, statements in
                                  this publication refer to conditions in the survey area in 1985. This soil survey
                                  was made cooperatively by the Soil Conservation Service, South Carolina
                                  Agricultural Experiment Station, and the South Carolina Land Resources
                                  Conservation Commission. It is part of the technical assistance furnished to the
                                  Dorchester Soil and Water Conservation District.
                                    Soil maps in this survey may be copied without permission. Enlargement of
                                  these maps, however, could cause misunderstanding of the detail of mapping.
                                  If enlarged, maps do not show the small areas of contrasting soils that could
                                  have been shown at a larger scale.
                                    All programs and services of the Soil Conservation Service are offered on a
                                  nondiscriminatory basis, without regard to race, color, national origin, religion,
                                  sex, age, marital status, or handicap.

                                    Cover: The ruins of St. George's Anglican Church In Old Fort Dorchester State Park are
                                  on Chisolm fine sand, 0 to 6 percent slopes. This church was one of the first structures built
                                  In the town of Dorchester.











            Contents


            Index to map units            ........................................................ iv       Wildlife habitat       ............................................................. 48
            Summary of tables             ........................................................v         Engineering          .................................................................. 49
            Foreword        ......................................................................... vii Soil properties        ............................................................... 55
            General nature of the county               .........................................1           Engineering index properties               ...................................... 55
            How this survey was made                 ............................................2          Physical and chemical properties                  .............................. 56
               Map unit composition             ..................................................3         Soil and water features             ............................................... 57
            General soil map units              .................................................5          Engineering index test data               ........................................ 58
                                                                                                         Classification of the soils              ............................................ 59
               Broad land use considerations                 .................................. 11       Soil series and their morphology                 ................................... 59
            Detailed soil map units              ................................................ 13     Formation of the soils              .................................................. 89
            Prime farmland           .............................................................. 39      Factors of soil formation            ............................................. 89
            Use and management of the soils                        ............................ 41          Morphology of the soils              .............................................. 91
               Crops and pasture           ....................................................... 41    References              ..................................................................... 93
               Woodland management and productivity                         .................  44        Glossary        .......................................................................... 95
               Recreation            .................................................................... 46 Tables  ..............................................................................  101


            Soil Series


            Albany series            ................................................................... 59 Jedburg series       ................................................................. 73
            Alpin series      ....................................................................... 60 Johns series            ..................................................................... 74
            Blanton series           .................................................................. 61 Leon series           ........................................................................ 74
            Bonneau sE?ries          ................................................................ 61 Lumbee series           ................................................................. 75
            Brookman series          .............................................................. 62   Lynchburg series           ............................................................. 76
            Capers series            ................................................................... 62 Lynn Haven series          .......................................................... 76
            Chipley series           ................................................................... 63 Mouzon series        ................................................................. 77
            Chisolm sEries           ................................................................. 63 Nakina series          ................................................................... 78
            Coosaw SE!ries           ................................................................. 64 Noboco series          .................................................................. 78
            Coxville series          .................................................................. 65 Ocilla series         ...................................................................... 79
            Daleville sories         ................................................................. 65 Ogeechee series           ............................................................. 80
            Echaw series             .................................................................... 66 Osier series: ... 80
            Elloree series           ................................................................... 67 Pantego series       ................................................................. 81
            Emporia series           ................................................................. 67 Pelham series          .................................................................. 81
            Eulonia series           .................................................................. 68 Plummer series        ................................................................ 82
            Foreston series          ................................................................ 69 Rains series            ..................................................................... 82
            Foxworth series          ............................................................... 70  Rutlege series          .................................................................. 83
            Goldsboro series           ............................................................. 70  Seagate series          ................................................................. 84
            Grifton series           ................................................................... 71 Wahee series         ................................................................... 84
            Handsboro series            ............................................................ 72  Yauhannah series            ............................................................ 85
            Izagora series           .................................................................. 72 Yemassee series           ............................................................. 86

                                                                                        Issued January 1990









             Index to Map Units

             AbA-Albany fine sand, 0 to 2 percent slopes                            ........... 13        Hb-Handsboro muck                  .................................................... 25
             ApB Alpin fine sand, 0 to 6 percent slopes                        ............... 14         Hp-Haplaquents, loamy                 ................................................ 25
             BIA-Blanton fine sand, 0 to 2 percent slopes                           ........... 14        IzA-Izagora silt loam, 0 to 2 percent slopes                       .............. 25
             BIB-Blanton fine sand, 2 to 6 percent slopes                           ........... 15        IzB-Izagora silt loam, 2 to 6 percent slopes                       .............. 26
             BoA-Bonneau fine sand, 0 to 2 percent slopes                           ........   15         Jd-Jedburg loam              ........................................................... 26
             BoB-Bonneau fine sand, 2 to 6 percent slopes                           ........   16         JoA-Johns loamy sand, 0 to 2 percent slopes                             ......... 27
             Br-Brookman clay loam, frequently flooded                          .............. 16         Le-Leon sand             ................................................................ 27
             Ca-Capers sifty clay loam                ............................................ 18     Lm-Lumbee fine sandy loam, occasionally flooded.                                  28
             ChA-Chipley sand, 0 to 2 percent slopes                         .................. 18        Ln-Lynchburg loamy sand                    ........................................... 28
             CoB-Chisolm fine sand, 0 to 6 percent slopes                           .........  18         Ly-Lynn Haven fine sand                  ............................................. 29
             Cs-Coosaw loamy fine sand                   ........................................ 19      Mo-Mouzon fine sandy loam, occasionally flooded..                                 29
             Cx-Coxville loam            ........................................................... 19   Na-Nakina fine sandy loam                   ......................................... 30
             Da-Daleville silt loam            .................................................... 20    NoA-Noboco loamy sand, 0 to 2 percent slopes                                ..... 30
             Ec-Echaw fine sand              ...................................................... 20    OcA-Ocilla sand, 0 to 2 percent slopes                        ..................... 31
             Eo-Elloree loamy fine sand, occasionally flooded                            ....  21         Og-Ogeechee fine sandy loam                       ................................... 32
             EpB-Emporia loamy fine sand, 2 to 6 percent                                                  Os-Osier loamy fine sand, frequently flooded                          ........... 32
                   slopes    ........................................................................ 21  Pa-Pantego sandy loam                  ............................................... 33
             EuA-Eulonia fine sandy loam, 0 to 2 percent                                                  Pe-Pelharn sand             ............................................................ 33
                   slopes    ........................................................................ 22  Pm-Plummer loamy sand                    ............................................. 34
             EuB-Eulonia fine sandy loam, 2 to 6 percent                                                  Ra-Rains sandy loam                 ................................................... 34
                   slopes    ........................................................................ 22  Ru-Rutlege loamy fine sand, frequently flooded                            ....... 34
             FoA-Foreston loamy fine sand, 0 to 2 percent                                                 Se-Seagate sand               .......................................................... 35
                   slopes    ........................................................................ 23  Wa-Wahee fine sandy loam                     ........................................ 35
             FxB-Foxworth fine sand, 0 to 6 percent slopes                          ........   23         YaA-Yauhannah loamy fine sand, 0 to 2 percent
             GoA-Goldsboro loamy sand, 0 to 2 percent slopes. 24                                                 slopes     ........................................................................ 36
             Gr-Grifton fine sandy loam, frequently flooded                         .........  24         Ye-Yemassee fine sandy loam                       ................................... 36























             iv









         Summary of Tables

                                       Temperature and precipitation (table 1)                    ........................................................... 102
                                       Freeze dates in spring and fall (table 2)                   .......................................................... 103
                                                           Probability. Temperature.
                                       Growing season (table 3)               ................................................................................... 103
                                       Acreage and proportionate extent of the soils (table 4)                            ................................ 104
                                                           Acres. Percent.
                                       Land capability classes and yields per acre of crops and pasture (table
                                          5)   ....................................................................................................................... 105
                                                           Corn Soybeans Tobacco Wheat Oats Bahlagrass
                                                           Improved bennudagrass.
                                       Capability classes and subclasses (table 6)                      .................................................... 108
                                                           Total acreage. Major management concerns.
                                       Woodland management and productivity (table 7)                             ......................................... 109
                                                           Management concerns. Potential productivity. Trees to
                                                           plant
                                       Recreational development (table 8)                   .................................................................. 113
                                                           Camp areas. Picnic areas. Playgrounds Paths and trails.
                                                           Goff fairways.
                                       Wildlife habitat (table 9)           ..................................................................................... 116
                                                           Potential for habitat elements Potential as habitat for-
                                                           Openland wildlife, Woodland wildlife, Wetland wildlife.
                                       Building site development (table 10)                   ................................................................ 119
                                                           Shallow excavations. Dwellings without basements.
                                                           Dwellings with basements. Small commercial buildings.
                                                           Local roads and streets. Lawns and landscaping.
                                       Sanitary facilities (table 11)            ................................................................................ 122
                                                           Septic tank absorption fields Sewage lagoon areas
                                                           Trench sanitaly landfill Area sanitaly landfill. Dally cover
                                                           for landfill.
                                       Construction materials (table 12)                 ...................................................................... 126
                                                           Roadfill Sand Topsoll
                                       Water management (table 13)                   ........................................................................... 129
                                                           Limitations for-Pond reservoir areas, Embankments,
                                                           dikes, and levees; Aquifer-fed excavated ponds. Features
                                                           affecting-Drainage, Irrigation, Grassed waterways-
                                       Engineering index properties (table 14)                     ........................................................... 133
                                                           Depth. USDA texture. Classification-Unified, AASHTO.
                                                           Percentage passing sle ve-4, 10, 40, 200 Liquid 11mit
                                                           Plasticity index.                           ProPerty of CSC Library
                I
                                                                                             US DepartME)nt of conunerce
                                                                                              NOAA Cc)@@u3t@,l serviccos center Library                                                  v
               C=                                                                             2234 Sour-h @"ob:joz-, Lvenue
                                                                                              Charleston, SC 29405-2413























                                           Physical and chemical properties of the soils (table 15)                            ............................... 138
                                                               Depth Clay Moist bulk density. Permeability. Available
                                                               water capacity Soil reaction Salinity Shrink-swell
                                                               potential. Erosion factors. Wind erodibility group. Organic
                                                               matter
                                           Soil and water features (table 16)                 ..................................................................... 141
                                                               Hydrologic group Flooding High water table. Risk of
                                                               corrosion.
                                           Engineering index test data (table 17)                    ............................................................. 144
                                                               Classification. Grain-size distribution. Liquid limit. Plasticity
                                                               index.
                                           Classification of the soils (table 18)                .................................................................. 145
                                                               Family or higher taxonomic class.
































             ~vi
 










       Foreword


                                This soil survey contains information that can be used in land-planning
                            programs in Dorchester County, South Carolina. It contains predictions of soil
                            behavior for selected land uses. The survey also highlights limitations and
                            hazards inherent in the soil, improvements needed to overcome the limitations,
                            and the impact of selected land uses on the environment.
                                This soil survey is designed for many different users. Farmers, foresters,
                            and agronomists can use it to evaluate the potential of the soil and the
                            management needed for maximum food and fiber production. Planners,
                            community officials, engineers, developers, builders, and home buyers can use
                            the survey to plan land use, select sites for construction, and identify spacial
                            practices needed to insure proper performance. Conservationists, teache-rs,
                            students, and specialists in recreation, wildlife management, waste disposal,
                            and pollution control can use the survey to help them understand, protect, and
                            enhance the environment.
                                Great differences in soil properties can occur within short distances Some
                            soils are seasonally wet or subject to flooding. Some are too unstable to be
                            used as a foundation for buildings or roads. Clayey or wet soils are poorly
                            suited to use as septic tank absorption fields. A high water table makes a soil
                            poorly suited to basements or underground installations.
                                These and many other soil properties that affect land use are described in
                            this soil survey. Broad areas of soils are shown on the general soil map. The
                            location of each soil is shown on the detailed soil maps. Each soil in the survey
                            area is described. Information on specific uses is given for each soil. Help in
                            using this publication and additional information are available at the local office
                            of the Soil Conservation Service or the Cooperative Extension Service.


                            Billy R. Abercrombie
                            State Conservationist
                            Soil Conservation Service


















                                                                                                                                  vii






























































                                                        Location of Dorchester County In South Carolina.








     Soil Survey of
     Dorchester County, South Carolina

                   By Robert T. Eppinette, Soil Conservation Service

                   Soils surveyed by Robert T. Eppinette and Randall K. Fowler,
                   Soil Conservation Service, and Warren M. Stuck, South Carolina
                   Land Resources Conservation Commission


                   United States Department of Agriculture, Soil Conservation Service
                   In cooperation with the
                   South Carolina Agricultural Experiment Station and the
                   South Carolina Land Resources Conservation Commission






        DORCHESTER COUNTY is in the southeastern part of              of South Carolina. The others were Charleston and
     South Carolina. The county is about 569 square miles, or         Georgetown. The town's prosperity declined rapidly
     364,000 acres, and has a population of about 65,000. St.         when many of the settlers moved to Midway, Georgia, to
     George, the county seat, has a population of about               establish a new missionary settlement.
     5,000. Summerville, the largest city, has a population of          From about 1700 to 1860, rice plantations flourished
     about 44,000.                                                    along the Ashley River. To escape the swarms of
        Dorchester County is in the Atlantic Coast Flatwoods          mosquitoes breeding in the rice fields, plantation owners
     Major Land Resource Area. Most of the soils in the               built summer homes on the higher, well drained soils in
     county are nearly level. In a few small areas, mainly            the community they later named Summerville. Nearly all
     along major rivers and swamps, the soils are gently              of the rice plantations were destroyed during the Civil
     sloping. The elevation ranges from 3 to 4 feet above sea         War. This, along with the severe storms of the late 19th
     level along the Ashley River to about 120 feet above sea         century, virtually eliminated rice production along the
     level near Reevesville.                                          Ashley River. From about 1880 to 1950, cotton was the
        The county is bounded on the north by Orangeburg              major agricultural crop.
     County, on the east by Berkeley County, on the south     by        Most of the towns in Dorchester County were built
     Charleston County, and is separated from Colleton                along the railroad between Charleston and Branchville.
     County on the west by the Edisto River.                          This was the first commercial railroad in the United
                                                                      States. St. George, the county seat, was a watering
     General Nature of the County                                     station for steam engines hauling freight and passengers
                                                                      between Charleston and Columbia.
        Dorchester County was established in 1867 from parts            Dorchester County has a wide diversity of land use.
     cf Colleton and Berkeley Counties. In 1697, the first            The areas around St. George remain mostly agricultural,
     settlers founded the town of Dorchester on the Ashley            while the Summerville area is experiencing the fastest
     River. This group of settlers, led by the Reverend Joseph        growth in land development in South Carolina. Nearly a
     Lord, came from Dorchester, Massachusetts, seeking               fourth of the land in the county is owned and managed
     religious freedom.                                               by paper companies for pulpwood and timber production.
        The town of Dorchester prospered for about sixty              Several sawmills scattered throughout the county employ
     years and became the third largest town in the Province          hundreds of people.








            2                                                                                                                       Soil Survey



            Climate                                                             the steepness, length, and shape of slopes; the general
                                                                                pattern of drainage; and the kinds of crops and native
              Prepared by the National Climatic Data Center, Asheville, North   plants growing on the soils. They dug many holes to
            Carolina.
                                                                                study the soil profile, which is the sequence of natural
              Dorchester County is hot and humid in summer, but                 layers, or horizons, in a soil. The profile extends from the
            the coast is frequently cooled by sea breezes. Winter is            surface down into the unconsolidated material from
            cool, with occasionally brief cold spells. Rains occur              which the soil formed. The unconsolidated material is
            throughout the year and are fairly heavy; snowfall is rare.         devoid of roots and other living organisms and has not
            Annual precipitation is adequate for all crops. Every few           been changed by other biological activity.
            years a hurricane crosses the area.                                    The soils in the survey area occur in an orderly pattern
              Table 1 gives data on temperature and precipitation               that is related to the geology, the landforms, relief,
            for the survey area as recorded at Summerville in the               climate, and the natural vegetation of the area. Each
            period 1951 to 1981. Table 2 shows probable dates of                kind of soil is associated with a particular kind of
            the first freeze in fall and the last freeze in spring. Table       landscape or with a segment of the landscape. By
            3 provides data on length of the growing season.                    observing the soils in the survey area and relating their
              In winter the average temperature is 48 degrees F,                position to specific segments of the landscape, a soil
            and the average daily minimum temperature is 36                     scientist develops a concept, or model, of how the soils
            degrees. The lowest temperature on record, which                    were formed. Thus, during mapping, this model enables
            occurred at Summerville on February 12, 1973, is 4                  the soil scientist to predict with considerable accuracy
            degrees. In summer the average temperature is 79                    the kind of soil at a specific location on the landscape.
            degrees, and the average daily maximum temperature is                  Commonly, individual soils on the landscape merge
            89 degrees. The highest recorded temperature, which                 into one another as their characteristics gradually
            occurred at Summerville on August 18, 1954, is 106                  change. To construct an accurate soil map, however, soil
            degrees.                                                            scientists must determine the boundaries between the
              Growing degree days are shown in table 1. They are                soils. They can observe only a limited number of soil
            equivalent to "heat units." During the month, growing               profiles. Nevertheless, these observations, supplemented
            degree days accumulate by the amount that the average               by an understanding of the soil-landscape relationship,
            temperature each day exceeds a base temperature (50                 are sufficient to verify predictions of the kinds of soil in
            degrees F). The normal monthly accumulation is used to              an area and to determine the boundaries.
            schedule single or successive plantings of a crop                      Soil scientists recorded the characteristics of the soil
            between the last freeze in spring and the first freeze in           profiles that they studied. They noted soil color, texture,
            fall.                                                               size and shape of soil aggregates, distribution of plant
              The total annual precipitation is 50 inches. Of this, 31          roots, acidity, and other features that enable them to
            inches, or 60 percent, usually falls in April through               identify soils. After describing the soils in the survey area
            September. The growing season for most crops falls                  and determining their properties, the soil scientists
            within this period. In 2 years out of 10, the rainfall in April     assigned the soils to taxonomic classes (units).
            through September is less than 24 inches. The heaviest              Taxonomic classes are concepts. Each taxonomic class
            1-day rainfall during the period of record was 7.9 inches           has a set of soil characteristics with precisely defined
            at Summerville on July 2, 1966. Thunderstorms occur on              limits. The classes are used as a basis for comparison to
            about 56 days each year, and most occur in summer.                  classify soils systematically. The system of taxonomic
              The average seasonal snowfall is 1 inch. The greatest             classification used in the United States is based mainly
            snow depth at any one time during the period of record              on the kind and character of soil properties and the
            was 4 inches.                                                       arrangement of horizons within the profile. After the soil
              The average relative humidity in midafternoon is about            scientists classified and named the soils in the survey
            55 percent. Humidity is higher at night, and the average            area, they compared the individual soils with similar soils
            at dawn is about 85 percent. The sun shines 70 percent              in the same taxonomic class in other areas so that they
            of the time possible in surnmer and 60 percent in winter.           could confirm data and assemble additional data based
            The prevailing wind is from the north-northeast. Average            on experience and research.
            windspeed is highest, 10 miles per hour, in spring.                    While a soil survey is in progress, samples of some of
                                                                                the soils in the area are generally collected for laboratory
            How This Survey Was Made                                            analyses and for engineering tests. Soil scientists
                                                                                interpreted the data from these analyses and tests as
              This survey was made to provide information about the             well as the field-observed characteristics and the soil
            soils in the survey area. The information includes a                properties in terms of expected behavior of the soils
            description of the soils and their location and a                   under different uses. Interpretations for all of the soils
            discussion of the suitability, limitations, and management          were field tested through observation of the soils in
            of the soils for specified uses. Soil scientists observed           different uses under different levels of management.








     Dorchester County, South Carolina                                                                                                 3



     Some interpretations are modified to fit local conditions,          may extend beyond the limits defined for a taxonomic
     and new interpretations sometimes are developed to                  class. Areas of soils of a single taxonomic class rarely, if
     meet local needs. Data were assembled from other                    ever, can be mapped without including areas of soils of
     sources, such as research information, production                   other taxonomic classes. Consequently, every map unit
     records, and field experience of specialists. For example,          is made up of the soil or soils for which it is named and
     data on crop yields under defined levels of management              some soils that belong to other taxonomic classes. In
     were assembled from farm records and from field or plot             the detailed soil map units, these latter soils are called
     experiments on the same kinds of soil.                              inclusions or included soils. In the general soil map units,
        Predictions about soil behavior are based not only on            they are called soils of minor extent.
     soil properties but also on such variables as climate and              Most inclusions have properties and behavioral
     biological activity. Soil conditions are predictable over           patterns similar to those of the dominant soil or soils in
     long periods of time, but they are not predictable from             the map unit, and thus they do not affect use and
     year to year. For example, soil scientists can state with a         management. These are called noncontrasting (similar)
     fairly high degree of probability that a given soil will have       inclusions. They may or may not be mentioned in the
     a high water table within certain depths in most years,             map unit descriptions. Other inclusions, however, have
     but they cannot assure that a high water table will                 properties and behavior divergent enough to affect use
     always be at a specific level in the soil on a specific             or require different management. These are contrasting
     date.                                                               (dissimilar) inclusions. They generally occupy small areas
        After soil scientists located and identified the                 and cannot be shown separately on the soil maps
     significant natural bodies of soil in the survey area, they         because of the scale used in mapping. The inclusions of
     drew the boundaries of these bodies on aerial                       contrasting soils are mentioned in the map unit
     photographs and identified each as a specific map unit.             descriptions. A few inclusions may not have been
     Aerial photographs show trees, buildings, fields, roads,            observed, and consequently are not mentioned in the
     and rivers, all of which help in locating boundaries                descriptions, especially where the soil pattern was so
     accurately.                                                         complex that it was impractical to make enough
     Map Unit Composition                                                observations to identify all of the kinds of soils on the
                                                                         landscape,
        A map unit delineation on a soil map represents an                  The presence of inclusions in a map unit in no way
     area dominated by one major kind of soil or an area                 diminishes the usefulness or accuracy of the soil data.
     dominated by several kinds of soil. A map unit is                   The objective of soil mapping is not to delineate pure
     identified and named according to the taxonomic                     taxonomic classes of soils but rather to separate the
     classification of the dominant soil or soils. Within a              landscape into segments that have similar use and
     taxonomic class there are precisely defined limits for the          management requirements. The delineation of such
     properties of the soils. On the landscape, however, the             landscape segments on the map provides sufficient
     soils are natural objects. In common with other natural             information for the development of resource plans, but
     objects, they have a characteristic variability in their            onsite investigation is needed to plan for intensive uses
     properties. Thus, the range of some observed properties             in small areas.











                                                                                                                                              5




      General Soil Map Units

        The general soil map at the back of this publication                 are well drained. They have a grayish sandy surface
      shows broad areas that have a distinctive pattern of                   layer, a brownish sandy subsurface layer, and a
      soils, relief, and drainage. Each map unit on the general              brownish, yellowish, and grayish loamy subsoil.
      soil map is a unique natural landscape. Typically, a map                  The Osier soils are nearly level and are in
      unit consists of one or more major soils and some minor                drainageways and shallow depressions. These soils are
      soils. It is named for the major soils. The soils making up            poorly drained. They have a grayish sandy surface layer
      one unit can occur in other units but in a different                   and a grayish and brownish sandy underlying material.
      pattern.                                                                  Of minor extent in this map unit are the Blanton,
        The general soil map can be used to compare the                      Chipley, Ocilla, Pelham, Plummer, and Rutlege soils. The
      suitability of large areas for general land uses. Areas of             Blanton soils are on the higher sandy ridges and are
      suitable soils can be identified on the map. Likewise,                 somewhat excessively drained. The Chipley and Ocilla
      areas where the soils are not suitable can be identified.              soils are on lower ridges and side slopes. The Chipley
        Because of its small scale, the map is not suitable for              soils are moderately well drained, and the Ocilla soils are
      planning the management of a farm or field or for                      somewhat poorly drained. The Pelham and Plummer
      selecting a site for a road or a building or other structure.          soils are in drainageways; and shallow depressions and
      The soils in any one map unit differ from place to place               are poorly drained. The Rutlege soils are in
      in slope, depth, drainage, and other characteristics that              drainageways and are very poorly drained.
      affect management.                                                        Most areas of this map unit are woodland. Small
      Dominantly Nearly Level or Gently Sloping Soils On                     cleared patches are used as food plots for wildlife
      Upland Terraces or Small Ridges                                        management or for row crops.
                                                                                The soils of this map unit are suited or not suited to
      I. Albany-Bonneau-Osier                                                row crops. These soils have low nutrient-holding capacity
      Somewhat poorly drained, well drained, and poorly                      and need frequent fertilizing. The soils on sandy ridges
      drained soils that have a thick, sandy surface layer and a             become droughty during dry periods. Conservation tillage
      loamy subsoll or that are sandy throughout                             and cover crops help maintain organic residue near the
        In this map unit, the landscape typically is nearly level            soil surface and improve the soil moisture and nutrient
      to gently sloping ridges or upland terraces dissected by               relationships. The soils at a lower elevation and in
      drainageways. The natural vegetation on the sandy                      drainageways or depressions have problems caused by
      ridges is mostly pine with thick understory vegetation of              wetness. Surface and subsurface drainage systems can
      mostly sweetgum, maple, and oak. The vegetation in the                 reduce these problems.
      drainageways is mostly water-tolerant hardwoods. Some                     These soils are well suited to not suited to use as
      areas that average about 20 acres have been cleared.                   pastureland. The major concerns in management are the
      Only a few dwellings or structures are in areas of this                low nutrient-holding capacity, droughty conditions during
      map unit.                                                              dry periods, and wetness of soils in drainageways and
        This map unit makes up about 8 percent of the survey                 depressions. Proper stocking, pasture rotation, and
      area. It is about 19 percent Albany soils, 12 percent                  restricted grazing during dry or wet periods help keep the
      Bonneau soils, 10 percent Osier soils, and 59 percent                  pasture and soil in good condition.
      soils of minor extent.                                                    These soils are well suited or suited to use as
        The Albany soils are nearly level and are on low sandy               woodland. The major concern in management is the
      ridges and side slopes of upland terraces. These soils                 sandy texture. Using equipment that has wide tracks or
      are somewhat poorly drained. They have a brownish                      enlarged tires can reduce this problem.
      sandy surface layer, a brownish and yellowish sandy                       These soils are well suited to not suited to engineering
      subsurface layer, and a brownish and grayish loamy                     uses related to dwellings and other struciures. Wetness
      subsoil.                                                               is the main limitation. Surface and subsurface drainage
        The Bonneau soils are nearly level to gently sloping                 systems can reduce the problems caused by wetness on
      and are on sandy ridges of upland terraces. These soils                all but the Osier soils.








            6                                                                                                                   Soil Survey



            2. Bonneau-Ocilla-Blantcln                                        are low nutrient-holding capacity, droughty conditions
            Well drained, somewhat poorly drained, and somewhat               during dry periods, and wetness of soils on lower side
            excessively drained soils that have a thick, sandy                slopes and in depressions or drainageways. Proper
            surface layer and a loamy subsoil                                 stocking, pasture rotation, and restricted grazing during
                                                                              dry or wet periods help keep the pasture and soil in
              In this map unit, the landscape typically is concave            good condition.
            upland terraces parallel to drainageways and major                   These soils are well suited or suited to use as
            swamps. Most areas of this map unit are being                     woodland. Moderate equipment limitations and seedling
            developed to residential and commercial uses. The                 mortality caused by the sandy texture are concerns in
            natural vegetation in the drainageways dissecting this            management. The soils on lower side slopes and in
            map unit is mixed pine and hardwood with a thick                  drainageways or depressions also have problems during
            understory of greenbrier, blackberry, and cane. Many              wet periods. Equipment that has wide tires or tracks can
            residential and commercial structures and a few farm              reduce equipment limitations caused by the sandy
            structures are in areas of this map unit. County and city         texture and wetness. Seedling mortality caused by
            roads provide access to all areas.                                droughtiness is reduced if seedlings are planted in
              This map unit makes up about 3 percent of the survey            furrows.
            area. It is about 22 percent Bonneau soils, 18 percent               These soils are well suited to poorly suited to
            Ocilla soils, 12 percent Blanton soils, and 48 percent            engineering uses related to dwellings and other
            soils of minor extent.                                            structures. Wetness is the major concern in management
              The Bonneau soils are nearly level to gently sloping            of soils on lower side slopes and in drainageways.
            and are on upland terraces. These soils are well drained.         Surface and subsurface drainage systems can reduce
            They have a grayish sandy surface layer, a brownish               the problems caused by wetness.
            sandy subsurface layer, and a brownish, yellowish, and
            grayish loamy subsoil.                                            3. Echaw-Leon-Lynn Haven
              The Ocilla soils are nearly level and are on lower side
            slopes on upland terraces. These soils are somewhat               Moderately well drained, poorly drained, and vely Poorly
            poorly drained. They have a brownish sandy surface                drained soils that are sandy throughout
            layer, a brownish and yellowish sandy subsurface layer,
            and a brownish and grayish loamy subsoil.                            In this map unit, the landscape typically is long, sandy
              The Blanton soils are nearly level to gently sloping and        ridges and long, narrow drainageways running parallel to
            are on upland terraces. These soils are somewhat                  the ridges. The natural vegetation is mostly pine on the
            excessively drained. They have a grayish sandy surface            ridges and mixed pine and hardwood in the
            layer, a brownish sandy subsurface layer, and a                   drainageways. Some areas that average about 20 acres
            yellowish and brownish loamy subsoil.                             have been cleared. Only a few dwellings or structures
              Of minor extent in this map unit are the Noboco,                are in areas of this map unit.
            Emporia, Izagora, Albany, Daleville, and Grifton soils.              This map unit makes up about 2 percent of the survey
            The Noboco and Emporia soils are on nearly level ridges           area. It is about 55 percent Echaw soils, 11 percent
            and side slopes and are well drained. The Izagora soils           Leon soils, 9 percent Lynn Haven soils, and 25 percent
            are on nearly level terraces and are moderately well              soils of minor extent.
            drained. Albany soils are on low sandy ridges and are                The Echaw soils are nearly level and are on sandy
            somewhat poorly drained. The Daleville and Grifton soils          ridges. These soils are moderately well drained. They
            are in drainageways and are poorly drained.                       have a grayish sandy surface layer, a brownish sandy
              Most areas of this map unit are in residential or               subsurface layer, and an organic stained, brownish and
            commercial uses. Small areas are cropland or                      black sandy subsoil.
            pastureland. The rest of this map unit, mostly in                    The Leon soils are nearly level and are on lower
            depressions and drainageways, is woodland.                        ridges and side slopes. These soils are poorly drained.
              The soils of this map unit are suited to row crops;             They have a grayish sandy surface layer and subsurface
            however, they have low nutrient-holding capacity and              layer and an organic stained, brownish and grayish
            need frequent fertilizing. The soils on sandy ridges              sandy subsoil.
            become droughty during dry periods. Conservation tillage             The Lynn Haven soils are nearly level and are in long,
            and cover crops help maintain organic residue near the            narrow, shallow depressions or drainageways. These
            soil surface and improve the soil moisture and nutrient           soils are very poorly drained. They have a grayish sandy
            relationships. The soils on lower ridges and in                   surface layer and subsurface layer and an organic
            drainageways or depressions have problems caused by               stained, brownish sandy subsoil.
            wetness. Surface and subsurface drainage systems can                 Of minor extent in this map unit are the Chipley,
            reduce these problems.                                            Foreston, Albany, and Rutlege soils. The Chipley and
              The soils of this map unit are well suited or suited to         Foreston soils are on the sandy ridges and are
            use as pastureland. The major management concerns                 moderately well drained. The Albany soils are at an









      Dorchester County, South Carolina                                                                                                     7



      intermediate elevation and are somewhat poorly drained.                  The Yemassee soils are nearly level and are on low
      The Rutlege soils are in the drainageways and                         ridges. These soils are somewhat poorly drained. They
      depressions and are very poorly drained.                              have a grayish loamy surface layer, a brownish loamy
        About 40 percent of the acreage in this map unit has                subsurface layer, and a grayish loamy subsoil.
      been cleared. Most cleared areas are used for row                        The Chisolm soils are nearly level to gently sloping
      crops. Small cleared patches are used as food plots for               and are on higher ridges. These soils are well drained.
      wildlife management. The rest of this map unit is                     They have a brownish sandy surface layer, a yellowish
      woodland.                                                             sandy subsurface layer, and a brownish and grayish
        The soils of this map unit are suited or not suited to              loamy subsoil.
      row crops. Most of the soils have low nutrient-holding                   Of minor extent in this map unit are the Blanton,
      capacity and need frequent fertilizing. The soils on ridges           Yauhannah, Elloree, and Ogeechee soils. The Blanton
      become droughty during dry periods. Conservation tillage              soils are on the high ridges and are somewhat
      and cover crops help maintain organic residue near the                excessively drained. The Yauhannah soils are on side
      soil surface and improve soil moisture and nutrient                   slopes and lower ridges and are moderately well drained.
      relationships. The soils at a lower elevation and in                  The Elloree and Ogeechee soils are in drainageways
      drainageways or depressions have problems because of                  and are poorly drained.
      wetness. Surface and subsurface drainage systems can                     Most areas of this map unit are woodland. Large
      reduce these problems.                                                sections have been clearcut and planted to pine. Small
        These soils are suited or poorly suited to use as                   areas have been cleared and are in row crops or
      pastureland. Wetness and low nutrient-holding capacity                pasture. Areas near Ashley Phosphate Road are being
      are the major concerns in management. Proper stocking,                developed to commercial and residential uses.
      pasture rotation, and restricted grazing during wet                      The soils of this map unit are well suited or suited to
      periods help, keep the pasture and soil in good condition.            row crops. The soils on ridges are droughty during dry
        These soils are suited or poorly suited to use as                   periods and have low nutrient-holding capacity. The soils
      woodland. Wetness is the major concern in                             on the lower ridges and on side slopes are wet.
      management. Limiting planting and harvesting operations               Conservation tillage and cover crops help maintain
      to drier periods can reduce problems caused by                        organic residue near the soil surface and improve soil
      wetness. On the poorly drained soils, seedling survival               moisture and nutrient relationships. Surface and
      rates improve if seedlings are planted on beds.                       subsurface drainage systems can reduce problems
        These soils are suited or not suited to engineering                 caused by wetness.
      uses related to dwellings and other structures. Wetness                  These soils are well suited to use as pastureland;
      is the main limitation. Surface and subsurface drainage               however, low nutrient-holding capacity and droughtness
      systems can reduce the problems caused by wetness in                  are concerns in management. Proper stocking, pasture
      the Leon soils, but they are not effective for the Lynn               rotation, and restricted grazing during dry periods help
      Haven soils.                                                          keep the pasture and soil in good condition.
      4. Coosaw-Yemassee-Chisolm                                               These soils are well suited or suited to use as
                                                                            woodland. Moderate equipment limitations during wet
      Somewhat poorly drained and well drained soils that                   periods and seedling mortality during dry periods are
      have a sandv or loamy surface layer and a loamy subsoil               concerns in management. Operating equipment during
        In this map unit, the landscape typically is nearly level           dry periods reduce equipment limitations, and planting
      to gently sloping ridges or side slopes on upland                     seedlings in furrows reduce seedling mortality.
      terraces that are dissected by narrow drainageways or                    These soils are suited or poorly suited to engineering
      broad swamps. The natural vegetation is mixed pine and                uses related to dwellings and other structures. Wetness
      hardwood on the ridges and side slopes and mostly                     is the main limitation. Surface and subsurface drainage
      hardwood in the drainageways or swamps. A few areas,                  systems can reduce these problems caused by wetness.
      averaging about 10 acres, have been cleared. Dwellings                5. Goldisboro-Rains-Lynchlburg
      and other structures are along the highways transecting
      areas of this map unit.                                               Moderately well drained to poorly drained soils that have
        This map unit makes up about 3 percent of the survey                a sandy or loamy surface layer and a thick, loamy
      area. It is about 30 percent Coosaw soils, 18 percent                 subsoil
      Yemassee soils, 12 percent Chisolm soils, and 40                         In this map unit, the landscape typically has little relief.
      percent soils of minor extent.                                        It is nearly level upland terraces dissected by shallow
        The Coosaw soils are nearly level and are on side                   drainageways (fig. 1). The natural vegetation is mostly
      slopes and low ridges. These soils are somewhat poorly                hardwoods with a thick understory of greenbrier, cane,
      drained. They have a brownish sandy surface layer and                 and blackberry. Dwellings and farm structures are
      subsurface layer and a yellowish and grayish loamy                    common. County roads provide access to all areas of
      subsoil.                                                              this map unit.







            8                                                                                                                 Soil Survey







                                                                                            Emporia


                                                                                                       I Ile
                                   Goldsboro
                                                       Lynchburg
                                                                                                    Noboco
                               V"                      Rains
                                      S
                                                                    -Pelham
                           Pantego
                                                                                  Bo n n-ea u


                                                                             -A
                                                  Lynchbu g                 A'        sood
                                                                               A'
                                                              V
                                         Goldsboro                                       T
                                                                                    rn,nts
                                                                            r0rioe Sedi
                                                                       Loarny

                                                                          1







                              Figure l.-Typical pattern of soils on upland terraces. The soils formed in loamy marine sediment.



              This map unit makes up about 33 percent of the                 drainageways and are poorly drained. The Pantego and
            survey area. It is about 23 percent Goldsboro soils, 18          Nakina soils are in depressions and drainageways and
            percent Rains soils, 17 percent Lynchburg soils, and 42          are very poorly drained.
            percent soils of minor extent.                                     Most areas of this map unit are cropland. Small areas
              The Goldsboro soils are on broad upland terraces.              are pastureland. The rest of this. map unit, mostly in
            These soils are moderately well drained. They have a             depressions and drainageways, is woodland.
            brownish sandy surface layer and subsurface layer and a            The soils of this map unit are well suited to row crops.
            loamy subsoil that is yellowish and brownish in the upper        Wetness is a limitation; however, surface and subsurface
            part and grayish in the lower part.                              drainage systems can reduce problems caused by
              The Rains soils are in shallow depressions and                 wetness. Residue management increases organic matter
            drainageways on upland terraces. These soils are poorly          content, improves fertility, and helps to maintain tilth.
            drained. They have a grayish loamy surface layer and               These soils are well suited to use as pastureland. The
            subsurface layer and a grayish loamy subsoil.                    major concern in management is wetness, but surface
              The Lynchburg soils are in intermediate positions on           drainage can reduce problems caused by wetness.
            lower ridges on upland terraces. These soils are                 Proper stocking, pasture rotation, and restricted grazing
            somewhat poorly drained. They have a brownish sandy              during wet periods help keep the pasture and soil in
            surface layer, a brownish loamy subsurface layer, and a          good condition.
            grayish loamy subsoil.                                             These soils are well suited to use as woodland. The
              Of minor extent in this map unit are the Bonneau,              major concern in management is wetness. Planting and
            Noboco, Ocilla, Coxville, Grifton, Elloree, Pantego, and         harvesting during drier periods can reduce problems
            Nakina soils. Bonneau and Noboco soils are on higher             caused by wetness. Plant competition can be reduced by
            ridges than the Lynchburg soils and are well drained.            proper site preparation, prescribed burning, spraying of
            The Ocilla soils are on lower ridges and side slopes and         herbicides, or girdling.
            are somewhat poorly drained. The Coxville, Grifton, and            These soils are suited or poorly suited to engineering
            Elloree soils are in shallow depressions and                     uses related to dwellings and other structures. Wetness








       Dorchester County, South Carolina                                                                                                   9



       is the main limitation. Surface and subsurface drainage                These soils are well suited to use as woodland;
       systems can reduce problems caused by wetness.                       however, wetness is a concern in management. Planting
                                                                            and harvesting trees during drier periods can reduce
       6. Jedburg-Daleville-lzagora                                         problems caused by wetness. Plant competition can be
                                                                            reduced by site preparation, prescribed burning, spraying
       Moderately well drained to poorly drained soils that have            of herbicides, or girdling. '
       ï¿½ loamy surface layer and a thick, loamy subsoll that has              These soils are suited or poorly suited to engineering
       ï¿½ high silt content                                                  uses related to dwellings and other structures. Wetness
         In this map unit, the landscape typically is nearly level          is the main limitation. Surface and subsurface drainage
       to gently sloping upland terraces dissected by shallow               systems can reduce problems caused by wetness.
       drainageways and broad, shallow depressions. The
       natural vegetation in the drainageways or depressions is             Dominantly Nearly Level Soils in Major Swamps or
       mixed pine and hardwood with a thick understory of                   on Low Stream Terraces
       greenbrier, cane, and blackberry. Dwellings and farm
       structures are common. County roads provide access to                7. Grifton-Mouzon
       all areas of this map unit.
         This map unit makes up about 14.5 percent of the                   Poorly drained soils that have a loamy surface layer and
       survey area. It is about 25 percent Jedburg soils, 20                a loamy subsoil
       percent Daleville soils, 14 percent Izagora soils, and 41              In this map unit, the landscape typically is nearly level
       percent soils of minor extent.                                       flood plains of major creeks and swamps. The natural
         The Jedburg soils are nearly level and are on broad                vegetation is mostly sweetgum, water oak, swamp
       upland terraces. These soils are somewhat poorly                     chestnut oak, and loblolly pine. Understory vegetation is
       drained. They have a brownish and grayish surface layer,             mostly cabbage palmetto, gallberry, and myrtle. Some
       a brownish loamy subsurface layer, and a grayish loamy               areas that average about 10 acres have been cleared.
       subsoil.                                                             Only a few dwellings or structures are in areas of this
         The Daleville soils are nearly level and are in                    map unit.
       drainageways and shallow depressions on upland                         This map unit makes up about 9 percent of the survey
       terraces. These soils are poorly drained. They have a                area. It is about 43 percent Grifton soils, 20 percent
       brownish loamy surface layer, a grayish loamy                        Mouzon soils, and 37 percent soils of minor extent.
       subsurface layer, and a grayish loamy subsoil.                         The Grifton soils are nearly level and are on flood
         The Izagora soils are nearly level to gently sloping and           plains of major swamps. These soils are poorly drained.
       are on upland terraces. These soils are moderately well              They have a brownish loamy surface layer, a grayish
       drained. They have a brownish loamy surface layer and                loamy subsurface layer, and a grayish loamy subsoil.
       a loamy subsoil that is yellowish and brownish in the                  The Mouzon soils are on low upland terraces. These
       upper part and grayish in the lower part.                            soils are poorly drained. They have a brownish loamy
         Of minor extent in this map unit are the Bonneau,                  surface layer, a grayish sandy subsurface layer, a grayish
       Noboco, Emporia, Mouzon, and Grifton soils. Bonneau,                 loamy subsoil, and a grayish sandy substratum.
       Noboco, and Emporia soils are on higher ridges and side                Of minor extent in this map unit are the Ocilla, Elloree,
       slopes and are well drained. The Mouzon and Griflon                  Osier, and Plummer soils. Ocilla soils are on low sandy
       soils are in major drainageways and swamps and are                   ridges and are somewhat poorly drained. The Elloree,
       poorly drained.                                                      Osier, and Plummer soils are on low side slopes and in
         About a third of the acreage in this map unit is                   drainageways and are poorly drained.
       cropland. Small areas are pastureland. A large part of                 Most of the acreage in this map unit is used for water-
       this map unit near Summerville is being developed and                tolerant trees. A few areas have been clearcut and
       converted to residential uses. The rest of this map unit,            replanted to improved loblolly pine. Other areas have
       mostly in depressions and drainageways, is woodland.                 been cleared and are used as pastureland.
         The soils of this map unit are well suited to row crops;             The soils in this map unit are poorly suited or not
       however, wetness is a limitation. Surface and subsurface             suited to crops, pasture, and engineering uses related to
       drainage systems can reduce problems caused by                       dwellings and other structures. A seasonal high water
       wetness. Residue management increases organic                        table and flooding are the main concerns in
       matter, improves fertility, and helps to maintain tilth.             management.
         These soils are well suited to use as pastureland. The               These soils are well suited or suited to water-tolerant
       major concern in management is wetness. Surface                      trees. The major concerns in management are severe
       drainage can reduce problems caused by wetness.                      equipment limitations and seedling mortality rates.
       Proper stocking, pasture rotation, and restricted grazing            Harvesting and planting trees during dry periods can
       during wet periods help keep the pasture and soil in                 reduce equipment limitations. Equipment that has wide
       good condition.                                                      tires or tracks can operate more efficiently on these wet







           10                                                                                                                         Soil Survey


           soils. Seedling mortality is reduced if seedlings are                 Restricted grazing during wet periods reduces soil
           planted on raised beds.                                               compaction and improves the quality of forage.
                                                                                    The soils of this map unit are well suited or suited to
           8. Mouzon-Brookman-Wahee                                              use as woodland. The major concerns in management
                                                                                 are the moderate to severe equipment limitations and
           Somewhat poorly drained to vely poorly drained soils                  seedling mortality. Harvesting and planting trees during
           that have a loamy surface layer and a loamy and clayey                dry periods reduce equipment limitations, and equipment
           subsoil                                                               that has wide tires or tracks operates more efficiently on
              In this map unit, the landscape typically is nearly level,         the wet soils. Seedling mortality is reduced if seedlings
           broad, low upland terraces, and drainageways. The                     are planted on raised beds.
           natural vegetation is mostly sweetgum, water oak,                        Because of wetness, flooding, and the high shrink-
           swamp chestnut oak, cypress, and loblolly pine.                       swell potential of the clayey subsoil, these soils are
           Understory vegetation is mostly cabbage palmetto,                     poorly suited or not suited to engineering uses related to
           gallberry, and myrtle. Some, areas that average about 10              dwellings or other structures.
           acres have been cleared. Only a few dwellings or
           structures are in areas of this map unit.                             Dominantly Nearly Level Soils on the Edisto River
              This map unit makes up about 21 percent of the                     Flood Plain
           survey area. It is about 40 percent Mouzon soils, 19
           percent Brookman soils, 8 percent Wahee soils, and 33                 9. Chipley-Osier-Lumbee
           percent soils of minor extent.
              The Mouzon soils are on broad low upland terraces.                 Moderately well drained and poorly drained soils that are
           These soils are poorly drained. They have a brownish                  sandy throughout or that have a thin, loamy surface layer
           loamy surface layer, a grayish sandy subsurface layer, a              and subsoll underlain by a sandy substratum
           grayish loamy subsoil, and a grayish sandy substratum.                   In this map unit, the landscape typically is a nearly
              The Brookman soils are in drainageways. These soils                level, broad, flood plain terrace. The natural vegetation is
           are very poorly drained. They have a black loamy                      mostly hardwood in the flooded parts of this map unit
           surface layer and a black and grayish clayey and loamy                and is mixed pine and hardwood on the sandy ridge.
           subsoil.                                                              Most areas of this map unit are owned by large
              The Wahee soils are on low ridges on upland terraces.              companies. Only a very few dwellings or structures are in
           These soils are somewhat poorly drained. They have a                  areas of this map unit.
           brownish loamy surface layer, a brownish loamy
           subsurface layer, and a clayey and loamy subsoil that is                 This map unit makes up about 6 percent of the survey
           brownish in the upper part and grayish in the lower part.             area. It is about 24 percent Chipley soils, 22 percent
              Of minor extent in this map unit are the Eulonia,                  Osier soils, 18 percent Lumbee soils, and 36 percent
           Yauhannah, Yemassee, Coosaw, Grifton, and Elloree                     soils of minor extent.
           soils. Eulonia and Yauhannah soils are on high ridges                    The Chipley soils are on small, rounded or elongated
           and are moderately well drained. The Yemassee and                     ridges. These soils are moderately well drained. They
           Coosaw soils are on low ridges and are somewhat                       have a grayish sandy surface layer. The underlying
           poorly drained. The Grifton and Elloree soils are in                  material is sand that is brownish in the upper part and
           drainageways and are poorly drained.                                  grayish in the lower part.
              Most areas of this map unit are woodland that is                      The Osier soils are in drainageways and depressions
           owned by paper companies. Large areas have been                       adjacent to the Edisto River. These soils are poorly
           clearcut and replanted to improved loblolly pine. The few             drained. They have a grayish sandy surface layer, and
           small cleared areas are used for crops or recreational                the underlying material is grayish and brownish sand.
           purposes.                                                                The Lumbee soils are on broad flood plains. These
              The Mouzon and Brookman soils are not suited to use                soils are poorly drained. They have a grayish loamy
           as cropland or pastureland because of a seasonal high                 surface layer and a grayish loamy subsoil underlain by a
           water table, slowly permeable subsoil, and flooding.                  grayish sandy substratum.
              The Wahee soils are well suited to row crops and                      Of minor extent in this map unit are the Johns,
           small grains; however, wetness and the clayey subsoil                 Yauhannah, Grifton, Ogeechee, Rutlege, and Nakina
           are concerns in management. Drainage systems and                      soils. Johns and Yauhannah soils are on high ridges and
           land shaping reduce problems caused by wetness.                       are moderately well drained. The Grifton and Ogeechee
           Incorporating organic matter into the surface layer helps             soils are in drainageways and on broad terraces and are
           maintain the tilth.                                                   poorly drained. The Rutlege and Nakina soils are in
              The Wahee soils are well suited to use as pastureland;             drainageways and are very poorly drained.
           however, wetness is a concern in management. Surface                     Most areas of this map unit are woodland. Large areas
           drainage can reduce problems caused by wetness.                       have been clearcut and planted in improved loblolly pine.









        Dorchester County, South Carolina



        A few cleared areas, averaging about 40 acres, are in                  Nearly all of the acreage of this map unit is in native
        row crops.                                                          marsh grasses. Some of the more inland areas were
          The soils of this map unit are suited to not suited to            previously used for production of rice.
        row crops. Chipley soils have low nutrient-holding                     The soils of this map unit are not suited to row crops,
        capacity, and fertilizer is needed during the growing               pasture, woodland, or to engineering uses related to
        season. Osier and Lumbee soils are wet and are subject              dwellings and other structures. Flooding is a major
        to flooding. Drainage systems can reduce problems                   hazard that is difficult to reduce. These soils are best
        caused by wetness in the Lumbee soils.                              suited to use as natural habitat for wetland wildlife.
          These soils are well suited to not suited to use as
        pastureland. Wetness and low nutrient-holding capacity              Broad Land Use Considerations
        are major management problems. Drainage systems can                    The soils in Dorchester County vary widely in their
        reduce problems caused by wetness. Split applications               suitability for major land uses. About 15 percent of the
        of fertilizers improve forage quality.                              land is used for cultivated crops, mainly soybeans, corn,
          These soils are well suited or suited to use as                   and small grains. This cropland is scattered throughout
        woodland. Because of wetness, equipment should be                   the county but is concentrated to some extent in general
        operated during drier periods and seedlings need to be              soil map units 5 and 6, which are suited or well suited to
        planted on raised beds.                                             crops. Soils in map units 1, 2, 3, and 4 are dominantly
          These soils are poorly suited or not suited to                    sandy and require more land use treatments for good
        engineering uses related to dwellings and other                     yields. Soils in map units 7, 6, and 9 are in very low
        structures. The major concerns in management are                    areas and are poorly suited or not suited to crops. Some
        wetness and the hazard of flooding in areas adjacent to             of these soils are subject to frequent flooding. They
        the Edisto River. Drainage systems can reduce problems              require intensive land use treatments for satisfactory
        caused by wetness if adequate outlets are available.                yields. Soils in map unit 10 are flooded with salt water
        Dominantly Nearly Level Soils That are Flooded Daily                and are not suited to crops.
        by Sea Water                                                           About 2 percent of the land in the county is pasture.
                                                                            Except for the soils in general soil map units 7 and 10
        10. Capers-Handsboro                                                and parts of 1, 8, and 9, the soils in Dorchester County
                                                                            are well suited to poorly suited to use as pasture. The
        Very poorly drained soils that have a loamy surface layer           high water tables, mild temperatures, and moderately
        and a clayey substratum or that have a mucky surface                high rainfall enhance the suitability of the soils for
        layer underlain by a clayey substratum                              pasture grasses. Soils in map unit 10 are flooded almost
          In this map unit, the landscape typically has little relief.      daily by salt water and are not suited to use as pasture.
        It consists of broad, nearly level areas adjacent to tidal             About 77 percent of the land in the county is
                                                                            woodland. Soils in general soil map units 1, 2, 3, 4, 5, 6,
        creeks or rivers. These soils are flooded regularly by salt         and 9 are well suited or suited to pines. The soils in map
        water. The vegetation is dominantly native marsh                    units 1, 2, 3, and 4 are droughty for pines, but
        grasses, such as black needlebrush, smooth corclgrass,              satisfactory to good yields are common. The soils in map
        and big cordgrass. Most areas have no public roads or               units 7 and 8 are flooded for long periods and are suited
        structures.                                                         only to water-tolerant hardwoods. Soils in map unit 10
          This map unit makes up about 0.5 percent of the                   are flooded with salt water and are not suited to trees.
        survey area. It is about 55 percent Capers soils, 11                   Less than 6 percent of the county is urban or built-up
        percent Handsboro soils, and 34 percent soils of minor              land. Although most of the soils in the county have
        extent.                                                             severe limitations for urban development, small areas in
          The Capers soils are on tidal flats. These soils are              all of the map units except possibly 7 and 10 are suited
        very poorly drained. They have a brownish and black                 to development. The high water table in most of the soils
        loamy surface layer and are underlain by grayish clay.              is the main limitation for urban development. In addition
          The Handsboro soils are in tidal marshes. These soils             to having a high water table, some soils in map units 8
        are very poorly drained. They have a grayish and                    and 9 are frequently flooded.
        brownish mucky surface layer and are underlain by                      Potential for use as habitat for wildlife is generally high
        grayish clayey material.                                            throughout the county. Soils in map units 1, 2, 3, 4, 5,
          Of minor extent in this map unit are the Wahee,                   and 6 generally are suited to use as habitat for openland
        Mouzon, and Brookman soils. The Wahee and Mouzon                    wildlife. Soils in map units 7, 8, and 9 generally are
        soils are on small islands or low ridges. The Wahee soils           suited to use as habitat for woodland wildlife. The soils
        are somewhat poorly drained, and the Mouzon soils are               in map units 7, 8, 9, and 10 are poorly drained and
        poorly drained. The Brookman soils are at the upper end             frequently flooded. These soils provide suitable habitat
        of tidal areas and are very poorly drained.                         for wetland wildlife.










                                                                                                                                          13




        Detailed Soil Map Units

          The map units on the detailed soil maps at the back of              Table 4 gives the acreage and proportionate extent of
        this survey represent the soils in the survey area. The             each map unit. Other tables (see "Summary of Tables")
        map unit descriptions in this section, along with the soil          give properties of the soils and the limitations,
        maps, can be used to determine the suitability and                  capabilities, and potentials for many uses. The Glossary
        potential of a soil for specific uses. They also can be             defines many of the terms used in describing the soils.
        used to plan the management needed for those uses.
        More information on each map unit, or soil, is given                  AbA-Albany fine sand, 0 to 2 percent slopes. This
        under "Use and Management of the Soils."                            soil is on nearly level upland terraces and sandy ridges.
          Each map unit on the detailed soil maps represents an             It is somewhat poorly drained. The areas of this soil are
        area on the landscape and consists of one or more soils             irregular in shape and commonly are 20 to 60 acres.
        for which the unit is named.                                          Typically, the surface layer is dark grayish brown fine
          A symbol identifying the soil precedes the map unit               sand about 7 inches thick. The subsurface layer from a
        name in the soil descriptions. Each description includes            depth of 7 to 26 inches is very pale brown fine sand. It is
        general facts about the soil and gives the principal                brownish yellow fine sand from 26 to 54 inches. The
        hazards and limitations to be considered in planning for            subsoil from 54 to 59 inches is pale brown sandy loam,
        specific uses.                                                      and from 59 to 75 inches, it is gray, mottled sandy clay
          Soils that have profiles that are almost alike make up            loam.
        a soil series. Except for differences in texture of the               Included with this soil in mapping are a few small
        surface layer or of the underlying material, all the soils of       areas of Alpin, Foxworth, and Osier soils. Also included
        a series have major horizons that are similar in                    are a few small areas of soils that have slopes of more
        composition, thickness, and arrangement.                            than 2 percent. The included soils make up about 10
          Soils of one series can differ in texture of the surface          percent of the map unit.
                                                                              This Albany soil is very strongly acid to medium acid
        layer or of the underlying material. They also can differ in        except where lime has been added. Permeability is rapid
        slope, wetness, degree of erosion, and other                        in the surface and subsurface layers and moderate in the
        characteristics that affect their use. On the basis of such         subsoil. The available water capacity is low. The
        differences, a soil series is divided into soilphases. Most         seasonal high water table is 1 foot to 2.5 feet below the
        of the areas shown on the detailed soil maps are phases             surface.
        of soil series. The name of a soil phase commonly                     About 60 percent of the acreage of this soil is
        indicates a feature that affects use or management. For             woodland, and about 20 percent is cropland. The rest is
        example, Bonneau fine sand, 0 to 2 percent slopes, is               pastureland and in engineering uses related to dwellings
        one of several phases in the Bonneau series.                        and other structures.
          Most map units include small scattered areas of soils               This soil is suited to row crops and small grains. The
        other than those for which the map unit is named. Some              seasonal high water table and low nutrient-holding
        of these included soils have properties that differ                 capacity are major management problems. Surface and
        substantially from those of the major soil or soils. Such           subsurface drainage systems help lower the high water
        differences could significantly affect use and                      table. Water control structures generally are needed with
        management of the soils in the map unit. The included               drainage systems to maintain adequate soil moisture
        soils are identified in each map unit description. Some             levels during droughty periods. Subsurface drains
        small areas of strongly contrasting soils are identified by         generally need sand filters to prevent clogging. Because
        a special symbol on the soil maps.                                  of leaching, split applications of fertilizer can help
          This survey includes miscellaneous areas. Such areas              maintain proper plant growth. Residue management,
        have little or no soil material and support little or no            cover crops, and conservation tillage improve natural
        vegetation. Water is an example. Miscellaneous areas                fertility and reduce wind erosion.
        are shown on the soil maps. Some that are too small to                This Albany soil is suited to use as pastureland.
        be shown are identified by a special symbol on the soil             Suitable pasture plants include bermudagrass and
        maps.                                                               bahiagrass. Wetness and low nutrient-holding capacity








          14                                                                                                                        Soil Survey



          are major management problems. Surface drainage can                  large cultivated fields. Stripcropping with close-growing
          lower the high water table. Proper stocking, pasture                 crops reduces soil blowing and protects young plants.
          rotation, and restricted grazing during wet periods help             Conservation tillage, crop residue on or near the surface,
          keep the pasture in good condition.                                  and cover crops increase water infiltration, improve
            This soil is well suited to use as woodland. Suitable              natural fertility, and decrease soil blowing.
          trees include loblolly pine and longleaf pine. Because of               This Alpin soil is suited to use as pastureland. Major
          wetness, equipment use limitations, plant competition,               management problems are droughtiness, low available
          and seedling mortality are moderate. Surface drainage                water capacity, and low nutrient-holding capacity.
          can help lower the high water table and reduce wetness               Bermudagrass and bahiagrass grow well if they are
          problems. Seedlings survive and grow well if competing               properly fertilized and managed. The use of this soil for
          vegetation is controlled or removed. This can be                     pasture or hay is also effective in controlling soil blowing.
          accomplished by site preparation, prescribed burning,                   This soil is suited to use as woodland. Suitable trees
          spraying, cutting, or girdling.                                      include loblolly pine and longleaf pine. Because of the
            This soil is suited to most engineering uses related to            sandy texture, equipment use limitations and seedling
          dwellings and other structures. Wetness is a severe                  mortality are moderate. Seedling mortality can be
          limitation for septic tank absorption fields. Adding                 reduced if seedlings are planted in a furrow. Using
          suitable fill material or increasing the size of the                 equipment that has wide tires or tracks reduces the
          absorption field can reduce this limitation. Wetness is              equipment use limitation.
          also a severe limitation for dwellings without basements.               This soil is well suited to most engineering uses
          Surface drainage can lower the high water table and                  related to dwellings and other structures. Seepage could
          reduce wetness problems. This soil has severe                        be a problem in densely developed urban areas on side
          limitations for lawns and landscaping because of the           low   slopes and where absorption fields are near
          available water capacity and droughtiness during the                 drainageways. Droughtiness is a severe limitation for
          summer. Frequent, light applications of water can reduce             lawns and landscaping. This limitation can be reduced by
          these problems.                                                      regular applications of water.
            This Albany soil is in capability subclass 111w.                      This Alpin soil is in capability subclass IVs.

            ApB-Alpin fine sand, 0 to 6 percent slopes. This                      BIA-Blanton fine sand, 0 to 2 percent slopes. This
          soil is on nearly level to gently sloping upland terraces.     It    soil is on nearly level upland terraces and small ridges
          is excessively drained. The areas of this soil are irregular         adjacent to flood plains. It is somewhat excessively
          in shape and commonly are about 10 to 300 acres.                     drained. The areas commonly are elongated and are
            Typically, the surface layer is brown fine sand about 7            about 10 to 150 acres.
          inches thick. The subsurface layer is very pale brown                   Typically, the surface layer is light brownish gray fine
          fine sand from a depth of 7 to 27 inches and is brownish             sand about 3 inches thick. The subsurface layer from a
          yellow fine sand from 27 to 54 inches. From 54 to 85                 depth of 3 to 44 inches is brown and very pale brown
          inches, it is very pale brown fine sand that has strong              fine sand. The subsoil from 44 to 55 inches is brownish
          brown loamy sand strata that are 0.25 to 1 inch thick.               yellow sandy clay loam and from 55 to 80 inches is
            Included with this soil in mapping are a few small                 yellowish brown sandy clay and sandy clay loam that
          areas of Bonneau, Chipley, and Osier soils. Also                     have gray mottles.
          included are a few small areas of soils that have slopes                Included with this soil in mapping are small areas of
          of more than 6 percent. The included soils make up                   Ocilla, Goldsboro, Osier, Pelham, and Lynn Haven soils.
          about 5 percent of the map unit.                                     The included soils make up about 15 percent of the map
            This Alpin soil is very strongly acid to slightly acid             unit.
          except where lime has been added. Permeability is rapid                 This Blanton soil is very strongly acid to medium acid
          in the upper part of the soil and moderately rapid in the            except where lime has been added. Permeability is rapid
          lower part. The available water capacity is very low. This           in the surface and subsurface layers and moderate in the
          soil does not have a seasonal high water table within 6              subsoil. The available water capacity is low. The perched
          feet of the surface.                                                 seasonal high water table is 5 to 6 feet below the
            About 80 percent of the acreage of this soil is                    surface.
          woodland. The rest is cropland, pastureland, or in                      About 70 percent of the acreage of this soil is
          engineering uses related to dwellings and other                      woodland. The rest is cropland, pastureland, or in
          structures.                                                          engineering uses related to dwellings and other
            This soil is poorly suited to row crops and small grains           structures.
          because of droughtiness, soil blowing, and low nutrient-                This soil is suited to row crops and small grains. Major
          holding capacity. Fertilizers are more efficient to crop             management problems are droughtiness and low
          production if they are applied at intervals rather than in a         nutrient-holding capacity. Irrigation and split applications
          single application. Soil blowing is a moderate hazard in             of fertilizers can reduce these problems. Cover crops








       Dorchester County, South Carolina                                                                                                  15



       and conservation tillage help maintain organic residue               of fertilizers can reduce these problems. Cover crops
       near the soil surface, improve soil moisture and nutrient            and conservation tillage help maintain organic residue
       relationships, and reduce problems caused by wind                    near the soil surface, improve soil moisture and nutrient
       erosion.                                                             relationships, and reduce the hazard of erosion.
          This Blanton soil is suited to use as pastureland.                  This Blanton soil is suited to use as pastureland.
       Suitable pasture plants include bahiagrass and improved              Suitable pasture plants include bahiagrass and improved
       bermudagrass. Major management problems are                          bermudagrass. Major management problems are
       droughtiness and low nutrient-holding capacity. Proper               droughtiness and low nutrient-holding capacity. Proper
       grazing, weed control, and fertilizer improve the quality of         grazing, weed control, and fertilizer improve the quality of
       the forage.                                                          the forage.
          This soil is suited to use as woodland. Loblolly pine is            This soil is suited to use as woodland. Suitable trees
       the dominant tree. Equipment use limitations, plant                  include loblolly pine and longleaf pine. Because of the
       competition, and seedling mortality are moderate. The                sandy texture, equipment use limitations, plant
       sandy texture limits use of equipment, but the limitations           competition, and seedling mortality are moderate.
       can be reduced by using tracks or wide tires on vehicles.            Equipment use limitations can be reduced by using
       Because of the low available water capacity, seedling                tracks or wide tires on vehicles. Because of the low
       survival is lower in areas where understory plants are               available water capacity, seedling survival is lower in
       numerous. Site preparation and planting seedlings in                 areas where understory plants are numerous. Site
       furrows can reduce this limitation.                                  preparation and planting seedlings in furrows can reduce
          This soil is suited to most engineering uses related to           this limitation.
       dwellings and other structures. Wetness is a moderate                  This soil is suited to most engineering uses related to
       limitation for septic tank absorption fields. This soil has          dwellings and other structures. Wetness is a moderate
       only slight limitations for dwellings without basements.             limitation for septic tank absorption fields. This soil has
       Droughtiness is a severe limitation for lawns and                    only slight limitations for dwellings without basements.
       landscaping. This limitation can be reduced by regular               Droughtiness is severe limitation for lawns and
       applications of water.                                               landscaping. This limitation can be reduced by regular
          This Blanton soil is in capability subclass Ills.                 applications of water.
                                                                              This Blanton soil is in capability subclass Ills.
          BIB-Blanton fine sand, 2 to 6 percent slopes. This
       soil is on gently sloping upland terraces and small ridges             BoA-Bonneau fine sand, 0 to 2 percent slopes.
       adjacent to flood plains. It is somewhat excessively                 This soil is on nearly level upland terraces. It is well
       drained. The areas of this soil are elongated and                    drained. The areas of this soil are irregular in shape and
       commonly are 10 to 150 acres.                                        commonly are 10 to 40 acres.
          Typically, the surface layer is light brownish gray fine            Typically, the surface layer is gray fine sand about 3
       sand about 3 inches thick. The subsurface layer from a               inches thick. The subsurface layer from a depth of 3 to
       depth of 3 to 44 inches is brown and very pale brown                 27 inches is very pale brown fine sand. The subsoil from
       fine sand. The subsoil from 44 to 55 inches is brownish              27 to 42 inches is brownish yellow sandy loam, from 42
       yellow sandy clay loam and from 55 to 80 inches is                   to 53 inches is light yellowish brown sandy loam that has
       yellowish brown sandy clay and sandy clay loam that has              gray mottles, and from 53 to 61 inches is light gray
       gray mottles.                                                        sandy clay loam. The substratum from 61 to 80 inches is
          Included with this soil in mapping are small areas of             red sandy loam.
       Ocilla, Goldsboro, Osier, Pelham, and Lynn Haven soils.                Included with this soil in mapping are a few small
       The included soils make up about 15 percent of this map              areas of Blanton, Lynchburg, and Rains soils. Also
       unit.                                                                included are a few areas of soils that have slopes of
          This Blanton soil is very strongly acid to medium acid            more than 2 percent. The included soils make up about
       except where lime has been added. Permeability is rapid              10 percent of the map unit.
       in the surface and subsurface layers and moderate in the               This Bonneau soil is very strongly acid to medium acid
       subsoil. The available water capacity is low. The perched            in the surface and subsurface layers except where lime
       seasonal high water table is 5 to 6 feet below the                   has been added, and it is very strongly acid or strongly
       surface.                                                             acid in the subsoil. Permeability is moderate, and the
          About 70 percent of the acreage of this soil is                   available water capacity is low to moderate. The
       woodland. The rest is cropland, pastureland, or in                   seasonal high water table is 3.5 to 5 feet below the
       engineering uses related to dwellings and other                      surface.
       structures.                                                            About 60 percent of the acreage of this soil is
          This soil is suited to row crops and small grains.    Major       cropland. The rest is woodland, pastureland, or in
       management problems are droughtiness and low                         engineering uses related to dwellings and other
       nutrient-holding capacity. Irrigation and split applications         structures.









          16                                                                                                                       Soil Survey



            This soil is suited to row crops and small grains. Major              About 60 percent of the acreage of this soil is
          management problems are droughtiness and low                         cropland. The rest is woodland, pastureland, or in
          nutrient-holding capacity. Irrigation and split applications         engineering uses related to dwellings and other
          of fertilizers can reduce these. problems. Cover crops               structures.
          and conservation tillage help maintain organic residue                  This soil is suited to row crops and small grains. Major
          near the soil surface, improve soil moisture and nutrient            management problems are droughtiness and low
          relationships, and reduce problems caused by wind                    nutrient-holding capacity. Irrigation and split applications
          erosion.                                                             of fertilizers can reduce these problems. Cover crops
            This Bonneau soil is well suited to use as pastureland.            and conservation tillage help maintain organic residue
          Suitable pasture plants include bahiagrass and improved              near the soil surface, improve soil moisture and nutrient
          bermudagrass. Droughtiness and low nutrient-holding                  relationships, and reduce problems caused by wind
          capacity are'concerns in management. Proper grazing,                 erosion.
          weed control, and fertilizer improve the quality of the                 This soil is well suited to use as pastureland. Suitable
          forage.                                                              pasture plants include bahiagrass and improved
            This soil is suited to use as woodland. Loblolly pine is           bermudagrass. Major management problems are
          the dominant tree. Equipment use limitations, plant                  droughtiness and low nutrient-holding capacity. Proper
          competition, and seedling mortality are moderate. The                grazing, weed control, and fertilizer improve the quality of
          sandy texture limits use of equipment, but these                     the forage.
          limitations can be reduced by using tracks or wide tires                This soil is suited to use as woodland. Loblolly pine is
          on vehicles. Because of the low available water capacity,            the dominant tree. The equipment use limitation, plant
          seedling survival is lower in areas where understory                 competition, and seedling mortality are moderate. The
          plants are numerous. Site preparation and planting                   sandy texture limits use of equipment, but this limitation
          seedlings in furrows reduce this limitation.                         can be reduced by using tracks or wide tires on vehicles.
            This soil is well suited to most engineering uses;                 Because of the low available water capacity, seedling
          however, wetness is a severe limitation for septic tank              survival is lower in areas where understory plants are
          absorption fields. This soil hats only slight limitations for        numerous. Site preparation and planting seedlings in
          dwellings without basements. Droughtiness is a                       furrows reduce this limitation.
          moderate limitation for lawns and landscaping. This                     This soil is well suited to most engineering uses
          limitation can be reduced by regular applications of                 related to dwellings and other structures. Wetness is a
          water.                                                               severe limitation for septic tank absorption fields. This
                                                                               soil has slight limitations for dwellings without
            This Bonneau soil is in capability subclass Ils.                   basements. Droughtiness is a moderate limitation for
            BoB-Bonneau fine sand, 2 to 6 percent slopes.                      lawns and landscaping. This limitation can be reduced by
                                                                               regular applications of water.
          This soil is on gently sloping steam terraces. It is well               This Bonneau soil is in capability subclass Ils.
          drained. The areas of this soil are irregular in shape and
          commonly are 10 to 40 acres.                                            Br-Brookman clay loam, frequently flooded. This
            Typically, the surface layer is gray fine sand about 3             soil is in nearly level, large drainageways mainly in the
          inches thick. The subsurface layer from a depth of 3 to              southeastern part of the county at an elevation of less
          27 inches is very pale brown fine sand. The subsoil from             than 42 feet. It is very poorly drained. The areas of this
          27 to 42 inches is brownish yellow sandy loam, from 42               soil are irregular or elongated in shape and commonly
          to 53 inches is light yellowish brown sandy clay loam                are 200 to 2,000 acres.
          that has gray mottles, and from 53 to 61 inches is light                Typically, the surface layer is black clay loam about 8
          gray sandy clay loam. The substratum from 61 to 80                   inches thick. The subsoil from a depth of 8 to 22 inches
          inches is red sandy loam.                                            is black clay, from 22 to 49 inches is dark gray clay, and
            Included with this soil in mapping are a few small                 from 49 to 76 inches is gray clay loam and sandy clay
          areas of Blanton, Lynchburg, and Rains soils. Also                   loam. The substratum from 76 to 80 inches is grayish
          included are a few small areas of soils that have slopes             brown loamy sand.
          of less than 2 percent. These included soils make up                    Included with this soil in mapping are small areas of
          about 10 percent of the map unit.                                    Eulonia, Osier, and Wahee soils. The included soils
            This Bonneau soil is very strongly acid to medium acid             make up about 15 percent of the map unit.
          in the surface and subsurface layers except where lime                  This Brookman soil is very strongly acid to slightly acid
          has been added, and it is very strongly acid or strongly             in the upper part of the profile and strongly acid to mildly
          acid in the subsoil. Permeability is moderate, and the               alkaline in the lower part. Permeability is slow, and the
          available water capacity is low to moderate. The                     available water capacity is moderate to high. The shrink-
          seasonal high water table is 3.5 to 5 feet below the                 swell potential is moderate. The seasonal high water
          surface.                                                             table is at the surface to 1 foot below the surface. This








      Dorchester County, South Carolina                                                                                                  17



      soil is subject to frequent flooding for brief to long                because of the seasonal high water table and frequent
      periods in winter and early in spring.                                flooding.
        Almost all areas of this soil are in water-tolerant                   This Brookman soil is poorly suited to use as
      hardwoods (fig. 2). A few small areas are in engineering              pastureland because of the seasonal high water table
      uses related to dwellings and other structures or in                  and frequent flooding.
      recreational uses.                                                      This soil is well suited to water-tolerant trees. Suitable
         This soil is not suited to row crops and small grains              trees include water tupelo and sweetgum. Loblolly pine




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            Figure 2.-Water-tolerant hardwood trees are the dominant vegetation In most areas of Brookman clay loam, frequently flooded.









           18                                                                                                                            Soil Survey



           is suitable to plant if surface water can be removed.                   low. The seasonal high water table is 2 to 3 feet below
           Equipment use limitations, plant competition, and                       the surface.
           seedling mortality are severe. Harvesting and planting                     About 70 percent of the acreage of this soil is
           trees during dry periods reduce the equipment limitation.               woodland. The rest is cropland, pastureland, or in
           Equipment that has wide tires or tracks can operate                     engineering uses related to dwellings and other
           more efficiently on this wet soil. Site preparation and                 structures.
           planting seedlings on raised beds increase seedling                        This soil is poorly suited to row crops and small grains
           survival.                                                               because the nutrient-holding capacity and available
             This soil is not suited to most engineering uses related              water capacity are low. For more efficient crop
           to dwellings and other structures. Wetness and the                      production, fertilizers and irrigation water need to be
           hazard of flooding are severe. limitations for septic tank              applied at intervals rather than in a single application.
           absorption fields, for dwellings without basements, and                 This prevents leaching of fertilizers and development of
           for lawns and landscaping.                                              a high water table.
             This Brookman soil is in capability subclass VIw.                        This Chipley soil is suited to use as pastureland.
                                                                                   Suitable pasture plants include bahiagrass and improved
             Ca-Capers silty clay loam. This soil is on nearly                     bermudagrass. Major management problems are the low
           level broad tidal flats that aria flooded with salt water.       It     nutrient-holding capacity and available water capacity.
           is very poorly drained. The areas of this soil commonly                 Proper grazing, weed control, and fertilizers improve the
           are about 200 to 500 acres.                                             quality of the forage.
             Typically, the surface layer is very dark grayish brown                  This soil is suited to use as woodland. Suitable trees
           or black silty clay loam 21 inches thick. The underlying                include longleaf pine and loblolly pine. Equipment use
           material from a depth of 21 'to 28 inches is black clay,                limitations and plant competition are moderate.
           from 28 to 50 inches is gray clay, from 50 to 58 inches is              Equipment that has wide tires or tracks operates more
           greenish gray silty clay, and from 58 to 80 inches is pale              efficiently on this soil. Seedlings have better survival
           green sandy clay loam.                                                  rates if competing vegetation is controlled either by site
             Included with this soil in mapping are small areas of                 preparation, prescribed burning, cutting, or girdling.
           Brookman, Mouzon, and Nakina soils. The included soils                     This soil is poorly suited to most engineering uses
           make up about 10 percent of the map unit.                               related to dwellings and other structures. Wetness is a
             This Capers soil is medium acid to mildly alkaline. The               severe limitation for septic tank absorption fields and a
           content of organic matter is high. Permeability is very                 moderate limitation for dwellings without basements. This
           slow, and the available water capacity is very low. The                 soil requires specially designed septic tank absorption
           shrink-swell potential is high. The high water table is                 fields because of the high water table. The wetness
           between 1 foot above the surface and 1 foot below the                   limitation can be reduced around dwellings by installing
           surface throughout the year. This soil is flooded with salt             surface or subsurface drainage systems and by adding
           water once or twice a day.                                              suitable fill material. Droughtiness and the low nutrient-
             Most areas of this soil am in marshland. Because of                   holding capacity are severe limitations for lawns and
           flooding and the high salt content, this soil is not suited             landscaping. Regular applications of water during dry
           to use as cropland, pastureland, woodland, or to                        periods and frequent applications of fertilizers can
           engineering uses related to dwellings and other                         reduce these limitations.
           structures.                                                                This Chipley soil is in capability subclass Ills.
             This Capers soil is in capability subclass VlIIw.
                                                                                      CoB-Chisolm fine sand, 0 to 6 percent slopes.
             ChA-Chipley sand, 0 to 2 percent slopes. This soil                    This soil is on smooth and convex terraces in the
           is on nearly level ridges on flood plains throughout the                southeastern part of the county. It is well drained. The
           county. It is moderately well drained. The areas of this                areas of this soil are irregular in shape and commonly
           soil are irregular in shape and commonly are 5 to 100                   are 10 to 50 acres.
           acres.                                                                     Typically, the surface layer is brown fine sand about
             Typically, the surface layer is dark gray sand 7 inches               10 inches thick. The subsurface layer from a depth of 10
           thick. The underlying material from 7 to 30 inches is light             to 30 inches is brownish yellow loamy fine sand. The
           yellowish brown and pale brown sand and from 30 to 75                   subsoil from 30 to 48 inches is yellowish brown fine
           inches is light gray sand.                                              sandy loam and sandy clay loam; from 48 to 58 inches is
             Included with this soil in mapping are small areas of                 mottled light gray, red, and brownish yellow sandy clay
           Leon, Echaw, Coosaw, Ocilla, and Osier soils. The                       loam; and from 58 to 80 inches is mottled light gray fine
           included soils make up about 10 percent of the map unit.                sandy loam stratified with loamy and sandy material.
             This Chipley soil is very strongly acid to slightly acid.                Included with this soil in mapping are small areas of
           Permeability is rapid, and the available water capacity is              Coosaw, Nakina, Ogeechee, Elloree, and Yemassee








      Dorchester County, South Carolina                                                                                                19



      soils. The included soils make up about 10 percent of                 About 60 percent of the acreage of this soil is
      the map unit.                                                      woodland. The rest is cropland, pastureland, or in
        This Chisolm soil is very strongly acid to medium acid.          engineering uses related to dwellings and other
      Permeability is moderate, and the available water                  structures.
      capacity is low. The seasonal high water table is 3.5 to 5            This soil is suited to row crops and small grains;
      feet below the surface.                                            however, wetness and the low nutrient-holding capacity
        About 70 percent of the acreage of this soil is                  can cause problems. Surface and subsurface drainage
      woodland. The rest is in engineering uses related to               systems help lower the seasonal high water table and
      dwellings and other structures, or it is used as cropland          reduce wetness problems. Split applications of fertilizers
      or pastureland.                                                    help maintain proper plant growth. Residue management
        This soil is suited to row crops and small grains. Major         improves fertility and reduces soil blowing.
      management problems are low nutrient-holding capacity                 This Coosaw soil is well suited to use as pastureland.
      and droughtiness. Split applications of fertilizers help           Suitable pasture plants include improved bermudagrass
      maintain proper plant growth. Irrigation and proper                and bahiagrass. Major management problems are
      management of crop residue help minimize droughtiness              wetness and low nutrient-holding capacity. Surface and
      and reduce soil blowing.                                           subsurface drainage systems can lower the water table
        This Chisolm soil is well suited to use as pastureland.          and reduce wetness problems. Proper grazing, weed
      Suitable pasture plants include improved bermuclagrass             control, and fertilizers improve the quality of the forage.
      and bahiagrass. Major management problems are low                     This soil is suited to use as woodland. Suitable trees
      nutrient-holding capacity and droughtiness. Proper                 include loblolly pine and longleaf pine. Equipment use
      grazing, weed control, and fertilizer improve the quality of       limitations, plant competition, and seedling mortality are
      the forage.                                                        moderate. Equipment that has wide tires or tracks
        This soil is suited to use as woodland. Suitable trees           operates more efficiently in this wet, sandy soil. Plant
      include loblolly pine and longleaf pine. Equipment use             competition prevents good early growth of seedlings.
      limitations, plant competition, and seedling mortality are         Site preparation, prescribed burning, cutting, and girdling
      moderate. Equipment that has wide tires or tracks                  help insure maximum growth of seedlings.
      operates more efficiently on this soil. Seedlings have a              This soil is poorly suited to most engineering uses
      better survival rate if they are planted in furrows and the        related to dwellings and other structures. Wetness is a
      competing vegetation is controlled.                                severe limitation for septic tank absorption fields and a
        This soil is suited to most engineering uses related to          moderate limitation for dwellings without basements. This
      dwellings and other structures. Wetness is a moderate              soil requires specially designed septic tank absorption
      limitation for septic tank absorption fields. This soil has        fields because of the high water table. The wetness
      slight limitations for dwellings without basements.                limitation can be reduced around foundations by using
      Droughtiness is a moderate limitation for lawns and                suitable fill material. Droughtiness is a moderate
      landscaping. This limitation can be reduced by regular             limitation for lawns and landscaping. This limitation can
      applications of water.                                             be reduced by regular applications of water.
        This Chisolm soil is in capability subclass Ils.                    This Coosaw soil is in capability subclass IIIw.

        Cs-Coosaw loamy fine sand. This soil is on nearly                   Cx-Coxville loam. This soil is in nearly level or
      level, low ridges in the southeastern part of the county.    It    slightly depressed areas or along small drainageways. It
      is somewhat poorly drained. The areas of this soil are             is poorly drained. The areas of this soil are irregular in
      irregular in shape and commonly are 15 to 50 acres.                shape or oval and commonly are 10 to 50 acres.
        Typically, the surface layer is dark grayish brown                  Typically, the surface layer is very dark gray loam
      loamy fine sand about 7 inches thick. The subsurface               about 6 inches thick. The subsoil from a depth of 6 to 11
      layer from a depth of 7 to 26 inches is very pale brown            inches is grayish brown loam, from 11 to 35 inches is
      fine sand. The subsoil from 26 to 43 inches is yellowish           gray clay loam, and from 35 to 80 inches is dark gray
      brown or brownish yellow sandy clay loam and from 43               clay.
      to 78 inches is gray and light gray sandy clay loam.                  Included with this soil in mapping are small areas of
        Included with this soil in mapping are small areas of            Lynchburg, Pantego, and Pelham soils. The included
      Blanton, Chisolm, Ogeechee, and Elloree soils. The                 soils make up about 10 percent of the map unit.
      included soils make up about 15 percent of the map unit.              This Coxville soil is extremely acid to strongly acid.
        This soil is very strongly acid or strongly acid except          Permeability is moderately slow, and the available water
      where lime has been added. Permeability is moderate,               capacity is high. The shrink-swell potential is moderate.
      and the available water capacity is moderate. The                  The seasonal high water table is at the surface to 1.5
      ,seasonal high water table is 2 to 3 feet below the                feet below the surface. This soil is subject to poncling for
      surface.                                                           brief periods during wet seasons.









            20                                                                                                                            Soil Survey



               About 80 percent of the acreage of this soil is                      moderately slow, and the available water capacity is
            woodland. The rest is cropland, pastureland, or in                      moderate. The shrink-swell potential is moderate. The
            engineering uses related to dwellings and other                         seasonal high water table is at the surface to 1 foot
            structures.                                                             below the surface.
               This soil is well suited to row crops and small      grains;            About 85 percent of the acreage of this soil is
            however, wetness and the dayey subsoil can cause                        woodland. The rest is cropland, pastureland, or in
            problems. Surface drainage and land shaping remove                      engineering uses related to dwellings and other
            excess surface water and allso help lower the seasonal                  structures.
            high water table. Residue management helps to maintain                     This soil is well suited to row crops and small grains.
            tilth and improve the fertility of this soil.                           The major management problem is the seasonal high
               This Coxville soil is well suited to use as pastureland.             water table. In a few areas, ponding is an additional
            Suitable pasture plants include tall fescue, bahiagrass,                hazard. If this soil is used for cultivated crops, adequate
            and improved bermuclagrass. The major management                        drainage is necessary for good yields. Drainage can be
            problem is wetness. Surface drainage and land shaping                   accomplished by using open ditches, tile drains, or a
            remove excess water. Restricted grazing during wet                      combination of these. Land shaping to remove surface
            periods helps to prevent cornpaction and improves                       water reduces wet spots in fields. Returning crop residue
            forage quality.                                                         to the soil improves fertility, reduces crusting, and
               This soil is suited to use as woodland. Loblolly pine is             increases the water infiltration rate.
            the dominant tree. Equipment use limitations and plant                     This Daleville soil is well suited to use as pastureland.
            competition are severe, and seedling mortality is                       Suitable pasture plants include bahiagrass or tall fescue.
            moderate. Surface drainage! helps lower the seasonal                    The major management problem is the seasonal high
            high water table. Equipment that has wide tires or tracks               water table. In some areas, brief ponding is a concern in
            operates more efficiently on this wet soil. Seedlings                   management. Shallow surface drains can remove excess
            survive better if they are planted on raised beds. Site                 water and lower the water table. Proper stocking,
            preparation, prescribed burning, cutting, and girdling                  pasture rotation, timely deferment of grazing, and
            reduce plant competition and help insure maximum                        restricted use during wet periods help keep the pasture
            growth of seedlings.                                                    and soil in good condition.
               This soil is poorly suited to most engineering uses                     This soil is well suited to use as woodland. Suitable
            related to dwellings and other structures. Wetness and                  trees include loblolly pine and sweetgum. Because of the
            moderately slow permeability are severe limitations for                 seasonal high water table, the equipment use limitation
            septic tank absorption fields, for dwellings without                    and seedling mortality are severe and plant competition
            basements, and for lawns and landscaping. This soil is                  is moderate. Equipment that has wide tires or tracks
            not suited to septic tank absorption fields because of the              operates more efficiently on this wet soil. Planting on
            high water table. Effluent can be pumped to a suitable                  raised beds reduces seedling mortality. Site preparation,
            site to reduce this limitation. Surface drainage and land               prescribed burning, cutting, and girdling reduce plant
            shaping help move excess surface water away from                        competition.
            dwellings and reduce wetness problems for lawns and                        This soil is poorly suited to most engineering uses
            landscaping.                                                            related to dwellings and other structures. The seasonal
               This Coxville soil is in capability subclass Illw.                   high water table is a severe limitation for septic tank
                                                                                    absorption fields, for dwellings without basements, and
               Da-Daleville silt loam. This soil is in slight                       for lawns and landscaping. To reduce this limitation for
            depressions and drainageways on upland terraces. It is                  absorption fields, sewage effluent can be pumped to a
            nearly level and poorly drained. The areas of this soil are             suitable site. The problems caused by the high water
            irregular in shape and commonly are 20 to 200 acres.                    table can also be reduced by adding fill material, by land
               Typically, the surface layer is very dark grayish brown              shaping to remove surface water, and by installing
            silt loam about 8 inches thick. The subsurface layer from               surface drainage systems.
            a depth of 8 to 15 inches is light gray silt loam. The                     This Daleville soil is in capability subclass Illw.
            subsoil from 15 to 26 inches is light gray silt loam, from
            26 to 67 inches is light gray silty clay loam, and from 67                 Ec-Echaw fine sand. This soil is on nearly level
            to 80 inches is gray clay loam.                                         ridges on upland terraces mainly in the central part of
               Included with this soil in mapping are small areas of                the county. It is moderately well drained. The areas of
            Ocilla, Osier, and Grifton soils. Also included are small               this soil are elongated in shape and commonly are 20 to
            areas of soils that are subject to ponding from November                100 acres.
            through March. The included soils make up about 20                         Typically, the surface layer is dark gray fine sand
            percent of the map unit.                                                about 7 inches thick. The subsurface layer from a depth
               The soil is very strongly acid or strongly acid except               of 7 to 45 inches is pale brown or light yellowish brown
            where lime has been addE?d. Permeability is slow to                     fine sand. The subsoil from 45 to 52 inches is brown








      Dorchester County, South Carolina                                                                                                   21



      loamy fine sand, from 52 to 60 inches is dark reddish                   This Elloree soil is very strongly acid to neutral in the
      brown fine sand, and from 60 to 80 inches is black fine              upper part of the profile and strongly acid to moderately
      sand.                                                                alkaline in the lower part. Permeability is moderate, and
         Included with this soil in mapping are small areas of             the available water capacity is moderate. The seasonal
      Albany, Leon, and Osier soils. The included soils make               high water table is at the surface to 1 foot below the
      up about 15 percent of the map unit.                                 surface. This soil is subject to occasional flooding for
         This Echaw soil is very strongly acid to medium acid.             long periods during wet seasons.
      Permeability is moderately rapid, and the available water               Nearly all areas of this soil is woodland. A few small
      capacity is low. The seasonal high water table is 2.5 to 5           areas are cropland, pastureland, or in engineering uses
      feet below the surface.                                              related to dwellings and other structures.
         About 50 percent of the acreage of this soil is                      This soil is not suited to row crops and small grains
      woodland. About 35 percent is cropland. The rest is                  because of the seasonal high water table and occasional
      pastureland or in engineering uses related to dwellings              flooding.
      and other structures.                                                   This Elloree soil is suited to use as pastureland.
         This soil is suited to row crops and small grains. Major          Bahiagrass is the main pasture plant. Wetness and
      management problems are the low nutrient-holding                     occasional flooding are major management problems.
      capacity and low available water capacity. Split                     Surface and subsurface drainage help lower the
      applications of fertilizer provide available nutrients.              seasonal high water table and reduce wetness problems.
      Maintaining crop residue on the surface can improve the              Restricted grazing during wet periods helps to conserve
      soil fertility, prevent rapid drying of the soil surface, and        the soil and improve forage quality.
      reduce wind erosion.                                                    This soil is suited to use as woodland. Loblolly pine is
         This Echaw soil is suited to use as pastureland.                  the dominant tree. Because of the seasonal high water
      Suitable pasture plants include improved bermudagrass                table, the equipment use limitation, plant competition,
      and bahiagrass. Major management problems are low                    and seedling mortality are severe. Drainage systems
      nutrient-holding capacity and low available water                    help lower the water table and reduce wetness
      capacity. Rotation grazing and application of fertilizers            problems. Equipment that has wide tires or tracks
      help maintain high quality forages.                                  operates more efficiently on this wet soil. Site
         This soil is suited to use as woodland. Suitable trees            preparation and planting seedlings on beds increase
      include loblolly pine and longleaf pine. Because of the              seedling survival.
      sandy texture and seasonal wetness, the equipment use                   This soil is not suited to engineering uses related to
      limitation and plant competition are moderate. Using                 dwellings and other structures. Wetness and the hazard
      equipment that has specially designed tracks or tires and            of flooding are severe limitations for septic tank
      site preparation reduce these problems.                              absorption fields, for dwellings without basements, and
                                                                           for lawns and landscaping. These limitations are difficult
         This soil is suited to most engineering uses related to           and costly to reduce.
      dwellings and other structures. Wetness is a severe                     This Elloree soil is in capability subclass VIw.
      limitation for septic tank absorption fields. Increasing the
      size of the absorption field and adding suitable fill                   EpB-Emporia loamy fine sand, 2 to 6 percent
      material can reduce this limitation. This soil has a slight          slopes. This soil is on gently sloping upland terraces. It
      limitation for dwellings without basements and a                     is well drained. The areas of this soil are irregular in
      moderate limitation for lawns and landscaping.                       shape and commonly are 10 to 100 acres.
         This Echaw soil is in capability subclass Ills.                      Typically, the surface layer is dark grayish brown
                                                                           loamy fine sand about 5 inches thick. The subsurface
         Eo-Elloree loamy fine sand, occasionally flooded.                 layer from a depth of 5 to 14 inches is very pale brown
      This soil is in broad depressions and along                          loamy fine sand. The subsoil from 14 to 41 inches is
      drainageways. It is poorly drained. The areas of this soil           strong brown sandy clay loam and from 41 to 54 inches
      are irregular in shape and commonly are 15 to 30 acres.              is mottled reddish yellow, red, and light gray sandy clay
         Typically, the surface layer is very dark gray loamy fine         loam. The substratum from 54 to 75 inches is light gray
      sand about 8 inches thick. The subsurface layer from a               sandy clay loam and sandy loam.
      depth of 8 to 20 inches is dark grayish brown loamy fine                Included with this soil in mapping are a few small
      sand and from 20 to 23 inches is light brownish gray fine            areas of Jedburg and Daleville soils, These included
      sand. The subsoil from 23 to 72 inches is gray sandy                 soils make up about 10 percent of the map unit.
      clay loam. The substratum from 72 to 80 inches is light                 This Emporia soil is very strongly acid to medium acid
      gray loamy sand.                                                     except where lime has been added. Permeability is
         Included with this soil in mapping are small areas of             moderate in the upper part of the subsoil and moderately
      Albany, Nakina, Rutlege, and Yemassee soils. The                     slow or slow in the lower part. The available water
      included soils make up about 30 percent of the map unit.             capacity is moderate. The shrink-swell potential is low in









            22                                                                                                                       Soil Survey



            the upper part of the subsoil and moderate in the lower              engineering uses related to dwellings and other
            part. The perched seasonal high water table is 3 to 4.5              structures.
            feet below the surface.                                                 This soil is well suited to row crops and small grains.
              About 70 percent of the acreage of this soil is                    Major management problems are the seasonal high
            cropland. The rest is pastureland, woodland, or in                   water table and clayey subsoil. Drainage ditches and
            engineering uses related to dwellings and other                      land shaping can remove excess water. Crop residue
            structures.                                                          management and conservation tillage improve the tilth of
              This soil is well suited to row crops and small grains.            this soil.
            Erosion is a moderate hazaird. Contour stripcropping,                   This Eulonia soil is well suited to use as pastureland.
            conservation tillage, and grassed waterways can help                 Suitable pasture plants include improved bermudagrass
            control erosion. Leguminous cover crops also prevent                 and bahiagrass. The major management problem is the
            soil erosion and improve tho fertility of this soil.                 seasonal high water table, but excess water can be
              This Emporia soil is well suited to use as pastureland.            removed by drainage ditches and land shaping.
            Suitable pasture plants include tall fescue,                            This soil is suited to use as woodland. Loblolly pine is
            bermudagrass, and bahiagrass. Rotation grazing and                   the dominant tree. Equipment use limitations, plant
            restricting grazing during wet periods help maintain good            completion, and seedling mortality are moderate.
            forage quality.                                                      Equipment that has wide tires or tracks operates more
              This soil is well suited to use as woodland. Suitable              efficiently on this soil. Plant competition prevents good
            trees include loblolly pine and sweetgum. Seedling                   early growth of seedlings. Site preparation, prescribed
            mortality and plant competition are moderate. Site                   burning, cutting, and girdling help insure maximum
            preparation, prescribed burning, cutting, and girdling help          growth of seedlings.
            insure maximum growth and survival of seedlings.                        This soil is poorly suited to most engineering uses
              This soil is well suited to most engineering uses                  related to dwellings and other structures. Wetness and
            related to dwellings and other structures. Wetness and               moderately slow permeability are severe limitations for
            the slow permeability are severe limitations for septic              septic tank absorption fields. Modifying absorption fields
            tank absorption fields. Specially designed septic tank               by increasing the size and adding suitable fill material
            absorption fields can reduce these limitations. This soil            can reduce these limitations. Wetness is a moderate
            has only slight limitations for dwellings without                    limitation for dwellings without basements. Drainage and
            basements. Droughtiness is a moderate limitation for                 land shaping can reduce problems caused by wetness.
            lawns and landscaping.                                               Wetness is a moderate limitation for lawns and
              This Emporia soil is in capability subclass lie.                   landscaping. Land shaping and shallow ditches can
                                                                                 remove excess surface water.
              EuA-Eulonia fine sandy loam, 0 to 2 percent                           This Eulonia soil is in capability subclass l1w.
            slopes. This soil is on broad, nearly level upland
            terraces in the southeastern part of the county. It is                  EuB-EuIonia fine sandy loam, 2 to 6 percent
            moderately well drained. The areas of this soil are                  slopes. This soil is on gently sloping upland terraces in
            irregular in shape and commonly are 10 to 50 acres.                  the southeastern past of the county. It is moderately well
              Typically, the surface layer is dark grayish brown fine            drained. The areas of this soil are irregular in shape and
            sandy loam about 4 inches thick. The subsurface layer                commonly are 10 to 50 acres.
            from a depth of 4 to 11 inches is light yellowish brown                 Typically, the surface layer is dark grayish brown fine
            fine sandy loam. The subsoil from 11 to 15 inches is                 sandy loam about 4 inches thick. The subsurface layer
            strong brown sandy clay loam, from 15 to 27 inches is                from a depth of 4 to 11 inches is light yellowish brown
            yellowish red sandy clay, and from 27 to 49 inches is                fine sandy loam. The subsoil from 11 to 15 inches is
            yellowish red and strong brown sandy clay loam. The                  strong brown sandy clay loam, from 15 to 27 inches is
            substratum from 49 to 80 inches is strong brown loamy                yellowish red sandy clay, and from 27 to 49 inches is
            fine sand.                                                           yellowish red and strong brown sandy clay loam. The
              Included with this soil in mapping are small areas of              substratum from 49 to 80 inches is strong brown loamy
            Chisolm, Mouzon, Ogeechee, Wahee, and Yemassee                       fine sand.
            soils. The included soils make up about 15 percent of                   Included with this soil in mapping are small areas of
            the map unit.                                                        Chisolm, Mouzon, Ogeechee, Wahee, and Yemassee
              This Eulonia soil is very strongly acid to medium acid             soils. The included soils make up about 15 percent of
            except where lime has been added. Permeability is                    the map unit.
            moderately slow, and the available water capacity is                    This soil is very strongly acid to medium acid except
            moderate. The seasonal high water table is 1.5 to 3.5                where lime has been added. Permeability is moderately
            feet below the surface.                                              slow, and the available water capacity is moderate. The
              About 80 percent of the acreage of this soil is                    seasonal high water table is 1.5 to 3.5 feet below the
            woodland. The rest is cropland, pastureland, or in                   surface.








      Dorchester County, South Carolina                                                                                                 23



         About 80 percent of the acreage of this soil is                   is low to moderate. The seasonal high water table is 2 to
      woodland. The rest is cropland, pastureland, or in                   3.5 feet below the surface.
      engineering uses related to dwellings and other                        About 55 percent of the acreage of this soil is
      structures.                                                          cropland. About 30 percent is woodland, and the rest is
         This soil is well suited to row crops and small grains;           pastureland or in engineering uses related to dwellings
      however, the seasonal high water table, clayey subsoil,              and other structures.
      and moderate hazard of erosion are concerns in                         This soil is well suited to row crops and small grains;
      management. Drainage ditches and land shaping can                    however, the high water table and low nutrient-holding
      remove excess water. Residue management, such as                     capacity are concerns in management. Surface and
      cover crops or conservation tillage, helps control                   subsurface drainage systems help lower the seasonal
      erosion.                                                             high water table. Water control structures may be
         This Eulonia soil is well suited to use as pastureland.           needed with drainage systems to maintain adequate soil
      Suitable pasture plants include improved bermudagrass                moisture levels for plants. Filters may be needed on
      or bahiagrass. The major management problem is the                   subsurface drains to prevent clogging. Because of
      seasonal high water table; however, excess water can                 leaching, split applications of fertilizers are needed to
      be removed by drainage ditches and land shaping.                     maintain proper plant growth. Residue management
         This soil is suited to use as woodland. Loblolly pine is          helps control wind erosion and improves the fertility of
      the dominant tree. Equipment use limitations, plant                  this soil.
      competition, and seedling mortality are moderate.                      This Foreston soil is well suited to use as pastureland.
      Equipment that has wide tires or tracks operates more                Suitable pasture plants include bahiagrass and
      efficiently on this soil. Plant competition prevents good            bermudagrass. Major management problems are
      early growth of seedlings. Site preparation, prescribed              wetness and low nutrient-holding capacity; however,
      burning, cutting, and girdling help insure maximum                   surface drainage systems help lower the seasonal high
      growth of seedlings.                                                 water table and fertilizing and rotation grazing can
         This soil is poorly suited to most engineering uses               improve forage quality.
      related to dwellings and other structures. Wetness and                 This soil is well suited to use as woodland. Loblolly
      moderately slow permeability are severe limitations for              pine is the dominant tree. Because of the seasonal high
      septic tank absorption fields. Modifying absorption fields
      by increasing the size and adding suitable fill material             water table, equipment use limitations and plant
      reduce these limitations. Wetness is a moderate                      competition are moderate. Surface drainage and site
      limitation for dwellings without basements. Wetness is               preparation can reduce problems caused by wetness.
      also a moderate limitation for lawns and landscaping.                  This soil is suited to most engineering uses related to
      I                                                                    dwellings and other structures. The seasonal high water
      A.And shaping can remove excess surface water.
         This Eulonia soil is in capability subclass Ile.                  table is a severe limitation for septic tank absorption
                                                                           fields. Specially designed septic tank absorption fields
         FoA-Foreston loamy fine sand, 0 to 2 percent                      are needed. Adding suitable fill material or increasing the
      slopes. This soil is on nearly level upland terraces in the          size of the absorption field can also reduce this
      central part of the county. It is moderately well drained.           limitation. Wetness is a moderate limitation for dwellings
      The areas of this soil are irregular in shape and                    without basements, but surface drainage systems help
      commonly are 10 to 100 acres.                                        lower the seasonal high water table. The low nutrient-
         Typically, the surface layer is very dark gray loamy fine         holding capacity and droughtiness are moderate
      sand about 8 inches thick. The subsurface layer from a               limitations for lawns and landscaping. Annual
      depth of 8 to 13 inches is yellowish brown loamy fine                applications of fertilizer can reduce this limitation.
      sand. The subsoil from 13 to 23 inches is yellowish                    This Foreston soil is in capability subclass l1w.
      brown fine sandy loam, and from 23 to 32 inches is
      brownish yellow fine sandy loam. A subsurface layer of                 FxB-Foxworth fine sand, 0 to 6 percent slopes.
      light brownish gray fine sand is at a depth of 32 to 53              This soil is on nearly level to gently sloping upland
      inches. The lower part of the subsoil from 53 to 80                  terraces and ridges. It is moderately well drained. The
      inches is light gray stratified fine sandy loam, sandy clay          areas of this soil are irregular in shape and commonly
      loam, and loamy sand.                                                range from 10 to 30 acres.
         Included with this soil in mapping are small areas of               Typically, the surface layer is very dark grayish brown
      Albany, Blanton, Lynn Haven, Ocilla, and Osier soils. The            fine sand about 7 inches thick. The subsoil from a depth
      included soils make up about 20 percent of the map unit.             of 7 to 14 inches is yellowish brown fine sand, and from
         This Foreston soil is very strongly acid to medium acid           14 to 47 inches is strong brown fine sand. The
      except where lime has been added. Permeability is                    substratum from 47 to 77 inches is very pale brown fine
      moderately rapid in the upper part of the subsoil and                sand that has gray moftles, and from 77 to 85 inches, it
      moderate in the lower part. The available water capacity             is light gray fine sand.








            24                                                                                                                             Soil Survey



               Included with this soil in miapping are a few small                   yellowish brown sandy clay loam, from 25 to 48 inches is
            areas of Alpin, Blanton, Leon, and Osier soils. The                      brownish yellow sandy clay loam that has a few gray
            included soils make up about 15 percent of the map unit.                 mottles; and from 48 to 62 inches is gray sandy clay
               This Foxworth soil is very strongly acid to medium acid               loam. The substratum from 62 to 80 inches is gray sandy
            except where lime has been added. Permeability is very                   clay loam stratified with sandy loam.
            rapid, and the available water capacity is low. The                         Included with this soil in mapping are a few small
            seasonal high water table is 3.5 to 6 feet below the                     areas of Bonneau, Chipley, Foreston, Lynchburg, and
            surface.                                                                 Rains soils. The included soils make up about 15
               About 80 percent of the acreage of this soil is                       percent of the map unit.
            woodland. The remainder is cropland, pastureland,           or in           This Goldsboro soil is very strongly acid or strongly
            engineering uses related todwellings and other                           acid except where lime has been added. Permeability is
            structures.                                                              moderate, and the available water capacity is moderate.
               This soil is poorly suited to row crops and small grains              The seasonal high water table is 2 to 3 feet below the
            because of droughtiness and the low nutrient-holding                     surface.
            capacity. Irrigation and application of fertilizers reduce                  About 75 percent of the acreage of this soil is
            these problems and improve crop yields. Residue                          cropland. The rest is pastureland, woodland, or in
            management, such as planting cover crops and                             engineering uses related to dwellings and other
            conservation tillage, improve the soil moisture and                      structures.
            nutrient relationships and protect this soil from wind                      This soil is well suited to row crops and small grains;
            erosion.                                                                 however, the seasonal high water table is a concern in
               This Foxworth soil is SUitEd to use as pastureland.                   management. Surface and subsurface drainage systems
            Suitable pasture plants include bermuclagrass and                        help lower the seasonal high water table and reduce
            bahiagrass. Major management problems are                                problems caused by wetness. Residue management can
            droughtiness and low nutrient-holding capacity, but                      increase organic matter content and improve fertility.
            irrigation, rotation grazing, and application of fertilizers                This Goldsboro soil is well suited to use as
            can reduce these problems and improve forage quality.                    pastureland. Suitable pasture plants include bahiagrass
               This soil is suited to use as woodland. Longleaf pine is              and bermudagrass. The major management problem is
            the dominant tree. Because of the sandy texture,                         wetness. Rotation grazing and restricting grazing during
            equipment use limitations, plant competition, and                        wet periods improve forage quality. Surface drainage
            seedling mortality are moderate. Equipment that has                      systems can reduce problems caused by wetness.
            wide tires or tracks operates more efficiently on this soil.                This soil is well suited to use as woodland. Suitable
            Seedlings have a better survival rate if they are planted                trees include lobfolly pine and sweetgum. Because of a
            in furrows. Plant competition prevents good early growth                 seasonal high water table, equipment use limitations and
            of seedlings. Site preparation, prescribed burning,                      plant competition are moderate. Surface drainage
            cutting, and girdling help insure maximum growth of                      systems and site preparation can reduce these
            seedlings.                                                               problems. Equipment that has wide tires or tracks can
               This soil is suited to most engineering uses related to               operate more efficiently on this soil.
            dwellings and other structures. Wetness and the poor                        This soil is suited to most engineering uses related to
            filtering capacity are moderate limitations for septic tank              dwellings and other structures. Wetness is a severe
            absorption fields. Adding suitable fill material or                      limitation for septic tank absorption fields. Adding
            increasing the size of the absorption field can reduce                   suitable fill material and increasing the size of the
            these limitations. This soil has slight limitations for                  absorption field can reduce this limitation. Wetness is a
            dwellings without basements. Droughtiness and the low                    moderate limitation for dwellings without basements, but
            nutrient-holding capacity are moderate limitations for                   land shaping and surface drainage can reduce problems
            lawns and landscaping. Regular applications of water                     caused by wetness. This soil has only slight limitations
            and fertilizers can reduce these limitations.                            for lawns and landscaping.
               This Foxworth soil is in capability subclass Ills.                       This Goldsboro soil is in capability subclass l1w.

               GoA-Goldsboro loamy sand, 0 to 2 percent                                 Gr-Grifton fine sandy loam, frequently flooded.
            slopes. This soil is on nearly level upland terraces. It is              This soil is on nearly level flood plains of major swamps
            moderately well drained. The areas of this soil are                      and along small drainageways. It is poorly drained. The
            irregular in shape and commonly range from 10 to 100                     areas of this soil are irregular or elongated in shape and
            acres.                                                                   are 10 to 200 acres.
               Typically, the surface layer is very dark grayish brown                  Typically, the surface layer is dark grayish brown fine
            loamy sand about 7 inches thick. The subsurface layer                    sandy loam about 6 inches thick. The subsurface layer
            from a depth of 7 to 14 inches is light yellowish brown                  from a depth of 6 to 10 inches is light gray fine sandy
            loamy sand. The subsoil from 14 to 25 inches is                          loam. The subsoil from 10 to 49 inches is gray sandy







      Dorchester County, South Carolina                                                                                                25



      clay loam. The substratum from 49 to 61 inches is light              the surface. This soil is subject to flooding or ponding
      gray sandy clay loam, from 61 to 67 inches is gray sandy             daily by tidal action.
      loam, and from 67 to 80 inches is gray sand.                           About 95 percent of the acreage of this soil is in black
         Included with this soil in mapping are small areas of             needlerush and other marsh grasses. The rest has been
      Mouzon, Osier, Pelham, Plummer, Elloree, and                         filled in and is in engineering uses related to dwellings
      Yemassee soils. The included soils make up about 25                  and other structures.
      percent of the map unit.                                               Because of daily flooding by tidal action, this soil is not
         This Grifton soil is very strongly acid to slightly acid in       suited to row crops and small grains, pastureland,
      the surface and subsurface layers and medium acid to                 woodland, or engineering uses related to dwellings and
      moderately alkaline in the subsoil. Permeability is                  other structures.
      moderate, and the available water capacity is moderate                 This Handsboro soil is in capability subclass VlIIw.
      to high. The seasonal high water table is 0.5 to 1 foot
      below the surface. This soil is subject to frequent                    Hp-Haplaquents, loamy. This map unit consists of
      flooding for brief periods during wet seasons.                       wet, loamy soil material in areas where the soil has been
         Most areas of this soil are woodland. A few small                 removed to a depth of 3 to 15 feet. The areas generally
      areas are cropland, pastureland, or in engineering uses              are small but range from 5 to more than 50 acres.
      related to dwellings and other structures.                             This soil is dominantly loamy to a depth of about 5
         This soil is not suited to row crops and small grains             feet and sandy below that. It is dominantly gray with
      because of the seasonal high water table, frequent                   mottles of yellow and strong brown.
      flooding, and the absence of adequate drainage outlets.                This soil is low in natural fertility and in content of
         This Grifton soil is poorly suited to use as pastureland          organic matter. The available water capacity is moderate
      because of flooding, the seasonal high water table, and              to low. This soil commonly is very strongly acid but
      the absence of adequate drainage outlets.                            ranges to neutral.
         This soil is suited to water-tolerant trees, including              About half of the acreage of this soil is woodland. The
      sweetgum and water tupelo. Loblolly pine is suitable to              rest is used as cropland, pasture, or recreation sites. The
      plant if surface water is removed. Because of flooding,              suitability of the soil in this map unit for specific land
      seedling mortality, plant competition, and equipment use             uses varies with texture and drainage.
      limitations are severe. Restricting equipment use during               The soil is suited to pine trees and pasture where
      wet periods, adequate site preparation, and planting                 excess surface water has been removed. Some areas
      seedlings on raised beds can reduce these management                 are adapted to use as cropland, recreation sites, and
      problems.                                                            habitat for wildlife. The soil in this map unit is so variable
         This soil is not suited to engineering uses related to            that onsite investigation is needed to determine its
      dwellings and other structures. The hazard of flooding               suitability and limitations for any proposed use.
      severely limits the use of this soil for septic tank                   Haplaquents, loamy, is in capability subclass VIw.
      absorption fields, for dwellings without basements, and
      for lawns and landscaping. Flooding is difficult and costly            UA-lzagora silt loam, 0 to 2 percent slopes. This
      to reduce.                                                           soil is on nearly level upland terraces and low ridges. It
         This Grifton soil is in capability subclass VIw.                  is moderately well drained. The areas of this soil are
                                                                           irregular in shape and commonly are 20 to 40 acres.
         Hb-Handsboro muck. This soil is in nearly level tidal               Typically, the surface layer is dark grayish brown silt
      marshes that are flooded once or twice daily by sea                  loam about 6 inches thick. The subsoil from a depth of 6
      water. It is very poorly drained. The areas of this soil are         to 13 inches is yellowish brown silt loam; from 13 to 56
      irregular in shape and commonly are 25 to 100 acres.                 inches is brownish yellow silt loam, silty clay loam, or
         Typically, the organic layers are dark reddish gray,              silty clay that has few to many mottles; and from 56 to
      dark brown, and dark reddish brown, slightly                         80 inches is light gray silty clay loam.
      decomposed to highly decomposed roots and stems                        Included with this soil in mapping are small areas of
      about 48 inches thick. The underlying material from a                Jedburg, Bonneau, and Daleville soils. The included soils
      depth of 48 to 80 inches is greenish gray silty clay.                make up about 15 percent of the map unit.
         Included with this soil in mapping are small areas of               This lzagora soil is extremely acid to strongly acid
      Capers, Mouzon, and Brookman soils. Also included are                except where lime has been added. Permeability is
      small spoil areas. The included soils make up about 15               moderate in the upper part of the subsoil and slow in the
      percent of the map unit.                                             lower part. The available water capacity is moderate.
         This Handsboro soil is neutral to moderately alkaline             The seasonal high water table is 1.5 to 2.5 feet below
      when wet and is extremely acid or very strongly acid                 the surface.
      when dry. Permeability is moderate. The high water table               About 60 percent of the acreage of this soil is
      ranges from 3 feet above the surface to 0.5 foot below               cropland. About 30 percent is woodland. The rest is









                                                                                                                                            Soil Survey



            pastureland or in engineering uses related to dwellings                     This soil is well suited to row crops and small grains;
            and other structures.                                                    however, the seasonal high water table and hazard of
              This soil is well suited to row crops and small grains;                erosion are concerns in management. Tile drains can be
            however, the seasonal high Water table is a concern in                   used to lower the water table. Crop residue management
            management. Open ditches, tile drains, or a combination                  and conservation tillage improve fertility, increase water
            of these can be used to lower the water table. Crop                      infiltration, and reduce the hazard of erosion.
            residue management improves fertility and increases                         This Izagora soil is well suited to use as pastureland.
            water infiltration.                                                      Suitable pasture plants include bermudagrass,
              This Izagora soil is well suited to use as pastureland.                bahiagrass, ryegrass, and clovers. Proper stocking,
            Suitable pasture plants include bermudagrass,                            pasture rotation, and restricted grazing during wet
            bahiagrass, ryegrass, and clovers. Proper stocking,                      periods help keep the pasture in good condition.
            pasture rotation, and restricted grazing during wet                         This soil is well suited to use as woodland. Suitable
            periods help keep the pasture in good condition.                         trees include loblolly pine and sweet gum. Because of
              This soil is well suited to use as woodland. Suitable                  seasonal wetness, equipment use limitations and plant
            trees include loblolly pine and sweetgum. Because of                     competition are moderate. Equipment that has wide tires
            seasonal wetness, equipment use limitations and plant                    or tracks operates more efficiently on this soil. Tree
            competition are moderate. Equipment that has wide tires                  seedlings survive and grow well if competing vegetation
            or tracks operates more efficiently on this soil. Tree                   is controlled or removed. This can be accomplished by
            seedlings survive and grow well if competing vegetation                  site preparation, prescribed burning, cutting, or girdling.
            is controlled or removed. This can be accomplished by                       This soil is suited to most engineering uses related to
            site preparation, prescribed burning, cutting, or girdling.              dwellings and other structures. Wetness and slow
              This soil is suited to most engineering uses related to                permeability are severe limitations for septic tank
            dwellings and other structures. Wetness and slow                         absorption fields. Adding suitable fill material and
            permeability are severe limitations for septic tank                      increasing the size of the absorption field can reduce
            absorption fields. Adding suitable fill material and                     this limitation. Wetness is a moderate limitation for
            increasing the size of the absorption field can reduce                   dwellings without basements. Problems caused by
            this limitation. Wetness is a moderate limitation for                    wetness can be reduced by adding fill material, by
            dwellings without basements. Wetness problems can be                     installing drainage systems, and by land shaping to
            reduced by adding fill material, by installing drainage                  remove surface water. The soil has only slight limitations
            systems, and by land shaping to remove surface water.                    for lawns and landscaping.
            This soil has only slight limitations for lawns and                         This Izagora soil is in capability subclass Ile.
            landscaping.
              This Izagora soil is in capability subclass l1w.                          Jd-Jedburg loam. This soil is on nearly level upland
                                                                                     terraces. It is somewhat poorly drained. The areas of this
              UB-lzagora slit loam,2 to 6 percent slopes. This                       soil are irregular in shape and commonly are 10 to 80
            soil is on gently sloping upland terraces and low ridges.                acres.
            It is moderately well drained. The areas of this soil are                   Typically, the surface layer is very dark gray and dark
            irregular in shape and commonly are 20 to 40 acres.                      grayish brown loam about 8 inches thick. The subsoil
              Typically, the surface layer is dark grayish brown silt                from a depth of 8 to 15 inches is light yellowish brown
            loam about 6 inches thick. The subsoil from a depth of 6                 loam; from 15 to 36 inches is light gray loam; from 36 to
            to 13 inches is yellowish brown silt loam, from 13 to 56                 55 inches is pinkish gray silt loam; from 55 to 75 inches
            inches is brownish yellow silt loam, silty clay loam, or                 is mottled light gray, yellowish brown, and red loam; and
            silty clay that has few to many mottles, and from 56 to                  from 75 to 80 inches is light gray sandy clay loam.
            80 inches is light gray siltyclay loam.                                     Included with this soil in mapping are small areas of
              Included with this soil in mapping are small areas of                  Emporia, Ocilla, and Daleville soils. The included soils
            Jedburg, Bonneau, and Daleville soils. The included soils                make up about 10 percent of the map unit.
            make up about 15 percent of the map unit.                                   This soil is very strongly acid to medium acid except
              This Izagora soil is extremely acid to strongly acid                   where lime has been added. Permeability is moderate,
            except where lime has been added. Permeability is                        and the available water capacity is moderate. The
            moderate in the upper part of the subsoil and slow in the                seasonal high water table is 0.5 foot to 1.5 feet below
            lower part. The available water capacity is moderate.                    the surface.
            The seasonal high water table is 1.5 to 2.5 feet below                      About 70 percent of the acreage of this soil is
            the surface.                                                             woodland. The rest is cropland, pastureland, or in
              About 60 percent of the acreage of this soil is                        engineering uses related to dwellings and other
            cropland. About 30 percent is woodland. The rest is                      structures.
            pastureland or in engineering uses related to dwellings                     This soil is well suited to row crops and small grains;
            and other structures.                                                    however, the seasonal high water table is a concern in







       Dorchester County, South Carolina                                                                                               27



       management. Surface and subsurface drainage systems                engineering uses related to dwellings and other
       can lower the water table. Crop residue management                 structures.
       improves fertility, reduces crusting, and increases water             This soil is well suited to row crops and small grains,
       infiltration.                                                      however, the seasonal high water table and rare flooding
         This Jedburg soil is well suited to use as pastureland.          are concerns in management. Surface drainage systems
       Suitable pasture plants include improved bermudagrass              help lower the seasonal high water table. Diking is
       and bahiagrass. The major management problem is the                needed in some areas to prevent flooding. Conservation
       seasonal high water table. Shallow surface drains can be           tillage helps to preserve soil moisture and control wind
       used to reduce the problem caused by wetness. Proper               erosion.
       stocking, pasture rotation, timely deferment of grazing,              This Johns soil is well suited to use as pastureland.
       and restricted use during wet periods help keep the                Bahiagrass is the main forage on this soil. Surface
       pasture and soil in good condition.                                drainage is needed to lower the seasonal high water
         This soil is well suited to use as woodland. Suitable            table. Restricted grazing during wet periods prevents sod
       trees include loblolly pine and sweetgum. Because of the           damage and improves forage quality.
       seasonal high water table, equipment use limitations and              This soil is well suited to use as woodland. Loblolly
       plant competition are severe. Planting and harvesting              pine is the dominant tree. Because of the seasonal high
       need to be carried out during dry periods. Tree seedlings          water table, equipment use limitations and plant
       survive and grow well if competing vegetation is                   competition are moderate. Equipment that has wide tires
       controlled or removed. This can be accomplished by site            or tracks operates more efficiently when this soil is wet.
       preparation, prescribed burning, cutting, or girdling.             Bedding seedlings and surface drainage can reduce
         This soil is poorly suited to most engineering uses              problems caused by wetness. Site preparation can
       related to dwellings and other structures. Wetness is a            reduce plant competition.
       severe limitation for septic tank absorption fields, for              This soil is poorly suited to most engineering uses
       dwellings without basements, and for lawns and                     related to dwellings and other structures. The seasonal
       landscaping. This soil requires specially designed septic          high water table and possible flooding severely limit the
       tank absorption fields. Limitations for dwellings without          use of this soil for septic tank absorption fields and for
       basements and for lawns and landscaping can be                     dwellings without basements. Adding suitable fill material
       reduced by using drainage systems and by shaping the               and increasing the size of the absorption field can
       surface to direct water from buildings.                            reduce these problems. Land shaping, additions of fill
         This Jedburg soil is in capability subclass l1w.                 material, and surface drainage can reduce wetness
                                                                          around dwellings. Dikes or large amounts of fill material
         JoA-Johns loamy sand, 0 to 2 percent slopes.                     are needed in areas where this soil is subject to flooding.
       This soil is on nearly level flood plains of the Edisto            Wetness is a moderate limitation for lawns and
       River. It is somewhat poorly drained to moderately well            landscaping. Surface drainage and land shaping can
       drained. The areas are irregular in shape and commonly             reduce this limitation.
       are 10 to 30 acres.                                                   This Johns soil is in capability subclass l1w.
         Typically, the surface layer is very dark gray loamy
       sand about 6 inches thick. The subsurface layer from a                Le-Leon Sand. This soil is on nearly level upland
       depth of 6 to 12 inches is light yellowish brown sandy             terraces throughout the county. It is poorly drained. The
       loam. The subsoil from 12 to 20 inches is brownish                 areas of this soil are irregular in shape and commonly
       yellow sandy clay loam and from 20 to 31 inches is light           are 10 to 30 acres.
       yellowish brown sandy clay loam that has gray mottles.                Typically, the surface layer is very dark gray sand
       The substratum from 31 to 80 inches is strong brown,               about 6 inches thick. The subsurface layer from a depth
       light brownish gray, and light gray sand and coarse sand.          of 6 to 17 inches is light brownish gray coarse sand. The
         Included with this soil in mapping are small areas of            subsoil from 17 to 25 inches is dark reddish brown
       Chipley, Lumbee, and Osier soils. The included soils               coarse sand and from 25 to 65 inches is very dark gray
       makeup about 15 percent of the map unit.                           coarse sand. The substratum from 65 to 80 inches is
         This Johns soil is very strongly acid or strongly acid           brown coarse sand.
       except where lime has been added. Permeability is                     Included with this soil in mapping are a few small
       moderate, and the available water capacity is moderate.            areas of Chipley, Echaw, Lynn Haven, Osier, and
       The seasonal high water table is 1.5 to 3 feet below the           Seagate soils. The included soils make up about 20
       surface. This soil is subject to rare flooding and, in some        percent of the map unit.
       areas, it is subject to more frequent flooding for very               This Leon soil is extremely acid to strongly acid except
       brief periods during winter and spring.                            where lime has been added. Permeability is rapid in the
         About 80 percent of the acreage of this soil is                  surface and subsurface layers and moderate to
       woodland. The rest is cropland, pastureland, or in                 moderately rapid in the subsoil. The available water








         28                                                                                                                     Soil Survey



         capacity is low. The seasonal high water table is at the            subject to occasional flooding or ponding for brief
         surface to 1 foot below the Surface.                                periods in winter and early in spring.
            About 85 percent of the acireage of this soil is                    This soil is used mostly as woodland. In a few small
         woodland. The rest is cropland, pastureland, or in                  areas along the Edisto River, it is used for recreational
         engineering uses related to dwellings and other                     purposes.
         structures.                                                            This soil is not suited to row crops and small grains
            This soil is poorly suited to row crops and small grains         because of the seasonal high water table and occasional
         because of the low nutrient-holding capacity and                    flooding.
         seasonal high water table. Applying fertilizers at intervals           This Lumbee soil is suited to use as pastureland.
         helps to maintain proper plant growth. The fertility of this        Suitable pasture plants include tall fescue and
         soil can also be enhanced by planting leguminous cover              bahiagrass. Wetness and flooding are major
         crops. Surface and subsurface drainage systems help                 management problems. Surface drainage that has
         lower the water table. Water control structures may be              adequate outlets can reduce problems caused by
         needed with drainage systems to maintain adequate soil              wetness. Diking helps to prevent flooding.
         moisture levels for plants.                                            This soil is well suited to use as woodland. Suitable
            This Leon soil is suited to use as pastureland. Suitable         trees include loblolly pine, sweetgum, and water tupelo.
         pasture plants include common bermudagrass and                      Equipment use limitations, plant competition, and
         bahiagrass. Major management problems are the low                   seedling mortality are severe. Equipment that has wide
         nutrient-holding capacity and the seasonal high water               tires or tracks operates more efficiently on this wet soil.
         table. Weed control, applications of fertilizers, and               Site preparation and planting seedlings on raised beds
         rotation grazing help maintain good quality forage.                 reduce mortality rates and plant competition. Diking
            This soil is poorly suited to use as woodland. Improved          helps to prevent flooding from adjacent rivers and
         loblolly pine is the dominant tree. Seedling mortality,             streams. If adequate outlets are available, surface
         plant competition, and equipment use limitations are                drainage can reduce problems caused by wetness.
         moderate. Seedlings have a better survival rate if they                This soil is not suited to most engineering uses related
         are planted on raised beds. Plant competition can be                to dwellings and other structures. Wetness and flooding
         reduced by prescribed burning, site preparation, or                 severely limit the use of this soil for septic tank
         herbicides. Equipment that has wide tires or tracks                 absorption fields, for dwellings without basements, and
         operates more efficiently on this wet soil.                         for lawns and landscaping. These problems are difficult
            This soil is poorly suited to most engineering uses              and costly to reduce.
         related to dwellings and other structures. Wetness is a                This Lumbee soil is in capability subclass VIw.
         severe limitation for septic tank absorption fields, for
         dwellings without basements,, and for lawns and                        Ln-Lynchburg loamy sand. This soil is on nearly
         landscaping. This soil is not suited to septic tank                 level upland terraces. It is somewhat poorly drained. The
         absorption fields because of the high water table. Adding           areas of this soil are irregular in shape and commonly
         fill material and installing drainage systems can reduce            are 20 to 50 acres.
         the limitations for dwellings without basements and for                Typically, the surface layer is dark grayish brown
         lawns and landscaping.                                              loamy sand about 7 inches thick. The subsurface layer
            This Leon soil is in capability subclass lVw.                    from a depth of 7 to 13 inches is brown sandy loam. The
                                                                             subsoil from 13 to 17 inches is yellowish brown sandy
            Lm-Lumbee fine sandy loam, occasionally                          clay loam, from 17 to 54 inches is gray sandy clay loam,
         flooded. This soil is on nearly level flood plains, in              and from 54 to 80 inches is gray sandy clay.
         drainageways of major rivers, and in swamps. It is poorly              Included with this soil in mapping are a few small
         drained. The areas of this soil are irregular in shape and          areas of Coxville, Noboco, Ocilla, Pantego, and Pelham
         commonly are 50 to 200 acres.                                       soils. The included soils make up about 20 percent of
            Typically, the surface layer is very dark gray fine sandy        the map unit.
         loam about 5 inches thick. The subsoil from a depth of 5               This Lynchburg soil is extremely acid to strongly acid
         to 26 inches is gray sandy clay loam and from 26 to 37              except where lime has been added. Permeability is
         inches is gray sandy loam. The substratum from 37 to 70             moderate, and the available water capacity is moderate.
         inches is gray and light gray sand.                                 The seasonal high water table is 0.5 foot to 1.5 feet
            Included with this soil in mapping are a few small               below the surface.
         areas of Osier, Nakina, Rains, and Rutlege soils. The                  About 80 percent of the acreage of this soil is
         included soils make up about 15 percent of the map unit.            woodland. The rest has been cleared and drained and is
            This Lumbee soil is very strongly acid or strongly acid.         cropland, pastureland, or in engineering uses related to
         Permeability is moderate, and the available water                   dwellings and other structures.
         capacity is moderate. The seasonal high water table is at              This soil is well suited to row crops and small grains;
         the surface to 1.5 feet below the surface. This soil is             however, the seasonal high water table is a concern in








       Dorchester County, South Carolina                                                                                              29



       management. Surface and subsurface drainage systems                pastureland, or in engineering uses related to dwellings
       help lower the water table and reduce problems caused              and other structures.
       by wetness. Planting crops on raised beds helps to                    This soil is not suited to row crops and small grains
       prevent damage caused by wetness.                                  because of the high water table and the absence of
          This Lynchburg soil is well suited to use as                    suitable drainage outlets.
       pastureland. Suitable pasture plants include bahiagrass,              This Lynn Haven soil is poorly suited to use as
       bermudagrass, and fescue. The major management                     pastureland because of the seasonal high water table
       problem is the seasonal high water table. Restricted               and the absence of suitable drainage outlets.
       grazing during wet periods help keep the pasture and                  This soil is suited to use as woodland. Loblolly pine is
       soil in good condition. Surface drainage systems help              the dominant tree. Because of the high water table,
       lower the seasonal high water table.                               equipment use limitations, plant competition, and
          This soil is well suited to use as woodland. Suitable           seedling mortality are moderate. Equipment that has
       trees include loblolly pine and sweetgum. Because of the           wide tires or tracks operates more efficiently on this wet
       seasonal high water table, equipment use limitations are           soil. Removing competing vegetation helps seedling
       moderate and plant competition is severe. Surface                  survival and growth. This can be accomplished by site
       drainage can reduce these limitations. Equipment that              preparation, prescribed burning, spraying, cutting, or
       has wide tires or tracks operates more efficiently on this         girdling. Seedlings have a better survival rate if they are
       wet soil. Site preparation, prescribed burning, cutting,           planted on raised beds.
       and girdling reduce plant competition and help insure                 This soil is not suited to most engineering uses related
       maximum growth of seedlings.                                       to dwellings and other structures. The high water table is
          This soil is poorly suited to most engineering uses             a severe limitation for septic tank absorption fields, for
       related to dwellings and other structures. Wetness is a            dwellings without basements, and for lawns and
       severe limitation for septic tank absorption fields, for           landscaping. This limitation is difficult and costly to
       dwellings without basements, and for lawns and                     reduce.
       landscaping. Because of the high water table, this soil               This Lynn Haven soil is in capability subclass IVw.
       requires specially designed septic tank absorption fields.            Mo-Mouzon fine sandy loam, occasionally
       Problems caused by wetness can be reduced by adding                flooded. This soil is on broad, nearly level, low upland
       fill material around buildings and by land shaping to              terraces. It is poorly drained. The areas of this soil are
       remove water. Surface drainage systems help lower the              irregular or elongated in shape and range from 100 to
       high water table around buildings and reduce damage to             2,000 acres.
       lawns and shrubs.                                                     Typically, the surface layer is very dark grayish brown
          This Lynchburg soil is in capability subclass l1w.              fine sandy loam about 5 inches thick. The subsurface
          Ly-Lynn Haven fine sand. This soil is in slight                 layer from a depth of 5 to 8 inches is light gray loamy
                                                                          fine sand. The subsoil from 8 to 61 inches is gray sandy
       depressions and drainageways mainly in the central part            clay loam. The substratum from 61 to 80 inches is light
       of the county. It is very poorly drained. The areas of this        brownish gray and light gray sandy clay loam, sandy
       soil are elongated in shape and commonly are 5 to 100              loam, and loamy sand.
       acres.                                                                Included with this soil in mapping are small areas of
          Typically, the surface layer is very dark gray fine sand        Brookman, Coosaw, Eulonia, Osier, and Elloree soils.
       about 10 inches thick. The subsurface layer from a depth           The included soils make up about 20 percent of the map
       of 10 to 19 inches is light gray fine sand. The subsoil            unit.
       from 19 to 38 inches is dark reddish brown fine sand                  This Mouzon soil is very strongly acid to slightly acid in
       and from 38 to 49 inches is dark brown loamy fine sand.            the surface and subsurface layers and strongly acid to
       The substratum from 49 to 75 inches is grayish brown               moderately alkaline in the subsoil. Permeability is slow,
       fine sand.                                                         and the available water capacity is moderate to high.
          Included with this soil in mapping are a few areas of           The seasonal high water table ranges from the surface
       Echaw, Leon, Osier, and Pelham soils. The included                 to 1 foot below the surface. This soil is subject to
       soils make up about 20 percent of the map unit.                    occasional flooding along major drainageways during wet
          This soil is extremely acid to strongly acid except             periods.
       where lime has been added. Permeability is moderately                 This soil is used mostly as woodland. A few small
       rapid to moderate, and the available water capacity is             areas are cropland, pastureland, or in engineering uses
       low. The seasonal high water table is at the surface to 1          related to dwellings and other structures.
       foot below the surface. In some areas, this soil is                   This soil is not suited to row crops, small grains, and
       ponded for brief periods during rainy seasons.                     pasture. The major management problems are a
          This soil is used mostly as woodland. A few small               seasonal high water table, flooding, and a slowly
       areas have been cleared and drained and are cropland,              permeable subsoil. Surface drainage can reduce









          30                                                                                                                       Soil Survey



          problems caused by wetness. Crop residue management                   operates more efficiently on this wet soil. Seedlings have
          can improve the tilth of this soil.                                   a better survival rate if they are planted on raised beds.
             This soil is well suited to water-tolerant trees. Suitable           This soil is not suited to most engineering uses related
          trees include sweetgum and swamp tupelo. Because of                   to dwellings and other structures because of wetness
          the seasonal high water tabIE?, equipment use limitations,            and ponding. These limitations are difficult and costly to
          seedling mortality, and plant competition are severe.                 reduce.
          Equipment that has wide tires or tracks can operate                     This Nakina soil is in capability subclass VIw.
          more efficiently on this wet soil. Planting and harvesting
          during dry periods reduce equipment limitations. Seedling               NoA-Noboco loamy sand, 0 to 2 percent slopes.
          mortality is reduced if seedlings are planted on beds.                This soil is on nearly level upland terraces. It is well
          Site preparation, prescribed burning, girdling, and cutting           drained. The areas of this soil are irregular in shape and
          reduce plant competition.                                             commonly are 20 to 50 acres.
             This soil is not suited to most engineering uses related             Typically, the surface layer is dark grayish brown
          to dwellings and other structures. Flooding and wetness               loamy sand about 6 inches thick. The subsurface layer
          severely limit the use of this :soil for septic tank                  from a depth of 6 to 14 inches is light yellowish brown
          absorption fields, for dwellings without basements, and               loamy sand. The subsoil from 14 to 61 inches is
          for lawns and landscaping. These limitations are difficult            yellowish brown sandy clay loam; from 61 to 70 inches is
          and costly to reduce.                                                 mottled yellowish brown, gray, and red sandy clay loam;
             This Mouzon soil is in capability subclass VIw.                    and from 70 to 80 inches is gray sandy clay loam.
             Na-Nakina fine sandy loam. This soil is in shallow                   Included with this soil in mapping are a few small
          depressions and drainageways of small streams. It is                  areas of Albany, Blanton, Bonneau, Lynchburg, and
          nearly level and very poorly drained. The areas of this               Rains soils. Also included are a few small areas of soils
          soil are elongated and commonly are 20 to 40 acres.                   that have slopes of morethan 2 percent. The included
             Typically, the surface layer is black fine sandy loam              soils make up about 15 percent of the map unit.
          about 11 inches thick. The subsurface layer from a depth                This Noboco soil is very strongly acid or strongly acid
          of 11 to 18 inches is dark gray fine sandy loam. The                  except where lime has been added. Permeability is
          subsoil from 18 to 61 inches is gray sandy clay loam and              moderate, and the available water capacity is moderate.
          clay loam. The substratum from 61 to 80 inches is dark                The seasonal high water table is 2.5 to 4 feet below the
          gray or light olive gray sandy clay loam.                             surface.
             Included with this soil in mapping are small areas of                About 75 percent of the acreage of this soil is
          Brookman, Lynn Haven, MOUzon, and Yemassee soils.                     cropland. The rest is pastureland, woodland, or in
          The included soils make up about 15 percent of the map                engineering uses related to dwellings and other
          unit.                                                                 structures.
             This Nakina soil is very strongly acid to slightly acid in           This soil is well suited to row crops and small grains
          the surface layer and extremely acid to moderately                    (fig. 3) and has no major management problems for this
          alkaline in the subsoil. Permeability is moderate or                  use. Residue management, such as conservation tillage
          moderately rapid, and the available water capacity is                 and cover crops, improves the natural fertility.
          moderate. The seasonal high water table is at the                       This Noboco soil is well suited to use as pastureland
          surface to 1 foot below the surface. This soil is subject             and has no major management problems for this use.
          to rare flooding and to ponding during wet periods.                   Suitable pasture plants include improved bermudagrass
             This soil is used mostly as; woodland. A few small                 and bahiagrass. Rotation grazing and annual applications
          areas have been cleared and drained and are cropland,                 of fertilizer help maintain good forage quality.
          pastureland, or in engineering uses related to dwellings                This soil is suited to use as woodland. Suitable trees
          and other structures.                                                 include loblolly pine and longleaf pine. The moderate
             This soil is not suited to row crops and small grains              plant competition can be reduced by proper site
          because of the seasonal high water table and the                      preparation.
          absence of suitable drainage outlets.
             This Nakina soil is not suited to use as pastureland                 This soil is well suited to most engineering uses
          because of the seasonal high water table and the                      related to dwellings and other structures. Wetness is a
          absence of suitable drainage outlets.                                 severe limitation for septic tank absorption fields.
             This soil is suited to water-tolerant trees. Suitable              Increasing the size of the absorption field can reduce
          trees include water oak and sweetgum. Because of                      this problem. This soil has a slight limitation for dwellings
          wetness and ponding, equipment use limitations, plant                 without basements. Droughtiness is a moderate limitation
          competition, and seedling mortality are severe. Planting              for lawns and landscaping. This can be overcome by
          and harvesting during dry periods reduce equipment                    supplemental watering during dry periods.
          limitations. Equipment that has wide tires or tracks                    This Noboco soil is in capability class 1.








       Dorchester County, South Carolina                                                                                             31













                                                                    V,





                                                                                                                                      1`4
                                                                                                                                 R71%,






       rk



                   7-







       Figure 3.-Noboco loamy sand, 0 to 2 percent slopes, Is well suited to use as cropland. Tobacco Is one of the main crops on this soil.



         OcA-0cilla sand, 0 to 2 percent slopes. This soil is             engineering uses related to dwellings and other
       on nearly level upland terraces on lower side slopes. It is        structures.
       somewhat poorly drained. The areas of this soil                      This soil is suited to row crops and small grains. The
       commonly are about 10 to 50 acres.                                 major management problem is a seasonal high water
         Typically, the surface layer is dark grayish brown sand          table. Surface and subsurface drainage systems help
       about 6 inches thick. The subsurface layer from a depth            lower the seasonal high water table and reduce
       of 6 to 23 inches is yellowish brown and brownish yellow           problems caused by wetness. Residue management,
       loamy sand. The subsoil from 23 to 52 inches is                    such as conservation tillage and cover crops, reduces
       yellowish brown sandy loam and from 52 to 80 inches is             wind erosion and improves the natural fertility of this soil.
       gray and light gray sandy loam.                                      This Ocilla soil is suited to use as pastureland.
         Included with this soil in mapping are small areas of            Suitable pasture plants include improved bermudagrass
       Pelham, Osier, Seagate, and Rains soils. The included              and bahiagrass. The major management problem is the
       soils make u p about 20 percent of the map unit.                   seasonal high water table. Surface drainage can reduce
         This Ocilla soil is very strongly acid or strongly acid          problems caused by wetness. Rotation grazing and
       except where lime has been added. Permeability is                  annual applications of fertilizers help maintain good
       moderate, and the available water capacity is low. The             forage quality.
       seasonal high water table is 1 foot to 2.5 feet below the            This soil is suited to use as woodland. Loblolly pine is
       surface.                                                           the dominant tree. Because of the seasonal high water
         About 70 percent of the acreage of this soil is                  table, equipment use limitations, plant competition, and
       woodland. The rest is cropland, pastureland, or in                 seedling mortality are moderate. Surface drainage can








           32                                                                                                                      Soil Survey



           reduce problems caused by,vvetness. Proper site                      table and reduces problems caused by wetness. Proper
           preparation increases seedling survival.                             site preparation and harvesting and planting trees during
             This soil is poorly suited to most engineering uses                dry periods also reduce the problems caused by
           related to dwellings and other structures. Wetness is a              wetness. Bedding seedlings helps to lower mortality
           severe limitation for septic tank absorption fields. Adding          rates.
           suitable fill material or increasing the size of the                   This soil is poorly suited to most engineering uses
           absorption field can reduce problems caused by                       related to dwellings and other structures. Wetness and
           wetness. Wetness is a moderate limitation for dwellings              flooding severely limit the use of this soil for septic tank
           without basements and for lawns and landscaping.                     absorption fields, for dwellings without basements, and
           Surface drainage can reduce problems caused by                       for lawns and landscaping. This soil is not suited to
           wetness.                                                             septic tank absorption fields because of the seasonal
             This Ocilla soil is in capability subclass IIIw.                   high water table. Sewage effluent can be pumped to a
                                                                                suitable site to reduce this problem. The wetness
             Og-Ogeechee fine sanely loam. This soil is on                      limitation can be reduced for dwellings without
           nearly level upland terraces iand in drainageways. It is             basements by adding fill material and by shaping the
           poorly drained. The areas of this soil are irregular or              surface to divert surface water from buildings. Surface
           elongated in shape and commonly are 10 to 200 acres.                 drainage on lawns and landscaped areas helps to lower
             Typically, the surface layer is very dark gray fine sandy          the seasonal high water table and reduces problems
           loam about 4 inches thick. The subsurface layer from a               caused by wetness.
           depth of 4 to 12 inches is gray fine sandy loam. The                   This Ogeechee soil is in capability subclass IIIw.
           subsoil from 12 to 57 inches is gray sandy clay loam
           with strata of sand in the lower part. The substratum                  Os-0sler loamy fine sand, frequently flooded.
           from 57 to 65 inches is gray fine sand.                              This soil is in nearly level, depressional areas and on
             Included with this soil in mapping are small areas of              lowlands adjacent to streams. It is poorly drained. The
           Coosaw, Nakina, Mouzon, Osier, and Yauhannah soils.                  areas of this soil are elongated or irregular in shape and
           The included soils make up about 20 percent of the map               commonly are 20 to 50 acres.
           unit.                                                                  Typically, the surface layer is very dark gray loamy fine
             This Ogeechee soil is very strongly acid or strongly               sand about 3 inches thick. The underlying material from
           acid except where lime has been added. Permeability is               a depth of 3 to 80 inches is grayish and brownish fine
           moderate, and the available water capacity is moderate               sand and sand.
           to high. The seasonal high water table is at the surface               Included with this soil in mapping are small areas of
           to 0.5 foot below the surfaCe. This soil is subject to rare          Leon, Lynn Haven, Pelham, and Plummer soils. The
           flooding or ponding for brief periods during wet periods.            included soils make up about 30 percent of the map unit.
             This soil is used mostly as woodland. A few small                    This soil is extremely acid to medium acid.
           areas have been cleared and are cropland, pastureland,               Permeability is very rapid. The available water capacity is
           or in engineering uses related to dwellings and other                very low, and the seasonal high water table is at the
           structures.                                                          surface to 1 foot below the surface. This soil is subject
             This soil is well suited to row crops and small grains;            to frequent flooding for brief periods from December to
           however, the seasonal highwater table is a concern in                April.
           management. In a few areas, ponding is also a major                    This soil is used mostly as woodland. A few small
           concern. Surface and subsurface drainage systems help                areas have been cleared and drained and are cropland,
           lower the water table and reduce problems caused by                  pastureland, or in engineering uses related to dwellings
           wetness. Bedding crops improves plant survival rates                 and other structures.
           and prevents seeds from decaying.                                      This soil is not suited to row crops and small grains or
             This Ogeechee soil is well suited to use as                        to use as pastureland because of the seasonal high
           pastureland. Suitable pasture plants include tall fescue,            water table and frequent flooding.
           bahiagrass, and bermudagrass. The major management                     This soil is suited to water-tolerant trees. Suitable
           problem is the seasonal high water table. Surface and                trees include water tupelo and baldcypress. Because of
           subsurface drainage systems help lower the water table               the seasonal high water table and frequent flooding,
           and reduce problems caused by wetness. Restricted                    equipment use limitations, plant competition, and
           grazing during wet periods helps to prevent compaction               seedling mortality are severe. Removing excess surface
           and improves the quality of the forage.                              water, planting seedlings on raised beds, and controlling
             This soil is well suited to use as woodland. Suitable              competing vegetation by site preparation, controlled
           trees include loblolly pine and sweetgum. Because of the             burning, cutting, spraying, or girdling can reduce these
           seasonal high water table, equipment use limitations are             problems.
           severe and plant competition and seedling mortality is                 This soil is not suited to most engineering uses related
           moderate. Surface drainage helps to lower the water                  to dwellings and other structures. Wetness and frequent








       Dorchester County, South Carolina                                                                                               33



       flooding severely limit the use of this soil for septic tank       is light brownish gray loamy sand. The subsoil from 35 to
       absorption fields, for dwellings without basements, and            80 inches is light gray sandy loam and sandy clay loam.
       for lawns and landscaping. These problems are difficult               Included with this soil in mapping are a few small
       and costly to reduce.                                              areas of Albany, Echaw, Rains, and Seagate soils. The
         This Osier soil is in capability subclass Vw.                    included soils make up about 20 percent of the map unit.
                                                                             This soil is very strongly acid or strongly acid except
         Pa-Pantego sandy loam. This soil is in nearly level              where lime has been added. Permeability is rapid in the
       or slightly depressional areas on upland terraces. It is           surface and subsurface layers and moderate in the
       very poorly drained. The areas of this soil are either oval        subsoil. The available water capacity is low. The
       or elongated and commonly are 20 to 60 acres.                      seasonal high water table is 0.5 foot to 1.5 feet below
         Typically, the surface layer is black sandy loam about           the surface. Some small areas of this soil are subject to
       12 inches thick. The subsurface layer from a depth of 12           brief ponding during wet periods,
       to 18 inches is light brownish gray loamy sand. The                   Most areas of this soil are woodland. A few small
       subsoil from 18 to 37 inches is gray sandy clay loam,              areas are cropland, pastureland, or in engineering uses
       from 37 to 74 inches is gray sandy clay, and from 74 to            related to dwellings and other structures.
       80 inches is gray sandy clay loam.                                    This soil is suited to row crops and small grains;
         Included with this soil in mapping are a few small               however, the low nutrient-holding capacity and the
       areas of Lynchburg, Coxville, and Nakina soils. The                seasonal high water table are concerns in management.
       included soils make up about 10 percent of the map unit.           Drainage can be provided by open ditches or tile drains.
         This Pantego soil is extremely acid to strongly acid.            Where tile drains are used, a filter is needed to prevent
       Permeability is moderate, and the available water                  sand from entering tile lines. Water control structures in
       capacity is moderate to high. The seasonal high water              open ditches help control desired water levels during dry
       table is at the surface to 1.5 feet below the surface.             periods. Because of the rapid leaching of nutrients from
       Some areas of this soil are ponded briefly during wet              this soil, more frequent applications of fertilizer and lime
       periods.                                                           are needed for good plant growth. Maintaining crop
         This soil is used mostly as woodland. A few small                residue on or near the surface reduces soil blowing,
       areas have been drained and cleared for other uses.                helps to maintain soil tilth and organic matter content,
         This soil is not suited to row crops and small grains            and improves yields.
       because of the seasonal high water table and the                      This Pelham soil is suited to use as pastureland.
       absence of suitable drainage outlets.                              Bahiagrass is the dominant pasture plant. Major
         This Pantego soil is poorly suited to use as                     management problems are the seasonal high water table
                                                                          and low nutrient-holding capacity. Shallow surface drains
       pastureland because of the seasonal high water table               can remove excess surface water. The use of this soil
       and the absence of suitable drainage outlets.                      for pasture or hay is also effective in controlling soil
         This soil is suited to water-tolerant trees, such as             blowing. Proper stocking, pasture rotation, deferred
       baldcypress, water tupelo, and water oak. Because of               grazing, and restricted use during wet periods help keep
       the seasonal high water table, equipment use limitations,          the pasture and soil in good condition.
       plant competition, and seedling mortality are severe. Site            This soil is suited to use as woodland. Loblolly pine is
       preparation and planting and harvesting during dry                 the dominant tree. Because of the seasonal high water
       periods can reduce equipment use limitations. Seedling             table, equipment use limitations, plant competition, and
       mortality is reduced if seedlings are planted on raised            seedling mortality are severe. Surface drainage helps
       beds.                                                              lower the water table and reduces the problems caused
         This soil is poorly suited to most engineering uses              by wetness. Seedlings should be planted on raised beds.
       related to dwellings and other structures. Wetness and             Competing vegetation can be controlled by site
       the absence of suitable drainage outlets are severe                preparation, prescribed burning, spraying, cutting, or
       limitations for septic tank absorption fields, for dwellings       girdling.
       without basements, and for lawns and landscaping.                     This soil is poorly suited to most engineering uses
       These limitations are difficult and costly to reduce.              related to dwellings and other structures. It is not suited
         This Pantego soil is in capability subclass VIw.                 to septic tank absorption fields because of the seasonal
                                                                          high water table and brief ponding. Sewage effluent can
         Pe-Pelham sand. This soil is in nearly level                     be pumped to a suitable site to reduce this problem.
       depressions and drainageways. It is poorly drained. The            Wetness and ponding severely limit the use of this soil
       areas of this soil are elongated or irregular in shape and         for septic tank absorption fields, for dwellings without
       commonly are 20 to 100 acres.                                      basements, and for lawns and landscaping. Additions of
         Typically, the surface layer is very dark gray sand              fill material, land shaping, and shallow surface drainage
       about 7 inches thick. The subsurface layer from a depth            can reduce these limitations.
       of 7 to 14 inches is gray sand and from 14 to 35 inches               This Pelham soil is in capability subclass IIIw.








           34                                                                                                                      Soil Survey



              Pm-Plummer loamy sand. This soil is in                              Included with this soil in mapping are small areas of
           drainageways and depressions. It is nearly level and                 Coxville, Goldsboro, Pantego, and Pelham soils. The
           poorly drained. The areas of this soil are irregular or              included soils make up about 20 percent of the map unit.
           elongated in shape and commonly are 20 to 50 acres.                    This soil is very strongly acid or strongly acid except
              Typically, the surface layer is very dark gray loamy              where lime has been added. Permeability is moderate,
           sand about 9 inches thick. The subsurface layer from a               and the available water capacity is moderate. The
           depth of 9 to 45 inches is gray and light gray sand and              seasonal high water table is at the surface to 1 foot
           from 45 to 58 inches is grayish brown sand. The subsoil              below the surface.
           from a depth of 58 to 75 inches is light gray sandy loam.              Most areas of this soil are woodland. Small areas are
              Included with this soil in mapping are small areas of             cropland, pastureland, or in engineering uses related to
           Chipley, Pelham, Seagate, and Rutlege soils. The                     dwellings and other structures.
           included soils make up abOUt 20 percent of the map unit.               This soil is well suited to row crops and small grains;
              This Plummer soil is extremely acid to strongly acid.             however, wetness is a limitation. Surface and subsurface
           Permeability is rapid in the surface and subsurface layers           drainage systems help lower the seasonal high water
           and moderate in the subsoil. The available water                     table and reduce problems caused by wetness. Planting
           capacity is low. The seasonal high water table ranges                crops on raised beds helps to prevent seed decay or
           from 2 feet above the surface to 1.5 feet below the                  drowning. Land shaping to remove surface water
           surface. This soil is subject to ponding in winter and in            reduces wet spots in fields. Returning crop residue to the
           spring.                                                              soil improves fertility, reduces crusting, and increases the
              Most areas of this soil are woodland. Small areas are             water infiltration rate.
           cropland, pastureland, or in engineering uses related to               This Rains soil is well suited to use as pastureland.
           dwellings and other structures.                                      Suitable pasture plants include bahiagrass and tall
              This soil is not suited to row crops and small grains             fescue. The major management problem is the seasonal
           because of the seasonal high water table, poncling, and              high water table. Sufficient drainage is needed to remove
           the absence of suitable drainage outlets.                            excess surface water and to lower the water table. This
              This Plummer soil is poorly suited to use as                      can be obtained by using shallow surface drains. Proper
           pastureland because of the seasonal high water table,                stocking, pasture rotation, timely deferment of grazing,
           ponding, and the absence of suitable drainage outlets.               and restricted use during wet periods help keep the
              This soil is poorly suited to use as woodland. Suitable           pasture and soil in good condition.
           trees include pond pine, baldcypress, and swamp tupelo.                This soil is well suited to use as woodland. Suitable
                                                                                trees include loblolly pine and sweetgum. Because of the
           Because of wetness and ponding, equipment use                        seasonal high water table, equipment use limitations,
           limitations, plant competition, and seedling mortality are           plant competition, and seedling mortality are severe.
           severe. Site preparation and planting and harvesting                 Equipment that has wide tires or tracks operates more.
           during dry periods can reduce these problems.                        efficiently on this wet soil. Planting and harvesting during
           Equipment that has wide tires or tracks operates more                dry periods reduces equipment use limitations. Seedling
           efficiently on this wet soil. Seedlings have a better                mortality is reduced if seedlings are planted on raised
           survival rate if they are plarited on raised beds.                   beds. Site preparation, prescribed burning, cutting, and
              This soil is not suited to most engineering uses related          girdling can reduce plant competition.
           to dwellings and other structures. Wetness and ponding                 This soil is poorly suited to most engineering uses
           severely limit the use of this soil for septic tank                  related to dwellings and other structures. It is not suited
           absorption fields, for dwellings without basements, and              to septic tank absorption fields because of the seasonal
           for lawns and landscaping. These limitations are difficult           high water table. Sewage effluent can be pumped to a
           and costly to reduce.                                                suitable site to reduce this limitation. Wetness is a
              This Plummer soil is in capability subclass Vw.                   severe limitation for septic tank absorption fields, for
                                                                                dwellings without basements, and for lawns and
              Ra-Rains sandy loam. This soil is on nearly level,                landscaping. This limitation can be reduced around
           broad flats and in shallow depressions and                           dwellings without basements by adding fill material, by
           drainageways. It is poorly drained. The areas of this soil           shaping the surface to remove surface water, and by
           are elongated or irregular in shape and commonly are 10              installing surface drainage systems. Surface drainage
           to 100 acres.                                                        systems also help to prevent wetness damage to lawns
              Typically, the surface layer is very dark gray sandy              and landscaping.
           loam about 4 inches thick. The subsurface layer from a                 This Rains soil is in capability subclass IIIw.
           depth of 4 to 9 inches is gray sandy loam. The subsoil
           from 9 to 42 inches is gray sandy clay loam, from 42 to                Ru-Rutlege loamy fine sand, frequently flooded.
           56 inches is gray clay loam, and from 56 to 80 inches is             This soil is in drainageways of small streams and
           sandy clay loam with strata of sandy loam.                           swamps. It is nearly level and very poorly drained. The









      Dorchester, County, South Carolina                                                                                                35



      areas of this soil are irregular or elongated in shape and             This Seagate soil is extremely acid to medium acid
      commonly are 30 to 100 acres.                                        except where lime has been added. Permeability is rapid
         Typically, the surface layer is very dark gray loamy fine         in the upper layers and moderate in the lower part of the
      sand about 13 inches thick. The subsurface layer from a              subsoil. The available water capacity is low. The
      depth of 13 to 21 inches is dark gray loamy fine sand.               seasonal high water table is 1.5 to 2.5 feet below the
      The underlying material from 21 to 65 inches is light                surface.
      brownish gray and light gray fine sand and from 65 to 75               Most areas of this soil are woodland. A few small
      inches is grayish brown sand.                                        areas are cropland, pastureland, or in engineering uses
         Included with this soil in mapping are small areas of             related to dwellings and other structures.
      Albany, Chipley, and Osier soils. The included soils make              This soil is suited to row crops and small grains. The
      up about '15 percent of the map unit.                                seasonal high water table and low nutrient-holding
         This Rutlege soil is extremely acid to strongly acid.             capacity are concerns in management. Surface and
      Permeability is rapid, and the available water capacity is           subsurface drainage systems help lower the seasonal
      low. The seasonal high water table is at the surface to 1            high water table. Water control structures in connection
      foot below the surface. This soil is subject to frequent             with drainage systems help to maintain adequate soil
      flooding or ponding for brief periods in winter and in               moisture levels for crops throughout the year. Split
      spring.                                                              applications of fertilizer help maintain proper plant
         Most areas of this soil are woodland. Small areas are             growth. Residue management helps to prevent soil
      cropland, pastureland, or in engineering uses related to             blowing, increases organic matter content, and improves
      dwellings and other structures.                                      natural fertility.
         This soil is not suited to row crops and small grains               This Seagate soil is suited to use as pastureland.
      because of the seasonal high water table, flooding or                Suitable pasture plants include bahiagrass and
      ponding, and the absence of suitable drainage outlets.               bermudagrass. The major management problem is the
         This Rutlege soil is poorly suited to use as pastureland          seasonal high water table, but surface drainage systems
      because of the seasonal high water table, flooding or                can reduce the problems caused by wetness. Rotation
      ponding, and the absence of suitable drainage outlets.               grazing, restricted grazing during wet periods, and annual
         This soil is suited to water-tolerant trees, such as              application of fertilizers help keep the pasture and soil in
      sweetgum and baldcypress. Because of wetness,                        good condition.
      flooding, and ponding, equipment use limitations, plant                This soil is suited to use as woodland. Loblolly pine is
      competition, and seedling mortality are severe. Site                 the dominant tree. Because of the high water table,
      preparation and planting or harvesting during dry periods            equipment use limitations, plant competition, and
      can reduce these limitations. Equipment that has wide                seedling mortality are moderate. Equipment that has
      tires or tracks operates more efficiently on this wet soil.          wide tires or tracks operates more efficiently on this wet
      Seedlings have a better survival rate if they are planted            soil. Seedlings have a better survival rate if they are
      on raised beds.                                                      planted on raised beds. Site preparation, prescribed
         This soil is not suited to most engineering uses related          burning, cutting, and girdling can reduce plant
      to dwellings and other structures. Wetness, flooding, and            competition.
      ponding severely limit the use of this soil for septic tank            This soil is poorly suited to most engineering uses
      absorption fields, for dwellings without basements, and              related to dwellings and other structures. Wetness is a
      for lawns and landscaping. These limitations are difficult           severe limitation for septic tank absorption fields and a
      and costly to reduce.                                                moderate limitation for dwellings without basements and
         This Rutlege soil is in capability subclass VIw.                  for lawns and landscaping. This soil requires specially
                                                                           designed septic tank absorption fields because of
         Se-Seagate sand. This soil is on nearly level upland              problems caused by the seasonal high water table.
      terraces. It is somewhat poorly drained. The areas of this           Adding fill material to the building site, shaping the
      soil are irregular in shape and commonly are 5 to 25                 surface to divert water from buildings, and installing
      acres.                                                               drainage systems reduce problems caused by wetness
         Typically, the surface layer is black sand about 6                around dwellings without basements and on lawns.
      inches thick. The subsurface layer from a depth of 6 to                This Seagate soil is in capability subclass IIIw.
      14 inches is gray sand. The subsoil from 14 to 18 inches
      is dark reddish brown loamy sand. A subsurface layer of                Wa-Wahee fine sandy loam. This soil is on broad,
      yellow sand is at a depth of 18 to 32 inches. The lower              nearly level, low upland terraces. It is somewhat poorly
      part of the subsoil from 32 to 79 inches is gray fine                drained. The areas of this soil are irregular in shape and
      sandy loam.                                                          commonly are 20 to 40 acres.
         Included with this soil in mapping are small areas of               Typically, the surface layer is dark grayish brown fine
      Echaw, Leon, Pelham, and Elloree soils. The included                 sandy loam about 6 inches thick. The subsurface layer
      soils make up about 15 percent of the map unit.                      from 6 to 10 inches is brown fine sandy loam. The









           36                                                                                                                   Soil Survey



           subsoil from 10 to 15 inches; is yellowish brown clay              sandy loam and sandy clay loam and from 52 to 76
           loam, from 15 to 26 inches is gray clay, and from 26 to            inches is light gray sandy clay loam that has mottles in
           59 inches is gray sandy clay loam. The substratum from             shades of brown, yellow, gray, or red. The substratum
           59 to 80 inches is light brownish gray sandy clay loam             from 76 to 80 inches is gray fine sandy loam.
           and clay.                                                            Included with this soil in mapping are small areas of
             Included with this soil in rnapping are small areas of           Coosaw, Eulonia, Ogeechee, and Wahee soils. Also
           Mouzon and Brookman soils. The included soils make up              included are small areas of soils that have slopes of 2 to
           about 15 percent of the map unit.                                  6 percent. The included soils make up about 20 percent
             This soil is extremely acid to strongly acid except              of this map unit.
           where lime has been added, Permeability is slow, and                 This Yauhannah soil is extremely acid to medium acid
           the available water capacity is moderate to high. The              except where lime has been added. Permeability is
           shrink-swell potential is moderate. The seasonal high              moderate, and the available water capacity is moderate.
           water table is 0.5 foot to 1.5 feet below the surface. This        The seasonal high water table is 1.5 to 2.5 feet below
           soil is ponded briefly during wet periods.                         the surface.
             Most areas of this soil are woodland. A few small                  Most areas of this soil are woodland (fig. 4). A few
           areas are cropland, pastureland, or in engineering uses            small areas are cropland, pastureland, and in
           related to dwellings and other structures.                         engineering uses related to dwellings and other
             This soil is well suited to row crops and small grains;          structures.
           however, wetness and the dayey subsoil are concerns in               This soil is well suited to row crops and small grains;
           management. Drainage systems and land shaping can                  however, the seasonal high water table is a concern in
           help reduce problems caused by wetness. Crop residue               management. Surface or subsurface drainage systems
           management can improve the tilth of this soil.                     help lower the water table and reduce problems caused
             This Wahee soil is well Suited to use as pastureland.            by wetness.
           Suitable pasture plants include tall fescue and                      This Yauhannah soil is well suited to use as
           bahiagrass. Wetness is a major management problem,                 pastureland. Suitable pasture plants include improved
           but surface drainage systerns can reduce this problem.             bermudagrass and bahiagrass. Wetness is a major
           Restricted grazing during wet periods reduces soil                 management problem, but drainage systems can lower
           compaction and improves the quality of the forage.                 the seasonal high water table and reduce the problems
             This soil is suited to use as woodland. Suitable trees           caused by wetness. Restricted grazing during wet
           include loblolly pine, sweetgum, American sycamore, and            periods help maintain good forage quality, reduce soil
           water oak. Equipment use limitations and seedling                  compaction, and prevent sod damage.
           mortality are moderate, and plant competition is severe.             This soil is well suited to use as woodland. Suitable
           Surface drainage and site preparation are needed along             trees include loblolly pine, yellow poplar, sweetgum, and
           with equipment that has wide tires or tracks.                      American Sycamore. Because of wetness, equipment
             This soil is poorly suited to engineering uses related to        use limitations and plant competition are moderate.
           dwellings and other structures. It is not suited to use as         Equipment that has wide tires or tracks operates more
           septic tank absorption fields because of the seasonal              efficiently on this soil. Proper site preparation increases
           high water table and slow permeability. Sewage effluent            seedling survival.
           can be pumped to a suitable site. Moderate shrink-swell              This soil is poorly suited or suited to most engineering
           potential and wetness are problems for dwellings without           uses related to dwellings and other structures. Because
           basements. Surface drainage and land shaping can                   of the seasonal high water table, this soil has severe
           reduce these problems. Specially designed foundations              limitations for septic tank absorption fields and requires
           help prevent construction problems, such as cracked                specially designed systems. Wetness is a moderate
           brick walls or concrete slabs. Wetness is also a problem           limitation for dwellings without basements and for lawns
           for lawns and landscaping, but land shaping and                    and landscaping. Surface and subsurface drainage
           drainage systems can remove excess water.                          systems help lower the high water table. Shaping the
             This Wahee soil is in capability subclass l1w.                   surface to divert water from dwellings can reduce
                                                                              problems caused by wetness.
             YaA-Yauhannah loamy fine sand, 0 to 2 percent                      This Yauhannah soil is in capability subclass l1w.
           slopes. This soil is on nearly level, broad terraces in the
           southeastern part of the county. It is moderately well               Ye-Yemassee fine sandy loam. This soil is on
           drained. The areas of this soil are irregular in shape and         nearly level terraces in the southeastern part of the
           commonly are 20 to 80 acres.                                       county. It is somewhat poorly drained. The areas of this
             Typically, the surface layer is grayish brown loamy fine         soil are irregular in shape and commonly are 10 to 30
           sand about 4 inches thick. The subsurface layer from a             acres.
           depth of 4 to 18 inches is pale yellow loamy fine sand.              Typically, the surface layer is very dark gray fine sandy
           The subsoil from 18 to 52 inches is brownish yellow fine           loam about 6 inches thick. The subsurface layer from a







     Dorchester County, South Carolina                                                                                       37








                                                                        A


















                                                                                          4













                      Al




                                             jc,!







      Figure 4.-Yauhannah loamy fine sand, 0 to 2 percent slopes, Is well suited to production of Christmas trees and other timber products.



      depth of 6 to 10 inches is yellowish brown fine sandy           moderate, and the available water capacity is moderate.
      loam and from 10 to 15 inches is light yellowish brown          The seasonal high water table is 1 foot to 1.5 feet below
      fine sandy loam. The subsoil from 15 to 48 inches is            the surface.
      gray sandy clay loam and from 48 to 80 inches is light            Most areas of this soil are woodland. A few small
      gray sandy clay loam with strata of clay and sandy loam.        areas are cropland, pastureland, or in engineering uses
        Included with this soil in mapping are a few small            related to dwellings and other structures.
      areas of Nakina, Ogeechee, Wahee, and Elloree soils.              This soil is well suited to row crops and small grains.
      The included soils make up about 25 percent of the map          Wetness is the major management problem, but surface
      unit.                                                           and subsurface drainage systems help lower the high
        This Yemassee soil is extremely acid to strongly acid         water table and reduce the problems caused by
      except where lime has been added. Permeability is










           38



           wetness. Residue management improves the natural                    wetness. Equipment that has wide tires or tracks
           fertility of this soil.                                             operates more efficiently on this wet soil. Proper site
             This Yemassee soil is well suited to use as                       preparation, prescribed burning, cutting, and girdling
           pastureland. Suitable pasture plants include improved               reduce plant competition.
           bermudagrass and bahiagrass. Wetness is a major                       This soil is poorly suited to most engineering uses
           management problem because of the seasonal high                     related to dwellings and other structures. Wetness is a
           water table. Surface drainage can reduce problems                   severe limitation for septic tank absorption fields and for
           caused by wetness. Restricted grazing during wet                    dwellings without basements. Specially designed septic
           periods help keep the soil in good condition and improve            tank absorption fields are needed because of the
           forage quality.                                                     seasonal high water table. Wetness problems can be
             This soil is well suited to use as woodland. Suitable             reduced around dwellings without basements by adding
           trees include loblolly pine, American sycamore, and                 fill material or by land shaping to divert surface water
           yellow poplar. Because of wetness, equipment use                    away from buildings. Wetness is a moderate limitation for
           limitations are moderate and plant competition is severe.           lawns and landscaping.
           Surface drainage can reduce problems caused by                        This Yemassee soil is in capability subclass l1w.










                                                                                                                                39





      Prime Farmland


        In this section, prime farmland is defined and                 Department of Agriculture recognizes that government at
      discussed, and the prime farmland soils in Dorchester            local, state, and federal levels, as well as individuals,
      County are listed.                                               must encourage and facilitate the wise use of our
        Prime farmland is one of several kinds of important            nation's prime farmland.
      farmland defined by the U.S. Department of Agriculture.             Prime farmland soils, as defined by the U.S.
      It is of major importance in meeting the nation's short-         Department of Agriculture, are soils that are best suited
      and long-range needs for food and fiber (fig. 5). The            to producing food, feed, forage, fiber, and oilseed crops.
      acreage of high-quality farmland is limited, and the U.S.        Such soils have properties that are favorable for the




                                                                                          *Ae



      bow&&



















                                                                                 271,-




                                              N
                          7                                                             me
                                                                  4k




                 Figure 5.-Noboco loamy sand, 0 to 2 percent slopes, is one of several prime farmland soils in Dorchester County.









           40



           economic production of sustained high yields of crops.              are scattered throughout the county. In some areas,
           The soils need only to be treated and managed using                 prime farmland is used as woodland or pastureland.
           acceptable farming methods. The moisture supply, of                     The following map units, or soils, make up prime
           course, must be adequate, and the growing season has                farmland in Dorchester County. The location of each
           to be sufficiently long. Prime farmland soils produce the           map unit is shown on the detailed soil maps at the back
           highest yields with minimal inputs of energy and                    of this publication. The extent of each unit is given in
           economic resources. Farming these soils results in the              table 4. The soil qualities that affect use and
           least damage to the environment.                                    management are described in the section "Detailed Soil
             Prime farmland soils may presently be in use as                   Map Units." This list does not constitute a
           cropland, pasture, or woodland, or they may be in other             recommendation for a particular land use.
           uses. They either are used for producing food or fiber or               Soils that have limitations, such as a high water table
           are available for these uses. Urban or built-up land,               or flooding, may qualify as prime farmland if these
           public land, and water areas cannot be considered prime             limitations are overcome by such measures as drainage
           farmland. Urban or built-up land is any contiguous unit of          or flood control. In the following list, the measures
           land 10 acres or more in size that is used for such                 needed to overcome the limitations of a map unit, if any,
           purposes as housing, industrial, and commercial sites,              are shown in parentheses after the map unit name.
           sites for institutions or public buildings, small parks, golf       Onsite evaluation is necessary to determine if the
           courses, cemeteries, railroad yards, airports, sanitary             limitations have been overcome by the corrective
           landfills, sewage treatment plants, and water control               measures.
           structures. Public land is land not available for farming in        EpB     Emporia loamy fine sand, 2 to 6 percent slopes
           national forests, national parks, military reservations, and        EuA     Eulonia fine sandy loam, 0 to 2 percent slopes
           state parks.                                                        EuB     Eulonia fine sandy loam, 2 to 6 percent slopes
             Prime farmland soils usually get an adequate and                  FoA     Foreston loamy fine sand, 0 to 2 percent slopes
           dependable supply of Moisture from precipitation or                 GoA     Goldsboro loamy sand, 0 to 2 percent slopes
           irrigation. The temperature and growing season are                  IzA     Izagora silt loam, 0 to 2 percent slopes
           favorable. The acidity or alkalinity level of the soils is          IzB     Izagora silt loam, 2 to 6 percent slopes
           acceptable. The soils have few or no rocks and are                  Jd      Jedburg loam (where artificially drained)
           permeable to water and air. They are not excessively                JoA     Johns loamy sand, 0 to 2 percent slopes (where
           erodible or saturated with water for long periods and are                   artificially drained)
           not subject to frequent flooding during the growing                 Ln      Lynchburg loamy sand (where artificially drained)
           season. The slope ranges mainly from 0 to 6 percent,                NoA     Noboco loamy sand, 0 to 2 percent slopes
           but most slopes are less than 2 percent.                            YaA     Yauhannah loamy fine sand, 0 to 2 percent slopes
             About 114,400 acres, or 131 percent of Dorchester                 Ye      Yemassee fine sandy loam (where artificially
           County, is prime farmland. The areas of prime farmland                      drained)










                                                                                                                                             41




       Use and Management of the Solis

          This soil survey is an inventory and evaluation of the             yields of the main crops and hay and pasture plants are
       soils in the survey area. It can be used to adjust land               listed for each soil.
       uses to the limitations and potentials of natural                        Planners of management systems for individual fields
       resources and the environment. Also, it can help avoid                or farms should consider the detailed information given
       soil-related failures in land uses.                                   in the description of each soil under "Detailed Soil Map
          In preparing a soil survey, soil scientists,                       Units." Specific information can be obtained from the
       conservationists, engineers, and others collect extensive             local office of the Soil Conservation Service or the
       field data about the nature and behavior characteristics              Cooperative Extension Service.
       of the soils. They collect data on erosion, droughtiness,                About 60,000 acres in Dorchester County was used as
       flooding, and other factors that affect various soil uses             pasture, hayland, or cropland in 1982, according to the
       and management. Field experience and collected data                   Soil Conservation Service County Resources Inventory.
       on soil properties and performance are used as a basis                Of this, about 43,000 acres was used for field crops,
       for predicting soil behavior.                                         mainly soybeans, corn, tobacco, and wheat.
          Information in this section can be used to plan the use               The soils in Dorchester County have good suitability
       and management of soils for crops and pasture; as                     for increased production of food. In 1982, more than
       rangeland and woodland; as sites for buildings, sanitary              240,000 acres of potentially good cropland was used as
       facilities, highways and other transportation systems, and            woodland or pastureland. In addition, the production of
       parks and other recreation facilities; and for wildlife               food can be increased by extending the latest crop
       habitat. It can be used to identity the potentials and                production technology to all cropland in the county. This
       limitations of each soil for specific land uses and to help           soil survey can greatly facilitate the application of such
       prevent construction failures caused by unfavorable soil              technology.
       properties.                                                              In general, the soils in the county that are well suited
          Planners and others using soil survey information can              to cro IPs and pasture are also well suited to urban
       evaluate the effect of specific land uses on productivity             development. According to the 1982 County Resources
       and on the environment in all or part of the survey area.             Inventory, an estimated 14,400 acres in Dorchester
       The survey can help planners to maintain or create a                  County was urban and built-up land. Urban and built-up
       land use pattern that is in harmony with nature.                      land in the county has been growing at the rate of about
          Contractors can use this survey to locate sources of               400 acres per year. The use of this soil survey to help
       sand, roadfill, and topsoil. They can use it to identify              make land use decisions that can influence the future
       areas where wetness or very firm soil layers can cause                role of farming in the county is discussed in the section
       difficulty in excavation.                                             "Broad Land Use Considerations.'
          Health officials, highway officials, engineers, and                   Soil erosion is a major concern on less than 1 percent
       others may also find this survey useful. The survey can               of the land in Dorchester County. It is a hazard on less
       help them plan the safe disposal of wastes and locate                 than 5 percent of the pasture and cropland. Water
       sites for pavements, sidewalks, campgrounds,                          erosion commonly is a hazard on soils that have slopes
       playgrounds, lawns, and trees and shrubs.                             of more than 2 percent and on soils that have very long
                                                                             slopes of 1 to 2 percent. The Emporia, Eulonia, Izagora,
       Crops and Pasture                                                     and Nobocci soils have a significant hazard of erosion if
                                                                             they are used for crops. Wind erosion is a concern on
          Gene E. Hardee, conservation agronomist, Soil Conservation         clean tilled, sandy soils; however, most of the damage
       Service, helped prepare this section.                                 by wind movement of soil particles is damage to young
          General management needed for crops and pasture is                 plants rather than actual soil loss.
       suggested in this section. The crops or pasture plants                   Loss of the surface layer through erosion reduces
       best suited to the soils, including some not commonly                 productivity on soils and causes sedimentation in
       grown in the survey area, are identified; the system of               streams. Productivity is reduced as the surface layer is
       land capability classification used by the Soil                       lost and part of the subsoil is incorporated into the plow
       Conservation Service is explained; and the estimated                  layer. Loss of the surface layer is especially damaging








           42                                                                                                                        Soil Survey



           on soils that have a clayey subsoil, for example, on the              Foxworth, Ocilla, Pelham, and Seagate soils. This
           Eulonia soils. Erosion also reduces productivity on deep,             limitation can be reduced through crop residue
           sandy soils, such as the Alpin, Blanton, Bonneau,                     management, proper crop selection, and irrigation. These
           Chisolm, and Foxworth soils, largely because of loss of               soils are well suited to pasture grasses, such as
           nutrients and fine soil particles. Soil erosion on farmland           bahiagrass and bermudagrass, and drought-tolerant
           results in sediment entering streams. Control of the                  crops, such as rye and grain sorghum. Because of the
           erosion minimizes the pollution of streams by sediment                rapid leaching of nutrients from these soils, frequent
           and improves the quality of viater for municipal use, for             applications of fertilizer and lime are needed for good
           recreation, and for use by fish and wildlife.                         plant growth.
             Water erosion can best be controlled by using a                       Because soil fertility is naturally low in most soils in
           combination of structural measures, which remove                      Dorchester County, regular applications of lime and
           excess water from the field, and cropping and tillage                 fertilizer are needed. Nearly all of the soils are naturally
           systems, which provide cover and reduce runoff.                       medium acid, strongly acid, or very strongly acid. Regular
           Structural measures, such as diversions, terraces, and                applications of ground limestone are needed to raise and
           grassed waterways, reduce the length of slope and                     maintain the pH sufficient for good crop growth.
           safely remove excess water from the field.                            Available phosphorus and potash are naturally low in
             Contour tillage reduces the amount and velocity of                  most of these soils. Fertilizers should be applied in split
           runoff. A cropping system that includes sod crops in the              applications on the deep, sandy soils to reduce losses
           rotation and tillage that leaves plant residue on the                 by leaching. On all soils, additions of lime and fertilizer
           surface provide protective Surface cover, reduce runoff,              should be based on the results of soil tests, on the need
           and increase infiltration. On livestock farms that require            of the crop, and on the expected level of yields. The
           pasture and hay, the legume and grass forage crops in                 Cooperative Extension Service can help in determining
           the cropping system reduce erosion and provide nitrogen               the amounts of fertilizer and lime to apply.
           for the following crop.                                                 Soil tilth is an important factor in the germination of
             In Dorchester County, areas of sloping soils generally              seeds and in the infiltration of water into the soil. The
           are small and irregular in shape and topography. Contour              surface layer of most soils in Dorchester County is sand
           farming, contour stripcropping, and conservation tillage,             or loamy sand and is granular, porous, and has weak
           which reduce the amount and velocity of runoff and do                 structure. Generally, these conditions are ideal for good
           not concentrate the runoff, are effective and compatible              germination of seeds and infiltration of water; however,
           on these soils (fig. 6). Inforrnation on the design of                the soils generally are very low in organic matter, and
           erosion control practices for each soil in the county is              the retention of moisture in the surface layer is low.
           available in the local office of the Soil Conservation                  Fall tillage generally is not a good practice on the
           Service.                                                              gently sloping soils that are subject to erosion by water
             Damage to young plants by soil blowing is a major                   or on soils that are subject to soil blowing. If fall tillage
           concern in management on the Alpin, Blanton, Bonneau,                 operations are performed following corn or soybeans,
           Chipley, Chisolm, Coosaw, Echaw, Foreston, and                        equipment should be used that leaves a significant
           Noboco soils, especially in large, unprotected fields.                amount of crop residue on the surface. On crops, such
           Conservation tillage, permanent vegetated strips, and                 as tobacco, where fall tillage is an important component
           strips of close-growing crops protect sandy soils that are            in insect and disease control, a winter cover crop should
           subject to blowing.                                                   be planted following the tillage.
             Soil drainage is a major concern in management on                     The soils and climate of Dorchester County are suited
           about 75 percent of the soils in Dorchester County.                   to field crops including many that are not commonly
           Drainage to the extent needed for cropland and hayland                grown. Soybeans, corn, and tobacco are the principal
           is feasible on many of the soils that have a wetness                  row crops. A small acreage is used for grain sorghum.
           problem. It generally is feasible on the Albany, Chipley,             Wheat, oats, and pearl millet are the common close-
           Coosaw, Coxville, Eulonia, Daleville, Foreston,                       growing crops. Barley, ryegrass, sudangrass, and several
           Goldsboro, Izagora, Jedburo, Johns, Lynchburg,                        close-growing legumes, such as arrowleaf clover,
           Ogeechee, Pelham, Rains, Seagate, Wahee, Yauhannah,                   crimson clover, and sericea lespedeza, can be grown for
           and Yemassee soils and in some areas of the Leon,                     forage or seed. The principal perennial grasses grown
           Lynn Haven, and Lumbee soils. Drainage is generally not               for forage are Pensacola bahiagrass and Coastal
           feasible on the Brookman, C apers, Elloree, Grifton,                  bermudagrass.
           Handsboro, Mouzon, Nakina, Osier, Pantego, Plummer,                     Special crops in the county include collards, Irish
           and Rutlege soils because of lack of outlets or the                   potatoes, mustard, sweet corn, turnips, and pecans.
           hazard of frequent flooding.                                          Large areas of cropland can be adapted to these and
             Low available water capacity is a limitation on Albany,             other special crops, such as blueberries, cabbage, field
           Alpin, Blanton, Bonneau, Chipley, Echaw, Foreston,                    peas, lima beans, cucumbers, and strawberries. Deep







      Dorchester County, South Carolina                                                                                        43





                                                                              40A









                                                  N
                                                                                                                  4-























                                                                                                  n




                                                                         7.

                                                                                                          ff


                                                                                                         A,
                                                                                                                               IN111

      Figure 6.-Conservation tillage can help control erosion and increase organic matter content. This soil is Goldsboro loamy sand, 0 to 2
          percent slopes.




      soils that have good natural drainage, moderate to high          Yields Per Acre
      available water capacity, and that warm early in the               The average yields per acre that can be expected of
      spring are especially well suited to many vegetables. In
      this county, crops generally can be planted and                  the principal crops under a high level of management
      harvested early on Emporia and Noboco soils.                     are shown in table 5. In any given year, yields may be
        The latest information and suggestions for growing             higher or lower than those indicated in the table because
      crops can be obtained from local offices of the                  of variations in rainfall and other climatic factors.
      Cooperative Extension Service and the Soil Conservation            The yields are based mainly on the experience and
      Service.                                                         records of farmers, conservationists, and extension
                                                                       agents. Available yield data from nearby counties and








          44                                                                                                                     Soil Survey



          results of field trials and demonstrations are also                    Class IV soils have very severe limitations that reduce
          considered.                                                         the choice of plants or that require very careful
             The management needed to obtain the indicated                    management, or both.
          yields of the various crops depends on the kind of soil                Class V soils are not likely to erode, but they have
          and the crop. Management can include drainage, erosion              other limitations, impractical to remove, that limit their
          control, and protection from flooding; the proper planting          use.
          and seeding rates; suitable high-yielding crop varieties;              Class VI soils have severe limitations that make them
          appropriate and timely tillage:: control of weeds, plant            generally unsuitable for cultivation.
          diseases, and harmful insects; favorable soil reaction                 Class VII soils have very severe limitations that make
          and optimum levels of nitrogen, phosphorus, potassium,              them unsuitable for cultivation.
          and trace elements for each crop; effective use of crop                Class VIII soils and miscellaneous areas have
          residue, barnyard manure, and green manure crops; and               limitations that nearly preclude their use for commercial
          harvesting that insures the smallest possible loss.                 crop production.
             The estimated yields reflect the productive capacity of             Capability subclasses are soil groups within one class.
          each soil for each of the principal crops. Yields are likely        They are designated by adding a small letter, e, w, or s,
          to increase as new production technology is developed.              to the class numeral, for example, Ile. The letter e shows
          The productivity of a given soil compared with that of              that the main limitation is risk of erosion unless a close-
          other soils, however, is not likely to change.                      growing plant cover is maintained; w shows that water in
             Crops other than those shown in table 5 are grown in             or on the soil interferes with plant growth or cultivation
          the survey area, but estimated yields are not listed                (in some soils the wetness can be partly corrected by
          because the acreage of such crops is small. The local               artificial drainage); and s shows that the soil is limited
          office of the Soil Conservation Service or of the                   mainly because it is shallow, droughty, or stony.
          Cooperative Extension Service can provide information                  There are no subclasses in class I because the soils
          about the management and productivity of the soils for              of this class have few limitations. The soils in class V are
          those crops.                                                        subject to little or no erosion, but they have other
                                                                              limitations that restrict their use to pasture, rangeland,
          Land Capability Classification                                      woodland, wildlife habitat, or recreation. Class V contains
             Land capability classification shows, in a general way,          only the subclasses indicated by w or s.
          the suitability of soils for use as cropland. Crops that               The acreage of soils in each capability class and
          require special management are excluded. The soils are              subclass is shown in table 6. The capability classification
          grouped according to their limitations for field crops, the         of each map unit is given in the section "Detailed Soil
          risk of damage if they are used for crops, and the way              Map Units."
          they respond to management. The criteria used in
          grouping the soils do not include major, and generally              Woodland Management and Productivity
          expensive, landforming that would change slope, depth,
          or other characteristics of the soils, nor do they include             Norman Runge, forester, Soil Conservation Service, helped prepare
          possible but unlikely major reclamation projects.                   this section.
          Capability classification is not a substitute for                      Soils vary in their ability to produce trees. Depth,
          interpretations designed to show suitability and                    fertility, texture, and the available water capacity
          limitations of groups of soils for woodland and for                 influence tree growth. Elevation, aspect, and climate
          engineering purposes.                                               determine the kinds of trees that can grow on a site.
             In the capability system, soils are generally grouped at         Available water capacity and depth of the root zone are
          three levels: capability class, subclass, and unit. Only            major influences of tree growth. Elevation and aspect
          class and subclass are used in this survey. These levels            are of particular importance in mountainous areas.
          are defined in the following paragraphs.                               This soil survey can be used by woodland managers
             Capability classes, the broadest groups, are                     planning ways to increase the productivity of forest land.
          designated by Roman numerals I through VIII. The                    Some soils respond better to fertilization than others,
          numerals indicate progressively greater limitations and             and some are more susceptible to landslides and
          narrower choices for practical use. The classes are                 erosion after roads are built and timber is harvested.
          defined as follows:                                                 Some soils require special efforts to reforest. In the
             Class I soils have few limitations that restrict their use.      section "Detailed Soil Map Units," each map unit in the
             Class 11 soils have moderate limitations that reduce the         survey area suitable for producing timber presents
          choice of plants or that require moderate conservation              information about productivity, limitations for harvesting
          practices.                                                          timber, and management concerns for producing timber.
             Class III soils have severe limitations that reduce the          Table 7 summarizes this forestry information and rates
          choice of plants or that require special conservation               the soils for a number of factors to be considered in
          practices, or both.                                                 management. Slight, moderate, and severe are used to









       Dorchester County, South Carolina                                                                                          45



       indicate the degree of the major soil limitations to be          harvesting operations expose the soil. The risk is slight if
       considered in forest management.                                 no particular preventive measures are needed under
         The first tree listed for each soil under the column           ordinary conditions; moderate if erosion control
       "Common trees" is the indicator species for that soil. An        measures are needed for particular silvicultural activities;
       indicator species is a tree that is common in the area           and severe if special precautions are needed to control
       and that is generally the most productive on a given soil        erosion for most silvicultural activities. Ratings of
       (fig. 7).                                                        moderate or severe indicate the need for construction of
         Ratings of the erosion hazard indicate the probability         higher standard roads, additional maintenance of roads,
       that damage may occur if site preparation activities or          additional care in planning of harvesting and




                                                                     -T, X,
                                                J
          N      W      I'( 7N

                                                                                                                                _V,
                                                                           41S

                                                                                                                 A


                                                           it

                                                                                         AKL











                A
















                                                    A






                                                                                                                            'T
                                                                                                                             7
                                                                                                                             p












                             Figure 7.-Loblolly pine Is the indicator species on Albany fine sand, 0 to 2 percent slopes.









          46                                                                                                                        Soil Survey



          reforestation operations, or use of specialized                       and maintenance are needed. The risk is severe if
          equipment.                                                            competition from undesirable plants prevents adequate
             Ratings of equipment limitation indicate limits on the             natural or artificial reforestation unless the site is
          use of forest management equipment, year-round or                     intensively prepared and maintained. A moderate or
          seasonal, because of such soil characteristics as slope,              severe rating indicates the need for site preparation to
          wetness, stoniness, or susceptibility of the surface layer            ensure the development of an adequately stocked stand.
          to compaction. As slope gradient and length increase, it              Managers must plan site preparation measures to ensure
          becomes more difficult to use wheeled equipment. On                   reforestation without delays.
          the steeper slopes, tracked Equipment must be used.                      The potential productivity of common trees on a soil is
          The rating is slight if equipment use is restricted by soil           expressed as a site index. Common trees are listed in
          wetness for less than 2 months and if special equipment               the order of their observed general occurrence.
          is not needed. The rating is moderate if slopes are steep             Generally, only two or three tree species dominate.
          enough that wheeled equipment cannot be operated                         The soils that are commonly used to produce timber
          safely across the slope, if soill wetness restricts                   have the yield predicted in cubic feet and board feet.
          equipment use from 2 to 6 months per year, if stoniness               The yield is predicted at the point where mean annual
          restricts ground-based equipment, or if special                       increment culminates. The productivity of the soils in this
          equipment is needed to avoid or reduce soil compaction.               survey is mainly based on loblolly pine.
          The rating is severe if slopes are steep enough that                     The site index is determined by taking height
          tracked equipment cannot be operated safely across the                measurements and determining the age of selected
          slope, if soil wetness restricts equipment use for more               trees within stands of a given species. This index is the
          than 6 months per year, if stoniness restricts ground-                average height, in feet, that the trees attain in a specified
          based equipment, or if special equipment is needed to                 number of years. This index applies to fully stocked,
          avoid or reduce soil compaction. Ratings of moderate or               even-aged, unmanaged stands.
          severe indicate a need to choose the most suitable                       The productivity class represents an expected volume
          equipment and to carefully plan the timing of harvesting              produced by the most important trees, expressed in
          and other management operations.                                      cubic feet per acre per year. Cubic feet per acre can be
             Ratings of seedling mortality refer to the probability of          converted to board feet by multiplying by a factor of
          death of naturally occurring or properly planted seedlings            about 5. For example, a productivity class of 114 means
          of good stock in periods of normal rainfall as influenced             the soil can be expected to produce about 568 board
          by kinds of soil or topographic features. Seedling                    feet per acre per year at the point where mean annual
          mortality is caused primarily by too much water or too                increment culminates.
          little water. The factors used in rating a soil for seedling             Trees to plant are those that are used for reforestation
          mortality are texture of the surface layer, depth and                 or, if suitable conditions exist, natural regeneration. They
          duration of the water table, rock fragments in the surface
          layer, rooting depth, and the aspect of the slope.                    are suited to the soils and will produce a commercial
          Mortality generally is greatest on soils that have a sandy            wood crop. Desired product, topographic position (such
          or clayey surface layer. The risk is slight if, after site            as a low, wet area), and personal preference are three
          preparation, expected mortality is less than 25 percent;              factors of many that can influence the choice of trees to
          moderate if expected mortality is between 25 and 50                   use for reforestation.
          percent; and severe if expected mortality exceeds 50
          percent. Ratings of moderate or severe indicate that it               Recreation
          may be necessary to use containerized or larger than
          usual planting stock or to make special site preparations,               In table 8, the soils of the survey area are rated
          such as bedding, furrowing, installing surface drainage,              according to the limitations that affect their suitability for
          or providing artificial shade for seedlings. Reinforcement            recreation. The ratings are based on restrictive soil
          planting is often needed if the risk is moderate or severe.           features, such as wetness, slope, and texture of the
             Ratings of plant competition indicate the likelihood of            surface layer. Susceptibility to flooding is considered. Not
          the growth or invasion of undesirable plants. Plant                   considered in the ratings, but important in evaluating a
          competition becomes more severe on the more                           site, are the location and accessibility of the area, the
          productive soils, on poorly drained soils, and on soils               size and shape of the area and its scenic quality,
          having a restricted root zone that holds moisture. The                vegetation, access to water, potential water
          risk is slight if competition from undesirable plants                 impoundment sites, and access to public sewerlines. The
          reduces adequate natural or artificial reforestation but              capacity of the soil to absorb septic tank effluent and the
          does not necessitate intensive site preparation and                   ability of the soil to support vegetation are also
          maintenance. The risk is moderate if competition from                 important. Soils subject to flooding are limited for
          undesirable plants reduces natural or artificial                      recreational use by the duration and intensity of flooding
          reforestation to the extent that intensive site preparation           and the season when flooding occurs. In planning








       Dorchester County, South Carolina                                                                                                47



       recreation facilities, onsite assessment of the height,                Camp areas require site preparation, such as shaping
       duration, intensity, and frequency of flooding is essential.         and leveling the tent and parking areas, stabilizing roads
          In table 8, the degree of soil limitation is expressed as         and intensively used areas, and installing sanitary
       slight, moderate, or severe. Slight means that soil                  facilities and utility lines (fig. 8). Camp areas are subject
       properties are generally favorable and that limitations are          to heavy foot traffic and some vehicular traffic. The best
       minor and easily overcome. Moderate means that                       soils have gentle slopes and are not wet or subject to
       limitations can be overcome or alleviated by planning,               flooding during the period of use. The surface absorbs
       design, or special maintenance. Severe means that soil               rainfall readily but remains firm, and it is not dusty when
       properties are unfavorable and that limitations can be               dry.
       offset only by costly soil reclamation, special design,                Picnic areas are subject to heavy foot traffic. Most
       intensive maintenance, limited use, or by a combination              vehicular traffic is confined to access roads and parking
       of these measures.                                                   areas. The best soils for picnic areas are firm when wet,
          The information in table 8 can be supplemented by                 are not dusty when dry, and are not subject to flooding
       other information in this survey, for example,                       during the period of use.
       interpretations for septic tank absorption fields in table             Playgrounds require soils that can withstand intensive
       11 and interpretations for dwellings without basements               foot traffic. The best soils are almost level and are not
       and for local roads and streets in   table 10.




















                                                                                                              'AW*
               ot
                                                                                                                               W
                                                                                         0%

       M"It,

















                   Figure B.-Izagora slit loam, 0 to 2 percent slopes, is suited to use for camp areas and other recreational activities.









          48                                                                                                                           Soil Survey



          wet or subject to flooding during the season of use. The                Moderately intensive management is required for
          surface is firm after rains and is not dusty when dry.                  satisfactory results. A rating of poor indicates that
             Paths and trails for hiking and horseback riding should              limitations are severe for the designated element or kind
          require little or no cutting and filling. The best soils are            of habitat. Habitat can be created, improved, or
          not wet, are firm after rains, are not dusty when dry, and              maintained in most places, but management is difficult
          are not subject to flooding more than once a year during                and must be intensive. A rating of vely poor indicates
          the period of use.                                                      that restrictions for the element or kind of habitat are
             Golf fairways are subject to heavy foot traffic and                  very severe and that unsatisfactory results can be
          some light vehicular traffic. Cutting or filling may be                 expected. Creating, improving, or maintaining habitat is
          required. The best soils for use as golf fairways are firm              impractical or impossible.
          when wet, are not dusty when dry, and are not subject to                   The elements of wildlife habitat are described in the
          prolonged flooding during the period of use. The                        following paragraphs.
          suitability of the soil for tees or greens is not considered               Grain and seed crops are domestic grains and seed-
          in rating the soils.                                                    producing herbaceous plants. Soil properties and
                                                                                  features that affect the growth of grain and seed crops
          Wildlife Habitat                                                        are depth of the root zone, texture of the surface layer,
                                                                                  available water capacity, wetness, slope, and flood
             Dorchester County has a wide variety of wildlife habitat             hazard. Soil temperature and soil moisture are also
          and a diveristy of game and nongame wildlife species.                   considerations. Examples of grain and seed crops are
          Habitat varies from the dry sandy ridges and upland                     corn, wheat, oats, soybeans, millet, sorghums, and
          hardwood sites to the bottom land hardwood swamps.                      barley.
          Farm ponds, lakes, streams, and adjacent wetlands                          Grasses and legumes are domestic perennial grasses
          produce favorable conditions for many fish species and                  and herbaceous legumes. Soil properties and features
          forresident and migratory waterfowl.                                    that affect the growth of grasses and legumes are depth
             The principal wildlife species in this county are quail,             of the root zone, texture of the surface layer, available
          rabb: it, squirrel, deer, turkey, dove, furbearers, and a               water capacity, wetness, flood hazard, and slope. Soil
          variety of ducks. Good populations of quail and rabbits                 temperature and soil moisture are also considerations.
          are in the western part of thEl county. Woodland game                   Examples of grasses and legumes are bahiagrass,
          animals, birds, and ducks arE.1 most abundant along the                 lovegrass, lespedezas, and clover.
          Edisto River.                                                              Wild herbaceous plants are native or naturally
             Soils affect the kind and arnount of vegetation that is              established grasses and forbs, including weeds. Soil
          available to wildlife as food and cover. They also affect               properties and features that affect the growth of these
          the construction of water impoundments. Man's activities                plants are depth of the root zone, texture of the surface
          also influence the quantity and quality of habitat by his               layer, available water capacity, wetness, and flood
          decisions to alter the vegetation patterns on the                       hazard. Soil temperature and soil moisture are also
          landscape.  . The kind and abLindance of wildlife depend                considerations. Examples of wild herbaceous plants are
          largely on the amount and distribution of food, cover,                  ragweed, goldenrod, beggarweed, partridge pea,
          and water.'. Wildlife habitat cen be created or improved                cordgrass, and dropseeds.
          by planting appropriate vegetation, by maintaining the                     Hardwood trees and woody understory produce nuts
          existing plant cover, or by promoting the natural                       or other fruit, buds, catkins, twigs, bark, and foliage. Soil
          establishment of desirable plants.                                      properties and features that affect the growth of
             In table 9, the soils in the survey area are rated                   hardwood trees and shrubs are depth of the root zone,
          acco@ding to their potential for providing habitat for                  the available water capacity, and wetness. Examples of
          various kinds of wildlife. This information can be used in              these plants are oak, poplar, cherry, sweetgum, apple,
          planning parks, wildlife refuges, nature study areas, and               hawthorn, dogwood, hickory, blackberry, and grape.
          other developments for wildlife; in selecting soils that are            Examples of fruit-producing shrubs that are suitable for
          suitable for establishing, improving, or maintaining                    planting on soils rated good are pyracantha, Rem-red
          specific elements of wildlife @habitat; and in determining              honeysuckle, autumn olive, and crabapple.
          the intensity of management needed for each element of                     Coniferous plants furnish browse and seeds. Soil
          the habitat.                                                            properties and features that affect the growth of
             The potential of the soil is rated good, fair, poor, or              coniferous trees, shrubs, and ground cover are depth of
          very poor. A rating of good indicates that the element or               the root zone, available water capacity, and wetness.
          kind of habitat is easily established, improved, or                     Examples of coniferous plants are pine, cedar, and
          maintained. Few or no limitations affect management,                    juniper.
          and satisfactory results can be expected. A rating of fair                 Wetlandplants are annual and perennial, wild
          indicates that the element or kind of habitat can be                    herbaceous plants that grow on moist or wet sites.
          established, improved, or maintained in most places.                    Submerged and floating aquatic plants are excluded. Soil









       Dorchester County, South Carolina                                                                                                            49



       properties and features affecting wetland plants are                        Government ordinances and regulations that restrict
       texture of the surface layer, wetness, reaction, salinity,                certain land uses or impose specific design criteria were
       and slope. Examples of wetland plants are smartweed,                      not considered in preparing the information in this
       wild millet, wildrice, alder, buttonbush, cordgrass, rushes,              section. Local ordinances and regulations must be
       sedges, and reeds.                                                        considered in planning, in site selection, and in design.
          Shallow water areas have an average depth of less                        Soil properties, site features, and observed
       than 5 feet. Some are naturally wet areas. Others are                     performance were considered in determining the ratings
       created by dams, levees, or other water-control                           in this section. During the fieldwork for this soil survey,
       structures. Soil properties and features affecting shallow                determinations were made about grain-size distribution,
       water areas are wetness, slope, and permeability.                         liquid limit, plasticity index, soil reaction, depth to
       Examples of shallow water areas are marshes, swamps,                      bedrock, hardness of bedrock within 5 to 6 feet of the
       waterfowl feeding areas, and ponds.                                       surface, soil wetness, depth to a seasonal high water
          The habitat for various kinds of wildlife is described in              table, slope, likelihood of flooding, natural soil structure
       the following paragraphs.                                                 aggregation, and soil density. Data were collected about
          Habitat for openland wildlife consists of cropland,                    kinds of clay minerals, mineralogy of the sand and silt
       pasture, meadows, and areas that are overgrown with                       fractions, and the kind of adsorbed cations. Estimates
       grasses, herbs, shrubs, and vines. These areas produce                    were made for erodibility, permeability, corrosivity, shrink-
       grain and seed crops, grasses and legumes, and wild                       swell potential, available water capacity, and other
       herbaceous plants. The wildlife attracted to these areas                  behavioral characteristics affecting engineering uses.
       include bobwhite quail, doves, meadowlark, field                            This information can be used to: evaluate the potential
       sparrow, cottontail, and red fox.                                         of areas for residential, commercial, industrial, and
          Habitat for woodland wildlife consists of areas of                     recreational uses; make preliminary estimates of
       deciduous plants or coniferous plants or both and                         construction conditions; evaluate alternative routes for
       associated grasses, legumes, and wild herbaceous                          roads, streets, highways, pipelines, and underground
       plants. Wildlife attracted to these areas include wild                    cables; evaluate alternative sites for sanitary landfills,
       turkey, woodcock, thrushes, woodpeckers, squirrels,           gray        septic tank absorption fields, and sewage lagoons; plan
       fox, raccoon, and deer.                                                   detailed onsite investigations of soils and geology; locate
          Habitat for wetland wildlife consists of open, marshy,                 potential sources of sand, earthfill, and topsoil; plan
       or swampy shallow water areas. Some of the wildlife                       drainage systems, irrigation systems, ponds, terraces,
       attracted to such areas are ducks, geese, herons, shore                   and other structures for soil and water conservation; and
       birds, mink, otter, and beaver.                                           predict performance of proposed small structures and
                                                                                 pavements by comparing the performance of existing
       Engineering                                                               similar structures on the same or similar soils.
                                                                                   The information in the tables, along with the soil maps,
          This section provides information for planning land                    the soil descriptions, and other data provided in this
       uses related to urban development and to water                            survey can be used to make additional interpretations.
       management. Soils are rated for various uses, and the                       Some of the terms used in this soil survey have a
       most limiting features are identified. The ratings are                    special meaning in soil science and are defined in the
       given in the following tables: Building site development,                 Glossary.
       Sanitary facilities, Construction materials, and Water
       management. The ratings are based on observed                             Building Site Development
       performance of the soils and on the estimated data and
       test data in the "Soil Properties" section.                                 Table 10 shows the degree and kind of soil limitations
          Information in this section is intended for land use                   that affect shallow excavations, dwellings with and
       planning, for evaluating land use alternatives, and for                   without basements, small commercial buildings, local
       planning site Invest1gations pnor to design and                           roads and streets, and lawns and landscaping. The
       construction The Information, however, has 11mitations                    limitations are considered slight if soil properties and site
       For example, estimates and other data generally apply                     features are generally favorable for the indicated use
       only to that part of the soil within a depth of 5 or 6 feet,              and limitations are minor and easily overcome; moderate
       and because of the map scale, sma# areas of different                     if soil properties or site features are not favorable for the
       soils may be included within the mapped areas of a                        indicated use and special planning, design, or
       specific soil.                                                            maintenance is needed to overcome or minimize the
          The information is not site specific and does not                      limitations; and severe if soil properties or site features
       eliminate the need for onsite investigation of the soils or               are so unfavorable or so difficult to overcome that
       for testing and analysis by personnel experienced In the                  special design, significant increases in construction
       design and construction of engineering works                              costs, and possibly increased maintenance are required.









           50                                                                                                                   Soil Survey



           Special feasibility studies may be required where the soil         dwellings no higher than three stories. Ratings are made
           limitations are severe.                                            for small commercial buildings without basements, for
              Shallow excavations are trenches or holes dug to a              dwellings with basements, and for dwellings without
           maximum depth of 5 or 6 feet for basements, graves,                basements (fig. 9). The ratings are based on soil
           utility lines, open ditches, and other purposes. The               properties, site features, and observed performance of
           ratings are based on soil properties, site features, and           the soils. A high water table, flooding, shrink-swell
           observed performance of the soils. The ease of digging,            potential, and organic layers can cause the movement of
           filling, and compacting is affected by the depth to a very         footings. Depth to a high water table and flooding affect
           firm dense layer, the stone content, soil texture, and             the ease of excavation and construction. Landscaping
           slope. The time of the year that excavations can be                and grading that require cuts and fills of more than 5 to
           made is affected by the depth to a seasonal high water             6 feet are not considered.
           table and the susceptibility of the soil to flooding. The            Local roads and streets have an all-weather surface
           resistance of the excavation walls or banks to sloughing           and carry automobile and light truck traffic all year. They
           or caving is affected by soil texture and the depth to the         have a subgrade of cut or fill soil material, a base of
           water table.                                                       gravel, crushed rock, or stabilized soil material, and a
              Dwellings and sma# com)rercial buildings are                    flexible or rigid surface. Cuts and fills are generally
           structures built on shallow foundations on undisturbed             limited to less than 6 feet. The ratings are based on soil
           soil. The load limit is the same as that for single-family         properties, site features, and observed performance of






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                 Figure g.-Drainage and land shaping are needed if Eulonla fine sandy loam, 2 to 6 percent slopes, Is used as sites for dwellings.









       Dorchester County, South Carolina                                                                                                     51



       the soils. Depth to a high water table, flooding, and slope           must be unsaturated soil material beneath the absorption
       affect the ease of excavating and grading. Soil strength              field to filter the effluent effectively. Many local
       (as inferred from the engineering classification of the               ordinances require that this material be of a certain
       soil) and depth to a high water table affect the traffic-             thickness.
       supporting capacity.                                                     Sewage lagoons are shallow ponds constructed to
         Lawns and landscaping require soils on which turf and               hold sewage while aerobic bacteria decompose the solid
       ornamental trees and shrubs can be established and                    and liquid wastes. Lagoons should have a nearly level
       maintained. The ratings are based on soil properties, site            floor surrounded by cut slopes or embankments of
       features, and observed performance of the soils. Soil                 compacted soil. Lagoons generally are designed to hold
       reaction, depth to a high water table, the available water            the sewage within a depth of 2 to 5 feet. Nearly
       capacity in the upper 40 inches, and the content of salts             impervious soil material for the lagoon floor and sides is
       and sulficlic materials affect plant growth. Flooding,                required to minimize seepage and contamination of
       wetness, slope, and the amount of sand, clay, or organic              ground water.
       matter in the surface layer affect trafficability after                  Table 11 gives ratings for the natural soil that makes
       vegetation is established.                                            up the lagoon floor. The surface layer and, generally, 1
       Sanitary Facilities                                                   or 2 feet of soil material below the surface layer are
                                                                             excavated to provide material for the embankments. The
         Table 11 shows the degree and the kind of soil                      ratings are based on soil properties, site features, and
       limitations that affect septic tank absorption fields,                observed performance of the soils. Considered in the
       sewage lagoons, and sanitary landfills. The limitations               ratings are slope, permeability, depth to a high water
       are considered slight if soil properties and site features            table, flooding, and content of organic matter.
       are generally favorable for the indicated use and                        Excessive seepage due to rapid permeability of the
       limitations are minor and easily overcome; moderate if                soil or a water table that is high enough to raise the level
       soil properties or site features are not favorable for the            of sewage in the lagoon causes a lagoon to function
       indicated use and special planning, design, or                        unsatisfactorily. Pollution results if seepage is excessive
       maintenance is needed to overcome or minimize the                     or if floodwater overtops the lagoon. A high content of
       limitations; and severe it soil properties or site features           organic matter is detrimental to proper functioning of the
       are so unfavorable or so difficult to overcome that                   lagoon because it inhibits aerobic activity. Slope can
       special design, significant increases in construction                 cause construction problems.
       costs, and possibly increased maintenance are required.                  Sanitary landfills are areas where solid waste is
         Table 11 also shows the suitability of the soils for use            disposed of by burying it in soil. There are two types of
       as daily cover for landfills. A rating of good indicates that         landfill-trench and area. In a trench landfill, the waste is
       soil properties and site features are favorable for the use
       and that good performance and low maintenance can be                  placed in a trench. It is spread, compacted, and covered
       expected; fair indicates that soil properties and site                daily with a thin layer of soil excavated at the site. In an
       features are moderately favorable for the use and one or              area landfill, the waste is placed in successive layers on
       more soil properties or site features make the soil less              the surface of the soil. The waste is spread, compacted,
       desirable than the soils rated good; and poor indicates               and covered daily with a thin layer of soil from a source
       that one or more soil properties or site features are                 away from the site.
       unfavorable for the use and overcoming the unfavorable                   Both types of landfill must be able to bear heavy
       properties requires special design, extra maintenance, or             vehicular traffic. Both types involve a risk of ground
       costly alteration.                                                    water pollution. Ease of excavation and revegetation
         Septic tank absorption fields are areas in which                    needs to be considered.
       effluent from a septic tank is distributed into the soil                 The ratings in table 11 are based on soil properties,
       through subsurface tiles or perforated pipe. Only that                site features, and observed performance of the soils.
       part of the soil between depths of 24 and 72 inches is                Permeability, depth to a water table, slope, and flooding
       evaluated. The ratings are based on soil properties, site             affect both types of landfill. Texture, highly organic
       features, and observed performance of the soils.                      layers, soil reaction, and content of salts affect trench
       Permeability, depth to a high water table, and flooding               type landfills. Unless otherwise stated, the ratings apply
       affect absorption of the effluent.                                    only to that part of the soil within a depth of about 6
         Unsatisfactory performance of septic tank absorption                feet, For deeper trenches, a limitation rated slight or
       fields, including excessively slow absorption of effluent,            moderate may not be valid. Onsite investigation is
       surfacing of effluent, and hillside seepage, can affect               needed.
       public health. Ground water can be polluted if highly                    Daily cover for landfill is the soil material that is used
       permeable sand or fractured bedrock is less than 4 feet               to cover compacted solid waste in an area type sanitary
       below the base of the absorption field, if slope is                   landfill. The soil material is obtained offsite, transported
       excessive, or if the water table is near the surface. There           to the landfill, and spread over the waste.








            52                                                                                                                               Soil Survey



               Soil texture, wetness, and slope affect the ease of                    is 1 to 3 feet. Soils rated poor have a plasticity index of
            removing and spreading the material during wet and dry                    more than 10 or a high shrink-swell potential. They are
            periods. Loamy or silty soils that are free of large stones               wet, and the depth to the water table is less than 1 foot.
            or excess gravel are the best cover for a landfill. Clayey                They may have layers of suitable material, but the
            soils are sticky or cloddy and are difficult to spread;                   material is less than 3 feet thick.
            sandy soils are subject to soil blowing.                                     Sand is a natural aggregate suitable for commercial
               After soil material has been removed, the soil material                use with a minimum of processing. It is used in many
            remaining in the borrow area must be thick enough over                    kinds of construction. Specifications for each use vary
            bedrock, a cemented pan, or the water table to permit                     widely. In table 12, only the probability of finding material
            revegetation. The soil material used as final cover for a                 in suitable quantity is evaluated. The suitability of the
            landfill should be suitable for plants. The surface layer                 material for specific purposes is not evaluated, nor are
            generally has the best workability, more organic matter,                  factors that affect excavation of the material.
            and the best potential for plants. Material from the                         The properties used to evaluate the soil as a source of
            surface layer should be stockpiled for use as the final                   sand are gradation of grain sizes (as indicated by the
            cover.                                                                    engineering classification of the soil) and the thickness
            Construction Materials                                                    of suitable material. Kinds of rock, acidity, and
                                                                                      stratification are given in the soil series descriptions.
               Table 12 gives information about the soils as a source                 Gradation of grain sizes is given in the table on
            of roadfill, sand, and topsoil. The soils are rated good,                 engineering index properties.
            fair, or poor as a source of roadfill and topsoil. They are                  A soil rated as a probable source has a layer of clean
            rated as a probable or improbable source of sand. The                     sand or a layer of sand that is up to 12 percent silty
            ratings are based on soil properties and site features                    fines. This material must be at least 3 feet thick. All
            that affect the removal of the soil and its use as                        other soils are rated as an improbable source. Coarse
            construction material. Normal compaction, minor                           fragments of soft bedrock, such as shale and marl, are
            processing, and other standard construction practices                     not considered to be sand.
            are assumed. Each soil is evaluated to a depth of 5 or 6                     Topsoil is used to cover an area so that vegetation
            feet.                                                                     can be established and maintained. The upper 40 inches
               Roadfill is soil material that is excavated in one place               of a soil is evaluated for use as topsoil. Also evaluated is
            and used in road embankments in another place. In this                    the reclamation potential of the borrow area.
            table, the soils are rated as a source of roadfill for low                   Plant growth is affected by toxic material and by such
            embankments, generally less than 6 feet high and less                     properties as soil reaction, available water capacity, and
            exacting in design than higher embankments.                               fertility. The ease of excavating, loading, and spreading
               The ratings are for the soil material below the surface                is affected by slope, a water table, soil texture, and
            layer to a depth of 5 or 6 feet. It is assumed that soil                  thickness of suitable material. Reclamation of the borrow
            layers will be mixed during excavating and spreading.                     area is affected by slope, a water table, and toxic
            Many soils have layers of contrasting suitability within                  material.
            their profile. The table showing engineering index                           Soils rated good have friable, loamy material to a
            properties provides detailed information about each soil                  depth of at least 40 inches. They are free of stones and
            layer. This information can help determine the suitability                cobbles, have little or no gravel, and have slopes of less
            of each layer for use as roadfill. The performance of soil                than 8 percent. They are low in content of soluble salts,
            after it is stabilized with lime or cement is not considered              are naturally fertile or respond well to fertilizer, and are
            in the ratings.
               The ratings are based on soil properties, site features                not so wet that excavation is difficult.
            and observed performance of the soils. The thickness oi                      Soils rated fair are sandy soils, loamy soils that have a
            suitable material is a major consideration. The ease of                   relatively high content of clay, soils that have only 20 to
            excavation is affected by large stones, a high water                      40 inches of suitable material, and soils that have an
            table, and slope. How well the soil performs in place                     appreciable amount of soluble salts. The soils are not so
            after it has been compacted and drained is determined                     wet that excavation is difficult.
            by its strength (as inferred from the engineering                            Soils rated poor are very sandy or clayey, have less
            classification of the soil) and shrink-swell potential.                   than 20 inches of suitable material, have a large amount
               Soils rated good contain significant amounts of sand.                  of soluble salts, or have a seasonal water table at or
            They have at least 5 feet of suitable material, low shrink-               near the surface.
            swell potential, and slopes of 15 percent or less. Depth                     The surface layer of most soils is generally preferred
            to the water table is more than 3 feet. Soils rated fair are              for topsoil because of its organic matter content. Organic
            more than 35 percent silt- and clay-sized particles and                   matter greatly increases the absorption and retention of
            have a plasticity index of less than 10. They have                        moisture and releases a variety of plant-available
            moderate shrink-swell potential. Depth to the water table                 nutrients as it decomposes.







      Dorchester County, South Carolina                                                                                                   53


      Water Management                                                     compaction characteristics. Unfavorable features include
        Table 13 gives information on the soil properties and              less than 5 feet of suitable material and a high content
      site features that affect water management. The degree               of stones or boulders, organic matter, or salts or sodium.
      and kind of soil limitations are given for pond reservoir            A high water table affects the amount of usable material.
      areas; embankments, dikes, and levees; and aquifer-fed               It also affects trafficability.
      ponds. The limitations are considered slight if soil                   Aquifer-fed excavatedponds are pits or dugouts that
      properties and site features are generally favorable for             extend to a ground-water aquifer or to a depth below a
                                                                           permanent water table. Excluded are ponds that are fed
      the indicated use and limitations are minor and are easily           only by surface runoff and embankment ponds that
      overcome; moderate if soil properties or site features are           impound water 3 feet or more above the original surface.
      not favorable for the indicated use and special planning,            Excavated ponds are affected by depth to a permanent
      design, or maintenance is needed to overcome or                      water table, permeability of the aquifer, and the salinity
      minimize the limitations; and severe if soil properties or           of the soil.
      site features are so unfavorable or so difficult to                    Drainage is the removal of excess surface and
      overcome that special design, significant increase in                subsurface water from the soil. How easily and
      construction costs, and possibly increased maintenance               effectively the soil is drained depends on the depth to
      are required.                                                        layers that affect the rate of water movement, the
        This table also gives the restrictive features that affect         permeability, the depth to a high water table or depth of
      each soil for drainage, irrigation, and grassed waterways.           standing water if the soil is subject to poncling, the slope,
        Pond reservoir areas hold water behind a dam or                    and the susceptibility to flooding. Excavating and grading
      embankment. Soils best suited to this use have low                   and the stability of clitchbanks are affected by slope and
      seepage potential in the upper 60 inches. The seepage                the hazard of cutbanks caving. The productivity of the
      potential is determined by the permeability of the soil              soil after drainage is adversely affected by extreme
      and the depth to fractured bedrock or other permeable                acidity or by toxic substances in the root zone, such as
      material. Excessive slope can affect the storage capacity            salts or sulfur. Availability of drainage outlets is not
      of the reservoir area.                                               considered in the ratings.
        Embankments, dikes, and levees are raised structures                 Irrigation is the controlled application of water to
      of soil material, generally less than 20 feet high,                  supplement rainfall and support plant growth. The design
      constructed to impound water or to protect land against              and management of an irrigation system are affected by
      overflow. In this table, the soils are rated as a source of          depth to the water table, the need for drainage, flooding,
      material for embankment fill. The ratings apply to the soil          available water capacity, intake rate, permeability,
      material below the surface layer to a depth of about 5               erosion hazard, and slope. The performance of a system
      feet. It is assumed that soil layers will be uniformly mixed         is affected by the depth of the root zone, the amount of
      and compacted during construction.                                   salts or sodium, and soil reaction.
        The ratings do not indicate the ability of the natural               Grassed watenvays are natural or constructed
      soil to support an embankment. Soil properties to a                  channels, generally broad and shallow, that conduct
      depth greater than the height of the embankment can                  surface water to outlets at a nonerosive velocity.
      affect performance and safety of the embankment.                     Wetness and slope affect the construction of grassed
      Generally, deeper onsite investigation is needed to                  waterways. A hazard of wind erosion, low available water
      determine these properties.                                          capacity, restricted rooting depth, toxic substances such
        Soil material in embankments must be resistant to                  as salts, and restricted permeability adversely affect the
      seepage, piping, and erosion and have favorable                      growth and maintenance of the grass after construction.










                                                                                                                                          55




      Soil Properties

         Data relating to soil properties are collected during the             Classification of the soils is determined according to
      course of the soil survey. The data and the estimates of              the Unified soil classification system (2) and the system
      soil and water features, listed in tables, are explained on           adopted by the American Association of State Highway
      the following pages.                                                  and Transportation Officials (1).
         Soil properties are determined by field examination of                The Unified system classifies soils according to
      the soils and by laboratory index testing of some                     properties that affect their use as construction material.
      benchmark soils. Established standard procedures are                  Soils are classified according to grain-size distribution of
      followed. During the survey, many shallow borings are                 the fraction less than 3 inches in diameter and according
      made and examined to identify and classify the soils and              to plasticity index, liquid limit, and organic matter
      to delineate them on the soil maps. Samples are taken                 content. Sandy and gravelly soils are identified as GW,
      from some typical profiles and tested in the laboratory to            GP, GM, GC, SW, SP, SM, and SC; silty and clayey soils
      determine grain-size distribution, plasticity, and                    as ML, CL, OL, MH, CH, and OH; and highly organic
      compaction characteristics. These results are reported in             soils as PT. Soils exhibiting engineering properties of two
      table 17.                                                             groups can have a dual classification, for example, SP-
         Estimates of soil properties are based on field                    sm.
      examinations, on laboratory tests of samples from the
      survey area, and on laboratory tests of samples of                       The AASHTO system classifies soils according to
      similar soils in nearby areas. Tests verify field                     those properties that affect roadway construction and
      observations, verify properties that cannot be estimated              maintenance. In this system, the fraction of a mineral soil
      accurately by field observation, and help characterize                that is less than 3 inches in diameter is classified in one
      key soils.                                                            of seven groups from A-1 through A-7 on the basis of
         The estimates of soil properties shown in the tables               grain-size distribution, liquid limit, and plasticity index.
      include the range of grain-size distribution and Atterberg            Soils in group A-1 are coarse grained and low in content
      limits, the engineering classifications, and the physical             of fines (silt and clay). At the other extreme, soils in
      and chemical properties of the major layers of each soil.             group A-7 are fine grained. Highly organic soils are
      Pertinent soil and water features also are given,                     classified in group A-8 on the basis of visual inspection.
                                                                               If laboratory data are available, the A-1, A-2, and A-7
      Engineering Index Properties                                          groups are further classified as A-1-a, A-1-b, A-2-4, A-2-
         Table 14 gives estimates of the engineering                        5, A-2-6, A-2-7, A-7-5, or A-7-6. As an additional
      classification and of the range of index properties for the           refinement, the suitability of a soil as subgrade material
      major layers of each soil in the survey area. Most soils              can be indicated by a group index number. Group index
      have layers of contrasting properties within the upper 5              numbers range from 0 for the best subgrade material to
      or 6 feet.                                                            20, or higher, for the poorest. The AASHTO classification
         Depth to the upper and lower boundaries of each layer              for soils tested, with group index numbers in
      is indicated. The range in depth and information on other             parentheses, is given in table 17.
      properties of each layer are given for each soil series                  Percentage (of soil particles) passing designated
      Lnder "Soil Series and Their Morphology."                             sieves is the percentage of the soil fraction less than 3
         Texture is given in the standard terms used by the                 inches in diameter based on an ovendry weight. The
      U.S. Department of Agriculture. These terms are defined               sieves, numbers 4, 10, 40, and 200 (USA Standard
      according to percentages of sand, silt, and clay in the               Series), have openings of 4.76, 2.00, 0.420, and 0.074
      fraction of the soil that is less than 2 millimeters in               millimeters, respectively. Estimates are based on
      diameter. "Loam," for example, is soil that is 7 to 27                laboratory tests of soils sampled in the survey area and
      percent clay, 28 to 50 percent silt, and less than 52                 in nearby areas and on estimates made in the field.
      percent sand. If the content of particles coarser than                   Liquid limit and plasticity index (Atterberg limits)
      sand is as much as 15 percent, an appropriate modifier                indicate the plasticity characteristics of a soil. The
      is added, for example, "gravelly." Textural terms are                 estimates are based on test data from the survey area,
      defined in the Glossary.                                              or from nearby areas, and on field examination.








            56                                                                                                                        Soil Survey



            Physical and Chemical Properties                                        Soil reaction is a measure of acidity or alkalinity and is
                                                                                  expressed as a range in pH values. The range in pH of
              Table 15 shows estimates of some characteristics and                each major horizon is based on many field tests. For
            features that affect soil behavior. These estimates are               many soils, values have been verified by laboratory
            given for the major layers of each soil in the survey area.           analyses. Soil reaction is important in selecting crops
            The estimates are based on field observations and on                  and other plants, in evaluating soil amendments for
            test data for these and similar soils.                                fertility and stabilization, and in determining the risk of
              Clay as a soil separate, or, component, consists of                 corrosion.
            mineral soil particles that are less than 0.002 millimeter              Salinity is a measure of soluble salts in the soil at
            in diameter. In this table, the estimated clay content of             saturation. It is expressed as the electrical conductivity
            each major soil layer is given as a percentage, by                    of the saturation extract, in millimhos per centimeter at
            weight, of the soil material that is less than 2 millimeters          25 degrees C. Estimates are based on field and
            in diameter.                                                          laboratory measurements at representative sites of
              The amount and kind of clay greatly affect the fertility            nonirrigated soils. The salinity of irrigated soils is
            and physical condition of the soil. They influence the                affected by the quality of the irrigation water and by the
            soil's adsorption of cations, moisture retention, shrink-             frequency of water application. Hence, the salinity of
            swell potential, permeability, plasticity, the ease of soil           soils in individual fields can differ greatly from the value
            dispersion, and other soil properties. The amount and                 given in the table. Salinity affects the suitability of a soil
            kind of clay in a soil also affect tillage and earthmoving            for crop production, the stability of soil if used as
            operations.                                                           construction material, and the potential of the soil to
              Moist bulk density is the weight of soil (ovendry) per              corrode metal and concrete.
            unit volume. Volume is measured when the soil is at field               Shrink-swell potential is the potential for volume
            moisture capacity, that is, the moisture content at 1/3               change in a soil with a loss or gain in moisture. Volume
            bar moisture tension. Weight is determined after drying               change occurs mainly because of the interaction of clay
            the soil at 105 degrees C. In this table, the estimated               minerals with water and varies with the amount and type
            moist bulk density of each major soil horizon is                      of clay minerals in the soil. The size of the load on the
            expressed in grams per cubic centimeter of soil material              soil and the magnitude of the change in soil moisture
            that is less than 2 millimeters in diameter. Bulk density             content influence the amount of swelling of soils in
            data are used to compute shrink-swell potential,                      place. Laboratory measurements of swelling of
            available water capacity, total pore space, and other soil
            properties. The moist bulk density of a soil indicates the            undisturbed clods were made for many soils. For others,
            pore space available for water and roots. A bulk density              swelling was estimated on the basis of the kind and
            of more than 1.6 can restrict water storage and root                  amount of clay minerals in the soil and on
            penetration. Moist bulk density is influenced by texture,             measurements of similar soils.
            kind of clay, content of organic matter, and soil structure.            If the shrink-swell potential is rated moderate to very
              Permeability refers to the ability of a soil to transmit            high, shrinking and swelling can cause damage to
            water or air. The estimates indicate the rate of                      buildings, roads, and other structures. Special design is
            movement of water through the soil when the soil is                   often needed.
            saturated. They are basedon soil characteristics                        Shrink-swell potential classes are based on the
            observed in the field, particularly structure, porosity, and          change in length of an unconfined clod as moisture
            texture. Permeability is considered in the design of soil             content is increased from air-dry to field capacity. The
            drainage systems, septic tank absorption fields, and                  change is based on the soil fraction less than 2
            construction where the rate of water movement under                   millimeters in diameter. The classes are low, a change of
            saturated conditions affects, behavior.                               less than 3 percent; moderate, 3 to 6 percent; and high,
              Available water capacity refers to the quantity of water            more than 6 percent. Vely high, greater than 9 percent,
            that the soil is capable of storing for use by plants. The            is sometimes used.
            capacity for water storage in each major soil layer is                  Erosion factor K indicates the susceptibility of a soil to
            stated in inches of water per inch of soil. The capacity              sheet and rill erosion by water. Factor K is one of six
            varies, depending on soil properties that affect the                  factors used in the Universal Soil Loss Equation (USLE)
            retention of water and the depth of the root zone. The                to predict the average annual rate of soil loss by sheet
            most important properties are the content of organic                  and rill erosion. Losses are expressed in tons per acre
            matter, soil texture, bulk density, and soil structure.               per year. These estimates are based primarily on
            Available water capacity is an important factor in the                percentage of silt, sand, and organic matter (up to 4
            choice of plants or crops to be grown and in the design               percent) and on soil structure and permeability. Values of
            and management of irrigation systems. Available water                 K range from 0.02 to 0.69. The higher the value, the
            capacity is not an estimatE! of the quantity of water                 more susceptible the soil is to sheet and rill erosion by
            actually available to plants at any given time.                       water.








       Dorchester County, South Carolina                                                                                                       57



         Erosion factor T is an estimate of the maximum                       infiltration rate, and tilth. It is a source of nitrogen and
       average annual rate of soil erosion by wind or water that              other nutrients for crops.
       can occur over a sustained period without affecting crop
       productivity. The rate is expressed in tons per acre per               Soil and Water Features
       year.
         Wind erodibility groups are made up of soils that have                 Table 16 gives estimates of various soil and water
       similar properties affecting their resistance to wind                  features. The estimates are used in land use planning
       erosion in cultivated areas. The groups indicate the                   that involves engineering considerations.
       susceptibility of soil to wind erosion and the amount of                 Hydrologic soil groups are used to estimate runoff
       soil lost. Soils are grouped according to the following                from precipitation. Soils are assigned to one of four
       distinctions:                                                          groups. They are grouped according to the intake of
         1. Sands, coarse sands, fine sands, and very fine                    water when the soils are thoroughly wet and receive
       sands. These soils are generally not suitable for crops.               precipitation from long-duration storms.
       They are extremely erodible, and vegetation is difficult to              The four hydrologic soil groups are:
       establish.                                                               Group A. Soils having a high infiltration rate (low runoff
         2. Loamy sands, loamy fine sands, and loamy very                     potential) when thoroughly wet. These consist mainly of
       fine sands. These soils are very highly erodible. Crops                deep, well drained to excessively drained sands or
       can be grown if intensive measures to control wind                     gravelly sands. These soils have a high rate of water
       erosion are used.                                                      transmission.
         3. Sandy loams, coarse sandy loams, fine sandy                         Group B. Soils having a moderate infiltration rate when
       loams, and very fine sandy loams. These soils are highly               thoroughly wet. These consist chiefly of moderately deep
       erodible. Crops can be grown if intensive measures to                  or deep, moderately well drained or well drained soils
       control wind erosion are used.                                         that have moderately fine texture to moderately coarse
         4L. Calcareous loamy soils that are less than 35                     texture. These soils have a moderate rate of water
       percent clay and more than 5 percent finely divided                    transmission.
       calcium carbonate. These soils are erodible. Crops can                   Group C. Soils having a slow infiltration rate when
       be grown if intensive measures to control wind erosion                 thoroughly wet. These consist chiefly of soils having a
       are used.                                                              layer that impedes the downward movement of water or
         4. Clays, silty clays, clay loams, and silty clay loams              soils of moderately fine texture or fine texture. These
       that are more than 35 percent clay. These soils are                    soils have a slow rate of water transmission.
       moderately erodible. Crops can be grown if measures to                   Group D. Soils having a very slow infiltration rate (high
       control wind erosion are used.                                         runoff potential) when thoroughly wet. These consist
         5. Loamy soils that are less than 18 percent clay and                chiefly of clays that have high shrink-swell potential, soils
       less than 5 percent finely divided calcium carbonate and               that have a permanent high water table, soils that have a
       sandy clay loams and sandy clays that are less than 5                  claypan or clay layer at or near the surface, and soils
       percent finely divided calcium carbonate. These soils are              that are shallow over nearly impervious material. These
       slightly erodible. Crops can be grown it measures to                   soils have a very slow rate of water transmission.
       control wind erosion are used.                                           Some of the soils are shown in table 16 with dual
         6. Loamy soils that are 18 to 35 percent clay and                    hydrologic groups, for example B/D. This means that
       less than 5 percent finely divided calcium carbonate,                  under natural conditions the soil is in group D, but by
       except silty clay loams. These soils are very slightly                 artificial methods the water table can be lowered to the
       erodible. Crops can easily be grown.                                   point that the soil fits into group B. Onsite investigation is
                                                                              needed, however, to determine the hydrologic group of
         7. Silty clay loams that are less than 35 percent clay               the soil at any particular location because there are
       and less than 5 percent finely divided calcium carbonate.              different degrees of drainage and water table control.
       These soils are very slightly erodible. Crops can easily                 Flooding, the temporary covering of the soil surface by
       be grown.                                                              flowing water, is caused by overflowing streams, by
         8. Stony or gravelly soils and other soils not subject               runoff from adjacent slopes, or by inflow from high tides.
       to wind erosion.                                                       Shallow water standing or flowing for short periods after
         Organic matter is the plant and animal residue in the                rainfall or snowmelt is not considered flooding. Standing
       soil at various stages of decomposition.                               water in swamps and marshes or in a closed depression
         In table 15, the estimated content of organic matter is              is considered ponding.
       expressed as a percentage, by weight, of the soil                        Table 16 gives the frequency and duration of flooding
       material that is less than 2 millimeters in diameter.                  and the time of year when flooding is most likely to
         The content of organic matter of a soil can be                       occur.
       maintained or increased by returning crop residue to the                 Frequency, duration, and probable dates of occurrence
       soil. Organic matter affects the available water capacity,             are estimated. Frequency generally is expressed as










            58



            none, rare, occasional, or frequent None means that                     unsaturated zone. In places an upper, or perched, water
            flooding is not probable. Rare means that flooding is                   table is separated from a lower one by a dry zone.
            unlikely but possible under unusual weather conditions                     The two numbers in the "High water table-Depth"
            (there is a near 0 to 5 percent chance of flooding in any               column indicate the normal range in depth to a saturated
            year). Occasional means that flooding occurs                            zone. Depth is given to the nearest half foot. The first
            infrequently under normal woather conditions (there is a                numeral in the range indicates the highest water level. A
            5 to 50 percent chance of flooding in any year).                        plus sign preceding the range in depth indicates that the
            Frequent means that flooding occurs often under normal                  water table is above the surface of the soil. "More than
            weather conditions (there is more than a 50 percent                     6.0" indicates that the water table is below a depth of 6
            chance of flooding in any year). Common is used when                    feet or that the water table exists for less than a month.
            classification as occasional or frequent does not affect                   Risk of corrosion pertains to potential soil-induced
            interpretations. Duration is expressed as vely brief (less              electrochemical or chemical action that dissolves or
            than 2 days), brief (2 to 7 days), long Q days to 1                     weakens uncoated steel or concrete. The rate of
            month), and very long (more than 1 month). The time of                  corrosion of uncoated steel is related to such factors as
            year that floods are most likely to occur is expressed in               soil moisture, particle-size distribution, acidity, and
            months. November-May, for example, means that                           electrical conductivity of the soil. The rate of corrosion of
            flooding can occur during the period November through                   concrete is based mainly on the sulfate and sodium
            May. About two-thirds to three-fourths of all flooding                  content, texture, moisture content, and acidity of the soil.
            occurs during the stated period.                                        Special site examination and design may be needed if
              The information on flooding is based on evidence in                   the combination of factors creates a severely corrosive
            the soil profile, namely, thin strata of gravel, sand, silt,     or     environment. The steel in installations that intersect soil
            clay deposited by floodwater; irregular decrease in                     boundaries or soil layers is more susceptible to corrosion
            organic matter content with increasing depth; and                       than steel in installations that are entirely within one kind
            absence of distinctive horizons, which are characteristic               of soil or within one soil layer.
            of soils that are not subject to flooding.                                 For uncoated steel, the risk of corrosion, expressed as
              Also considered are local information about the extent                low, moderate, or high, is based on soil drainage class,
            and levels of flooding and the relation of each soil on                 total acidity, electrical resistivity near field capacity, and
            the landscape to historic floods. Information on the                    electrical conductivity of the saturation extract.
            extent of flooding based on soil data is less specific than                For concrete, the risk of corrosion is also expressed
            that provided by detailed engineering surveys that                      as low, moderate, or high. It is based on soil texture,
            delineate flood-prone areas at specific flood frequency                 acidity, and the amount of sulfates in the saturation
            levels.                                                                 extract.
              High water table (seasonal) is the highest level of a                 Engineering Index Test Data
            saturated zone in the soil in most years. The depth to a
            seasonal high water table applies to undrained soils. The                  Table 17 shows laboratory test data for several
            estimates are based mainly on the evidence of a                         pedons sampled at carefully selected sites in the survey
            saturated zone, namely grayish colors or mottles in the                 area. The pedons are typical of the series and are
            soil. Indicated in table 16 are the depth to the seasonal               described in the section "Soil Series and Their
            high water table; the kind of water table, that is, perched,            Morphology." The soil samples were tested by South
            artesian, or apparent,, and the months of the year that                 Carolina Department of Highways and Public
            the water table commonly is highest. A water table that                 Transportation.
            is seasonally high for less than 1 month is not indicated                  The testing methods generally are those of the
            in table 16.                                                            American Association of State Highway and
              An apparent water table is a thick zone of free water                 Transportation Officials (AASHTO) or the American
            in the soil. It is indicated by the level at which water                Society for Testing and Materials (ASTM).
            stands in an uncased borehole after adequate time is                       The tests and methods are: AASHTO classification-M
            allowed for adjustment in the surrounding soil. An                      145 (AASHTO), D 3282 (ASTM); Unified classification-
            artesian water table is under hydrostatic head, generally               D 2487 (ASTM); Mechanical analysis-T 88 (AASHTO),
            below an impermeable layer. When this layer is                          D 2217 (ASTM); Liquid limit-T 89 (AASHTO), D 423
            penetrated, the water level rises in an uncased borehole.               (ASTM); Plasticity index-T 90 (AASHTO), D 424
            A perched water table is water standing above an                        (ASTM).










                                                                                                                                       59




       Classif ication of the Soils


         The system of soil classification used by the National            and characteristics considered are particle-size class,
       Cooperative Soil Survey has six categories (5). Beginning           mineral content, temperature regime, depth of the root
       with the broadest, these categories are the order,                  zone, consistence, moisture equivalent, slope, and
       suborder, great group, subgroup, family, and series.                permanent cracks. A family name consists of the name
       Classification is based on soil properties observed in the          of a subgroup preceded by terms that indicate soil
       field or inferred from those observations or on laboratory          properties. An example is fine-loamy, siliceous, thermic
       measurements. Table IS shows the classification of the              Typic Paleudults.
       soils in the survey area. The categories are defined in                SERIES. The series consists of soils that have similar
       the following paragraphs.                                           horizons in their profile. The horizons are similar in color,
         ORDER. Ten soil orders are recognized. The                        texture, structure, reaction, consistence, mineral and
       differences among orders reflect the dominant soil-                 chemical composition, and arrangement in the profile.
       forming processes and the degree of soil formation.                 There can be some variation in the texture of the surface
       Each order is identified by a word ending in sol. An                layer or of the substratum within a series. An example is
       example is Ultisol.                                                 the Noboco series, which is a member of the fine-loamy,
         SUBORDER. Each order is divided into suborders,                   siliceous, thermic family of Typic Paleudults.
       primarily on the basis of properties that influence soil
       genesis and are important to plant growth or properties
       that reflect the most important variables within the                Soil Series and Their Morphology
       orders. The last syllable in the name of a suborder                    In this section, each soil series recognized in the
       indicates the order. An example is Udult (Ud, meaning               survey area is described. The descriptions are arranged
       humid, plus ult, from Ultisol).                                     in alphabetic order.
         GREAT GROUP. Each suborder is divided into great                     Characteristics of the soil and the material in which it
       groups on the basis of close similarities in kind,                  formed are identified for each series. The soil is
       arrangement, and degree of development of pedogenic                 compared with similar soils and with nearby soils of
       horizons; soil moisture and temperature regimes; and                other series. A pedon, a small three-dimensional area of
       base status. Each great group is identified by the name             soil, that is typical of the series in the survey area is
       of a suborder and by a prefix that indicates a property of          described. The detailed description of each soil horizon
       the soil. An example is Paleudults (Pale, meaning                   follows standards in the Soil Survey Manual (4). Many of
       excessive development, plus udult, the suborder of the              the technical terms used in the descriptions are defined
       Ultisols that has an udic moisture regime).                         in Soil Taxonomy (5). Unless otherwise stated, colors in
         SUBGROUP. Each great group has a typic subgroup.                  the descriptions are for moist soil. Following the pedon
       Other subgroups are intergrades or extragrades. The                 description is the range of important characteristics of
       typic is the central concept of the great group; it is not          the soils in the series.
       necessarily the most extensive. Intergrades are                        The map units of each soil series are described in the
       transitions to other orders, suborders, or great groups.            section "Detailed Soil Map Units."
       Extragrades have some properties that are not
       representative of the great group but do not indicate               Albany Series
       transitions to any other known kind of soil. Each
       subgroup is identified by one or more adjectives                       The Albany series consists of soils that formed in
       preceding the name of the great group. The adjective                sandy and loamy marine sediment on nearly level upland
       Typic identifies the subgroup that typifies the great               terraces throughout the county. Slopes are 0 to 2
       group. An example is Typic Paleudults.                              percent. These soils are loamy, siliceous, thermic
         FAMILY. Families are established within a subgroup on             Grossarenic Paleudults.
       the basis of physical and chemical properties and other                Albany soils are associated on the landscape with
       Characteristics that affect management. Mostly the                  Alpin, Blanton, Bonneau, Chipley, Echaw, Foxworth,
       properties are those of horizons below plow depth where             Foreston and Ocilla soils. Alpin soils are higher on the
       there is much biological activity. Among the properties             landscape than the Albany soils and do not have an









           60                                                                                                                    Soil Survey



           argillic horizon. Chipley, Echaw, Foxworth, and Foreston            yellow, or gray. The E horizon is sand, fine sand, loamy
           soils are slightly higher on the landscape. Chipley and             sand, or loamy fine sand.
           Foxworth soils are Entisols, and Echaw soils are                      The Bt horizon has hue of 1 OYR, value of 5 or 6, and
           Spodosols. Foreston soils have a coarse-loamy particle              chroma of 3 to 6. It has mottles in shades of brown,
           size control section. Blanton and Bonneau soils are                 yellow, or gray. The Bt horizon is sandy loam or sandy
           slightly higher on the landscape. Blanton soils have a              clay loam.
           deeper seasonal high water table. Bonneau soils are in                The Btg horizon has hue of 10YR, value of 5 or 6, and
           an arenic subgroup. Ocilla soils are in positions similar to        chroma of 1 or 2. It has mottles in shades of brown,
           those of the Albany soils and are in an arenic subgroup.            yellow, or gray. The Btg horizon is sandy clay loam.
             Typical pedon of Albany fine sand, 0 to 2 percent
           slopes; about 3.5 miles south of Dorchester, 0.5 mile               Alpin Series
           south of the junction of South Carolina Highway 25 and
           South Carolina Highway 246, about 0.5 mile northwest                  The Alpin series consists of soils that formed in thick,
           on farm road, and 200 feet -south of road in a cultivated           sandy marine sediment on upland terraces. Slopes are 0
           field.                                                              to 6 percent. These soils are thermic, coated Typic
                                                                               Quartzipsamments.
           Ap-0 to 7 inches; dark grayish brown (10YR 4/2) fine                  Alpin soils are associated on the landscape with
               sand; single grained; loose; common fine roots;                 Albany, Blanton, Bonneau, Chipley, Foxworth, Osier, and
               slightly acid; abrupt wavy boundary.                            Pelham soils. None of these soils have lamella, and all
           E1-7 to 26 inches; very pale brown (10YR 7/4) fine                  are lower on the landscape than the Alpin soils. Albany
               sand; common uncoated sand grains; single grained;              and Blanton soils are in a grossarenic subgroup.
               loose; few fine roots; few fine pores; slightly acid;           Bonneau and Pelham soils are in an arenic subgroup.
               gradual wavy boundary.                                          Chipley soils have gray mottles within 30 inches of the
           E2-26 to 54 inches; brownish yellow (10YR 6/8) fine                 surface. Osier and Pelham soils are dominantly gray
               sand; common medium distinct light gray (10YR                   throughout.
               7/1) mottles and few medium distinct yellowish                    Typical pedon of Alpin fine sand, 0 to 6 percent
               brown (10YR 5/8) mottles; single grained; loose;                slopes; about 6 miles east of Grover, about 0.7 mile
               few fine roots; few fine pores; medium acid; gradual            southeast of the intersection of South Carolina Highway
               wavy boundary.                                                  19 and South Carolina Highway 135, and 50 feet south
           Bt-54 to 59 inches; pale brown (10YR 6/3) sandy loam;               of highway.
               many medium distinct gray (10YR 6/1) mottles and
               common medium distinct yellowish brown (10YR                    A-0 to 7 inches; brown (10YR 5/3) fine sand; single
               5/8) mottles; weak fine subangular blocky structure;                grained; loose; many fine and common medium
               very friable; few fine roots; very few faint clay films             roots; strongly acid; clear smooth boundary.
               along old root channels; strongly acid; clear wavy              E1-7 to 27 inches; very pale brown (10YR 7/4) fine
               boundary.                                                           sand; few uncoated sand grains; single grained;
           Btg1-59 to 68 inches; gray, (10YR 6/1) sandy clay                       loose; common fine and medium roots and few large
               loam; common medium distinct brownish yellow                        roots; medium acid; gradual wavy boundary.
               (10YR 6/6) mottles and few medium distinct                      E2-27 to 54 inches; brownish yellow (10YR 6/6) fine
               yellowish brown (10YR 5/8) mottles; moderate                        sand; few uncoated sand grains; single grained;
               medium subangular blocky structure; friable; very                   loose; common medium and few large roots;
               few faint clay films on faces of peds; few fine pores;              medium acid; clear smooth boundary.
               very strongly acid; clear wavy boundary.                        E&B-54 to 85 inches; very pale brown (10YR 7/3) fine
           Btg2-68 to 75 inches; gray (10YR 6/1) sandy clay                        sand; many uncoated sand grains; single grained;
               loam; many coarse distinct yellowish brown (10YR                    loose; common discontinuous strong brown (7.5YR
               5/8) mottles and common medium distinct brownish                    5/6) loamy sand lamella 0.25 to 1 inch thick;
               yellow (10YR 6/6) mottles; weak medium                              strongly acid.
               subangular blocky structure; friable; very few faint
               clay films on faces of peds; very strongly acid.                  Depth to horizons containing lamella ranges from 40
                                                                               to 70 inches.
             The solum is 60 to more than 80 inches thick.                       The A horizon has hue of 10YR, value of 4 or 5, and
             The A horizon has hue of I OYR, value of 3 to 6, and              chroma of 1 to 3. It is fine sand or sand.
           chroma of 1 or 2. It commonly is fine sand but ranges to              The E horizon has hue of 1 OYR, value of 5 to 7, and
           sand, loamy sand, or loamy fine sand.                               chroma of 3 to 6. It has few to many uncoated sand
             The E horizon has hue of 10YR, value of 5 to 7, and               grains. This horizon is sand or fine sand.
           chroma of 3 to 8. It has few to many uncoated sand                    The E&B horizon has hue of 10YR, value of 5 to 7,
           grains. Most pedons have mottles in shades of brown,                and chroma of 3 to 6. The lamella in this horizon has








        Dorchester County, South Carolina                                                                                                      61



        hue of 7.5YR or 10YR, value of 5 or 6, and chroma of 4                   The solurn ranges from 60 to more than 80 inches in
        or 6. This horizon is sand or fine sand, and the lamella is            thickness.
        loamy sand, loamy fine sand, or sandy loam.                              The A horizon has hue of 10YR, value of 4 to 6, and
                                                                               chroma of 1 to 3. It is fine sand or sand.
        Blanton Series                                                           The E horizon has hue of 10YR, value of 5 to 7, and
                                                                               chroma of 3 to 8. Some pedons have few to many
          The Blanton series consists of soils that formed in                  pockets of uncoated sand grains. The E horizon is sand,
        sandy and loamy marine sediments throughout the                        fine sand, loamy sand, or loamy fine sand.
        county. Slopes are 0 to 6 percent. These soils are                       The Bt horizon has hue of 1 OYR, value of 5 or 6, and
        loamy, siliceous, thermic Grossarenic Paleuclults.                     chroma of 4 to 8. It has mottles in shades of red, brown,
          B)anton soils are associated on the landscape with                   or yellow. The lower part of the Bt horizon has mottles in
        Albany, Alpin, Bonneau, Coosaw, and Ocilla soils. Alpin                shades of gray. The Bt horizon is sandy clay loam. Some
        and Bonneau soils are in positions similar to those of the             pedons have thin subhorizons of sandy loam, fine sandy
        Blanton soils. Alpin soils are sandy to 80 inches and                  loam, or sandy clay.
        have lamella between depths of 40 and 70 inches.
        Albany, Coosaw, and Ocilla soils are lower on the                      Bonneau Series
        landscape. Albany soils have a higher seasonal water
        table. Bonneau, Coosaw, and Ocilla soils are in an arenic                The Bonneau series consists of soils that formed in
        subgroup.                                                              sandy and loamy marine sediments on nearly level to
          Typical pedon of Blanton fine sand, 0 to 2 percent                   gently sloping upland terraces. Slopes are 0 to 6
        slopes; about 4.8 miles southeast of Harleyville on U.S.               percent. These soils are loamy, siliceous, thermic Arenic
        Highway 178, about 0.2 mile west on unimproved county                  Paleudults.
        road, and 200 feet northwest of road.                                    Bonneau soils are associated on the landscape with
                                                                               Blanton, Coxville, Goldsboro, Lynchburg, Noboco,
        A-0 to 3 inches; light brownish gray (10YR 6/2) fine                   Pelham, and Rains soils. Blanton soils are higher on the
             sand; single grained; loose; many fine and few                    landscape than the Bonneau soils and are in a
             medium roots; medium acid; clear smooth boundary.                 grossarenic subgroup. Noboco soils are in positions
        E1-3 to 8 inches; brown (10YR 5/3) fine sand; single                   similar to those of the Bonneau soils, and Goldsboro
             grained; loose; common fine and few medium roots;                 soils are in slightly lower positions on the landscape.
             medium acid; gradual wavy boundary.                               These soils are not in an arenic subgroup. Coxville,
        E2-8 to 44 inches; very pale brown (10YR 7/3) fine                     Lynchburg, Pelham, and Rains soils are lower on the
             sand; few fine distinct brownish yellow (10YR 6/6)                landscape and are Aquults. Coxville soils also have more
             mottles; single grained; loose; few uncoated sand                 than 35 percent clay in the control section.
             grains; few fine roots; slightly acid; clear smooth                 Typical peclon of Bonneau fine sand, 0 to 2 percent
             boundary.                                                         slopes; about 4.5 miles south of Byrds on South Carolina
        Btl-44 to 55 inches; brownish yellow (10YR 6/6) sandy                  Highway 161, about 2.5 miles southeast on woods road
             clay loam; few medium distinct yellowish red (5YR                 that bends toward the north, and 100 feet west of road.
             4/6) mottles and common medium distinct yellowish
             brown (10YR 5/8) mottles; moderate medium                         A-0 to 3 inches; gray (1 OYR 5/ 1) fine sand; single
             subangular blocky structure; friable; very few faint                   grained; loose; few large roots, common medium
             clay films on faces of peds; few fine roots; medium                    roots, and many fine roots; strongly acid; clear
             acid; gradual smooth boundary.                                         smooth boundary.
        Bt2-55 to 64 inches; yellowish brown (10YR 5/6) sandy                  E-3 to 27 inches; very pale brown (1 OYR 7/3) fine
             clay; common medium distinct brownish yellow                           sand; common medium faint white (10YR 8/2) sand
             (10YR 6/8) and light gray (10YR 7/1) mottles and                       grains and few medium distinct gray (10YR 5/1)
             few medium distinct red (2.5YR 4/8) mottles;                           stains along old root channels; single grained; loose;
             moderate medium subangular blocky structure;                           common fine roots, medium acid; clear smooth
             friable; very few distinct clay films on faces of peds;                boundary.
             very strongly acid; gradual wavy boundary.                        Btl-27 to 42 inches; brownish yellow (10YR 6/6) sandy
        Bt3-64 to 80 inches; yellowish brown (10YR 5/6) sandy                       loam; common medium faint yellowish brown (10YR
             clay loam; strata of fine sandy loam; many medium                      5/8) mottles and common medium distinct pale
             distinct light gray (10YR 7/1) mottles and common                      brown (10YR 6/3) mottles; weak medium
             medium distinct red (2.5YR 4/8) and brownish                           subangular blocky structure; very friable; few fine
             yellow (10YR 6/8) mottles; weak medium                                 roots; very few faint clay films on faces of peds; few
             subangular blocky structure; friable; very strongly                    fine pores; very strongly acid; gradual smooth
             acid.                                                                  boundary.








           62                                                                                                                         Soil Survey



           Bt2-42 to 53 inches; light yellowish brown (10YR 6/4)                 A-0 to 8 inches; black (1 OYR 2/ 1) clay loam; weak
                sandy loam; common medium prominent red (2.5YR                        medium subangular blocky structure; slightly sticky;
                4/8) mottles and common medium distinct gray                          many fine roots, common medium roots and few
                (10YR 6/1) mottles; weak medium subangular                            large roots; very strongly acid; gradual smooth
                blocky structure; very friable; very few faint clay films             boundary.
                on faces of peds; very strongly acid; gradual wavy               Btg1-8 to 22 inches; black (10YR 2/1) clay; weak
                boundary.                                                             medium prismatic structure; very sticky; common
           Btg-53 to 61 inches; light gray (10YR 7/1) sandy clay                      fine roots; few fine pores; few distinct clay films on
                loam; common medium distinct strong brown (7.5YR                      faces of peds; very strongly acid; gradual smooth
                5/8) and few medium prominent red (2.5YR 4/8)                         boundary.
                mottles; moderate medium subangular blocky                       Btg2-22 to 49 inches; dark gray (10YR 4/1) clay; weak
                structure; friable; few distinct clay films on faces of               medium prismatic structure; very sticky; few fine
                peds; very strongly acid; gradual wavy boundary.                      roots and pores; common distinct clay films on
           C-61 to 80 inches; red (2.5YR 4/6) sandy loam;                             faces of peds; strongly acid; gradual wavy boundary.
                common medium distinct light gray (10YR 7/1) and                 Btg3-49 to 57 inches; gray (10YR 5/1) clay loam; weak
                common medium distinct brownish yellow (10YR                          prismatic structure; slightly sticky; common distinct
                6/8) mottles; massive; very friable; very strongly                    clay films on faces of peds; medium acid; gradual
                acid.                                                                 wavy boundary.
              The solum ranges from 60 to more than 80 inches in                 BCg-57 to 76 inches; gray (1 OYR 5/ 1) sandy clay loam;
           thickness. The A horizon has hue of 1 OYR, value of 3 to                   common coarse distinct dark gray (10YR 4/1)
           5, and chroma of I to 3. It commonly is fine sand, but                     mottles along old root channels and on faces of
           ranges to sand, loamy sand, or loamy fine sand.                            peds; weak medium prismatic structure; nonsticky;
              The E horizon has hue of 1 OYR, value of 5 to 7, and                    neutral; clear smooth boundary.
           chroma of 3 to 6. Some pedons have mottles of                         Cg-76 to 80 inches; grayish brown (10YR 5/2) loamy
           uncoated sand grains. This horizon is fine sand, loamy                     sand; massive; very friable; neutral.
           sand, or loamy fine sand.                                                The solum ranges from 40 to more than 60 inches in
              The Bt horizon has hue of 7.5YR or 1 OYR, value of 5               thickness.
           to 7, and chroma of 3 to 8. It has mottles in shades of                  The A horizon has hue of 10YR, value of 2 or 3, and
           red, yellow, and brown with gray mottles in the lower                 chroma of 1 or 2. It commonly is clay loam but ranges to
           part. This horizon is commonly sandy loam or sandy clay               fine sandy loam or loam.
           loam but ranges to sandy clay in the lower part.                         The Btg horizon has hue of 10YR, value of 2 to 5, and
              The Btg horizon has hue of 10YR, value of 5 to 7, and              chroma of 1 or 2. Some pedons have mottles in shades
           chroma of 1 or 2. It has moftles in shades of red, yellow,            of red, yellow, or brown. This horizon is clay loam, sandy
           and brown. This horizon is sandy loam or sandy clay                   clay, or clay.
           loam. It is sandy clay in some pedons.                                   The BCg horizon has hue of 10YR to 5Y, value of 2 to
              The C horizon has hue of 2.5YR to I OYR, value of 4                6, and chroma of 1 or 2. Some pedons have mottles in
           to 7, and chroma of 1 to 8. It is sand, loamy sand, or                shades of red, yellow, brown, or gray. This horizon
           sandy loam.                                                           ranges from sandy clay loam to clay and has stratified
           Brookman Series                                                       lenses of loamy sand or sandy loam.
                                                                                    The Cg horizon has hue of 10YR to 5Y, value of 4 to
              The Brockman series consists of soils that formed in               6, and chroma of 1 or 2. Some pedons have red or
           clayey marine sediment on nearly level, large                         brown mottles. This horizon ranges from sand to clay, or
           drainageways mainly in the southeastern part of the                   it is stratified with variable textures.
           county. Slopes are dominantly less than 1 percent.
           These soils are fine, mixed, thermic Typic Umbraqualfs.               Capers Series
              Brookman soils are associated on the landscape with
           Eulonia, Mouzon, and Wahee soils. Eulonia and Wahee                      The Capers series consists of soils that formed in silty
           soils are higher on the landscape than the Brockman                   and clayey marine sediments on nearly level, broad tidal
           soils and have colors that have chroma of 3 or more in                flats and along lower reaches of larger streams flowing
           some part of the subsoil. Mouzon soils are slightly higher            into the tidal flats. The elevation is 2 to 5 feet above sea
           on. the landscape and have an ochric epipedon.                        level. Slopes are dominantly less than 1 percent but
              Typical pedon of Brookman clay loam, frequently                    range from 0 to 2 percent. These soils are fine, mixed,
           flooded; about 4 miles northeast of Delemars crossroads               nonacid, thermic Typic Sulfaquents.
           on South Carolina Highway 165, about 2.3 miles south                     Capers soils are associated on the landscape with
           on paper company road, and 50 feet north of large                     Brookman and Mouzon soils. Brockman and Mouzon
           drainage ditch.                                                       soils are higher on the landscape than the Capers soils








       Dorchester County, South Carolina                                                                                                      63



       and have an argillic horizon. Also, Brookman soils have                25 percent very coarse plus coarse sand in the control
       an umbric epipedon.                                                    section. This difference does not significantly alter use
          Typical peclon of Capers silty clay loam; about 13                  and behavior of the soils.
       miles southwest of Summerville at the intersection of                    Chipley soils are associated on the landscape with
       South Carolina Highway 317 and South Carolina                          Albany, Blanton, Coosaw, Echaw, Foxworth, and
       Highway 165, 7.3 miles east on South Carolina Highway                  Foreston soils. Albany, Coosaw, Echaw, and Foreston
       317, 3,500 feet north on unimproved paper company                      soils are in positions similar to those of the Chipley soils.
       road, and 200 feet east of road.                                       Blanton and Foxworth soils are higher on the landscape.
                                                                              Foxworth soils do not have aquic: colors. Albany,
       Al -0 to 11 inches; very dark grayish brown (1 OYR 3/2)                Blanton, Coosaw, and Foreston soils are Ultisols. Echaw
            silty clay loam; massive; friable; many roots, leaves,            soils have a spodic horizon.
            and stems; neutral; clear smooth boundary.                          Typical pedon of Chipley sand, 0 to 2 percent slopes;
       A2-11 to 21 inches; black (10YR 2/1) silty clay loam;                  about 2 miles southeast of Grover, 1.5 miles east of U.S.
            massive; slightly sticky; soil flows between fingers              Highway 15, 1.25 miles north of the Edisto River, and 50
            with some difficulty (n value 0.8); strong sulfide odor;          feet east of South Carolina Highway 3130.
            common to many fine and medium roots; few fine
            pores; mildly alkaline, clear smooth boundary.                    Ap-O to 7 inches; dark gray (10YR 4/1) sand; single
       Cgl-21 to 28 inches; black (10YR 2/1) clay; massive;                       grained; loose; many fine roots; strongly acid;
            sticky; soil flows between fingers with difficulty (n                 gradual smooth boundary.
            value 0.7); strong sulfide odor; few fine pores; mildly           C1-7 to 24 inches; light yellowish brown (10YR 6/4)
            alkaline, clear smooth boundary.                                      coarse sand; few medium distinct dark gray (10YR
       Cg2-28 to 50 inches; gray (5Y 5/1) clay; common                            4/1) and light gray (10YR 7/2) streaks along old
            medium distinct black (10YR 2/1) mottles and few                      root channels, single grained; loose; few fine roots;
            medium distinct light olive brown (2.5Y 5/4) mottles;                 strongly acid; gradual irregular boundary.
            streaks of sandy clay loam along old root channels;               C2-24 to 30 inches; very pale brown (10YR 7/3) coarse
            massive; slightly sticky; few fine and medium roots;                  sand; many fine faint streaks of light gray; single
            mildly alkaline; clear smooth boundary.                               grained; loose; few fine roots; strongly acid; gradual
       Cg3-50 to 58 inches; greenish gray (5G 6/1) silty clay;                    wavy boundary.
            few medium distinct light greenish gray (5BG 7/1)                 Cgl-30 to 60 inches; light gray (10YR 7/2) coarse
            and light olive brown (2.5Y 5/6) mottles; streaks of                  sand; common fine and medium distinct brownish
            dark gray sandy loam along old root channels;                         yellow (10YR 6/6) mottles; single grained; loose;
            massive; sticky; few fine and medium roots; mildly                    few fine roots; strongly acid; gradual wavy boundary.
            alkaline; gradual wavy boundary.                                  Cg2-60 to 75 inches; light gray (10YR 7/2) coarse
       Cg4-58 to 80 inches; pale green (5G 7/2) sandy clay                        sand; single grained; loose; strongly acid.
            loam; strata of light gray (2.5Y 7/2) coarse sand;
            common medium distinct greenish gray (5GY 5/1)                      Chipley soils are sand or coarse sand to a depth of 80
            mottles; massive; slightly sticky; few fine roots;                inches or more.
            mildly alkaline.                                                    The A horizon has hue of 1 OYR, value of 4 or 5, and
          Some pedons have an 0 horizon that has hue of                       chroma of 1 or 2.
       1 OYR, value of 2 or 3, and chroma of 1 or 2. It is fibric or            The upper part of the C horizon has hue of 7.5YR or
       hemic material.                                                        10YR, value of 5 to 7, and chroma of 3 to 6. It has
          The A horizon has hue of 10YR to 5Y, value of 2 to 5,               mottles in shades of brown, yellow, or gray. The lower
       and chroma of 1 or 2. It commonly is silty clay loam but               part of the C horizon has hue of 1 OYR, value of 5 to 7,
       ranges to silty clay or clay.                                          and chroma of 1 or 2. Some pedons have mottles in
          The Cg horizon has hue of 1 OYR to 5BG, value of 2 to               shades of brown, yellow, or gray.
       7, and chroma of 1 or 2. It is sandy clay loam, silty clay,
       or clay that has strata or pockets of sandy loam or                    Chisolm Series
       coarse sand.                                                             The Chisolm series consists of soils that formed in
       Chipley Series                                                         sandy and loamy marine sediments on nearly level to
                                                                              gently sloping terraces generally at an elevation of less
          The Chipley series consists of soils that formed in                 than 42 feet above sea level. Slopes are 0 to 6 percent.
       sandy marine sediment on nearly level ridges on flood                  These soils are loamy, siliceous, thermic Arenic
       plains. Slopes are 0 to 2 percent. These soils are                     Hapluclults.
       thermic, coated Aquic Quartzipsamments.                                  Chisolm soils are associated on the landscape with
          The Chipley soils in this survey area are taxadjuncts to            Albany, Blanton, Coosaw, Eulonia, Ogeechee, and
       the Chipley series because they typically have more than               Yauhannah soils. Albany, Coosaw, Eulonia, Ogeechee,









           64                                                                                                                      Soil Survey



           and Yauhannah soils are lower on the landscape than                  brown, yellow, or gray. The lower part of the Bt horizon
           the Chisolm soils. Blanton soils are in positions similar to         in most pedons is mottled in shades of gray, red, brown,
           those of the the Chisolm soils. Albany and Blanton soils             and yellow. This horizon is sandy loam, fine sandy loam,
           are in a grossarenic subgroup. Coosaw soils have a                   or sandy clay loam.
           higher seasonal water table. Eulonia soils have a clayey               The BCg horizon has hue of 1 OYR, value of 5 to 7,
           Bt horizon. Ogeechee soils Eire Aquults. Yauhannah soils             and chroma of 1 or 2; or it is mottled in shades of gray,
           are not in an arenic subgroup.                                       red, yellow, or brown. This horizon is sandy loam, fine
             Typical pedon of Chisolm fine sand, 0 to 6 percent                 sandy loam, or stratified sandy and loamy textures.
           slopes; about 13 miles southwest of Summerville at the                 Some pedons have a C horizon that has hue of 5YR
           intersection of South Carolina Highway 165 and South                 to 1 OYR, value of 4 to 7, and chroma of 1 to 8. It has
           Carolina Highway 317, 1.5 miles east on South Carolina               mottles in shades of red, brown, yellow, or gray. This
           Highway 317, about 0.7 mile northeast on County Road                 horizon is sand or loamy sand.
           1769, 0.1 mile northwest on dirt road, 0.75 mile
           northeast on paper company road, 0.1 mile east of
           junction of dirt road, and 30 feet east of road.                     Coosaw Series
           A-0 to 10 inches; brown (1 OYR 5/3) fine sand; weak                    The Coosaw series consists of soils that formed in
                fine granular structure; very friable; many fine roots,         thick deposits of sandy and loamy sediments on nearly
                common medium roots, and few large roots; medium                level, low ridges and terraces. Slopes are 0 to 2 percent.
                acid; clear smooth boundary.                                    These soils are loamy, siliceous, thermic Arenic
           E-10 to 30 inches; brownish yellow (10YR 6/6) loamy                  Hapludults.
                fine sand; common medium distinct pale brown                      Coosaw soils are associated on the landscape with
                (10YR 6/3) mottles; weak fine granular structure;               Albany, Chisolm, Elloree, and Yauhannah soils. Albany
                very friable; common medium and fine roots;                     soils are in positions similar to those of the Coosaw soils
                medium acid; clear wavy boundary.                               and are in a grossarenic subgroup. Chisolm and
           Btl-30 to 36 inches; yellowish brown (10YR 5/6) fine                 Yauhannah soils are higher on the landscape. Chisolm
                sandy loam; common rnedium faint yellowish brown                soils have a lower seasonal high water table, and
                (10YR 5/8) mottles; weak fine subangular blocky                 Yauhannah soils are not in an arenic subgroup. Elloree
                structure; very friable; common fine roots; few fine            soils are lower on the landscape and are Alfisols.
                pores; sand grains coated and bridged with clay;                  Typical pedon of Coosaw loamy fine sand; about 13
                medium acid; clear wavy boundary.                               miles south of Summerville, 4,000 feet east of the
           Bt2-36 to 48 inches; yellowish brown (10YR 5/6) sandy                junction of South Carolina Highway 317 and South
                clay loam; common medium distinct yellowish red                 Carolina Highway 165, 1,300 feet north of South Carolina
                (5YR 5/8) mottles and few medium distinct light                 Highway 317 on farm road, and 60 feet west of farm
                brownish gray (10YR W2) mottles; moderate                       road.
                medium subangular blocky structure; friable; few fine
                pores; very few faint clay films on faces of peds;              Ap-O to 7 inches; dark grayish brown (10YR 4/2) loamy
                strongly acid; gradual wavy boundary.                                fine sand; weak fine granular structure; very friable;
           Bt3-48 to 58 inches; coarsely mottled light gray (10YR                    common fine roots; very strongly acid; clear smooth
                6/1), red (2.5YR 4/8), and brownish yellow (10YR                     boundary,
                6/8) sandy clay loam; moderate medium subangular                E-7 to 26 inches; very pale brown (10YR 7/3) fine
                blocky structure; friable; few fine pores; very few                  sand; common medium faint light yellowish brown
                faint clay films on faces of peds; very strongly acid;               (10YR 6/4) and light brownish gray (10YR 6/2)
                gradual wavy boundary.                                               mottles; weak medium granular structure; very
           BCg-58 to 80 inches; light gray (10YR 7/1) fine sandy                     friable; few fine roots; strongly acid; clear wavy
                loam; strata of sandy clay loam and loamy fine                       boundary.
                sand; weak medium subangular blocky structure;                  Btl-26 to 31 inches; brownish yellow (10YR 6/6) sandy
                friable; very strongly acid.                                         clay loam; few medium distinct strong brown (7.5YR
             The solum ranges from 50 to 80 inches in thickness'                     5/6) mottles and few fine distinct light gray (10YR
             The A horizon has hue of 10YR, value of 4 to 7, and                     7/2) mottles; weak medium subangular blocky
           chroma of 1 to 4. It commonly is fine sand but is loamy                   structure; friable; very few faint clay films on faces of
           fine sand in some pedons.                                                 some peds; very strongly acid; gradual wavy
             The E horizon has hue of 1 OYR, value of 5 to 7, and                    boundary.
           chroma of 3 to 6. It has mottles in shades of brown or               Bt2-31 to 43 inches; yellowish brown (10YR 5/6) sandy
           yellow. This horizon is fine sand or loamy fine sand.                     clay loam; common medium distinct red (10R 4/6)
             The Bt horizon has hue of 5YR to 1 OYR, value of 5 to                   and light gray (10YR 7/2) mottles; weak medium
           7, and chroma of 4 to 8. It has mottles in shades of red,                 subangular blocky structure; friable; few faint clay








       Dorchester County, South Carolina                                                                                                        65



            films on faces of peds; very strongly acid; gradual                     fine roots, common medium roots, and few large
            wavy boundary.                                                          roots; few fine and medium pores; very strongly
       Btg-43 to 56 inches; gray (10YR 6/1) sandy clay loam;                        acid; clear wavy boundary.
            common medium prominent red (1OR 4/6) mottles                      BE-6 to 11 inches; grayish brown (1 OYR 5/2) loam;
            and common medium distinct brownish yellow                              common medium faint gray (1 OYR 5/ 1) mottles and
            (10YR 6/6) mottles; weak medium subangular                              few fine distinct brownish yellow (1 OYR 6/8) mottles;
            blocky structure; friable; very few faint clay films on                 moderate medium subangular blocky structure;
            faces of some peds; very strongly acid; gradual                         sticky; few faint clay films on faces of peds;
            wavy boundary.                                                          common fine and medium roots; few fine pores;
       BCg-56 to 78 inches; light gray (10YR 7/1) sandy clay                        extremely acid; clear wavy boundary.
            loam; pockets of fine sandy loam; common medium                    Btg1 -11 to 35 inches; gray (1 OYR 5/ 1) clay loam;
            prominent yellowish red (5YR 5/6) mottles, and few                      common medium distinct dark gray (10YR 4/1) and
            coarse prominent red (1 OR 4/6) mottles; weak                           brownish yellow (10YR 6/8) mottles and few fine
            medium subangular blocky structure; friable; very                       distinct dark yellowish brown (10YR 4/6) mottles;
            strongly acid.                                                          moderate medium subangular blocky structure; very
          The solurn ranges from 50 to more than 80 inches in                       sticky; few distinct clay films on faces of peds; few
       thickness.                                                                   fine and medium roots; few fine pores; extremely
          The A horizon has hue of 1 OYR, value of 3 to 5, and                      acid; gradual wavy boundary.
       chroma of 1 to 3. If the A horizon has value of less than               Btg2-35 to 80 inches; dark gray (10YR 4/1) clay; few
       3.5, it is less than 6 inches thick. The A horizon                           medium distinct strong brown (7.5YR 5/8) mottles;
       commonly is loamy fine sand but is fine sand or loamy                        moderate medium subangular blocky structure; very
       sand in some peclons.                                                        sticky; few distinct clay films on faces of peds; few
          The E horizon has hue of 10YR to 5Y, value of 6 to 8,                     fine roots; extremely acid.
       and chroma of 1 to 4. It is fine sand, loamy sand, or
       loamy fine sand.                                                          The solurn ranges from 60 to more than 80 inches in
          The upper part of the Bt horizon has hue of 7.5YR to                 thickness.
       2.5Y, value of 4 to 6, and chroma of 3 to 8. The lower                    The A horizon has hue of I OYR, value of 2 to 4, and
       part of the Bt horizon and the BC horizon have hue of                   chroma of 1 or 2. It commonly is loam but is sandy loam
       10YR to 5Y, value to 5 to 7, and chroma of 1 or 2. The                  or fine sandy loam in some pedons.
       Bt and BC horizons have mottles in shades of red,                         The Btg horizon has hue of 10YR, value of 4 to 6, and
       brown, yellow, or gray, or in a combination of these                    chroma of 1 or 2. It has mottles in shades of red, yellow,
       colors. These horizons commonly are sandy clay loam                     brown, or gray. This horizon is clay loam, sandy clay, or
       but are fine sandy loam and sandy loam in some                          clay.
       pedons.
       Coxville Series                                                         Daleville Series
          The Coxville series consists of soils that formed in                   The Daleville series consists of soils that formed in
       clayey marine sediment in nearly level depressional                     loamy marine sediment in depressions and drainageways
       areas and small drainageways. Slopes are 0 to 2                         on upland terraces. Slopes are 0 to 2 percent. These
       percent. These soils are clayey, kaolinitic, thermic Typic              soils are fine-loamy, siliceous, thermic Typic Paleaquults.
       Paleaquults.                                                              Daleville soils are associated on the landscape with
          Coxville soils are associated on the landscape with                  Jedburg, Emporia, Izagora, Noboco, and Grifton soils.
       Goldsboro, Lynchburg, Rains, and Grifton soils.                         Jedburg soils are slightly higher on the landscape than
       Goldsboro and Lynchburg soils are higher on the                         the Daleville soils and are in an aeric subgroup. Emporia,
       landscape than the Coxville soils and have less than 35                 Noboco, and Izagora soils are higher on the landscape
       percent clay in the B horizon. Lynchburg soils are in an                and are Udults. Grifton soils are in positions similar to
       aeric subgroup. Rains and Grifton soils are in positions                those of the Daleville soils and are Alfisols.
       similar to those of the Coxville soils and have less than                 Typical peclon of Daleville silt loam; about 2 miles
       35 percent clay in the B horizon.                                       southwest of Givhans on South Carolina Highway 244,
          Typical peclon of Coxville loam; about 1 mile south of               160 feet west of unimproved road, and 100 feet north of
       the intersection of U.S. Highway 15 and U.S. Highway                    paper company road.
       178 in Rosinville, about 0.5 mile west on South Carolina
       Highway 175, and 50 feet north of road.                                 Ap-O to 8 inches; very dark grayish brown (10YR 3/2)
                                                                                    silt loam; weak fine subangular blocky structure;
       A-0 to 6 inches; very dark gray (I OYR 3/1) loam; weak                       friable; many fine and medium roots; few large roots;
            fine subangular blocky structure; very friable; many                    very strongly acid; abrupt wavy boundary.








           66                                                                                                                        Soil Survey



           E-8 to 15 inches; light gray (10YR 7/1) silt loam;                    2 percent. These soils are sandy, siliceous, thermic Entic
                common medium distinct yellow (1 OYR 7/6) mottles                Haplohumods.
                and common medium faiint very pale brown (10YR                     Echaw soils are associated on the landscape with
                7/3) mottles; weak fine subangular blocky structure;             Albany, Chipley, Leon, Foreston, and Osier soils. Albany,
                friable; common fine and medium roots; few fine                  Chipley, and Foreston soils are in positions similar to
                pores; very strongly acid; clear wavy boundary.                  those of the Echaw soils. Albany and Foreston soils are
           Btgl -15 to 26 inches; light gray (1 OYR 7/ 1) silt loam;             Ultisols, and Chipley soils are Entisols. Leon and Osier
                common coarse distinct brownish yellow (10YR 6/8)                soils are lower on the landscape. Leon soils have a Bh
                mottles and few fine prominent yellowish red (5YR                horizon less than 30 inches from the surface. Osier soils
                5/8) mottles; moderate medium subangular blocky                  do not have a Bh horizon.
                structure; slightly hard; few fine roots; few faint clay           Typical pedon of Echaw fine sand; about 2.3 miles
                films on faces of peds; few fine pores; very strongly            south of Dorchester, 1,000 feet north of the junction of
                acid; gradual wavy boundary.                                     South Carolina Highway 248 and South Carolina
           Btg2-26 to 39 inches; light gray (10YR 6/1) silty clay                Highway 25, and 1,800 feet east of South Carolina
                loam; many coarse distinct yellowish brown (1 OYR                Highway 25.
                5/8) mottles and common medium prominent red
                (2.5YR 4/8) mottles; strong medium subangular                    Ap-O to 7 inches; dark gray (10YR 4/1) fine sand; weak
                blocky structure; friable; few distinct clay films on                 fine granular structure; very friable; common fine
                faces of peds; very strongly acid; gradual wavy                       and medium roots; slightly acid; clear smooth
                boundary.                                                             boundary.
           Btg3-39 to 67 inches; light gray (10YR 6/1) silty clay                E1-7 to 18 inches; very pale brown (10YR 7/3) fine
                loam; many coarse prominent red (2.5YR 4/8)                           sand; weak fine granular structure; very friable;
                mottles and common medium distinct brownish                           common fine and medium roots; medium acid;
                yellow (10YR 6/8) mottles; moderate medium                            gradual smooth boundary.
                subangular blocky structure; friable; few faint clay             E2-18 to 45 inches; light yellowish brown (10YR 6/4)
                films on faces of peds; 'very strongly acid; gradual                  fine sand; common medium distinct light gray (10YR
                wavy boundary.                                                        7/2) mottles, common medium faint brownish yellow
           BCg-67 to 80 inches; gray (10YR 6/1) clay loam;                            (10YR 6/6) mottles, and few fine distinct red (2.5YR
                pockets of sandy clay loam and strata of fine sandy                   5/6) mottles; weak fine granular structure; very
                loam; many coarse distinct brownish yellow (10YR                      friable; few fine roots; strongly acid; clear smooth
                6/8) mottles and common medium prominent red                          boundary.
                (2.5YR 4/8) mottles; weak medium subangular                      Bh1-45 to 52 inches; brown (7.5YR 4/2) loamy fine
                blocky structure; friable; very strongly acid.                        sand; common medium distinct pale brown (10YR
             The solurn ranges from 610 to more than 80 inches in                     6/3) mottles; weak fine subangular blocky structure
           thickness.                                                                 parting to weak fine granular; very friable, slightly
             The A horizon has hue oi 1 OYR, value of 3 or 4, and                     brittle in some parts; few fine pores; few fine dark
           chroma of 1 or 2. It commonly is silt loam but is fine                     reddish brown (5YR 3/2) bodies that are slightly firm
           sandy loam or loam in some pedons.                                         and brittle; coatings on most sand grains; strongly
             The E horizon has hue of 10YR or 2.5Y, value of 5 to                     acid; clear smooth boundary.
           7, and chroma of 1 or 2. This horizon has mottles in                  Bh2-52 to 60 inches; dark reddish brown (5YR 3/2)
           shades of yellow or brown. This horizon is fine sandy                      fine sand; few medium dark brown (7.5YR 4/2)
           loam, loam, or silt loam.                                                  mottles; weak fine subangular blocky structure
             The Btg horizon has hue of 10YR, value of 6 or 7, and                    parting to weak fine granular; very friable, slightly
           chroma of 1. It has mottles in shades of red, brown, or                    brittle in some parts; coatings on most sand grains;
           yellow. This horizon is sandy clay loam, loam, clay loam,                  strongly acid; gradual wavy boundary.
           silt loam, or silty clay loam.                                        Bh3-60 to 80 inches; black (5YR 2/1) fine sand;
             The BCg horizon has hue, of 1 OYR, value of 6 or 7,                      common medium distinct dark reddish gray (5YR
           and chroma of 1. It has mottles in shades of red, brown,                   4/2) mottles; weak fine subangular blocky structure
           yellow, or gray. This horizon is fine sandy loam, sandy                    parting to weak fine granular; very friable, slightly
           clay loam,'clay loam, or silty clay loam. Some pedons                      brittle in some parts; coatings on most sand grains;
           are stratified with sandier material.                                      very strongly acid.
           Echaw Series                                                            The soium ranges from 55 to more than 80 inches in
                                                                                 thickness.
             The Echaw series consists of soils that formed in thick               The A horizon has hue of 1 OYR, value of 3 to 5, and
           deposits of sandy marine sediment on ridges of upland                 chroma of 1 or 2. It commonly is fine sand but is sand or
           terraces in the central part of the county. Slopes are 0 to           loamy fine sand in some pedons.








       Dorchester County, South Carolina                                                                                             67



         The E horizon has hue of 1 OYR, value of 6 or 7, and                  mottles; moderate medium subangular blocky
       chroma of 3 to 8. Mottles in shades of brown, yellow, or                structure; firm; few distinct coatings on faces of
       gray are in some pedons. This horizon is fine sand,                     peds; few very fine roots; few very fine tubular
       loamy sand, or loamy fine sand.                                         pores; coatings of E material on faces of some
         The Bh horizon has hue of 5YR to 1 OYR, value of 2 to                 peds; strongly acid; clear wavy boundary.
       4, and chroma of 1 to 4. Mottles in shades of brown,               BCgl-43 to 51 inches; gray (10YR 5/1) sandy clay
       yellow, or gray are in some pedons. This horizon is fine                loam; strata of light gray (10YR 7/2) fine sand;
       sand, loamy sand, or loamy fine sand.                                   many coarse prominent yellowish red (5YR 4/6)
                                                                               mottles and common medium distinct light brownish
       Elloree Series                                                          gray (2.5Y 6/2) mottles; weak medium subangular
                                                                               blocky structure; friable; few fine roots; few very fine
         The Elloree series consists of soils that formed in thick             tubular pores; few small to medium reddish brown
       deposits of sandy and loamy sediments on broad, low                     (5YR 4/3) ironstone concretions; strongly acid; clear
       stream terraces, in depressions, and along                              wavy boundary.
       drainageways. Slopes are 0 to 2 percent. These soils are           BCg2-51 to 72 inches; light gray (1 OYR 6/ 1) sandy clay
       loamy, siliceous, thermic Arenic Ochraqualfs.                           loam; strata of loamy sand; common medium
         The Elloree soils in this survey area are taxadjuncts to              distinct light gray (5Y 7/2) mottles; weak medium
       the Bloree series because they typically are more acid in               subangular blocky structure; friable; few fine roots;
       the A horizon and the upper part of the 8 horizon and                   neutral; gradual wavy boundary.
       have a slightly thicker, darker color surface layer than is        Cg-72 to 80 inches; light gray (5Y 7/2) loamy sand;
       defined in the Elloree series. These differences do not                 common medium distinct gray (10YR 6/1) mottles;
       significantly alter the use and behavior of the soils.                  massive; very friable; neutral.
         Elloree soils are associated on the landscape with
       Albany, Coosaw, Nakina, Grifton, Mouzon, and                          The solurn ranges from 55 to more than 80 inches in
       Yemassee soils. Albany and Coosaw soils are higher on              thickness.
       the landscape than the Elloree soils and are Ultisols.                The A horizon has hue of 1 OYR to 5Y, value of 2 to 4,
       Also, Albany soils are in a grossarenic subgroup. Nakina           and chroma of 1; or it is neutral and has value of 2 to 4.
       soils are lower on the landscape and have an umbric                This horizon commonly is loamy fine sand but is fine
       epipedon. Grifton and Mouzon soils are in positions                sand or loamy sand in some pedons.
       similar to those of the Elloree soils and are not in an               The E horizon has hue of I OYR to 5Y, value of 4 to 7,
       arenic subgroup. Yemassee soils are slightly higher on             and chroma of 1 to 4. It is loamy fine sand, loamy sand,
       the landscape and are in an aeric subgroup.                        or fine sand.
         Typical peclon of Elloree loamy fine sand, occasionally             The Btg horizon has hue of 1 OYR to 5Y, value of 5 to
       flooded; about 6 miles southeast of Summerville, about             7, and chroma of 1 or 2. In some pedons, this horizon
       1.7 miles north of the intersection of South Carolina              has hue of 2.5Y or 5Y and chroma of 3 or 4. Mottles in
       Highway 642 and South Carolina Highway 259, 410 feet               shades or red, brown, yellow, or gray or a combination of
       northwest of South Carolina Highway 662 and South                  these colors are in most pedons. The Btg horizon
       Carolina Electric and Gas power pole 153988.                       commonly is sandy clay loam but ranges to sandy loam,
       A-0 to 8 inches; very dark gray (10YR 3/1) loamy fine              fine sandy loam, and clay loam.
            sand; weak medium granular structure; very friable;              The BCg horizon has hue of 1 OYR to 5GY, value of 5
            many very fine roots, common fine roots, and few              to 7, and chroma of 1 or 2; or it is neutral and has value
            medium roots; very strongly acid; clear smooth                of 5 to 7. It commonly has mottles in shades of red,
            boundary.                                                     brown, yellow, or gray or in a combination of these
       E1-8 to 20 inches; dark grayish brown (10YR 4/2)                   colors. This horizon is fine sandy loam or sandy clay
            loamy fine sand; common medium distinct brown                 loam.
            (10YR 5/3) mottles; weak fine granular structure;                The C horizon has colors similar to those of the BCg
            very friable, slightly brittle in some parts; common          horizon. It ranges from sandy to clayey material.
            fine roots and few medium roots; strongly acid; clear
            wavy boundary.                                                Emporia Series
       E2-20 to 23 inches; light brownish gray (10YR 6/2) fine
            sand; common medium distinct dark grayish brown                  The Emporia series consists of soils that formed in
            (10YR 4/2) mottles and common medium faint pale               loamy marine sediment on gently sloping upland
            brown (10YR 6/3) mottles; single grained; loose;              terraces. Slopes are 2 to 6 percent. These soils are fine-
            common fine roots; medium acid; abrupt wavy                   loamy, siliceous, thermic Typic Hapludults.
            boundary,                                                        Emporia soils are associated on the landscape with
       Btg-23 to 43 inches; gray (10YR 5/1) sandy clay loam;              Daleville, Goldsboro, Jedburg, Izagora, Lynchburg, and
            common medium distinct strong brown (7.5YR 5/8)               Rains soils. These soils are lower on the landscape than










           68
                                                                                                                                      Soil Survey



           the Emporia soils. Jedburg, Lynchburg, Daleville, and                 sandy clay loam that has strata of loamy sand, sandy
           Rains soils are Aquults. Izagora. and Goldsboro soils                 loam, or sandy clay.
           have mottles that have chroma of 2 or less within 30
           inches of the surface. Bonneau soils are in an arenic                 Eulonia Series
           subgroup.
              Typical pedon of Emporia loamy fine sand, 2 to 6                      The Eulonia series consists of soils that formed in
           percent slopes; about 4 miles west of Summerville on                  clayey marine sediment on nearly level or gently sloping
           South Carolina Highway 58, about 1,000 feet southwest                 upland terraces in the southeastern part of the county
           on a subdivision road from the intersection of South                  generally at an elevation of less than 42 feet above sea
           Carolina Highway 58 and South Carolina Highway 22,                    level. Slopes are 0 to 6 percent. These soils are clayey,
           about 500 feet north on a subdivision road, and 50 feet               mixed, thermic Aquic Hapludults.
           south of road.                                                           Eulonia soils are associated on the landscape with
           A-0 to 5 inches; dark grayish brown (10YR 4/2) loamy                  Chisolm, Mouzon, Ogeechee, Wahee, Yauhannah, and
                fine sand; weak fine granular structure; very friable;           Yemassee soils. Chisolm soils are higher on the
                common fine and medium roots; strongly acid;                     landscape than the Eulonia soils and are in an arenic
                gradual smooth boundary.                                         subgroup. Mouzon, Ogeechee, Wahee, and Yemassee
           E-5 to 14 inches; very pale brown (1 OYR 7/3) loamy                   soils are lower on the landscape. Mouzon and Ogeechee
                fine sand; common medium faint very pale brown                   soils are dominantly gray throughout the profile. Mouzon
                (1 OYR 8/3) mottles; weak fine subangular blocky                 soils are Alfisols, and Ogeechee soils have a fine-loamy
                structure; very friable; fEW fine roots and common               particle-size control section. Wahee and Yemassee soils
                medium roots; strongly acid; gradual wavy boundary               are in an aeric subgroup. Yemassee soils have a fine-
           Btl-14 to 41 inches; strong brown (7.5YR 5/8) sandy                   loamy particle-size control section. Yauhannah soils are
                clay loam; common medium distinct yellowish red                  in positions similar to those of the Eulonia soils and have
                (5YR 5/8) mottles; moderate medium subangular                    a fine-loamy particle-size control section.
                blocky structure; firm; few faint clay films on faces of            Typical peclon of Eulonia fine sandy loam, 0 to 2
                peds; few fine roots; few fine tubular pores; strongly           percent slopes; about 13 miles southwest of Summerville
                acid; gradual smooth boundary.                                   at the intersection of South Carolina Highway 317 and
           Bt2-41 to 54 inches; mottled reddish yellow (7.5YR                    South Carolina Highway 165, about 6 miles east on
                6/8), red (2.5YR 4/6), and light gray (10YR 7/1)                 South Carolina Hig    .hway 317, about 1.5 miles north on
                sandy clay loam; moderate medium subangular                      paper company unimproved road, and 50 feet west of
                blocky structure; firm; few distinct clay films on faces         road in planted pine.
                of peds; few fine tubular pores; very strongly acid;             Ap-O to 4 inches, dark grayish brown (1 OYR 4/2) fine
                gradual wavy boundary.                                                sandy loam; weak fine granular structure; very
           BC-54 to 75 inches; light gray (10YR 7/1) stratified                       friable; many fine roots and common medium roots;
                sandy clay loam and sandly loam; many medium                          strongly acid; clear smooth boundary.
                distinct yellowish brown (1 OYR 5/8) mottles and
                common medium prominent red (2.5YR 4/8)                          E-4 to 11 inches; light yellowish brown (1 OYR 6/4) fine
                mottles; weak medium subangular blocky structure;                     sandy loam; few medium distinct dark grayish brown
                friable; strongly acid.                                               (1 OYR 4/2) streaks along old root channels; weak
                                                                                      fine granular structure; very friable; common fine
              The solum ranges from 55 to more than 80 inches in                      roots; strongly acid; clear smooth boundary.
           thickness.                                                            Btl -11 to 15 inches; strong brown (7.5YR 5/6) sandy
              The A horizon has hue of 1 OYR, value of 4 or 5, and                    clay loam; common medium distinct very pale brown
           chroma of 1 to 3. It commonly is loamy fine sand but is                    (10YR 7/4) and yellowish red (5YR 5/6) mottles and
           loamy sand in some pedons.                                                 few fine distinct red (2.5YR 4/8) mottles; moderate
              The E horizon has hue of 1 OYR, value of 6 or 7, and                    medium subangular blocky structure; friable; very
           chroma of 3 or 4. It is loamy sand or loamy fine sand.                     few faint clay films on faces of some peds; few fine
              The Bt horizon has hue of 7.5YR or 1 OYR, value of 5                    roots and pores; strongly acid; gradual wavy
           to 7, and chroma of 6 or 8. It has mottles in shades of                    boundary.
           red, brown, and yellow. Mottles in shades of gray are in              Bt2-15 to 27 inches; yellowish red (5YR 5/6) sandy
           the lower part of the Bt horizon in most pedons. This                      clay; common medium distinct red (2.5YR 4/8)
           horizon is sandy clay loam. In some pedons, the lower                      mottles and few fine distinct pale brown (10YR 6/3)
           part of the Bt horizon is sandy clay.                                      mottles; strong medium subangular blocky structure;
              The BC horizon has hue of 7.5YR or 1 OYR, value of 5                    very firm; few distinct clay films on faces of peds;
           to 7, and chroma of 1 to 8. Some pedons are mottled in                     few fine roots; common fine pores; strongly acid;
           shades of red, brown, yellow, and gray. This horizon is                    clear wavy boundary.








       Dorchester County, South Carolina                                                                                                 69



       Bt3-27 to 35 inches; yellowish red (5YR 5/6) sandy                  soils are in an arenic subgroup. Blanton and Bonneau
            clay loam; strata of clay; common medium distinct              soils are higher on the landscape. Blanton soils are in a
            red (2.5YR 4/8) and reddish yellowish (7.5YR 6/8)              grossarenic subgroup, and Bonneau soils are in an
            mottles and few medium distinct light brownish gray            arenic subgroup. Lynn Haven soils are lower on the
            (10YR 6/2) mottles; moderate to strong medium                  landscape, are Spodosols, and have an umbric
            subangular blocky structure; very firm; few distinct           epipedon.
            clay films on faces of peds; few medium roots; few               Typical pedon of Foreston loamy fine sand, 0 to 2
            fine and medium pores; few fine flakes of mica;                percent slopes; about 500 feet north from the
            strongly acid; clear wavy boundary.                            intersection of U.S. Highway 78 and South Carolina
       BC-35 to 49 inches; strong brown (7.5YR 5/8) sandy                  Highway 25, about 0.5 mile east on unimproved county
            clay loam; common medium distinct light gray (1 OYR            road, and 500 feet north of road in a cultivated field.
            7/1) and yellowish red (5YR 5/8) mottles and few
            medium distinct reddish brown (5YR 5/4) mottles;               Ap-0 to 8 inches; very dark gray (10YR 3/1) loamy fine
            moderate medium subangular blocky structure;                        sand; weak fine granular structure; very friable;
            friable; few fine flakes of mica; very strongly acid;               many fine roots and few medium roots; medium
            gradual wavy boundary.                                              acid; clear smooth boundary.
       C-49 to 80 inches; strong brown (7.5YR 5/8) loamy fine              E-8 to 13 inches; yellowish brown (10YR 5/4) loamy
            sand; strata of sandy clay loam; common medium                      fine sand; common medium distinct pale brown
            distinct yellowish red (5YR 5/8) mottles and few                    (10YR 6/3) mottles and few medium distinct
            medium distinct light gray (10YR 7/2) and very pale                 yellowish brown (10YR 5/8) mottles; weak fine
            brown (1 OYR 7/4) mottles; weak fine subangular                     granular structure; very friable; few fine roots; few
            blocky structure; very friable; very strongly acid.                 fine pores; medium acid; gradual wavy boundary.
         The solum ranges from 49 to more than 72 inches in                Btl-13 to 23 inches; yellowish brown (10YR 5/6) fine
       thickness.                                                               sandy loam; few medium faint yellowish brown
         The A horizon has hue of 10YR, value of 4, and                         (10YR 5/8) mottles; weak medium subangular
       chroma of 1 or 2. It commonly is fine sandy loam but is                  blocky structure; very friable; very few faint clay films
       loamy fine sand in some pedons.                                          along old root channels, few fine roots; few fine
         The E horizon has hue of 1 OYR, value of 5 to 7, and                   pores; medium acid; gradual wavy boundary.
       chroma of 1 to 4. It is sandy loam or fine sandy loam.              Bt2-23 to 32 inches; brownish yellow (1 OYR 6/6) fine
         The Bt horizon has hue of 5YR to 1 OYR, value of 5 or                  sandy loam; common medium faint yellowish brown
       6, and chroma of 4 to 8. It is sandy clay or clay. In some               (10YR 5/8) mottles and common medium distinct
       pedons, the upper part of the Bt horizon is sandy clay                   light brownish gray (10YR 6/2) mottles; weak fine
       loam.                                                                    subangular blocky structure; very friable; very few
         The BC horizon has hue of 5YR to 1 OYR, value of 4 to                  faint clay films along old root channels; few fine
       7, and chroma, of 1 to 8. In some pedons, it is mottled in               roots; few fine pores; medium acid; clear wavy
       shades of red, yellow, brown, or gray. This horizon is                   boundary.
       sandy loam or sandy clay loam. Some pedons have                     F-32 to 53 inches; light brownish gray (10YR 6/2) fine
       pockets or strata of variable textures.                                  sand; common medium faint gray (1 OYR 6/ 1)
         The C horizon has hue of 7.5YR or 1 OYR, value of 5                    mottles and few medium distinct brown (10YR 4/3)
       to 7, and chroma of 2 to 8. It is loamy sand, loamy fine                 mottles; single grained; very friable; few fine roots;
       sand, or sandy loam. Some pedons have pockets or                         medium acid; clear wavy boundary.
       strata of variable textures.                                        Btg-53 to 80 inches; light gray (10YR 7/1) fine sandy
                                                                                loam; strata of sandy clay loam and loamy sand;
       Foreston Series                                                          common medium distinct brownish yellow (10YR
                                                                                6/8) and very pale brown (1 OYR 7/4) mottles; weak
         The Foreston series consists of soils that formed in                   medium subangular blocky structure; very friable;
       loamy marine sediment on nearly level upland terraces                    strongly acid.
       mainly in the central part of the county. Slopes are 0 to
       2 percent. These soils are coarse-loamy, siliceous,                   The solum is more than 60 inches thick.
       thermic Aquic Paleudults.                                             The A horizon has hue of 1 OYR, value of 3 or 4, and
         Foreston soils are associated on the landscape with               chroma of 1 or 2. It has mottles in shades of brown or
       Albany, Blanton, Bonneau, Echaw, Goldsboro, Ocilla,                 yellow. This horizon generally is loamy fine sand but is
       and Lynn Haven soils. Albany, Echaw, Goldsboro, and                 loamy sand in some pedons.
       Ocilla soils are in positions similar to those of the                 The E horizon has hue of 1 OYR, value of 4 to 6, and
       Foreston soils. Albany soils are in a grossarenic                   chroma of 3 to 6. It has mottles in shades of brown or
       subgroup. Echaw soils are Spodosols. Goldsboro soils                yellow. This horizon is fine sand, loamy sand, or loamy
       have a fine-loamy particle-size control section. Ocilla             fine sand.









          70                                                                                                                  Soil Survey



            The upper part of the Bt horizon has hue of 1 OYR,                   common fine roots; medium acid; gradual wavy
          value of 5 to 7, and chroma of 4 or 6. It has mottles in               boundary.
          shades of brown or yellow and has gray mottles between            C2-64 to 77 inches; very pale brown (10YR 7/3) fine
          depths of 20 and 30 inches. This horizon is sandy loam                 sand; common medium faint light gray (10YR 7/2)
          or fine sandy loam.                                                    mottles; single grained; loose; medium acid; gradual
            The F horizon has hue of 10YR, value of 5 to 7, and                  wavy boundary.
          chroma of 1 to 6. It has mottles in shades of yellow,             C3-77 to 85 inches; light gray (10YR 7/1) fine sand;
          brown, or gray. This horizon is fine sand, loamy sand, or              single grained; loose; medium acid.
          loamy fine sand.
            The lower part of the Bt horizon has hue of 10YR,                 This soil is sand or fine sand to a depth of more than
          value of 5 to 7, and chroma of 1 to 6. It has mottles in          Winches.
          shades of yellow, brown, or gray. This horizon is fine              The A horizon has hue of 10YR, value of 3 to 5, and
          sandy loam or sandy loam with strata of loamy sand or             chroma of 1 to 3.
          sandy clay loam.                                                    The Bw horizon has hue of 7.5YR or 1 OYR, value of 5
                                                                            to 7, and chroma of 3 to 8. This horizon is mottled in
          Foxworth Series                                                   shades of brown or yellow.
                                                                              The C horizon has hue of 10YR, value of 5 to 7, and
            The Foxworth series consists of soils that formed in            chroma of 1 to 6. It has mottles in shades of brown,
          sandy marine sediment on nearly level to gently sloping           yellow, or gray.
          stream terraces and ridges throughout the county.
          Slopes are 0 to 6 percent. These soils are thermic,
          coated Typic Quartzipsamnlents.                                   Goldsboro Series
            Foxworth soils are associated on the landscape with               The Goldsboro series consists of soils that formed in
          Albany, Alpin, Blanton, Chipleq, Osier, and Lynn Haven
          soils. Albany and Chipley soils are slightly lower on the         loamy marine sediment on nearly level upland terraces.
          landscape than the Foxworth soils. Albany soils are in a          Slopes are 0 to 2 percent. These soils are fine-loamy,
          grossarenic subgroup. Chipley soils have gray mottles             siliceous, thermic Aquic Paleudults.
          between depths of 20 and 40 inches. Alpin and Blanton               Goldsboro soils are associated on the landscape with
          soils are higher on the landscape. Alpin soils have               Bonneau, Lynchburg, Ocilla, Noboco, Pantego, and
          lamella between depths of 50 and 70 inches. Blanton               Rains soils. Bonneau and Noboco soils are slightly
          soils are in a grossarenic subgroup. Osier and Lynn               higher on the landscape than the Goldsboro soils.
          Haven soils are lower on the landscape. Osier soils have          Bonneau soils are in an arenic subgroup. Noboco soils
          dominant matrix chroma of 22 or less. Lynn Haven soils            do not have gray mottles within 30 inches of the surface.
          have an umbric epipedon and are Spodosols.                        Lynchburg and Ocilla soils are slightly lower on the
            Typical pedon of Foxworth fine sand, 0 to 6 percent             landscape. Lynchburg soils are in an aeric subgroup, and
          slopes; about 0.7 mile southeast of the entrance to               Ocilla soils are in an arenic epipedon. Pantego and
          Middleton Gardens on South Carolina Highway 61, about             Rains soils are lower on the landscape, are Aquults, and
          700 feet south of the caretaker's house along riding trail,       have dominant matrix with chroma of 2 or less
          and 100 feet west of trail.                                       throughout the profile. Pantego soils have an umbric
                                                                            epipedon.
          A-0 to 7 inches; very dark grayish brown (10YR 3/2)                 Typical pedon of Goldsboro loamy sand, 0 to 2
              fine sand; single grained; loose; common large and            percent slopes; about 0.2 mile northwest of overpass
              medium roots and many fine roots; strongly acid;              bridge where South Carolina Highway 86 crosses over
              clear smooth boundary.                                        U.S. Interstate 95, about 1.2 miles southwest on
          Bwl-7 to 14 inches; yellowish brown (10YR 5/6) fine               unimproved county road, and 50 feet northwest of road
              sand; single grained; loose; common streaks of very           in a cultivated field.
              dark grayish brown (10YR 3/2) surface material;
              common medium and fine roots; few fine pores;                 Ap-0 to 7 inches; very dark grayish brown (10YR 3/2)
              medium acid; gradual smooth boundary.                              loamy sand; weak fine granular structure; very
          Bw2-14 to 47 inches; strong brown (7.5YR 5/6) fine                     friable; common fine roots; strongly acid; clear
              sand; few medium distinct very pale brown (10YR                    smooth boundary.
              7/4) mottles; single grained; loose; common fine              E-7 to 14 inches; light yellowish brown (10YR 6/4)
              roots; common fine pores; medium acid; gradual                     loamy sand; few medium distinct dark gray (1 OYR
              smooth boundary.                                                   4/1) streaks in old root or worm holes; weak fine
          Cl-47 to 64 inches; very pale brown (10YR 7/4) fine                    subangular blocky structure; very friable; few fine
              sand; common medium distinct light gray (10YR                      roots; medium acid; clear smooth boundary.
              7/2) mottles and few medium distinct brownish                 Btl-14 to 25 inches; yellowish brown (10YR 5/8) sandy
              yellow (10YR 6/8) mottles; single grained; loose;                  clay loam; few fine distinct strong brown (7.5YR 5/8)









        Dorchester County, South Carolina                                                                                                         71



             mottles; moderate medium subangular blocky                            Grifton soils are associated on the landscape with
             structure; friable; very few faint clay films along old            Mouzon, Daleville, Ogeechee, Osier, Plummer, Rains,
             root holes; few fine roots; few fine pores; very                   and Elloree soils. All of these soils are in positions
             strongly acid; gradual wavy boundary.                              similar to those of the Grifton soils and are dominantly
        Bt2-25 to 48 inches; brownish yellow (10YR 6/6) sandy                   gray throughout. Mouzon soils are Albaqualfs. Daleville,
             clay loam; common medium distinct yellowish red                    Ogeechee, and Rains soils are Aquults, and Osier soils
             (5YR 5/8) mottles, common medium distinct light                    are Entisols. Elloree soils are in an arenic subgroup, and
             yellowish brown (10YR 6/4) mottles, and few                        Plummer soils are in a grossarenic subgroup.
             medium distinct gray (10YR 6/1) mottles; moderate                     Typical pedon of Grifton fine sandy loam, frequently
             medium subangular blocky structure; friable; very                  flooded; about 1.5 miles southwest of St. George on
             few faint clay films on faces of peds; few fine roots;             South Carolina Highway 49, 100 feet southeast of the
             very strongly acid; gradual wavy boundary.                         highway, about halfway between the two bridges
        Btg-48 to 62 inches; gray (1 OYR 6/ 1) sandy clay loam;                 crossing Polk Swamp.
             many coarse distinct yellowish brown (1 OYR 5/8)
             mottles, common medium distinct strong brown                       A-0 to 6 inches; dark grayish brown (10YR 4/2) fine
             (7.5YR 5/8) mottles, and few medium prominent red                       sandy loam; weak medium granular structure; very
             (2.5YR 4/8) mottles; weak medium subangular                             friable; common medium roots and many fine roots;
             blocky structure; very friable; few faint clay films on                 very strongly acid; clear wavy boundary.
             faces of peds; few fine roots; very strongly acid;                 E-6 to 10 inches; light gray (1 OYR 7/2) fine sandy
             clear wavy boundary.                                                    loam; common medium faint light brownish gray
        BCg-62 to 80 inches; gray (10YR 6/1) sandy clay loam;                        (10YR 6/2) mottles and common medium distinct
             strata of sandy loam; common medium prominent                           brownish yellow (10YR 6/6) mottles; weak medium
             red (2.5YR 4/8) mottles, common medium distinct                         subangular blocky structure; very friable; common
             yellowish brown (10YR 5/8) mottles, and few                             fine roots; few fine pores; slightly acid; clear wavy
             medium distinct reddish yellow (7.5YR 6/8) mottles;                     boundary.
             weak medium subangular blocky structure; very                      Btg1-10 to 35 inches; gray (10YR 5/1) sandy clay
             friable; very strongly acid.                                            loam; few medium distinct brownish yellow (10YR
                                                                                     6/6) mottles; moderate medium prismatic structure
          The solum ranges from 60 to more than 80 inches in                         parting to strong coarse subangular blocky; firm; few
        thickness.                                                                   fine roots; common fine pores; many distinct clay
          The A horizon has hue of 1 OYR, value of 3 to 6, and                       films on faces of peds; few to common small to
        chroma of 1 or 2. It commonly is loamy sand but is                           medium concretions of calcium carbonate; few sand
        loamy fine sand in some pedons.                                              coatings between peds; moderately alkaline; gradual
          The E horizon has hue of 10YR, value of 5 to 7, and                        wavy boundary.
        chroma of 3 to 6. It has mottles in shades of brown,                    Btg2-35 to 49 inches; gray (1 OYR 6/ 1) sandy clay
        yellow, or gray. This horizon is loamy sand or loamy fine                    loam; common medium distinct light olive brown
        sand.                                                                        (2.5Y 5/6) mottles; moderate medium subangular
          The Bt horizon has hue of I OYR, value of 5 to 7, and                      blocky structure; friable; few fine roots; few fine
        chroma of 4 to 8. It has mottles in shades of red, brown,                    pores; common distinct clay films on faces of peds;
        or yellow. Mottles in shades of gray are 18 to 30 inches                     common fine and medium concretions of calcium
        below the surface. This horizon is sandy clay loam.                          carbonate; moderately alkaline; gradual wavy
          The Btg horizon has hue of 1 OYR, value of 4 to 7, and                     boundary.
        chroma of 1 or 2. It has mottles in shades of red, brown,               Cgl-49 to 61 inches; light gray (10YR 7/1) sandy clay
        yellow, or gray. This horizon is sandy clay loam or sandy                    loam; strata of loamy sand; few medium distinct
        clay.                                                                        brownish yellow (10YR 6/6) mottles; massive;
          The BCg horizon has hue of 10YR, value of 5 to 7,                          friable; moderately alkaline; clear wavy boundary.
        and chroma of 1 or 2. It has mottles in shades of red,                  Cg2-61 to 67 inches; gray (10YR 6/1) sandy loam;
        brown, yellow, or gray. This horizon is sandy clay loam,                     strata of loamy sand; massive; very friable; neutral;
        sandy clay, or sandy loam. Some peclons are stratified.                      gradual wavy boundary.
                                                                                Cg3-67 to 80 inches; gray (10YR 6/1) sand; single
        Grifton Series                                                               grained; loose; moderately alkaline.
          The Grifton series consists of soils that formed in                      The solum ranges from 40 to more than 65 inches in
        loamy marine sediment on nearly level flood plains and                  thickness.
        along small drainageways throughout the county. Slopes                     The A horizon has hue of 1 OYR, value of 3 or 4, and
        are 0 to 2 percent. These soils are fine-loamy, siliceous,              chroma of 1 or 2. It commonly is fine sandy loam but is
        thermic Typic Ochraqualfs.                                              loamy fine sand in some peclons.









           72                                                                                                                        Soil Survey



             The E horizon has hue of 10YR, value of 4 to 7, and                      rubbed; structureless; slightly sticky; about 30
           chroma of 1 or 2. It is fine sand, loamy fine sand, or fine                percent mineral; moderately alkaline when wet;
           sandy loam.                                                                gradual smooth boundary.
             The Btg horizon has hue olf 10YR, value of 5 to 7, and              2Cg-48 to 80 inches; greenish gray (5BG 6/1) silty
           chroma of 1. It has mottles in shades of red, yellow,                      clay; few medium distinct reddish brown (2.5YR 5/4)
           brown, or gray. This horizon is fine sandy loam or sandy                   and dark gray (10YR 4/1) mottles; massive; very
           clay loam. Some pedons have strata of loamy sand and                       sticky; mildly alkaline when wet.
           sandy clay.
             The Cg horizon has hue of 1 OYR, value of 6 or 7, and                 The organic layers range from 30 to 48 inches in
           chroma of 1. Some pedons have mottles in shades of                    thickness.
           brown or yellow, and some pedons have strata of white                   The Oi horizon has hue of 2.5YR to 10YR, value of 3
           sand. This horizon is sand, loamy fine sand, or sandy                 or 4, and chroma of 2. Fiber content ranges from 60 to
           loam; or it is stratified with variable textures.                     90 percent. This horizon is muck.
                                                                                   The Oe horizon has hue of 2.5YR to 1 OYR, value of 3
           Handsboro Series                                                      or 4, and chroma of 2 or 3. Fiber content ranges from 30
             The Handsboro series consists of soils that formed in               to 60 percent.
           loamy and clayey marine sediment on nearly level tidal                  The Oa horizon has hue of 2.5YR to 10YR, value of 2
           marshes at an elevation of 3 to 6 feet above sea level.               to 4, and chroma of 1 or 2. Fiber content is less than 10
           These soils are flooded by sea water once or twice daily.             percent rubbed.
           Slopes are less than I percent. These soils are euic,                   The 2Cg horizon has hue of 5Y to 513G, value of 3 to
           thermic Typic Sulfihemists.                                           7, and chroma of 1 or 2. Most pedons have mottles in
             The Handsboro soils in this survey area are                         shades of yellow or brown. This horizon ranges from
           considered taxadjuncts to the Handsboro series because                loamy sand to clay.
           they have hemic or fibric material dominant in the
           surface tier, have a redder hue, and are underlain by a               Izagora Series
           continuous 2C horizon at a depth of about 48 inches.                    The Izagora series consists of soils that formed in
           Use and behavior of the soils in this survey area are                 loamy and silty marine sediments on nearly level to
           controlled by flooding, ponding, and excess humus and
           are not significantly different than for the Handsboro                gently sloping upland stream terraces and low ridges.
           series.                                                               Slopes are 0 to 6 percent. These soils are fine-loamy,
             Handsboro soils are associated on the landscape with                siliceous, thermic Aquic Paleudults.
           Capers, Mouzon, and Brookman soils. Capers soils are                    Izagora soils are associated on the landscape with
           in positions similar to thoseof the Handsboro soils. They             Jedburg, Emporia, Bonneau, Daleville, and Pelham soils.
           do not have organic material in more than half of the                 Jedburg, Daleville, and Pelham soils are lower on the
           upper 32 inches of the profile. Mouzon and Brockman                   landscape than the lzagora soils and are aquults.
           soils are slightly higher on the landscape and are                    Pelham soils are in an arenic subgroup. Emporia and
           Alfisois. Mouzon soils havean ochric epipedon, and                    Bonneau soils are higher on the landscape. Emporia
           Brookman soils have an umbric epipedon.                               soils do not have gray mottles within 24 inches of the
             Typical pedon of Handsboro muck; about 10.5 miles                   top of the argillic horizon. Bonneau soils are in an arenic
           southeast of Summerville, about 1 mile south of the                   subgroup.
           entrance to Arch Dale subdivision on South Carolina                     Typical pedon of lzagora silt loam, 0 to 2 percent
           Highway 642, about 150 feet into the marsh from the                   slopes; about 1.2 miles north of Givhans, about 300 feet
           south edge of the marsh.                                              south of small church, and 80 feet west of South
                                                                                 Carolina Highway 174 in a field.
           Oi-O to 6 inches; dark reddish gray (5YR 4/2) muck,
               pressed or rubbed fibric material; about 80 percent               Ap-0 to 6 inches; dark grayish brown (1 OYR 4/2) silt
               fiber when rubbed; structureless; nonsticky; many                      loam; weak medium subangular blocky structure;
               fine roots; about 20 percent mineral; moderately                       very friable; few medium roots and many fine roots;
               alkaline when wet; clear smooth boundary.                              medium acid; clear smooth boundary.
           Oe-6 to 24 inches; dark brown (10YR 3/3) broken                       Btl-6 to 13 inches; yellowish brown (10YR 5/6) silt
               faced, pressed or rubbed hemic material; about 50                      loam; moderate medium subangular blocky
               percent fiber undisturbed; structureless; nonsticky;                   structure; slightly sticky; few fine roots; few fine
               common fine roots; strong sulfide odor; about 10                       pores; few faint clay films on faces of peds; very
               percent mineral; moderately alkaline when wet; clear                   strongly acid; clear wavy boundary.
               smooth boundary.                                                  Bt2-13 to 26 inches; brownish yellow (10YR 6/6) silt
           Oa-24 to 48 inches; dark reddish brown (5YR 3/2)                           loam; common medium distinct yellowish red (5YR
               rubbed sapric material; about 5 percent fiber when                     5/8) mottles; moderate medium subangular blocky








       Dorchester County, South Carolina                                                                                                73



           structure; slightly sticky; few faint clay films on faces         Typical pedon of Jedburg loam; about 3 miles
           of peds; few fine pores; very strongly acid; gradual            southwest of Ridgeville, about 1 mile southeast of the
           wavy boundary.                                                  junction of South Carolina Highway 19 and South
       Bt3-26 to 41 inches; brownish yellow (10YR 6/6) silty               Carolina Highway 136, and 100 feet west of South
           clay loam; common medium distinct yellowish brown               Carolina Highway 136.
           (10YR 5/8) and light gray (10YR 7/1) mottles and
           few medium prominent red (2.5YR 4/8) mottles;                   A1-0 to 5 inches; very dark gray (10YR 3/1) loam;
           moderate medium subangular blocky structure;                         weak fine granular structure; very friable; many fine
           slightly sticky; few fine pores; few distinct clay films             roots, common medium roots, and few large roots;
           on faces of peds; very strongly acid; gradual wavy                   very strongly acid; clear smooth boundary.
           boundary.                                                       A2-5 to 8 inches; dark grayish brown (10YR 4/2) loam;
       Btg1-41 to 56 inches; brownish yellow (10YR 6/6) silty                   common fine distinct light brownish gray (10YR 6/2)
           clay; many medium prominent red (2.5YR 4/8)                          mottles; weak fine granular structure; very friable;
           mottles, many medium distinct light gray (10YR 7/1)                  common fine roots and few medium roots; few fine
           mottles, and common medium distinct very pale                        tubular pores; strongly acid; clear smooth boundary.
           brown (10YR 7/4) mottles; moderate medium                       BE-8 to 15 inches; light yellowish brown (10YR 6/4)
           subangular blocky structure; firm; very strongly acid;               loam; common medium faint brownish yellow (I OYR
           gradual wavy boundary.                                               6/6) mottles and common medium distinct light
       Btg2-56 to 80 inches; light gray (10YR 7/1) silty clay                   brownish gray (10YR 6/2) mottles; weak fine
           loam; many medium prominent red (2.5YR 4/8)                          subangular blocky structure; very friable; few fine
           mottles, many medium distinct brownish yellow                        roots and few medium roots; common fine tubular
           (10YR 6/6) mottles, and common medium distinct                       pores; very strongly acid; gradual wavy boundary.
           yellow (10YR 7/8) mottles; weak medium
           subangular blocky structure; firm; very strongly acid.          Btg1-15 to 36 inches; light gray (10YR 7/1) loam;
                                                                                common medium distinct brownish yellow (10YR
         The solurn ranges from 60 to 80 inches in thickness.                   6/8) mottles and common fine prominent red (2.5YR
         The A horizon has hue of 1 OYR, value of 3 or 4, and                   5/8) mottles; moderate medium subangular blocky
       chroma of 1 to 3. It commonly is silt loam but is fine                   structure; friable; very fine faint clay films on faces
       sandy loam or loam in some pedons.                                       of peds; few fine and medium roots; few fine tubular
         Some pedons have an E horizon that has hue of                          pores; strongly acid; gradual wavy boundary.
       1 OYR, value of 4 to 6, and chroma of 4. It is sandy loam,          Btg2-36 to 55 inches; pinkish gray (7.5YR 6/2) silt
       fine sandy loam, loam, or silt loam.                                     loam; common medium distinct light brownish gray
         The Bt horizon has hue of 7.5YR or 10YR, value of 5                    (1 OYR 6/2) mottles and common medium distinct
       or 6, and chroma of 6 to 8. It has mottles in shades of                  brownish yellow (10YR 6/8) and yellowish red (5YR
       red, brown, or yellow. Gray mottles are in the lower part                5/8) mottles; moderate medium subangular blocky
       of the horizon. The Btg horizon has hue of I OYR, value                  structure; friable; few distinct clay films on faces of
       of 5 to 7, and chroma of 1 or 2. The Bt and Btg horizons                 peds and in old root channels; few fine and medium
       are sandy clay loam, clay loam, silt loam, or silty clay                 roots; few fine tubular pores; strongly acid; gradual
       loam. Some pedons have silty clay in the lower part of                   wavy boundary.
       the B horizon.                                                      Btg3-55 to 75 inches; mottled light gray (10YR 7/1),
         Some pedons have a BO horizon that has hue of                          yellowish brown (10YR 5/8), and red (2.5YR 4/8)
       1 OYR, value of 5 to 7, and chroma of 1 to 8, and has                    loam; moderate medium subangular blocky
       mottles in shades of red, brown, yellow, or gray; or it is               structure; friable; common distinct clay films on
       mottled with these colors. This horizon is sandy clay                    faces of peds; few fine roots; few fine tubular pores;
       loam, silty clay loam, clay loam, or silty clay.                         strongly acid; gradual wavy boundary.
                                                                           BCg-75 to 80 inches; light gray (5Y 7/2) sandy clay
       Jedburg Series                                                           loam; common medium distinct gray (10YR 6/1)
         The Jedburg series consists of soils that formed in                    mottles and common fine distinct brownish yellow
       loamy and silty marine sediment on broad upland                          (10YR 6/8) mottles; weak medium subangular
       terraces. Slopes are 0 to 2 percent. These soils are fine-               blocky structure; friable; strongly acid.
       loamy, siliceous, thermic Aeric Paleaquults.                           The solurn is more than 60 inches thick.
         Jedburg soils are associated on the landscape with
       Emporia, Izagora, and Daleville soils. Emporia and                     The A horizon has hue of 1 OYR or 2.5Y, value of 2 to
       lzagora soils are higher on the landscape than the                  6, and chroma of 1 or 2. It commonly is loam but is
       Jedburg soils and are Udults. Daleville soils are lower on          loamy fine sand, fine sandy loam, or silt loam in some
       the landscape and are not in an aeric subgroup.                     pedons.









           74                                                                                                                    Soil Survey



             Some pedons have an E horizon that has hue of 1 OYR                   pores; sand grains coated and bridged with clay;
           or 2.5Y, value of 5 to 7, and chroma of 2 to 4. It is loamy             very strongly acid; gradual irregular boundary.
           fine sand, fine sandy loam, loam, or silt loam.                    2C1-31 to 42 inches; strong brown (7.5YR 5/8) sand;
             Some pedons have a Bt horizon that has hue of 7.5YR                   common medium distinct very pale brown (10YR
           to 2.5Y, value of 5 or 6, and chroma of 3 to 8. It has                  7/4) mottles and few medium distinct light gray
           mottles in shades of red, brcwn, yellow, and gray. This                 (10YR 7/2) mottles; single grained; loose; strongly
           horizon is loam, silt loam, or clay loam.                               acid; gradual wavy boundary.
             The Btg horizon has hue of 7.5YR to SY, value of 5 to            2C2-42 to 58 inches; light brownish gray (10YR 6/2)
           7, and chroma of 1 or 2. Most pedons have mottles in                    sand; common medium distinct very pale brown
           shades of red, brown, yellow, or gray. This soil is loam,               (10YR 7/4) and brownish yellow (10YR 6/6)
           silt loam, or clay loam.                                                mottles; single grained; loose; strongly acid; gradual
             The BCg horizon has hue of 1 OYR to 5Y, value of 5 to                 wavy boundary.
           7, and chroma of 1 or 2. It has common to many mottles             2C3-58 to 80 inches; light gray (1 OYR 7/2) coarse
           in shades of yellow, brown, red, or gray. This horizon is               sand; brownish yellow (10YR 6/6) stains on few
           sandy clay loam or clay loam.                                           sand grains; single grained; loose; common
           Johns Series                                                            uncoated quartz pebbles; medium acid.
                                                                                 The solum ranges from 25 to 39 inches in thickness.
             The Johns series consists of soils that formed in                Most pedons have small quartz pebbles in the lower part
           loamy marine and alluvial sediment on nearly level flood           of the C horizon.
           plains of the Edisto River. Slopes are 0 to 2 percent.                The A horizon has hue of 1 OYR, value of 3 to 5, and
           These soils are fine-loamy over sandy or sandy-skeletal,           chroma or 1 or 2. It commonly is loamy sand but is
           siliceous, thermic Aquic Hapludults.                               loamy fine sand in some peclons.
             Johns soils are associated on the landscape with                    Some pedons have an E horizon that has hue of
           Yernassee, Chipley, Lumbee, Osier, and Rutlege soils.              10YR, value of 5 to 7, and chroma of 3 to 6. Mottles in
           Chipley soils are in positions; similar to those of the            shades of brown or yellow are in some pedons. This
           Johns soils and are Entisols. Lumbee, Osier, and                   horizon is loamy sand or loamy fine sand.
           Rutlege soils are lower on the landscape and are                      The Bt horizon has hue of 1 OYR, value of 5 to 7, and
           dominantly gray throughout. Osier soils are Entisols, and          chroma of 4 to 8. In most pedons, mottles in shades of
           Rutlege soils have an umbric epipedon. Yemassee soils              brown, yellow, or gray are in the lower part of this
           are in an aeric subgroup.                                          horizon. The Bt horizon is sandy clay loam or sandy
             Typical pedon of Johns loamy sand, 0 to 2 percent                loam.
           slopes; about 6 miles southwest of Ridgeville, about 1                Some pedons have a Btg horizon that has hue of
           mile southeast of the junction of South Carolina Highway           1 OYR, value of 5 to 7, and chroma of 1 or 2. Mottles in
           19 and South Carolina Highway 25, about 0.5 mile                   shades of red, brown, or yellow are in some pedons. The
           southwest on dirt road, and 80 feet east of road.                  Btg horizon is sandy clay loam or sandy loam.
           A-0 to 6 inches; very dark gray (11 OYR 3/ 1) loamy sand;             The C horizon has hue of 7.5YR or 1 OYR, value of 5
               weak fine granular structure; very friable; few large          to 7, and chroma of 1 to 8. Most pedons have quartz
               roots and common medium and fine roots; strongly               pebbles, some of which are stained with brown or
               acid; clear smooth boundary.                                   yellow. The C horizon is sand or coarse sand.
           BE-6 to 12 inches; light yellowish brown (10YR 6/4)
               sandy loam; common medium distinct dark grayish                Leon Series
               brown (11 OYR 4/2) mottles of surface material along
               root channels; weak fine granular structure; very                 The Leon series consists of soils that formed in thick,
               friable; common fine roots; few fine pores; strongly           sandy marine sediment on nearly level upland stream
               acid; gradual smooth boundary.                                 terraces adjacent to the Edisto River flood plain. Slopes
           Btl-12 to 20 inches; brownish yellow (10YR 6/6) sandy              are 0 to 2 percent. These soils are sandy, siliceous,
               clay loam; moderate medium subangular blocky                   thermic Aeric Haplaquods.
               structure; friable; few fine roots; few fine pores; few           The soils in this survey area are taxadjuncts to the
               faint clay films on faces of peds; very strongly acid;         Leon series because typically the E and Bh horizons are
               gradual wavy boundary.                                         coarse sand. This difference does not significantly alter
           Bt2-20 to 31 inches; light yellowish brown (10YR 6/4)              the use and behavior of the soils.
               sandy clay loam; many medium faint brownish                       Leon soils are associated on the landscape with
               yellow (11 OYR 6/6) mottles and common medium                  Chipley, Echaw, Foxworth, Lynn Haven, and Osier soils.
               distinct light brownish gray (11 OYR 6/2) and yellowish        Chipley, Echaw, and Foxworth soils are higher on the
               red (5YR 5/6) mottles; weak medium subangular                  landscape than the Leon soils and have chroma of 3 or
               blocky structure; friable; few fine roots; few fine            more in the upper part of the profile. Chipley and









       Dorchester County, South Carolina                                                                                              75



       Foxworth soils are Entisols. Lynn Haven soils are lower            U.S. Highway 15 at St. Lukes Church, about 1.3 miles
       on the landscape and have an umbric epipeclon. Osier               west on unimproved paper company road, about 1.3
       soils are in positions similar to those of the Leon soils          miles southwest on paper company road, about 0.7 mile
       and are Entisols.                                                  south on paper company road, and 50 feet east of 90-
         Typical pedon of Leon sand; about 1.2 miles south of             degree bend in road.
       the intersection of South Carolina Highway 61 and South
       Carolina Highway 162, 0.7 mile west on unimproved                  Ap-O to 5 inches; very dark gray (11 OYR 3/ 1) fine sandy
       county road, 2,000 feet northeast on unimproved road,                  loam; weak fine subangular blocky structure; very
       and 300 feet northwest of road.                                        friable; many fine roots and common medium roots;
       A-0 to 6 inches; very dark gray (11 OYR 3/ 1) sand; single             very strongly acid; clear smooth boundary.
           grained; loose; common fine and medium roots; very             Btg1-5 to 10 inches; gray (10YR 5/1) sandy clay loam;
                                                                              common medium distinct strong brown (7.5YR 5/8)
           strongly acid; clear smooth boundary.                              and yellowish red (5YR 5/6) mottles; moderate
       E-6 to 17 inches; light brownish gray (10YR 6/2)                       medium subangular blocky structure; friable; very
           coarse sand; single grained; loose; few fine roots;                few faint clay films on faces of peds; common fine
           strongly acid; abrupt smooth boundary.                             roots and few medium roots; few fine pores; very
       Bhl -17 to 25 inches; dark reddish brown (5YR 2/2)                     strongly acid; gradual wavy boundary.
           coarse sand; weak fine granular structure; very                Btg2-10 to 26 inches; gray (10YR 6/1) sandy clay
           friable; few fine roots; weakly cemented; very                     loam; few medium distinct brownish yellow (10YR
           strongly acid; gradual smooth boundary.                            6/6) and pale brown (10YR 6/3) mottles; weak
       Bh2-25 to 65 inches; very dark gray (N 3/0) coarse                     medium subangular blocky structure; friable; very
           sand; few medium distinct dark reddish brown (5YR                  few faint clay films on faces of peds; common fine
           2/2) mottles; weak fine granular structure; very
           friable; very strongly acid; clear smooth boundary.                roots; strongly acid; gradual wavy boundary.
       C-65 to 80 inches; brown (10YR 5/3) coarse sand;                   BCg-26 to 37 inches; gray (10YR 6/1) sandy loam;
           structureless; loose; very strongly acid.                          strata of loamy sand and sand; common medium
                                                                              distinct brownish yellow (10YR 6/6) mottles and
         The A horizon has hue of 10YR, value of 2 to 4, and                  common medium distinct light yellowish brown
       chroma of 1, or it is neutral and has value of 2 to 4. This            (10YR 6/4) mottles; weak fine granular structure;
       horizon commonly is sand but is fine sand in some                      very friable; strongly acid; clear smooth boundary.
       peclons.                                                           2Cgl-37 to 56 inches; gray (10YR 6/1) sand; common
         The E horizon has hue of 1 OYR, value of 5 to 8, and                 medium distinct light yellowish brown (10YR 6/4)
       chroma of 1 to 2, or it is neutral and has value of 5 to 8.            mottles and few medium distinct yellowish brown
       This horizon is sand or coarse sand.                                   (10YR 5/8) mottles; single grained; loose; strongly
         The Bh horizon has hue of 5YR to 1 OYR, value of 2 to                acid; clear wavy boundary.
       4, and chroma of 1 or 2, or it is neutral and has value of         2Cg2-56 to 70 inches; light gray (1 OYR 7/2) coarse
       2 or 3. This horizon is coarse sand, sand, or loamy sand.              sand; single grained; loose; strongly acid.
         The C horizon has hue of 10YR, value of 3 to 5, and
       chroma of 2 to 4. It is sand, fine sand, or coarse sand.             The solum ranges from 24 to 39 inches in thickness.
                                                                            The A horizon has hue of I OYR, value of 2 to 4, and
       Lumbee Series                                                      chroma of 1 or 2. It commonly is fine sandy loam but is
         The Lumbee series consists of soils that formed in               loamy sand, loamy fine sand, or sandy loam in some
       loamy marine sediment on flood plains of the Edisto                peclons.
       River. Slopes are 0 to 2 percent. These soils are fine               Some peclons have an E horizon that has hue of
       loamy over sandy or sandy-skeletal, siliceous, thermic             1 OYR, value of 5 or 6, and chroma of 1 to 3. It is sandy
       Typic Ochraquults.                                                 loam, loamy sand, or loamy fine sand.
         Lumbee soils are associated on the landscape with                  The Btg horizon has hue of 10YR, value of 4 to 6, and
       Chipley, Johns, Osier, Grifton, and Nakina soils. Chipley          chroma of 1 or 2. It has mottles in shades of red, brown,
       and Johns soils are higher on the landscape than the               or yellow. This horizon is sandy loam, sandy clay loam,
       Lumbee soils. Osier and Grifton soils are in positions             or clay loam.
       similar to those of the Lumbee soils. Chipley and Osier              The BCg horizon has hue of 1 OYR, value of 5 to 7,
       soils are Entisols. Johns soils are Udults. Grifton soils          and chroma of 1 or 2. It has mottles in shades of red,
       have a solum that is 40 inches or more thick, and they             brown, or yellow. This horizon is sandy loam or loamy
       are Alfisols. Nakina soils are lower on the landscape and          sand. Some pedons are stratified with textures ranging
       have an umbric epipeclon.                                          from sandy loam to coarse sand.
         Typical peclon of Lumbee fine sandy loam,                          The 2Cg horizon has hue of 1 OYR, value of 5 to 7,
       occasionally flooded; about 0.5 mile south of Grover on            and chroma of 1 to 3. It has mottles in shades of brown









          76                                                                                                                     Soil Survey



          or yellow. This horiozn is sand, coarse sand, or loamy              Btg3-54 to 80 inches; gray (10YR 5/1) sandy clay; thin
          sand.                                                                    coatings of sandy clay loam and sandy loam on
                                                                                   faces of peds; common medium distinct red (1 OR
          Lynchburg Series                                                         4/6) and few fine distinct brownish yellow (10YR
                                                                                   6/6) mottles; moderate medium subangular blocky
             The Lynchburg series consists of soils that formed in                 structure; firm; very few faint clay films on faces of
          loamy marine sediment on nearly level upland terraces.                   peds; few fine roots; few fine pores; extremely acid.
          Slopes are 0 to 2 percent. These soils are fine-loamy,
          siliceous, thermic Aeric Paleaquults.                                  The solum ranges form 60 to more than 80 inches in
             Lynchburg soils are associated on the landscape with             thickness.
          Coxville, Goldsboro, Noboco, Pelham, Rains, and Grifton                The A horizon has hue of 10YR, value of 3 or 4, and
          soils. Coxville, Pelham, Rains, and Grifton soils are lower         chroma of 1 or 2. It commonly is loamy sand but is
          on the landscape than the Lynchburg soils and have                  loamy fine sand in some pedons.
          chroma of 2 or less throughout the profile. Coxville soils             Some pedons have an E horizon that has hue of
          have a clayey Bt horizon. Pelham soils are in an arenic             1 OYR, value of 4 to 7, and chroma of 1 to 4. It is loamy
          subgroup. Grifton soils are Alfisols. Goldsboro and                 sand or loamy fine sand.
          Noboco soils are higher on the landscape and are                       The BE horizon has hue of 1 OYR, value of 4 to 7, and
          Udults.                                                             chroma of 3 to 6. Yellow and brown mottles are in most
             Typical pedon of Lynchburg loamy sand; about 0.7                 pedons. This horizon is sandy loam.
          mile northwest of the intersection of South Carolina                   The Bt horizon has hue of 10YR, value of 5 or 6, and
          Highway 20 and U.S. Highway 178, 100 feet north of                  chroma of 3 to 6. It has mottles in shades of brown,
          highway or about 400 feet northwest of Shady Grove                  yellow, or gray. This horizon is sandy loam or sandy clay
          Church.                                                             loam. Some peclons do not have a Bt horizon.
          Ap-O to 7 inches; dark grayish brown (10YR 4/2) loamy                  The Btg horizon has hue of 10YR, value of 4 to 7, and
               sand; weak fine granular structure; very friable;              chroma of 1 or 2. It has mottles in shades of red, brown,
               common fine roots and few medium roots; medium                 yellow, or gray. This horizon is sandy clay loam. In some
               acid; clear smooth boundary.                                   pedons, it is sandy clay loam in the upper part and
          BE-7 to 13 inches; brown (1 OYR 5/3) sandy loam;                    sandy clay in the lower part.
               common medium faint yellowish brown (1 OYR 5/4)
               mottles and few fine faint grayish brown mottles;              Lynn Haven Series
               weak fine subangular blocky structure; very friable;
               few fine and medium roots; strongly acid; clear wavy              The Lynn Haven series consists of soils that formed in
               boundary.                                                      sandy marine sediment in nearly level, slight depressions
          Bt-13 to 17 inches; yellowish brown (10YR 5/4) sandy                and drainageways. Slopes are 0 to 2 percent. These
               clay loam; few fine distinct yellowish brown (10YR             soils are sandy, siliceous, thermic Typic Haplaquods.
               5/8) and grayish brown (10YR 5/2) mottles;                        Lynn Haven soils are associated on the landscape
               moderate medium subangular blocky structure;                   with Chipley, Echaw, Leon, Osier, Pelham, and Rutlege
               friable; very few faint clay films along old root              soils. Chipley and Echaw soils are higher on the
               channels; few fine roots; strongly acid; gradual wavy          landscape than the Lynn Haven soils and have chroma
               boundary.                                                      of 3 or more in the subsurface horizon. Chipley soils are
          Btg1-17 to 42 inches; gray (10YR 6/1) sandy clay                    Entisols. Leon, Osier, and Pelham soils are slightly
               loam; common medium distinct yellowish brown                   higher on the landscape. Leon soils do not have an
               (10YR 5/8) mottles, few medium prominent red                   umbric epipedon. Osier soils are Entisols, and Pelham
               (2.5YR 4/8) mottles, and few medium distinct                   soils are Aquults. Rutlege soils are in positions similar to
               yellowish brown (10YR 5/4) mottles; moderate                   those of the Lynn Haven soils and are Inceptisols.
               medium subangularblocky structure; friable; very                  Typical peclon of Lynn Haven fine sand; about 1 mile
               few faint clay films on faces of peds; few fine roots;         south of Dorchester, 185 feet east of unimproved
               few fine pores; strongly acid; gradual wavy                    secondary road 248, and 150 feet south of road in
               boundary.                                                      woodland.
          Btg2-42 to 54 inches; gray (1 OYR 6/ 1) sandy clay
               loam; thin coatings of sandy loam on faces of peds;            A-0 to 10 inches; very dark gray (10YR 3/1) fine sand;
               common medium distinct yellowish brown (1 OYR                       weak fine granular structure; very friable; many fine
               5/8) mottles and few medium prominent red (2.5YR                    and medium roots; very strongly acid; clear smooth
               4/8) mottles; moderate medium subangular blocky                     boundary.
               structure; friable; few faint clay films on faces of           E-10 to 19 inches; light gray (10YR 7/1) fine sand;
               peds; few fine roots; few fine pores; extremely acid;               common streaks of dark gray fine sand mostly along
               gradual wavy boundary.                                              old root channels; single grained; loose; few fine









       Dorchester County, South Carolina                                                                                               77



            and medium roots; many uncoated sand grains; very                 few large roots; very strongly acid; clear smooth
            strongly acid; abrupt wavy boundary.                              boundary.
       Bhl-19 to 38 inches; dark reddish brown (5YR 2/2)                  E-5 to 8 inches; light gray (10YR 7/1) loamy fine sand;
            fine sand; weak fine granular structure; weakly                   common medium distinct dark grayish brown (10YR
            cemented; friable; few fine roots; sand grains coated             4/2) mottles; weak fine granular structure; very
            with organic matter; very strongly acid; gradual wavy             friable; common fine roots and few medium roots;
            boundary.                                                         medium acid; abrupt smooth boundary.
       Bh2-38 to 49 inches; dark brown (7.5YR 3/2) loamy                  Btgl-8 to 22 inches; gray (10YR 5/1) sandy clay loam;
            fine sand; weak fine granular structure; friable; most            common medium distinct brownish yellow (10YR
            sand grains coated with organic matter; few small                 6/8) mottles and common medium distinct light
            pockets of uncoated sand grains; few medium                       yellowish brown (10YR 6/4) mottles; moderate
            fragments of ironstone; very strongly acid; gradual               medium subangular blocky structure; firm; common
            wavy boundary.                                                    fine pores; neutral, gradual wavy boundary.
       C-49 to 75 inches; grayish brown (10YR 5/2) fine sand;             Btg2-22 to 61 inches; gray (10YR 6/1) sandy clay
            single grained; loose; very strongly acid.                        loam; many medium distinct brownish yellow (10YR
         The sand extends to a depth of more than 80 inches.                  6/8) mottles; weak coarse prismatic structure
         The A horizon has hue of 1 OYR, value of 2 or 3, and                 parting to weak medium subangular blocky; firm; few
       chroma of 1; or it is neutral and has value of 2 or 3.                 faint clay films on faces of peds; few fine roots; few
         The E horizon has hue of 1 OYR or 2.5Y, value 5 to 7,                fine tubular pores; common fine and medium
       and chroma of 1 or 2. Some pedons have mottles that                    concretions of calcium carbonate; neutral; gradual
       have higher chroma.                                                    wavy boundary.
         The Bh horizon has hue of 5YR to 10YR, value of 2 or             BCg-61 to 68 inches; light brownish gray (2.5Y 6/2)
       3, and chroma of 1 to 4. Pockets of grayish sand are in                sandy clay loam; strata and pockets of sandy loam
       some pedons. This horizon is sand or loamy fine sand.                  and loamy sand; many medium distinct brownish
         The C horizon has hue of 1 OYR or 2.5Y, value of 4 to                yellow (10YR 6/8) mottles and few medium distinct
       7, and chroma of 1 to 3. Mottles in shades of red,                     greenish gray (5BG 6/1) mottles; weak medium
       brown, or yellow are in some pedons.                                   subangular blocky structure; friable; neutral; gradual
                                                                              smooth boundary.
       Mouzon Series                                                      Cg-68 to 80 inches; light gray (5Y 7/2) stratified sandy
                                                                              clay loam and loamy sand; common medium distinct
         The Mouzon Series consists of soils that formed in                   brownish yellow (10YR 6/8) mottles and common
       loamy marine sediment on broad, nearly level, low                      medium distinct greenish gray (5 BG 6/1) mottles;
       stream terraces. Slopes dominantly are less than 1                     massive; friable; neutral.
       percent, but range from 0 to 2 percent. These soils are
       fine-loamy, siliceous, thermic Typic Albaqualfs.                     The solurn ranges from 48 to more than 60 inches in
         Mouzon soils are associated on the landscape with                thickness.
       Brookman, Eulonia, Ogeechee, Wahee, and Grifton soils.               The A horizon has hue of I OYR, value of 3 to 5, and
       Brookman soils are lower on the landscape than the                 chroma of 1 or 2. It commonly is fine sandy loam but is
       Mouzon soils and have an umbric epipedon. Eulonia and              sandy loam in some pedons.
       Wahee soils are higher on the landscape and have a                   The E horizon has hue of 1 OYR, value of 4 to 7, and
       clayey particle-size control section. Eulonia soils are            chroma of 1 or 2. It is loamy fine sand or fine sandy
       Udults. Wahee soils are in an aeric subgroup. Ogeechee             loam.
       and Grifton soils are in positions similar to those of the           The Btg horizon has hue of 1 OYR to 5Y, value of 4 to
       Mouzon soils. Ogeechee and Grifton soils have a more               6, and chroma of 1 or 2. It is clay loam or sandy clay
       permeable Bt horizon.                                              loam. In some pedons, the lower part of the Btg horizon
         Typical peclon of Mouzon fine sandy loam,                        is sandy clay or clay.
       occasionally flooded; about 10 miles southwest of
       Summerville, about 2 miles northeast of the intersection             The BCg horizon has hue of 1 OYR to 5Y, value of 5 to
       of South Carolina Highway 84 and South Carolina                    7, and chroma of 1 or 2. It has mottles in shades of
       Highway 163, about 0.5 mile southeast of South Carolina            brown, yellow, or gray. This horizon is sandy clay loam,
       Highway 163 on a paper company road, 100 feet south                fine sandy loam, or sandy clay. Some pedons have
       of road.                                                           strata of sandy clay, sandy clay loam, sandy loam, or
                                                                          loamy sand.
       A-0 to 5 inches; very dark grayish brown (10YR 3/2)                  The Cg horizon has hue of 1 OYR to 5Y, value of 5 to
            fine sandy loam; weak fine granular structure; very           7, and chroma of 1 or 2. It is sand or loamy sand, or it is
            friable; many fine roots, common medium roots, and            stratified with sandy and loamy material.









          78                                                                                                                   Soil Survey



          Nakina Series                                                      Cg2-70 to 80 inches; light olive gray (5Y 6/2) sandy
                                                                                  clay loam; strata of sandy loam; common coarse
             The Nakina series consists, of soils that formed in                  distinct strong brown (7.5YR 5/8) mottles and
          loamy marine sediment in shallow depressions and                        common medium distinct gray (10YR 5/1) mottles;
          drainageways of small streams and rivers. Slopes are 0                  massive; friable; medium acid.
          to 2 percent. These soils are fine-loamy, siliceous,
          thermic Typic Umbraqualfs.                                            The solum ranges from 40 to more than 60 inches in
             Nakina soils are associated on the landscape with               thickness.
          Brookman, Lynn Haven, Grifton, Ogeechee, Mouzon,                      The A horizon has hue of 10YR, value of 2 or 3, and
          Elloree, and Yemassee soils. Brookman and Lynn Haven               chroma of 1 or 2. It commonly is fine sandy loam but is
          soils are in positions similar to those of the Nakina soils.       loamy fine sand in some pedons.
          Brookman soils have a clayE@y particle-size control                   The E horizon has hue of 1 OYR, value of 4 to 7, and
          section. Lynn Haven soils are sandy throughout and are             chroma of 1 or 2. It is loamy fine sand or fine sandy
          Spodosols. Grifton, OgeechE.@e, Mouzon, and Elloree soils          loam.
          are slightly higher on the landscape and have an ochric               The Btg horizon has hue of 1 OYR to 5Y, value of 4 to
          epipedon. Elloree soils are in an arenic subgroup.                 6, and chroma of 1 or 2. It has mottles in shades of
          Yemassee soils are higher on the landscape and are in              brown or yellow. This horizon is fine sandy loam, sandy
          an aeric subgroup.                                                 clay loam, or clay loam. Some pedons have strata of
             Typical pedon of Nakina fine sandy loam; about 9                variable textures in the lower part of the Btg horizon.
          miles southeast of Summerville, about 0.7 mile northeast              The Cg horizon has hue of 1 OYR to 5Y, value of 4 to
          of junction of South Carolina Highway 642 and Ashley               7, and chroma of 1 or 2. It has mottles in shades of
          Phosphate Road (South Carolina Highway 62), about 0.5              brown or yellow. This horizon is stratified with variable
          mile northwest on housing subdivision road, and 200 feet           textures.
          west of 90 degree curve of road.
          A-0 to 11 inches; black (1 OYR 2/ 1) fine sandy loam;              Noboco Series
               few streaks of dark gray along root channels; weak               The Noboco series consists of soils that formed in
               fine subangular blocky structure; very friable;               loamy marine sediment on nearly level upland terraces.
               common fine and few medium roots; very strongly               Slopes are 0 to 2 percent. These soils are fine-loamy,
               acid; clear smooth boundary.                                  siliceous, thermic Typic Paleudults.
          E-1 1 to 18 inches; dark gray (I OYR 4/ 1) fine sandy                 Noboco soils are associated on the landscape with
               loam; weak fine subangular blocky structure; very             Blanton, Bonneau, Daleville, Goldsboro, Izagora,
               friable; few fine roots and pores; very strongly acid;        Jedburg, Lynchburg, and Rains soils. Blanton and
               clear wavy boundary.                                          Bonneau soils are in positions similar to those of the
          Btg1-18 to 37 inches; gray (10YR 5/1) sandy clay                   Noboco soils. Blanton soils are in a grossarenic
               loam; common medium distinct brownish yellow                  subgroup. Bonneau soils are in an arenic subgroup.
               (10YR 6/6) mottles and common medium faint dark               Goldsboro and Izagora soils are slightly lower on the
               gray (10YR 4/1) mottles; moderate medium                      landscape and have mottles with chroma of 2 or less
               subangular blocky structure; friable; very few faint          within 30 inches of the surface. Daleville, Jedburg,
               clay films on faces of peds; few fine roots and               Lynchburg, and Rains soils are lower on the landscape.
               pores; very strongly acid; gradual wavy boundary.             Jedburg and Lynchburg soils are in an aeric subgroup.
          Btg2-37 to 45 inches; gray (10YR 5/1) sandy clay                   Daleville and Rains soils are Aquults.
               loam; pockets of sandy clay; common medium                       Typical pedon of Noboco loamy sand, 0 to 2 percent
               distinct strong brown (7.5YR 5/8) mottles; moderate           slopes; about 2.25 miles south of Reevesville on South
               medium subangular blocky structure; friable; few              Carolina Highway 16, about 0.5 mile east on county dirt
               faint clay films on faces of peds; few fine roots and         road, 50 feet south of power pole, in planted pine.
               pores; very strongly acid; gradual wavy boundary.
          BCg-45 to 61 inches; gray (10YR 5/1) clay loam; strata             Ap-O to 6 inches; dark grayish brown (10YR 4/2) loamy
               of sandy clay loam; cornmon coarse distinct strong                 sand; weak fine granular structure; very friable;
               brown (7.5YR 5/8) moUles; weak medium                              many fine and few medium roots; medium acid;
               subangular blocky structure; firm; few fine roots and              clear wavy boundary.
               pores; very strongly acid; gradual wavy boundary.             E-6 to 14 inches; light yellowish brown (10YR 6/4)
          Cgl-61 to 70 inches; dark, gray (10YR 4/1) sandy clay                   loamy sand; common streaks of dark gray (1 OYR
               loam; strata of sandy clay; common coarse distinct                 4/1) loamy sand along old root channels; weak fine
               strong brown (7.5YR 5/8) mottles and common                        granular structure; very friable; common fine roots;
               medium distinct light gray (5Y 7/2) mottles; massive;              few fine tubular pores; medium acid; clear smooth
               firm; medium acid; gradual wavy boundary.                          boundary.








       Dorchester County, South Carolina                                                                                                 79



       131:1-14 to 40 inches; yellowish brown (10YR 5/6) sandy             Echaw, Goldsboro, and Foreston soils are slightly higher
           clay loam; few medium distinct yellowish red (5YR               on the landscape than the Ocilla soils. Albany soils are
           5/8) mottles; weak medium subangular blocky                     in a grossarenic subgroup. Echaw soils are Spoclosols.
           structure; friable; few faint clay films along old root         Goldsboro soils are not in an arenic subgroup. Foreston
           channels and on faces of peds; few fine roots; few              soils have a coarse-loamy particle-size control section.
           fine tubular pores; strongly acid; gradual smooth               Blanton, Bonneau, and Foxworth soils are higher on the
           boundary.                                                       landscape. Blanton soils are in a grossarenic subgroup.
       Bt2-40 to 61 inches; yellowish brown (10YR 5/6) sandy               Bonneau soils do not have gray mottles within 36 inches
           clay loam; common medium distinct gray (11 OYR 6/ 1)            of the surface. Foxworth soils are Entisols. Osier and
           mottles and few medium distinct yellowish red (5YR              Pelham soils are lower on the landscape, and they have
           5/8) mottles; weak medium subangular blocky                     dominant chroma of 2 or less throughout the profile.
           structure; friable; few distinct clay films on faces of         Osier soils are Entisols.
           peds; few fine roots; few fine tubular pores; very                Typical pedon of Ocilla sand, 0 to 2 percent slopes;
           strongly acid; gradual wavy boundary.                           about 2.5 miles northwest of Rosinville, about 1 mile
       Bt3-61 to 70 inches; mottled yellowish brown (10YR                  north of the junction of South Carolina Highway 11 and
           5/8), gray (10YR 6/1), and red (2.5YR 4/8) sandy                South Carolina Highway 337, about 700 feet southeast
           clay loam; thin strata of loamy sand; weak medium               of South Carolina Highway 337 along frontage road by
           subangular blocky structure; friable; few distinct clay         Interstate Highway 26, and 150 feet south of frontage
           films on faces of peds; very strongly acid; gradual             road.
           wavy boundary.
       BCg-70 to 80 inches; gray (11 OYR 6/ 1) sandy clay loam;            A-0 to 6 inches; dark grayish brown (1 OYR 4/2) sand;
           thin strata of loamy sand; many medium prominent                     single grained; loose; many fine and common
           red (10R 4/8) mottles and common medium distinct                     medium roots; very strongly acid; clear wavy
           brownish yellow (1 OYR 6/8) mottles; weak medium                     boundary.
           subangular blocky structure; firm; very strongly acid.          E1-6 to 10 inches; yellowish brown (10YR 5/4) loamy
                                                                                sand; weak fine granular structure; loose; common
         The solum ranges from 60 to more than 80 inches in                     fine roots; strongly acid; gradual wavy boundary.
       thickness. Less than 5 percent of plinthite and iron                E2-110 to 23 inches; brownish yellow (10YR 6/6) loamy
       nodules are in the lower part of the subsoil in some                     sand; common medium distinct pale brown (10YR
       pedons.                                                                  6/3) mottles; weak fine granular structure; loose;
         The A horizon has hue of 10YR, value of 4 to 6, and                    common fine roots; few fine pores; strongly acid;
       chroma of 2 to 6. Some pedons have few uncoated sand                     gradual wavy boundary.
       grains. This horizon commonly is loamy sand but is sand,            Btl-23 to 31 inches; yellowish brown (10YR 5/8) sandy
       loamy fine sand, or sandy loam in some peclons.                          loam; common medium distinct gray (11 OYR 6/ 1) and
         The E horizon has hue of 10YR, value of 5 to 7, and                    yellowish red (5YR 5/8) mottles; weak medium
       chroma of 3 to 6. Some peclons have few uncoated sand                    subangular blocky structure; friable; very few faint
       grains. This horizon is sand, loamy sand, loamy fine                     clay films on faces of peds; common fine roots; few
       sand, or sandy loam.                                                     fine pores; very strongly acid; gradual wavy
         The Bt horizon has hue of 7.5YR or 10YR, value of 5                    boundary.
       to 7, and chroma of 6 or 8. Mottles are in shades of                Bt2-311 to 52 inches; yellowish brown (10YR 5/8) sandy
       brown, yellow, or red. The lower part of the Bt horizon
       has gray mottles. The Bt horizon is sandy clay loam or                   loam; many medium distinct gray (10YR 6/1) and
       clay loam. Some peclons are sandy clay in the lower part                 red (2.5YR 4/8) mottles; weak medium subangular
       of the Bt horizon.                                                       blocky structure; friable; very few faint clay films on
         The BCg horizon has hue of 1 OYR, value of 5 to 7,                     faces of peds; very strongly acid; gradual wavy
       and chroma of 1 or 2. It has mottles in shades of brown,                 boundary.
       yellow, or red. This horizon is sandy clay loam or sandy            Btg-52 to 65 inches; gray (10YR 6/1) sandy loam;
       clay. Most peclons have strata of loamy sand and sand.                   many medium distinct brownish yellow (10YR 6/6)
                                                                                mottles and few medium distinct yellowish red (5YR
       Ocilla Series                                                            5/8) mottles; moderate medium subangular blocky
                                                                                structure; friable; very few faint clay films on faces of
         The Ocilla series consists of soils that formed in sandy               peds; very strongly acid; gradual wavy boundary.
       and loamy marine sediments on upland terraces. Slopes               BCg-65 to 80 inches; light gray (10YR 7/1) sandy loam;
       are 0 to 2 percent. These soils are loamy, siliceous,                    strata of loamy sand; common medium distinct
       thermic Aquic Arenic Paleudults.                                         brownish yellow (10YR 6/6) mottles and few
         Ocilla soils are associated on the landscape with                      medium distinct yellowish red (5YR 5/8) mottles;
       Albany, Blanton, Bonneau, Echaw, Foxworth, Goldsboro,                    weak fine subangular blocky structure; very strongly
       Foreston, Osier, Pelham, and Rains soils. Albany,                        acid.








          80                                                                                                                  Soil Survey



             The solum ranges from 60 to more than 80 inches in                  medium roots; very few faint clay films on faces of
          thickness.                                                             peds; very strongly acid; gradual wavy boundary.
             The A horizon has hue of I OYR, value of 3 to 5, and            BCg-36 to 57 inches; gray (10YR 5/1) sandy clay loam;
          chroma of 1 or 2. It commonly is sand but is loamy sand                common coarse distinct yellowish brown (10YR 5/8)
          or loamy fine sand in some pedons.                                     mottles; stratified with pockets of light gray (10YR
             The E horizon has hue of 'I OYR, value of 5 to 7, and               7/1) sand; weak medium subangular blocky
          chroma of 3 to 6. It has mottles in shades of brown,                   structure; friable; very strongly acid; clear wavy
          yellow, or gray. This horizon is sand, loamy sand, or                  boundary.
          loamy fine sand.                                                   2Cg-57 to 65 inches; gray (10YR 6/1) fine sand; few
             The Bt horizon has hue of 1 OYR, value of 5 to 7, and               fine distinct yellowish brown (10YR 5/6) mottles;
          chroma of 3 to 8. It has motiles in shades of red, brown,              massive; very friable; few coatings on sand grains;
          yellow, or gray. This horizon is sandy loam or sandy clay              strongly acid.
          loam.
             The Btg horizon has hue of 1 OYR, value of 5 to 7, and            The solum ranges from 40 to 60 inches in thickness.
          chroma of 1 or 2. It has mottles in shades of red, brown,            The A horizon has hue of 1 OYR, value of 3 or 4, and
          or yellow. This horizon is sandy clay loam or sandy loam.
             The BCg horizon has hue of 1 OYR, value of 5 to 7,              chroma of 1 or 2. It commonly is fine sandy loam but is
          and chroma of 1 or 2. It has mottles in shades of red,             sandy loam, loamy fine sand, or loamy sand in some
          brown, or yellow. This horizon is sandy clay loam or               pedons.
          sandy loam. Most pedons have strata of loamy sand.                   The E horizon has hue of 1 OYR, value of 5 or 6, and
                                                                             chroma of 1 or 2. It has mottles in shades of brown or
          Ogeechee Series                                                    yellow. This horizon is fine sandy loam, sandy loam, or
                                                                             loamy fine sand.
             The Ogeechee series consists of soils that formed in              The Btg horizon has hue of 1 OYR, value of 4 to 6, and
          loamy marine sediment on nearly level stream terraces              chroma of 1 or 2. It has mottles in shades of red, brown,
          at an elevation of less than 42 feet above sea level.              yellow, or gray. It is sandy clay loam or clay loam.
          Slopes are 0 to 2 percent. These soils are fine-loamy,               The BCg horizon has hue of 1 OYR, value of 4 to 7,
          siliceous, thermic Typic Ochiraquults.                             and chroma of 1 or 2. It has mottles in shades of red,
             Ogeechee soils are associated on the landscape with             brown, yellow, or gray. This horizon is sandy clay loam or
          Nakina, Elloree, Grifton, Yauhannah, and Yemassee                  sandy loam. Some pedons are stratified sandy clay loam,
          soils. Nakina soils are lower on the landscape than the
          Ogeechee soils and have an umbric epipedon. Elloree                sandy loam, and sand.
          and Grifton soils are in positions similar to those of the           The C or 2C horizon has hue of 10YR, value of 5 to 7,
          Ogeechee soils. Elloree soils are in an arenic subgroup,           and chroma of 1 or 2. It has mottles in shades of red,
          and Grifton soils are Alfisols. Yauhannah and Yemassee             brown, yellow, or gray. This horizon is fine sand, sand, or
          soils are higher on the landscape and have dominant                loamy sand. Some pedons are stratified with variable
          chroma of 3 or more in the subsurface layer or the upper           textures.
          part of the subsoil.
             Typical pedon of Ogeechee fine sandy loam; about 2.8            Osier Series
          miles southwest of Ridgeville, southwest of Four Hole
          Swamp bridge on South Carolina Highway 56, 200 feet                  The Osier series consists of soils that formed in thick,
          east of Four Hole Swamp stream and 50 feet north of                sandy sediment in depressional areas and on lowlands
          road in woodland.                                                  near streams. Slopes are 0 to 2 percent. These soils are
                                                                             siliceous, thermic Typic Psammaquents.
          A-0 to 4 inches; very dark gray (10YR 3/1) fine sandy                Osier soils are associated on the landscape with
               loam; weak fine granular structure; very friable;             Albany, Chipley, Plummer, and Rutlege soils. Albany and
               many fine roots; strongly acid; clear smooth                  Chipley soils are higher on the landscape and have
               boundary.
          E-4 to 12 inches; gray (10'YR 6/1) fine sandy loam;                dominant chroma of 3 or more in the upper part of the
               common fine distinct brownish yellow (10YR 6/6)               profile. Plummer soils are in positions similar to those of
               mottles; weak fine granular structure; very friable;          the Osier soils. Albany and Plummer soils are Ultisols.
               common fine and medium roots; strongly acid;                  Rutlege soils are lower on the landscape and have an
               gradual wavy boundary.                                        umbric epipedon.
          Btg-12 to 36 inches; gray (10YR 6/1) sandy clay loam;                Typical pedon of Osier loamy fine sand, frequently
               common medium distinct yellowish brown (10YR                  flooded; about 4 miles southeast of Harleyville, 1,300
               5/6) mottles and few fine prominent yellowish red             feet north of the junction of South Carolina Highway 139
               (5YR 5/8) mottles; weak fine and medium                       and U.S. Highway 178, and 60 feet east of South
               subangular blocky structure; friable; few fine and            Carolina Highway 139.








        Dorchester County, South Carolina                                                                                               81



        A-0 to 3 inches; very dark grayish brown (1 OYR 3/2)                Btg1-18 to 37 inches; gray (10YR 5/1) sandy clay
            loamy fine sand; common medium distinct grayish                      loam; common medium distinct yellowish brown
            brown (10YR 5/2) mottles; weak medium granular                       (10YR 5/8) mottles; moderate medium subangular
            structure; very friable; common fine and few medium                  blocky structure; slightly sticky; very few faint clay
            roots; strongly acid; clear smooth boundary.                         films on faces of peds; common fine and few
        Cgl-3 to 26 inches; light gray (10YR 7/2) fine sand;                     medium roots; extremely acid; gradual wavy
            common medium distinct dark brown (1 OYR 4/3)                        boundary.
            streaks; single grained; loose; thin strata of loamy            Btg2-37 to 74 inches; gray (1 OYR 5/ 1) sandy clay; few
            sand; medium acid; gradual wavy boundary.                            medium distinct brownish yellow (10YR 6/8) mottles;
        Cg2-26 to 53 inches; light brownish gray (10YR 6/2)                      strong medium subangular blocky structure; firm; few
            fine sand; single grained; loose; strongly acid;                     faint clay films on faces of peds; few fine roots;
            gradual wavy boundary.                                               extremely acid; gradual wavy boundary.
        Cg3-53 to 80 inches; grayish brown (10YR 5/2) sand;                 BCg-74 to 80 inches; gray (1 OYR 5/ 1) sandy clay loam;
            single grained; loose; common uncoated sand                          few medium distinct brownish yellow (10YR 6/6)
            grains; strongly acid.                                               and light gray (10YR 7/2) mottles; weak medium
          The Osier soils are sandy to a depth of more than 80                   subangular blocky structure; firm; extremely acid.
        inches.                                                               The solum ranges from 60 to more than 80 inches in
          The A horizon has hue of 1 OYR or 2.5Y, value of 2 to             thickness.
        5, and chroma of 1 or 2. It commonly is loamy fine sand
        but is sand or fine sand in some pedons.                              The A horizon has hue of 1 OYR, value of 2 or 3, and
          The C horizon has hue of 1 OYR or 2.5Y, value of 3 to             chroma of 1 or 2. It commonly is sandy loam but is fine
        8, and chroma of 1 or 2, or it is neutral and has value of          sandy loam or loam in some peclons.
        3 to 8. Mottles range from none to many in shades of                  The E horizon has hue of 10YR, value of 4 to 6, and
        brown, yellow, or gray. This horizon is fine sand or sand.          chroma of 1 or 2. Some pedons have mottles of darker
        Some pedons have thin strata of material ranging from               color surface material. This horizon is loamy sand, loamy
        sand to sandy loam.                                                 fine sand, fine sandy loam, or sandy loam.
                                                                              The Btg horizon has hue of 1 OYR, value of 4 to 6, and
        Pantego Series                                                      chroma of 1 or 2. Some pedons have mottles in shades
                                                                            of brown or yellow. This horizon commonly is sandy clay
          The Pantego series consists of soils that formed in               loam but ranges to sandy clay in the lower part.
        loamy marine sediment in depressional areas on upland                 The BCg horizon has hue of 1 OYR, value of 5 to 7,
        terraces. Slopes are 0 to 2 percent. These soils are fine-          and chroma of 1 or 2. It has mottles in shades of brown,
        loamy, siliceous, thermic Umbric Paleaquults.                       yellow, or gray. This horizon is sandy loam, sandy clay
          Pantego soils are associated on the landscape with                loam, or sandy clay; or it is stratified with these textures.
        Coxville, Goldsboro, Lynchburg, Pelham, and Rains soils.
        These soils are higher on the landscape than the
        Pantego soils and do not have an umbric epipedon.                   Pelham Series
        Pelham soils are in an arenic subgroup. Coxville soils                The Pelham series consists of soils that formed in
        have more than 35 percent clay in the control section.              loamy marine sediment in nearly level depressions and
          Typical peclon of Pantego sandy loam; about 3 miles               drainageways. Slopes are 0 to 2 percent. These soils are
        north of the intersection of U.S. Highway 78 and South              loamy, siliceous, thermic Arenic Paleaquults.
        Carolina Highway 16 in Reevesville, about 0.5 mile west               Pelham soils are associated on the landscape with
        on South Carolina Highway 472, about 0.75 mile north                Albany, Lynchburg, Ocilla, Osier, Plummer, and Rains
        on unimproved county road, about 0.25 mile east on
        unimproved county road, 400 feet northwest of road                  soils. Albany, Lynchburg, and Ocilla soils are higher on
        along power line right-of-way, and 100 feet north of                the landscape than the Pelham soils and have chroma
        power line right-of-way.                                            of 3 or more in the upper part of the profile. Albany soils
                                                                            are in a grossarenic subgroup. Lynchburg soils are in an
        A-0 to 12 inches; black (10YR 2/1) sandy loam; weak                 aeric subgroup. Osier and Plummer soils are in positions
            medium subangular blocky structure; very friable;               similar to those of the Pelham soils. Osier soils are
            many fine and common medium roots; extremely                    Entisols. Plummer soils are in a grossarenic subgroup.
            acid; clear smooth boundary.                                    Rains soils are slightly lower on the landscape and are
        E-12 to 18 inches; light brownish gray (10YR 6/2)                   not in an arenic subgroup.
            loamy sand; common medium distinct dark gray                      Typical pedon of Pelham sand; about 3.6 miles north
            (1 OYR 4/ 1) mottles; single grained; very friable;             of St. George; 5,700 feet north of the junction of South
            common fine roots; weakly cemented; strongly acid;              Carolina Highway 54 and South Carolina Highway 73,
            clear wavy boundary.                                            and 45 feet east of center of South Carolina Highway 54.








           82                                                                                                                        Soil Survey



           A-0 to 7 inches; very dark gray (10YR 3/1) sand; weak                 drainageways and depressions. Slopes are 0 to 2
                fine granular structure; very friable; many fine and             percent. These soils are loamy, siliceous, thermic
                common medium roots; very strongly acid; clear                   Grossarenic Paleaquults.
                smooth boundary.                                                    Plummer soils are associated on the landscape with
           E1-7 to 14 inches; gray (10YR 6/1) sand; common fine                  Albany, Chipley, Osier, Pelham, and Rutlege soils.
                streaks of dark gray (1 OY R 4/ 1) fine sand mostly              Albany and Chipley soils are higher on the landscape
                along old root channels; single grained; loose; few              than the Plummer soils and have matrix colors with
                fine roots; strongly acid; gradual wavy boundary.                chroma of 3 or more in the upper part of the profile.
           E2-14 to 22 inches; light brownish gray (10YR 6/2)                    Chipley soils are Entisols. Osier and Pelham soils are in
                loamy sand; common medium moderately cemented                    positions similar to those of the Plummer soils. Osier
                bodies with dominantly yellowish red centers;                    soils are Entisols, and Pelham soils are in an arenic
                common medium faint dark grayish brown (1 OYR                    subgroup. Rutlege soils are lower on the landscape and
                4/2) mottles; weak medium subangular blocky                      have an umbric epipedon.
                structure; very friable; strongly acid; gradual wavy                Typical pedon of Plummer loamy sand; about 2 miles
                boundary.                                                        southwest of Dorchester, about 1 mile south of South
           E3-22 to 35 inches; light brownish gray (10YR 6/2)                    Carolina Highway 247 on South Carolina Highway 246,
                loamy sand; many medium faint pale brown (10YR                   about 1 000 feet southwest on road in woodland, and
                6/3) mottles and few fine distinct brownish yellow               250 feei northwest of the junction with another road.
                (10YR 6/6) mottles; weak medium subangular
                blocky structure; very friable; strongly acid; gradual           A-0 to 9 inches; very dark gray (10YR 3/1) loamy sand;
                wavy boundary.                                                        weak fine granular structure; very friable; common
           Btg-35 to 62 inches; light gray (10YR 7/1) sandy loam;                     fine roots; very strongly acid; abrupt smooth
                many medium distinct brownish yellow (10YR 6/6)                       boundary.
                mottles and common medium distinct strong brown                  E1-9 to 24 inches; gray (10YR 5/1) sand; common
                (7.5YR 5/6) mottles; moderate medium subangular                       medium faint grayish brown (10YR 5/2) mottles and
                blocky structure; firm; few fine distinct lenses of                   common medium distinct light yellowish brown
                white (10YR 8/1) uncoated sand grains; very                           (10YR 6/4) mottles; single grained; loose; few fine
                strongly acid; gradual wavy boundary.                                 roots; strongly acid; clear wavy boundary.
           BCg-62 to 80 inches; light gray (10YR 7/1) sandy clay                 E2-24 to 45 inches; light gray (10YR 7/1) sand; single
                loam; many medium distinct light yellowish brown                      grained; loose; strongly acid; gradual wavy
                (10YR 6/4) mottles and common medium distinct                         boundary.
                brownish yellow (10YR 6/6) mottles; moderate                     113-45 to 58 inches; grayish brown (10YR 5/2) sand;
                medium subangular blocky structure; firm; weakly                      many coarse distinct light gray (1 OYR 7/2) mottles;
                stratified; very strongly acid.                                       single grained; loose; very strongly acid; gradual
              The solum ranges from 60 to more than 80 inches in                      wavy boundary.
           thickness.                                                            Btg-58 to 75 inches; light gray (10YR 7/1) sandy loam;
              The A horizon has hue of 1 OYR to 5Y, value of 2 to 4                   weak fine subangular blocky structure; very friable;
           and chroma of 1 or 2. It commonly is sand but is loamy'                    sand grains bridged with clay; very strongly acid.
           .sand in some pedons.                                                    The solum ranges from 65 to more than 80 inches in
              The E horizon has hue of 10YR to 5Y, value of 5 to 7,              thickness.
           and chroma of 1 or 2. Most pedons have mottles in                        The A horizon has hue of 10YR, value of 2 to 4, and
           shades of red, brown, yellow, or gray. This horizon is                chroma of 1 or 2. It commonly is loamy sand but is
           sand or loamy sand.                                                   loamy fine sand in some pedons.
              The Btg horizon has hue of 1 OYR to 5Y, value of 4 to                 The E horizon has hue of 10YR, value of 5 to 7, and
           7, and chroma of 1 or 2; or it is neutral and has value of            chroma of 1 or 2. Some pedons have mottles in shades
           4 to 7. Mottles in shades of red, brown, or yellow are few            of brown or yellow. This horizon is sand or loamy sand.
           to many. This horizon is sandy loam or sandy clay loam.                  The Btg horizon has hue of 10YR, value of 5 to 7, and
              The BCg horizon has hue of 1 OYR, value of 4 to 7,                 chroma of 1 or 2. Some pedons have mottles in shades
           and chroma of 1 or 2. Mottles in shades of red, yellow,               of brown or yellow. This horizon is sandy loam, fine
           brown, or gray are in most pedons. This horizon is sandy              sandy loam, or sandy clay loam.
           clay loam. Most pedons have strata of sand or loamy
           sand in this horizon.
                                                                                 Rains Series
           Plummer Series                                                           The Rains series consists of soils that formed in loamy
              The Plummer series consists of soils that formed in                marine sediment on broad flats and in nearly level
           sandy and loamy marine Sediment in nearly level                       depressions and drainageways. Slopes are 0 to 2








       Dorchester County, South Carolina                                                                                                 83



       percent. These soils are fine-loamy, siliceous, thermic               The E horizon has hue of 1 OYR, value of 4 to 6, and
       Typic Paleaquults.                                                  chroma of 1 or 2. It has mottles in shades of brown and
         Rains soils are associated on the landscape with                  gray. This horizon is loamy fine sand, sandy loam, or fine
       .Coxville, Goldsboro, Lynchburg, Pantego, Pelham, and               sandy loam.
       Grifton soils. Coxville soils have a clayey particle-size             The Btg horizon has hue of 1 OYR, value of 4 to 7, and
       control section. Goldsboro soils are higher on the                  chroma of 1 or 2. It has mottles in shades of red, yellow,
       landscape than the Rains soils and are Udults.                      brown, or gray. This horizon is sandy clay loam with
       Lynchburg soils are slightly higher on the landscape and            strata of sandy loam or sandy clay in the lower part.
       are in an aeric subgroup. Pantego soils are lower on the
       landscape and have an umbric epipedon. Pelham soils                 Rutlege Series
       are in an arenic subgroup. Grifton soils are Alfisols.
         Typical peclon of Rains sandy loam; about 2 miles                   The Rutlege series consists of soils that formed in
       northwest of St. George, about 1.3 miles northwest of               thick, sandy marine sediment in nearly level
       the junction of South Carolina Highway 119 and South                drainageways of small streams and swamps. Slopes are
       Carolina Highway 39, and 100 feet east of South                     0 to 2 percent. These soils are sandy, siliceous, thermic
       Carolina Highway 39.                                                Typic Humaquepts.
                                                                             Rutlege soils are associated on the landscape with
       A-0 to 4 inches; very dark gray (10YR 3/1) sandy loam;              Albany, Blanton, Lynn Haven, Ocilla, Osier, and Plummer
            weak medium subangular blocky structure; very                  soils. Albany, Blanton, and Ocilla soils are higher on the
            friable; many fine and medium roots and few large              landscape than the Rutlege soils. Albany and Blanton
            roots; very strongly acid; clear smooth boundary.              soils are in a grossarenic subgroup. Ocilla soils are in an
       E-4 to 9 inches; gray (1 OYR 6/ 1) sandy loam; common               arenic subgroup. Lynn Haven soils are in positions
            medium distinct dark brown (10YR 3/3) mottles                  similar to those of the Rutlege soils and are Spodosols.
            along old root channels; weak medium subangular                Osier and Plummer soils are slightly higher on the
            blocky structure; very friable; common fine roots and          landscape and do not have an umbric epipeclon.
            few medium roots; few fine pores; very strongly acid;          Plummer soils are in a grossarenic subgroup.
            clear wavy boundary.                                             Typical pedon of Rutlege loamy fine sand, frequently
       Btg1-9 to 17 inches; gray (10YR 6/1) sandy clay loam;               flooded; about 1.3 miles south of Dorchester on South
            common medium distinct brownish yellow (10YR                   Carolina Highway 23 and 200 feet east of the highway in
            6/8) mottles; moderate medium subangular blocky                Halfway Gut Creek.
            structure; friable; very few faint clay films on faces of
            peds; few fine roots; few fine pores; very strongly            A1-0 to 13 inches; very dark gray (10YR 3/1) loamy
            acid; gradual wavy boundary.                                        fine sand; weak fine granular structure; very friable;
       Btg2-17 to 42 inches; gray (10YR 6/1) sandy clay                         common fine and few medium roots; very strongly
            loam; common medium distinct brownish yellow                        acid; gradual smooth boundary.
            (10YR 6/8) and yellowish red (5YR 5/8) mottles;                A2-13 to 21 inches; dark gray (1 OYR 4/ 1) loamy fine
            moderate medium subangular blocky structure;                        sand; single grained; loose; few fine roots; very
            friable; very few faint clay films on faces of peds;                strongly acid; clear smooth boundary.
            few fine roots; few fine pores; very strongly acid;            Cgl -21 to 34 inches; light brownish gray (1 OYR 6/2)
            gradual wavy boundary.                                              fine sand; few streaks of dark gray (10YR 4/1)
       Btg3-42 to 56 inches; gray (10YR 5/1) clay loam; strata                  along old root channels; single grained; loose;
            of sandy clay; common medium distinct brownish                      strongly acid; gradual smooth boundary.
            yellow (10YR 6/8), yellowish red (5YR 5/8), and                Cg2-34 to 44 inches; light gray (1 OYR 7/2) fine sand;
            brown (7.5YR 4/2) mottles; strong medium                            single grained; loose; strongly acid; gradual wavy
            subangular blocky structure; firm; few faint clay films             boundary.
            on faces of peds; few fine pores; very strongly acid;          Cg3-44 to 65 inches; light gray (10YR 7/2) fine sand;
            gradual wavy boundary.                                              single grained; loose; strongly acid; gradual wavy
       BCg-56 to 80 inches; gray (1 OYR 5/ 1) sandy clay loam;                  boundary.
            strata of sandy loam; common medium distinct red               Cg4-65 to 75 inches; grayish brown (10YR 5/2) sand;
            (2.5YR 4/8) and brownish yellow (10YR 6/8)                          single grained; loose; few small pebbles; strongly
            mottles; strong medium subangular blocky structure;                 acid.
            firm; very strongly acid.                                        The Rutlege soils are sand to a depth of 60 to 80
         The solum ranges from 60 to 80 inches in thickness.               inches. Small pebbles are in the lower part of the C
         The A horizon has hue of 1 OYR, value of 2 or 3, and              horizon in most pedons.
       chroma of 1 or 2. it commonly is sandy loam but is                    The upper part of the A horizon has hue of 10YR,
       loamy fine sand or fine sandy loam in some pedons.                  value of 2 or 3, and chroma of 1 or 2. The lower part








           84                                                                                                                    Soil Survey



           has hue of 1 OYR, value of 4, and chroma of 1 or 2. The                 5/8) and light yellowish brown (1 OYR 6/4) mottles
           A horizon commonly is loamy fine sand but is loamy                      and few medium distinct strong brown (7.5YR 5/8)
           sand in some pedons.                                                    mottles; weak medium subangular blocky structure;
             The Cg horizon has hue of 1 OYR, value of 5 to 7, and                 friable; very few faint clay films on faces of peds;
           chroma of 1 or 2. It is sand, fine sand, or loamy sand.                 few fine roots; few fine pores; very strongly acid;
                                                                                   gradual wavy boundary.
           Seagate Series                                                     Btg2-50 to 79 inches; gray (10YR 6/1) fine sandy loam;
                                                                                   few fine distinct brownish yellow (10YR 6/8) mottles
             The Seagate series consists of soils that formed in                   and few medium distinct light yellowish brown (1 OYR
           sandy and loamy marine sediments on nearly level                        6/4) mottles; moderate medium subangular blocky
           stream terraces throughout the county. Slopes are 0 to 2                structure; friable; very few faint clay films on faces of
           percent. These soils are sandy over loamy, siliceous,                   peds; few fine roots; few fine pores; very strongly
           thermic Ultic Haplohumods.                                              acid.
             The Seagate soils in this survey area are a taxadjunct
           to the Seagate series because they have more than 50                  Depth to the argillic horizon ranges from 20 to 40
           percent fine or coarser sand in the argillic horizon and           inches.
           are dominantly gray in the upper part of the Bt horizon.              The A horizon has hue of 10YR, value of 2 to 4, and
           These differences do not significantly alter the use and           chroma of 1 or 2. It commonly is sand but is fine sand or
           behavior of these soils.                                           loamy sand in some pedons.
             Seagate soils are associalled on the landscape with                 The E horizon has hue of 10YR, value to 5 to 7, and
           Chipley, Echaw, Leon, Lynchburg, Ocilla, and Pelham                chroma of 1 or 2. Most pedons have streaks or mottles
           soils. Chipley and Echaw soils are higher on the                   in shades of brown or gray. This horizon is sand or fine
           landscape than the Seagate soils and are sandy                     sand.
           throughout. Echaw soils have a Bh horizon 30 to 50                    The Bh horizon has hue of 5YR to I OYR, value of 2 or
           inches below the surface. Leon and Pelham soils are                3, and chroma of 1 to 3. Most pedons have streaks or
           lower on the landscape. Leon soils are sandy                       mottles in shades of brown or gray. This horizon is sand,
           throughout, and Pelham soils are Aquults. Lynchburg and            fine sand, or loamy fine sand.
           Ocilla soils are in positions similar to those of the                 The secondary E horizon has hue of 1 OYR, value of 5
           Seagate soils and are Ultisols.                                    to 7, and chroma of 2 to 6. It has mottles in shades of
             Typical pedon of Seagate sand; about 0.75 mile                   brown, yellow, or gray. This horizon is sand, fine sand, or
           northeast of overpass bridge at the intersection of U.S.           loamy fine sand.
           Interstate 26 and U.S. Highway 15, about 400 feet north               The Btg horizon has hue of 1 OYR, value of 5 to 7, and
           on paper company dirt road,, about 0.25 mile northwest             chroma of 1 or 2. Most pedons have mottles in shades
           on road in woodland, and 100 feet southwest of road.               of brown, yellow, or gray. This horizon is sandy clay
           A-0 to 6 inches; black (10YR 2/1) sand; weak fine                  loam, sandy loam, or fine sandy loam.
               granular structure; very friable; many fine and
               medium roots and few large roots; very strongly                Wahee Series
               acid; clear smooth boundary.
           E-6 to 14 inches; gray (1 OYR 5/ 1) sand; common                      The Wahee series consists of soils that formed in
               streaks of very dark gray (10YR 3/1) sand; single              clayey marine sediment on broad, nearly level, low
               grained; very friable; few fine roots; very strongly           stream terraces at an elevation of less than about 42
               acid; abrupt wavy boundary.                                    feet above sea level. Slopes are 0 to 2 percent. These
           Bh-14 to 18 inches; dark reddish brown (5YR 3/2)                   soils are clayey, mixed, thermic Aeric Ochraquults.
               loamy sand; small streaks of gray (10YR 5/1) and                  Wahee soils are associated on the landscape with
               light yellowish brown (I OYR 6/4) sand in old root             Brookman, Eulonia, Mouzon, Ogeechee, and Yemassee
               channels; structureless; friable, weakly cemented;             soils. Brookman soils are lower on the landscape than
               few fine roots; very strongly acid; abrupt wavy                the Wahee soils and have an umbric epipedon. Eulonia
               boundary.                                                      soils are higher on the landscape and are Udults.
           F-18 to 32 inches; yellow (10YR 7/6) sand; common                  Mouzon and Ogeechee soils are slightly lower on the
               medium distinct brownish yellow (10YR 6/8) and                 landscape, have a dominant matrix with chroma of 2 or
               light yellowish brown ("I OYR 6/4) mottles and few             less, and have a fine-loamy control section. Yemassee
               medium distinct strong brown (7.5YR 5/8) mottles;              soils are in positions similar to those of the Wahee soils
               single grained; very friable; few fine roots; few              and have a fine-loamy control section.
               weakly cemented nodules; strongly acid; clear wavy                Typical pedon of Wahee fine sandy loam; about 13
               boundary.                                                      miles southwest of Summerville at the intersection of
           Btg1-32 to 50 inches; gray (10YR 6/1) fine sandy loam;             South Carolina Highway 165 and South Carolina
               common medium distinct yellowish brown (10YR                   Highway 317, about 7.2 miles east of South Carolina









       Dorchester County, South Carolina                                                                                             85



       Highway 317, 800 feet north on paper company                        The E horizon has hue of 1 OYR or 2.5Y, value of 5 to
       unimproved road, and 150 feet west of road.                       7, and chroma of 3 or 4. Mottles in shades of brown,
                                                                         yellow, and gray are in most pedons. This horizon is fine
       Ap-O to 6 inches; dark grayish brown (10YR 4/2) fine              sandy loam.
           sandy loam; weak fine granular structure; very                  The Bt horizon has hue of 1 OYR, value of 5 or 6, and
           friable; common fine and few medium roots; strongly           chroma of 3 or 4. Mottles are in shades of brown, yellow,
           acid; clear smooth boundary.                                  red, or gray. This horizon is clay loam, sandy clay, or
       E-6 to 10 inches; brown (1 OYR 5/3) fine sandy loam;              clay. In some peclons, it is sandy clay loam.
           common medium faint grayish brown (10YR 5/2)                    The Btg horizon has hue of 10YR, value 5 or 6, and
           and yellowish brown (10YR 5/4) mottles and few                chroma of 1 or 2. Mottles in shades of red, brown,
           fine distinct brownish yellow (1 OYR 6/6) mottles;            yellow, or gray are in most pedons. This horizon is clay
           weak medium subangular blocky structure; friable;             loam, sandy clay, or clay. In some pedons, the lower part
           common fine and few medium roots; strongly acid;              of the Btg horizon is sandy clay loam.
           gradual smooth boundary.                                        The Cg horizon has hue of 1 OYR to 5Y, value of 6 or
       Bt-10 to 15 inches; yellowish brown (10YR 5/4) clay               7, and chroma of 1 or 2. It has mottles in shades of red,
           loam; common medium distinct grayish brown (10YR              yellow, or gray. This horizon is sandy loam or sandy clay
           5/2) and brownish yellow (10YR 6/6) mottles and               loam.
           few medium prominent red (2.5YR 4/8) mottles;                   The 2Cg horizon has hue of 2.5Y, value of 6, and
           moderate medium subangular blocky structure;                  chroma of 2. It has mottles in shades of brown or gray.
           friable; few fine and medium roots; few pores; very           This horizon is clay. Some pedons do not have a 2Cg
           few faint clay films along old root channels; very            horizon.
           strongly acid; gradual smooth boundary.
       Btgl-15 to 26 inches; gray (10YR 5/1) clay; common
           medium distinct brownish yellow (10YR 6/8) mottles            Yauhannah Series
           and common medium prominent red (2.5YR 4/6)
           mottles; strong coarse prismatic structure; very firm;          The Yauhannah series consists of soils that formed in
           few fine and medium roots; few pores; many distinct           loamy marine sediment on broad terraces at an elevation
           clay films on faces of peds; very strongly acid;              of less than about 42 feet above sea level. Slopes are 0
           gradual smooth boundary.                                      to 2 percent. These soils are fine-loamy, siliceous,
       Btg2-26 to 45 inches; gray (10YR 5/1) sandy clay                  thermic Aquic Hapluclults.
           loam; common medium distinct brownish yellow                    Yauhannah soils are associated on the landscape with
           (10YR 6/8) mottles and common medium prominent                Chisolm, Coosaw, Eulonia, Ogeechee, Wahee, and
           red (2.5YR 4/6) mottles; moderate medium                      Yemassee soils. Chisolm soils are slightly higher on the
           subangular blocky structure; firm; few fine roots; few        landscape than the Yauhannah soils and have an arenic:
           pores; few distinct clay films on faces of peds; very         epipedon. Coosaw, Wahee, and Yernassee soils are
           strongly acid; gradual wavy boundary.                         slightly lower on the landscape. Coosaw soils are in an
       BCg-45 to 59 inches; gray (10YR 6/1) sandy clay loam;             arenic: subgroup. Wahee and Yemassee soils are
           common coarse distinct strong brown (7.5YR 5/8)               Aquults. Eulonia soils are in positions similar to those of
           mottles and common medium distinct yellowish                  the Yauhannah soils and have a clayey particle-size
           brown (1 OYR 5/4) mottles; few streaks of white               control section. Ogeechee soils are lower on the
           (10YR 8/1) stripped sand grains; weak medium                  landscape and are Aquults.
           subangular blocky structure; friable; very strongly             Typical pedon of Yauhannah loamy fine sand, 0 to 2
           acid; gradual wavy boundary.                                  percent slopes; about 12 miles southwest of
       Cg-59 to 65 inches; light brownish gray (10YR 6/2)                Summerville, 1.5 miles north of the intersection of South
           sandy clay loam; common medium distinct gray                  Carolina Highway 165 and South Carolina Highway 84,
           (1 OYR 6/ 1) mottles and few medium distinct                  75 feet east of South Carolina Highway 165, and 200
           brownish yellow (1 OYR 6/8) mottles; massive;                 feet south of communications relay tower.
           friable; very strongly acid; clear smooth boundary.
       2Cg-65 to 80 inches; light brownish gray (2.5Y 6/2)               A-0 to 4 inches; grayish brown (1 OYR 5/2) loamy fine
           clay; common medium distinct pale olive (5Y 6/3)                   sand; weak fine granular structure; very friable;
           and strong brown (7.5YR 5/8) mottles and few                       many fine and medium roots; extremely acid; clear
           medium distinct greenish gray (5G 5/1) mottles;                    smooth boundary.
           massive; firm; very strongly acid.                            E-4 to 18 inches; pale yellow (2.5Y 7/4) loamy fine
                                                                              sand; few medium distinct yellowish brown (10YR
         The solum ranges from 56 to more than 65 inches in                   5/6) and grayish brown (10YR 5/2) mottles; weak
       thickness.                                                             fine granular structure; very friable; common fine
         The A horizon has hue of 10YR, value of 4 or 5, and                  and medium roots; very strongly acid; clear smooth
       chroma of 1 or 2. It is sandy loam or fine sandy loam.                 boundary.








           86                                                                                                                     Soil Survey



           BE-18 to 24 inches; brownish yellow (10YR 6/6) fine                 Yemassee Series
                sandy loam; few fine distinct strong brown (7.5YR
                5/8) mottles; weak medium subangular blocky                      The Yemassee series consists of soils that formed in
                structure; friable; few fine and medium roots;                 loamy marine sediment on nearly level terraces at an
                extremely acid; gradual smooth boundary.                       elevation of less than about 42 feet above sea level.
           Btl-24 to 38 inches; brownish yellow (10YR 6/6) sandy               Slopes are 0 to 2 percent. These soils are fine-loamy,
                clay loam; common medliurn distinct strong brown               siliceous, thermic Aeric Ochraquults.
                (7.5YR 5/6) mottles and few medium distinct light                Yemassee soils are associated on the landscape with
                gray (10YR 7/1) mottles; weak medium subangular                Coosaw, Eulonia, Nakina, Ogeechee, Elloree, Wahee,
                blocky structure; friable; very few faint clay films on        and Yauhannah soils. Coosaw and Wahee soils are in
                faces of peds; few fine and medium roots; extremely            positions similar to those of the Yemassee soils. Coosaw
                acid; gradual smooth boundary.                                 soils are in an arenic subgroup, and Wahee soils have a
           Bt2-38 to 52 inches; brownish yellow (10YR 6/6) sandy               clayey particle-size control section. Eulonia and
                clay loam; many medium distinct light gray (10YR               Yauhannah soils are higher on the landscape and are
                7/2) mottles, many medium prominent red (2.5YR                 Udults. Eulonia soils have a clayey control section.
                4/8) mottles, and common medium faint strong                   Nakina, Ogeechee, and Elloree soils are lower on the
                brown (7.5YR 5/6) mottles; moderate medium                     landscape and have dominant matrix chroma of 2 or less
                subangular blocky structure; very few faint clay films         throughout the profile. Nakina soils have an umbric
                on faces of peds; friablEl; extremely acid; gradual            epipedon. Elloree soils are in an arenic subgroup.
                smooth boundary.                                                 Typical pedon of Yemassee fine sandy loam; about 9
           BCg-52 to 76 inches; light gray (10YR 7/2) sandy clay               miles southeast of Summerville, about 2,300 feet
                loam; many medium distinct brownish yellow (10YR               northeast of the junction of South Carolina Highway 642
                6/6) mottles and common medium prominent red                   and Ashley Phosphate Road (South Carolina Highway
                (2.5 YR 4/8) mottles; weak medium subangular                   62), and 30 feet southeast of road near power pole
                blocky structure; friable; common fine lenses of               number 34183.
                white fine sand; few fine flakes of mica; extremely            A-0 to 6 inches; very dark gray (10YR 3/1) fine sandy
                acid; clear smooth boundary.                                       loam; weak fine granular structure; very friable;
           C-76 to 80 inches; light gray (2.5Y 7/2) fine sandy                     many fine and medium roots and common large
                loam: strata of sandy clay loam and loamy sand;                    roots; very strongly acid; clear smooth boundary.
                common medium distinct yellowish red (5YR 5/6)                 E1-6 to 10 inches; yellowish brown (10YR 5/4) fine
                and strong brown (7.5YR 5/6) mottles; massive;                     sandy loam; few fine distinct light gray (10YR 7/2)
                friable; few flakes of mica; very strongly acid.                   mottles and common medium faint brownish yellow
                                                                                   (10YR 6/6) mottles; weak medium subangular
             The solurn ranges from 45 to more than 60 inches in                   blocky structure; very friable; common fine roots and
           thickness. Few flakes of mica are in the lower part of the              few medium roots; common streaks of darker
           profile in most pedons.                                                 surface material in worm and root holes; strongly
             The A horizon has hue of 10YR, value of 4 or 5, and                   acid; clear wavy boundary.
           chroma of 1 to 3. This horiZon generally is loamy fine              E2-10 to 15 inches; light yellowish brown (10YR 6/4)
           sand, but in some pedons, it is loamy sand.                             fine sandy loam; common medium distinct brownish
             The E horizon has hue of 10YR or 2.5Y, value of 5 to                  yellow (10YR 6/8) and light brownish gray (10YR
           7, and chroma of 3 to 6. It has mottles in shades of                    6/2) mottles; weak medium subangular blocky
           brown or yellow. This horizon is loamy fine sand.                       structure; friable; very few faint clay films on faces of
             The Bt horizon has hue of 7.5YR or 1 OYR, value of 5                  peds; few medium and common fine roots; few fine
           or 6, and chroma of 4 to 8. It has mottles in shades of                 pores; strongly acid; clear wavy boundary.
           red, yellow, brown, or gray. This horizon is sandy loam or          Btgl-15 to 32 inches; gray (10YR 6/1) sandy clay
           sandy clay loam.                                                        loam; common medium distinct strong brown (7.5YR
             The BC horizon has hue of 10YR or 2.5Y, value of 5                    5/8) mottles and few medium prominent red (2.5YR
           to 7, and chroma of 1 to 4. It has mottles in shades of                 5/8) mottles; moderate medium subangular blocky
           red, yellow, or brown. This horizon is sandy loam or                    structure; friable; few distinct clay films on faces of
           sandy clay loam. Some pedons have strata of white fine                  peds; few fine roots and pores; strongly acid;
           sand.                                                                   gradual wavy boundary.
             The C horizon has hue of 1 OYR or 2.5Y, value of 6 or             Btg2-32 to 48 inches; gray (1 OYR 6/ 1) sandy clay
           7, and chroma of I or 2. It has mottles in shades of                    loam; pockets of clay loam; common medium
           yellow, brown, or red. This horizon is loamy sand, fine                 distinct strong brown (7.5YR 5/8) mottles and
           sandy loam, or sandy loam. Most pedons are stratified or                common medium prominent red (2.5YR 5/8)
           have pockets of sandy or clayey material.                               mottles; moderate medium subangular blocky









      Dorchester County, South Carolina                                                                                              87



           structure; friable; very few faint clay films on faces of      brown, or gray. This horizon is loamy fine sand or fine
           peds; few fine roots; very strongly acid; gradual              sandy loam.
           wavy boundary.                                                   The Bt horizon has hue of 1 OYR, value of 5 or 6, and
      BCg-48 to 80 inches; light gray (5Y 7/2) sandy clay                 chroma of 1 to 4. It has mottles in shades of yellow,
           loam; strata of clay and sandy loam; few medium                brown, or gray. This horizon is fine sandy loam or sandy
           distinct strong brown (7.5YR 5/8), yellow (5Y 7/6),            clay loam.
           and gray (10YR 6/1) mottles; weak medium                         The Btg horizon has hue of 1 OYR, value of 5 to 7, and
           subangular blocky structure; firm; very strongly acid.         chroma of 1 or 2. It has mottles in shades of red, yellow,
        The solum ranges from 40 to more than 80 inches in                brown, or gray. This horizon is sandy clay loam. The
      thickness.                                                          lower part of this horizon has pockets of heavier textured
        The A horizon has hue of 10YR, value of 2 to 5, and               material.
      chroma of 1 or 2. It commonly is fine sandy loam but is               The BCg horizon has hue of 10YR or 5Y, value of 5 to
      loamy sand or loamy fine sand in some pedons.                       7, and chroma of 1 or 2. It has mottles in shades of red,
        The E horizon has hue of 10YR, value of 5 or 6, and               yellow, brown, or gray. This horizon is clay or sandy clay
      chroma of 3 or 4. It has mottles in shades of yellow,               loam, or it is stratified with variable textures.










                                                                                                                                                 89





       Formation of the Soils


          This section describes the factors of soil formation as                   The Recent Terrace is at or near sea level and is
       they relate to the soils in the county and explains the                   flooded daily, or occasionally, by sea water. It shows
       processes of soil formation.                                              little evidence of soil development. Capers and
                                                                                 Handsboro soils formed in this material.
       Factors of Soil Formation                                                    The Pamlico Terrace ranges from sea level to about
                                                                                 25 feet above sea level. This terrace makes up the lower
          Soil is a collection of natural bodies on the earth's                  part of the county south of an imaginary line from
       surface. It contains living matter and supports or is                     highway 17A to Old Dorchester State Park. The soils on
       capable of supporting plants. Soil is the product of five                 this terrace are younger than most of the soils at the
       important factors of soil formation: parent material,                     higher elevations. The clayey soils have mixed
       climate, living organisms (plant and animals), relief, and                mineralogy. Among the clayey soils on this terrace are
       time.                                                                     the Brookman, Eulonia, and Wahee soils. The loamy
          Climate and living organisms are the active factors in                 soils that have siliceous mineralogy include the Chisolm,
       soil formation. Their effect on the parent material is                    Coosaw, Elloree, Mouzon, Ogeechee, Yauhannah, and
       modified by relief and by the length of time the parent                   Yemassee soils.
       material has been in place. The relative importance of                       The Talbot Terrace ranges from 25 to 42 feet above
       each factor differs, however, from one place to another.                  sea level. This terrace occupies a small part of the
       In some places one factor dominates in the formation                      county. It extends in a narrow band from south of
       and determines most of the properties of the soil, but                    Summerville west to the Edisto River. It also extends up
       generally it is the interaction of all five factors that                  through Great Cypress Swamp. The soils on this terrace
       determines the kind of soil formed.                                       generally are similar to those on the Pamlico Terrace.
          Although soil formation is complex, some                                  The Penholoway Terrace ranges from 42 to 70 feet
       understanding of the soil forming processes can be                        above sea level. It includes the areas around
       gained by considering each of the five factors separately.                Summerville, Knightsville, and Jedburg, and the area
       It should be remembered, however, that each of the five                   from Ridgeville to Givhans. The soils on this terrace are
       factors is affected by and also affects each of the other                 older and more weathered and have dominantly siliceous
       factors.                                                                  or kaolinitic mineralogy. They include the Izagora,
       Parent Material                                                           Jedburg, and Daleville soils.
                                                                                    The Wicomico Terrace ranges from about 70 to 100
          Parent material is the unconsolidated mass from which                  feet above sea level. Like the other marine terraces, it
       a soil forms. It determines the mineral and chemical                      parallels the shoreline and the Edisto River. Soils on this
       composition of the soil. In Dorchester County, the parent                 terrace are more highly developed than those on the
       material of most of the soils is marine or fluvial deposits.              lower terraces, and they have either siliceous or
       Most soils, including all of those within the county, have                kaolinitic mineralogy. Some of the more common soils in
       developed in material distinctly removed from their origin.               this area include the Goldsboro, Lynchburg, Noboco, and
       These deposits differ widely in their content of sand, silt,              Rains soils.
       and clay.                                                                    The Sunderland Terrace ranges from about 100 to 170
          All of the soils in the county were deposited or formed                feet above sea level. In Dorchester County, most of this
       during the Pleistocene, or glacial, epoch (3). During this                terrace is along the boundary with Orangeburg County
       period, the ocean moved over the area, perhaps several                    southeast to the vicinity of St. George. The soils in this
       times. As the ocean retreated, it left formations and                     area are somewhat similar to those of the adjacent
       terraces indicating former shorelines and soils of                        Wicomico Terrace.
       different ages. The terraces in Dorchester County, in                        Alluvial material consisting of sand, silt, and clay has
       sequence from the sea, are the Recent, Pamlico, Talbot,                   been deposited on the flood plain of the Four Hole
       Penholoway, Wicomico, and Sunderland Terraces (fig.                       Swamp, Edisto and Ashley Rivers. These fairly young
       10).                                                                      soils show limited evidence of soil development.








       90                                                                    Soil Survey








                            X,



                                      Wicomico
                                 St. Geo@
                Sunderland




                                                     Penholoway





                                                              Summerville
                            Penholoway        Talbot


                                                              Penholoway





                                                              N
                                                   Talbot






                                                        Pamlico









         Figure 10.-The terraces In Dorchester County were formed as the ocean moved over the area. They Indicate former shorelines.



       Climate                                 the less soluble and fine textured soil material downward
        The climate of Dorchester County has been important through the soil profile. The amount of water that
       in the formation of soils. It is temperate, and rainfall is percolates through the soil depends on the amount of
       fairly well distributed throughout the year. The high rainfall, the length of the frost-free season, the relief, and
       rainfall, warm temperatures, and long frost-free growing the permeability of the soil material.
       season have had a marked effect on the characteristics Weathering of the parent material is accelerated by
       of the soils that have developed in Dorchester County. moist conditions and warm temperature. The growth and
        Climate, particularly precipitation and temperature, activity of living organism is also increased by a warm,
       affects the physical, chemical, and biological humid climate.
       relationships in the soil. Water dissolves minerals, aids
       chemical and biological activity, and transports the Living Organisms
       dissolved mineral and organic material throughout the The number and kinds of plants and animals that live
       soil profile. Large amounts of rainwater promote leaching in and on the soils are determined mainly by the climate
       of the soluble bases and promote the translocation of









       Dorchester County, South Carolina                                                                                                            91



       and, to lesser extent, the parent material, relief, and age               the result of many soil-forming processes. These include
       of the soil.                                                              the accumulation of organic matter, the leaching of the
          Bacteria, fungi, and other micro-organisms are                         accumulation of organic matter, the leaching of soluble
       indispensable in soil formation. They hasten the                          salts, the reduction and translocation of iron, the
       weathering of minerals and the decomposing of organic                     formation of soil structure, the physical weathering
       matter. Larger plants alter the soil microclimate, furnish                caused by freezing and thawing, and the chemical
       organic matter, and transfer chemical elements from the                   weathering of primary minerals or rocks. Some of these
       subsoil to the surface layer.                                             processes are continually taking place in all soils, but the
          Most of the fungi, bacteria, and other micro-organisms                 number of active processes and the degree of their
       in the soils of the county are in the upper few inches of                 activity vary from one soil to another.
       the soil. The activity of earthworms and other small                        Most soils have four major horizons: A, E, B, and C.
       invertebrates is chiefly in the A horizon and upper part of               These major horizons can be further subdivided by the
       the B horizon. These organisms slowly but continuously                    use of subscripts and letters to indicate changes within
       mix the soil material. Bacteria and fungi decompose
       organic matter and release nutrients for plant use.                       one horizon. An example would be the Bt2 horizon,
          Animals play a secondary role in soil formation, but                   which is a layer within the B horizon that contains
       their influence is very great. By eating plants, they                     translocated clay from the E horizon.
       perform one step in returning plant material to the soil.                   The A horizon, or surface layer, has the largest
          The native trees in the better drained areas of                        accumulation of organic matter. If the soil has been
       Dorchester County are mainly loblolly pine, longleaf pine,                cleared and plowed, this layer is called the Ap horizon.
       oak, and hickory. Sweetgum, blackgum, yellow poplar,                      The Brookman and Pantego, soils are examples of soils
       maple, tupelo, ash, and cypress are in the wetter areas.                  that have a distinctive, dark A or Ap horizon.
       Large trees affect soil formation by bringing nutrients up                  The E horizon, or subsurface layer, is the zone of
       from varying depths and by providing large openings to                    maximum leaching, or eluviation, of clay and iron in the
       be filled by material from above as large roots decay.                    profile. Where considerable leaching has taken place, an
       Relief                                                                    E horizon is formed generally below the A horizon.
                                                                                 Normally, the E horizon is the lightest colored horizon in
          Relief, or lay of the land, influences soil formation                  the soil. It is well expressed in the Bonneau and Ocilla
       because it affects moisture, vegetation, temperature,              and    soils.
       erosion. A a result, several different soils may form from                  The B horizon, or subsoil, is below the A or E horizon.
       similar parent material.                                                  It is the horizon of maximum accumulation, or illuviation,
          Most of the soils in Dorchester County are nearly level                of the clay, iron, aluminum, or other compounds that
       and have shallow depressions and drainageways and                         have been leached from the E horizon. Goldsboro,
       low ridges with gentle slopes. Less than 1 percent of the                 Izagora, and Wahee soils are examples of soils that
       county is flooded daily or occasionally by saline water.                  have a well expressed B horizon. Some soils, such as
       These flooded areas and some of the other soils in low                    the Chipley and Rutlege soils, have not formed a B
       areas show little development.                                            horizon and the C horizon lies immediately under the A
       Time                                                                      horizon. The C horizon is made up of material that has
          The length of time required for a soil to develop                      been little altered by the soil-forming processes but may
       depends largely on the intensity of the other soil-forming                be modified by weathering.
       factors. The soils of Dorchester County range from                          Well drained and moderately well drained soils in
       immature, or young, to mature. In the higher areas of the                 Dorchester County have a yellowish brown or reddish
       uplands, most of the soils have well-developed horizons                   subsoil. These colors are mainly thin coatings of iron
       that are easily recognized. Where the parent material is                  oxides on the sand, silt, and clay particles. A soil is
       very sandy or flooded, little horizonation has taken place.               considered well drained if it is free of gray mottles (those
       'The alluvial soils deposited along streams frequently                    with a chroma of 2 or less) to a depth of at least 30
       have not been in place long enough for distinct horizon                   inches. The Noboco and Emporia soils are examples of
       development.                                                              the well drained soils. Moderately well drained soils are
                                                                                 wet for short periods and are generally free of gray
       Morphology of the Soils                                                   mottles to a depth of about 15 to 20 inches. The
                                                                                 Goldsboro and lzagora soils are examples of moderately
          If a vertical cut is dug into a soil, several layers or                well drained soils.
       horizons are evident. This differentiation of horizons is










                                                                                                                                      93





       References


       (1)  American Association of State Highway and                     (4)  United States Department of Agriculture. 1951
            Transportation Officials. 1982. Standard                           (Being revised). Soil survey manual. U.S. Dep. Agric.
            specifications for highway materials and methods of                Handb. 18, 503 pp., illus. (Supplements replacing
            sampling and testing. Ed. 13, 2 vol., illus.                       pp. 173-188 issued May 1962.)

       (2)  American Society for Testing and Materials. 1986.              (5) United States Department of Agriculture. 1975. Soil
            Standard test method for classification of soils for               taxonomy: A basic system of soil classification for
            engineering purposes. ASTM Stand. D 2487.                          making and interpreting soil surveys. Soil Conserv.
       (3)  Cooke, C. Wythe. 1936. Geology of the Coastal                      Serv., U.S. Dep. Agric. Handb. 436, 754 pp., illus.
            Plain of South Carolina. U.S. Dep. Inter., Geol. Surv.
            Bull. 867, 196 pp., illus.










                                                                                                                                         95




      Glossary

      Aggregate, soil. Many fine particles held in a single                Clay film. A thin coating of oriented clay on the surface
           mass or cluster. Natural soil aggregates, such as                    of a soil aggregate or lining pores or root channels,
           granules, blocks, or prisms, are called peds. Clods                  i.e., clay coating, clay skin.
           are aggregates produced by tillage or logging.                  Coarse textured soil. Sand or loamy sand.
      Alluvium. Material, such as sand, silt, or clay, deposited           Concretions. Grains, pellets, or nodules of various
           on land by streams.                                                  sizes, shapes, and colors consisting of concentrated
      Association, soil. A group of soils geographically                        compounds or cemented soil grains. The
           associated in a characteristic repeating pattern and                 composition of most concretions is unlike that of the
           defined and delineated as a single map unit.                         surrounding soil. Calcium carbonate and iron oxide
      Available water capacity (available moisture                              are common compounds in concretions.
           capacity). The capacity of soils to hold water                  Conservation tillage. A tillage system that does not
           available for use by most plants. It is commonly                     invert the soil and that leaves a protective amount
           defined as the difference between the amount of                      of crop residue on the surface throughout the year.
           soil water at field moisture capacity and the amount            Consistence, soil. The feel of the soil and the ease with
           at wilting point. It is commonly expressed as inches                 which a lump can be crushed by the fingers. Terms
           of water per inch of soil. The capacity, in inches, in               commonly used to describe consistence are-
           a 60-inch profile or to a limiting layer is expressed                Loose. -Noncoherent when dry or moist; does not
           as-                                                                  hold together in a mass.
                                                          Incl7es               Friable.-When moist, crushes easily under gentle
                 Very low ................................................................... o to 3pressure between thumb and forefinger and can be
                 Low ................................................................. ......... 3 to 6
                 Moderate ................................................................. 6 to 9pressed together into a lump.
                 High ........................................................................ 9 to 12 Firm.-When moist, crushes under moderate
                 Very high .................................................... more than 12 pressure between thumb and forefinger, but
      Base saturation. The degree to which material having                      resistance is distinctly noticeable.
           cation-exchange properties is saturated with                         Plastic.-When wet, readily deformed by moderate
           exchangeable bases (sum of Ca, Mg, Na, K),                           pressure but can be pressed into a lump; will form a
           expressed as a percentage of the total cation-                       11 wire" when rolled between thumb and forefinger.
           exchange capacity.                                                   Sticky.-When wet, adheres to other material and
      Capillary water. Water held as a film around soil                         tends to stretch somewhat and pull apart rather than
           particles and in tiny spaces between particles.                      to pull free from other material.
           Surface tension is the adhesive force that holds                     Hard.-When dry, moderately resistant to pressure;
           capillary water in the soil.                                         can be broken with difficulty between thumb and
      Cation. An ion carrying a positive charge of electricity.                 forefinger.
           The common soil cations are calcium, potassium,                      Soft.-When dry, breaks into powder or individual
           magnesium, sodium, and hydrogen.                                     grains under very slight pressure.
      Cation-exchange capacity. The total amount of                             Cemented.-Hard; little affected by moistening.
           exchangeable cations that can be held by the soil,              Control section. The part of the soil on which
           expressed in terms of milliequivalents per 100 grams                 classification is based. The thickness varies among
           of soil at neutrality (pH 7.0) or at some other stated               different kinds of soil, but for many it is that part of
           pH value. The term, as applied to soils, is                          the soil profile between depths of 10 inches and 40
           synonymous with base-exchange capacity, but is                       or 80 inches.
           more precise in meaning.                                        Corrosive. High risk of corrosion to uncoated steel or
      Clay. As a soil separate, the mineral soil particles less                 deterioration of concrete.
           than 0.002 millimeter in diameter. As a soil textural           Cover crop. A close-growing crop grown primarily to
           class, soil material that is 40 percent or more clay,                improve and protect the soil between periods of
           less than 45 percent sand, and less than 40 percent                  regular crop production, or a crop grown between
           silt.                                                                trees and vines in orchards and vineyards.










           96                                                                                                                        Soil Survey



           Cutbanks cave (in tables). The walls of excavations                        Vely poorly drained -Water is removed from the
                tend to cave in or slough.                                            soil so slowly that free water remains at or on the
           Drainage class (natural). Refers to the frequency and                      surface during most of the growing season. Unless
                duration of periods of saturation or partial saturation               the soil is artificially drained, most mesophytic crops
                during soil formation, as opposed to altered                          cannot be grown. Very poorly drained soils are
                drainage, which is commonly the result of artificial                  commonly level or depressed and are frequently
                drainage or irrigation bul may be caused by the                       poncled. Yet, where rainfall is high and nearly
                sudden deepening of channels or the blocking of                       continuous, they can have moderate or high slope
                drainage outlets. Seven classes of natural soil                       gradients.
                drainage are recognized:                                         Drainage, surface. Runoff, or surface flow of water,
                Excessively drained. -\Afater is removed from the                     from an area.
                soil very rapidly. Excessively drained soils are                 Eluviation. The movement of material in true solution or
                commonly very coarse textured, rocky, or shallow.                     colloidal suspension from one place to another
                Some are steep. All are free of the mottling related                  within the soil. Soil horizons that have lost material
                to wetness.                                                           through eluviation are eluvial; those that have
                Somewhat excessively drained.-Water is removed                        received material are illuvial.
                from the soil rapidly. Many somewhat excessively                 Erosion. The wearing away of the land surface by water,
                drained soils are sandy and rapidly pervious. Some                    wind, ice, or other geologic agents and by such
                are shallow. Some are so steep that much of the                       processes as gravitational creep.
                water they receive is lost as runoff. All are free of
                the mottling related to wetness.                                      Erosion (geologic)-Erosion caused by geologic
                We# drained.-Water is removed from the soil                           processes acting over long geologic periods and
                readily, but not rapidly. It is available to plants                   resulting in the wearing away of mountains and the
                throughout most of the growing season, and                            building up of such landscape features as flood
                wetness does not inhibit growth of roots for                          plains and coastal plains. Synonym: natural erosion.
                significant periods during most growing seasons.                      Erosion (accelerated)-Erosion much more rapid
                Well drained soils are commonly medium textured.                      than geologic erosion, mainly as a result of the
                They are mainly free of mottling.                                     activities of man or other animals or of a
                Moderately well drained-Water is removed from                         catastrophe in nature, such as fire, that exposes the
                the soil somewhat slowly during some periods.                         surface.
                Moderately well drained soils are wet for only a                 Excess salts (in tables). Excess water-soluble salts in
                short time during the growing season, but                             the soil restrict the growth of most plants.
                periodically they are wet long enough that most                  Excess sulfur (in tables). An excessive amount of sulfur
                mesophytic crops are affected. They commonly                          is in the soil. The sulfur causes extreme acidity if the
                have a slowly pervious layer within or directly below                 soil is drained, and the growth of most plants is
                the solum, or periodically receive high rainfall, or                  restricted.
                both.                                                            Fast intake (in tables). The movement of water into the
                Somewhat poorly drained. -Water is removed slowly                     soil is rapid.
                enough that the soil is wet for significant periods              Fertility, soil. The quality that enables a soil to provide
                during the growing season. Wetness markedly                           plant nutrients, in adequate amounts and in proper
                restricts the growth of mesophytic crops unless                       balance, for the growth of specified plants when
                artificial drainage is provided. Somewhat poorly                      light, moisture, temperature, tilth, and other growth
                drained soils commonly have a slowly pervious                         factors are favorable.
                layer, a high water table, additional water from                 Fibric soil material (peat). The least decomposed of all
                seepage, nearly continuous rainfall, or a combination                 organic soil material. Peat contains a large amount
                ofthese.                                                              of well preserved fiber that is readily identifiable
                Poorly drained.-Water is removed so slowly that                       according to botanical origin. Peat has the lowest
                the soil is saturated periodically during the growing                 bulk density and the highest water content at
                season or remains wet for long periods. Free water
                is commonly at or near the surface for long enough                    saturation of all organic soil material.
                during the growing season that most mesophytic                   Field moisture capacity. The moisture content of a soil,
                crops cannot be grown unless the soil is artificially                 expressed as a percentage of the ovendry weight,
                drained. The soil is not continuously saturated in                    after the gravitational, or free, water has drained
                layers directly below plow depth. Poor drainage                       away; the field moisture content 2 or 3 days after a
                results from a high water table, a slowly pervious                    soaking rain; also called normal field capacity,
                layer within the profilE!, seepage, nearly continuous                 normal molsture capacity, or capillary capacity.
                rainfall, or a combination of these.                             Fine textured soil. Sandy clay, silty clay, and clay.









        Dorchester County, South Carolina                                                                                                           97



        Flood plain. A nearly level alluvial plain that borders a                     The chief consideration is the inherent capacity of
             stream and is subject to flooding unless protected                       soil bare of vegetation to permit infiltration. The
             artificially.                                                            slope and the kind of plant cover are not considered
        Gleyed soil. Soil that formed under poor drainage,                            but are separate factors in predicting runoff. Soils
             resulting in the reduction of iron and other elements                    are assigned to four groups. In group A are soils
             in the profile and in gray colors and mottles.                           having a high infiltration rate when thoroughly wet
        Grassed waterway. A natural or constructed waterway,                          and having a low runoff potential. They are mainly
             typically broad and shallow, seeded to grass as                          deep, well drained, and sandy or gravelly. In group
             protection against erosion. Conducts surface water                       D, at the other extreme, are soils having a very slow
             away from cropland.                                                      intiltration rate and thus a high runoff potential. They
        Hemic soil material (mucky peat). Organic soil material                       have a claypan or clay layer at or near the surface,
             intermediate in degree of decomposition between                          have a permanent high water table, or are shallow
             the less decomposed fibric and the more                                  over nearly impervious bedrock or other material. A
             decomposed sapric material.                                              soil is assigned to two hydrologic groups if part of
        Horizon, soil. A layer of soil, approximately parallel to                     the acreage is artificially drained and part is
             the surface, having distinct characteristics produced                    undrained.
             by soil-forming processes. In the identification of soil            Illuviation. The movement of soil material from one
             horizons, an upper case letter represents the major                      horizon to another in the soil profile. Generally,
             horizons. Numbers or lower case letters that follow                      material is removed from an upper horizon and
             represent subdivisions of the major horizons. An                         deposited in a lower horizon.
             explanation of the subdivisions is given in the Soil                Infiltration. The downward entry of water into the
             Survey ManuaL The major horizons of mineral soil                         immediate surface of soil or other material. This
             are as follows:                                                          contrasts with percolation, which is movement of
             0 horizon.-An organic layer of fresh and decaying                        water through soil layers or material.
             plant residue at the surface of a mineral soil.                     Leaching. The removal of soluble material from soil or
             A horizon.-The mineral horizon at or near the                            other material by percolating water.
             surface in which an accumulation of hurnified                       Liquid limit. The moisture content at which the soil
             organic matter is mixed with the mineral material.                       passes from a plastic to a liquid state.
             Also, a plowed surface horizon, most of which was                   Loam. Soil material that is 7 to 27 percent clay particles,
             originally part of a B horizon.                                          28 to 50 percent silt particles, and less than 52
             E horizon.-The mineral horizon in which the main                         percent sand particles.
             feature is loss of silicate clay, iron, aluminum, or                Low strength. The soil is not strong enough to support
             some combination of these.                                               loads.
             B horizon.-The mineral horizon below an 0, A, or E                  Medium textured soil. Very fine sandy loam, loam, silt
             horizon. The B horizon is, in part, a layer of                           loam, or silt.
             transition from the overlying horizon to the                        Mineral soil. Soil that is mainly mineral material and low
             underlying C horizon. The B horizon also has                             in organic material. Its bulk density is more than that
             distinctive characteristics, such as accumulation of                     of organic soil.
             clay, sesquioxides, humus, or a combination of                      Minimum tillage. Only the tillage essential to crop
             these; prismatic or blocky structure; redder or                          production and prevention of soil damage.
             browner colors than those in the A horizon; or a                    Miscellaneous area. An area that has little or no natural
             combination of these. The combined A and B                               soil and supports little or no vegetation.
             horizons are generally called the solum, or true soil.              Morphology, soil. The physical makeup of the soil,
             If a soil does not have a B horizon, the A horizon                       including the texture, structure, porosity,
             alone is the solum.                                                      consistence, color, and other physical, mineral, and
             C horizon. -The mineral horizon or layer, excluding                      biological properties of the various horizons, and the
             indurated bedrock, that is little affected by soil-                      thickness and arrangement of those horizons in the
             forming processes and does not have the properties                       soil profile.
             typical of the A or B horizon. The material of a C                  Mottling, soil. Irregular spots of different colors that vary
             horizon may be either like or unlike that in which the                   in number and size. Mottling generally indicates poor
             solum formed. If the material is known to differ from                    aeration and impeded drainage. Descriptive terms
             that in the solum, the Arabic numeral 2 precedes the                     are as follows: abundance-few, common, and
             letter C.                                                                many-, size-fine, medium, and coarse; and
        Humus. The well decomposed, more or less stable part                          contrast-faint, distinct, and prominent. The size
             of the organic matter in mineral soils.                                  measurements are of the diameter along the
        Hydrologic soil groups. Refers to soils grouped                               greatest dimension. Fine indicates less than 5
             according to their runoff-producing characteristics.                     millimeters (about 0.2 inch); medium, from 5 to 15








                  98                                                                                                                                                                                                          Soil Survey



                          millimeters (about 0.2 to 0.6 inch); and coarse, more                                                        Plinthite. The sesquioxide-rich, humus-poor, highly
                          than 15 millimeters (about 0.6 inch).                                                                                weathered mixture of clay with quartz and other
                  Muck. Dark, finely divided, well decomposed organic soil                                                                     diluents. It commonly appears as red mottles,
                          material. (See Sapric soil material.)                                                                                usually in platy, polygonal, or reticulate patterns.
                  Munsell notation. A designation of color by degrees of                                                                       Plinthite changes irreversibly to an ironstone
                          the three simple variables-hue, value, and chroma.                                                                   hardpan or to irregular aggregates on repeated
                          For example, a notation of 1 OYR 6/4 is a color of                                                                   wetting and drying, especially if it is exposed also to
                          1 OYR hue, value of 6, and chroma of 4.                                                                              heat from the sun. In a moist soil, plinthite can be
                  Neutral soil. A soil having a pH value between 6.6 and                                                                       cut with a spade. It is a form of laterite.
                          7.3. (See Reaction, soil.)                                                                                   Plowpan. A compacted layer formed in the soil directly
                  Nutrient, plant. Any element taken in by a plant                                                                             below the plowed layer.
                          essential to its growth. Plant nutrients are mainly                                                          Ponding. Standing water on soils in closed depressions.
                          nitrogen, phosphorus, potassium, calcium,                                                                            Unless the soils are artificially drained, the water can
                          magnesium, sulfur, iron, manganese, copper, boron,                                                                   be removed only by percolation or
                          and zinc obtained from the soil and carbon,                                                                          evapotranspiration.
                          hydrogen, and oxygen obtained from the air and                                                               Poor filter (in tables). Because of rapid permeability, the
                          water.                                                                                                               soil may not adequately filter effluent from a waste
                  Organic matter. Plant and animal residue in the soil in                                                                      disposal system.
                          various stages of decomposition.                                                                             Poor outlets (in tables). In these areas, surface or
                  Parent material. The unconsolidated organic and                                                                              subsurface drainage outlets are difficult or expensive
                          mineral material in which soil forms.                                                                                to install.
                  Ped. An individual natural soil aggregate, such as a                                                                 Productivity, soil. The capability of a soil for producing
                          granule, a prism, or a block.                                                                                        a specified plant or sequence of plants under
                  Pedon. The smallest volume that can be called "a soil."                                                                      specific management.
                          A pedon is three dimensional and large enough to                                                             Profile, soil. A vertical section of the soil extending
                          permit study of all horizons. Its area ranges from                                                                   through all its horizons and into the parent material.
                          about 10 to 100 square feet (1 square meter to 10                                                            Reaction, soil. A measure of the acidity or alkalinity of a
                          square meters), depending on the variability of the                                                                  soil expressed in pH values. A soil that tests to pH
                          soil.                                                                                                                7.0 is described as precisely neutral in reaction
                  Percolation. The downward movement of water through                                                                          because it is neither acid nor alkaline. The degree of
                          the soil.                                                                                                            acidity or alkalinity is expressed as-
                  Percs slowly (in tables). The slow movement of water                                                                                                                                                          pH
                          through the soil adversely affects the specified use.                                                                          Extremely acid         .................................................. below 4.5
                  Permeability. The quality of the soil that enables water                                                                               Very strongly acid          ............................................ 4.5 to 5.0
                          to move through the profile. Permeability is                                                                                   Strongly acid       ..................................................... 5.1 to 5.5
                          measured as the number of inches per hour that                                                                                 Medium acid         ..................................................... 5.6 to 6.0
                          water moves through the saturated soil. Terms                                                                                  Slightly acid      ....................................................... 6.1 to 6.5
                          describing permeability are:                                                                                                   Neutral     ............................................................... 6.6 to 7.3
                                                                                                                                                         Mildly alkaline       ................................................... 7.4 to 7.8
                                     Very slow     .......................................... less than 0.06 inch                                        Moderately alkaline           .......................................... 7.9 to 8.4
                                     Slow  ........................................................ 0.06 to 0.2 inch                                     Strongly alkaline        ............................................... 8.5 to 9.0
                                     Moderately slow         ....................................... 0.2 to 0.6 inch                                     Very strongly alkaline          .............................. 9.1 and higher
                                     Moderate      ...................................... 0.6 inch to 2.0 inches
                                     Moderately rapid        .................................. 2.0 to 6.0 inches                      Relief. The elevations or inequalities of a land surface,
                                     Rapid  ...................................................... 6.0 to 20 inches                            considered collectively.
                                     Very rapid    ....................................... more than 20 inches                         Root zone. The part of the soil that can be penetrated
                  Phase, soil. A subdivision of a soil series based on                                                                         by plant roots.
                          features that affect its use and management. For                                                             Runoff. The precipitation discharged into stream
                          example, slope, stoniness, and thickness.                                                                            channels from an area. The water that flows off the
                  pH value. A numerical designation of acidity and                                                                             surface of the land without sinking into the soil is
                          alkalinity in soil. (See Reaction, soil.)                                                                            called surface runoff. Water that enters the soil
                  Piping (in tables). Subsurface tunnels or pipelike cavities                                                                  before reaching surface streams is called ground-
                          are formed by water moving through the soil.                                                                         water runoff or seepage flow from ground water.
                  Plasticity index. The numerical difference between the                                                               Salty water (in tables.) Water is too salty for
                          liquid limit and the plastic limit; the range of moisture                                                            consumption by livestock.
                          content within which the soil remains plastic.                                                               Sand. As a soil separate, individual rock or mineral
                  Plastic limit. The moisture content at which a soil                                                                          fragments from 0.05 millimeter to 2.0 millimeters in
                          changes from semisolid to plastic.                                                                                   diameter. Most sand grains consist of quartz. As a








           Dorchester County, South Carolina                                                                                                                                                99



                 soil textural class, a soil that is 85 percent or more                                 Solum. The upper part of a soil profile, above the C
                 sand and not more than 10 percent clay.                                                      horizon, in which the processes of soil formation are
           Sapric soil material (muck). The most highly                                                       active. The solurn in soil consists of the A, E, and B
                 decomposed of all organic soil material. Muck has                                            horizons. Generally, the characteristics of the
                 the least amount of plant fiber, the highest bulk                                            material in these horizons are unlike those of the
                 density, and the lowest water content at saturation                                          underlying material. The living roots and plant and
                 of all organic soil material.                                                                animal activities are largely confined to the solum.
           Seepage (in tables). The movement of water through the                                       Structure, soil. The arrangement of primary soil
                 soil adversely affects the specified use.                                                    particles into compound particles or aggregates. The
           Sequium. A sequence consisting of an illuvial horizon                                              principal forms of soil structure are-platy
                 and the overlying eluvial horizon. (See Eluviation.)                                         (laminated), prismatic (vertical axis of aggregates
           Series, soil. A group of soils that have profiles that are                                         longer than horizontal), columnar (prisms with
                 almost alike, except for differences in texture of the                                       rounded tops), blocky (angular or subangular), and
                 surface layer or of the underlying material. All the                                         granular. Structureless soils are either single grained
                 soils of a series have horizons that are similar in                                          (each grain by itself, as in dune sand) or massive
                 composition, thickness, and arrangement.                                                     (the particles adhering without any regular cleavage,
           Shrink-swell. The shrinking of soil when dry and the                                               as in many hardpans).
                 swelling when wet. Shrinking and swelling can                                          Subsoil. Technically, the B horizon; roughly, the part of
                 damage roads, dams, building foundations, and                                                the solum below plow depth.
                 other structures. It can also damage plant roots.                                      Substratum. The part of the soil below the solum.
           Silt. As a soil separate, individual mineral particles that                                  Subsurface layer. Technically, the A2 horizon. Generally
                 range in diameter from the upper limit of clay (0.002                                        refers to a leached horizon lighter in color and lower
                 millimeter) to the lower limit of very fine sand (0.05                                       in organic matter content than the overlying surface
                 millimeter). As a soil textural class, soil that is 80                                       layer.
                 percent or more silt and less than 12 percent clay.                                    Surface layer. The soil ordinarily moved in tillage, or its
           Site index. A designation of the quality of a forest site                                          equivalent in uncultivated soil, ranging in depth from
                 based on the height of the dominant stand at an                                              4 to 10 inches (10 to 25 centimeters). Frequently
                 arbitrarily chosen age. For example, if the average                                          designated as the "plow layer," or the "Ap horizon."
                 height attained by dominant and codominant trees in                                    Taxadjuncts. Soils that cannot be classified in a series
                 a fully stocked stand at the age of 50 years is 75                                           recognized in the classification system. Such soils
                 feet, the site index is 75 feet.                                                             are named for a series they strongly resemble and
           Slope. The inclination of the land surface from the                                                are designated as taxadjuncts to that series
                 horizontal. Percentage of slope is the vertical                                              because they differ in ways too small to be of
                 distance divided by horizontal distance, then                                                consequence in interpreting their use and behavior.
                 multiplied by 100. Thus, a slope of 20 percent is a                                    Terrace (geologic). An old alluvial plain, ordinarily flat or
                 drop of 20 feet in 100 feet of horizontal distance.                                          undulating, bordering a river, a lake, or the sea.
           Slow refill (in tables). The slow filling of ponds, resulting                                Texture, soil. The relative proportions of sand, silt, and
                 from restricted permeability in the soil.                                                    clay particles in a mass of soil. The basic textural
           Soil. A natural, three-dimensional body at the earth's                                             classes, in order of increasing proportion of fine
                 surface. It is capable of supporting plants and has                                          particles, are sand, loamy sand, sandy loam, loam,
                 properties resulting from the integrated effect of                                           silt loam, silt, sandy clay loam, clay loam, slIty clay
                 climate and living matter acting on earthy parent                                            loam, sandy clay, silty clay, and clay. The sand,
                 material, as conditioned by relief over periods of                                           loamy sand, and sandy loam classes may be further
                 time.                                                                                        divided by specifying "coarse," "fine," or "very
           Soil separates. Mineral particles less than 2 millimeters                                          fine."
                 in equivalent diameter and ranging between                                             Thin layer (in tables). An otherwise suitable soil material
                 specified size limits. The names and sizes of                                                that is too thin for the specified use.
                 separates recognized in the United States are as
                 follows:                                                                               Tilth, soil. The physical condition of the soil as related
                                                                                millime-                      to tillage, seedbed preparation, seedling emergence,
                                                                                 ters                         and root penetration.
                         Very coarse sand     ............................................. 2.0 to 1.0  Topsoil. The upper part of the soil, which is the most
                         Coarse sand    ..................................................... 1.0 to 0.5      favorable material for plant growth. It is ordinarily
                         Medium sand     .................................................. 0.5 to 0.25       rich in organic matter and is used to topdress
                         Fine sand   ...................................................... 0.25 to 0.10      roadbanks, lawns, and land affected by mining.
                         Very fine sand   .............................................. 0.10 to 0.05
                         Silt ................................................................ 0.05 to 0.002 Trace elements. Chemical elements, such as zinc,
                         Clay .......................................................... less than 0.002      cobalt, manganese, copper, and iron, are in soils in









         100                                                                                                                  Soil Survey



              extremely small amounts. They are essential to plant          Weathering. All physical and chemical changes
              growth.                                                            produced by atmospheric agents in rocks or other
         Unstable fill (in tables). There is a risk of caving or                 deposits at or near the earth's surface. These
              sloughing on banks of fill material.                               changes result in disintegration and decomposition
         Upland (geology). Land at a higher elevation, in general,               of the material.
              than the alluvial plain orstream terrace; land above
              the lowlands along streams.










                                                                                                                    101





      Tables








           102                                                                                                                              Soil Survey




                                                           TABLE I.--TEKPERATURE AND PRECIPITATION

                                             l[Data recorded in the period 1951-81 at Summerville, South Carolina]


                                                     Temperature                                                  Precipitation


                                                               2 years in                                     2  years in 10
                                                             10 will have--                                     will have--
                                                                                        Average                                   Average
               Month      lAveragelAveragf-lAverage                                    number oflAveragel                      !number oflAverage
                          I daily I daily I daily          Maximum         Minimum      growing    I          I Less  I More Idays withisnowfall
                          Imaximumilminimumi            itemperatureltemperaturel       decree     I          lthan--ithan--10 10 inchl
                                    I                                                              I          I       I        I  *
                          I                   I         I  higher       I   lower       days*                                     or more
                          I         I         I         I  than--          than--                  I          I       I        I
                                    I         I         I
                                    I        -+_
                          1   0F        OF        fE           OF              OF          Units   I    In        n   I   I,   I            I    In
           January  ----     57.9      34.4      46.2          79              14           111    1   3.36   1  1.681    4.811       7     1     .0
           February  ---     60.7      36.3      48.5          81              17           105        3.51   1  1.791,   5.011       7     1     .5
           March  ------     67.9   1  43.2      55.6          87              24      1    220    1   4.24   1  2.041    6.141       7     1     .0
           April  ------     76.4      51.1      63.8          91              32           414        2.78   1   .891    4.321       5     1     .0
           May --------      82.9      59.5      71.2          96              41      1    657    1   4.40   1  2.501    6.071       7     1     .0
           June  -------     87.6      66.6   1  77.1          99              52           813    '1  15.79  1  2 801    8.361       8     1     .0
           July  -------     89.9      70.1      80.0          99              59           930        6.73      3.581    9.50!       10          .0
           August   -----    89.4      69.7      79.6          98              59      1    918    1   6.43   1  3.531    8.991       9     1     .0
           September--I      85.0   1  65.1   1  75.1   1      95       1      49           753    1   4.75   1  1.431    6.771       6     1     .0
                          I         I         I         I               I                          I          I       I        I            I
           October  ----  1  76.9   1  52.5   1  64.7   1      91              30      1    456    1   2.72   1   .911    4.211       4     1     .0
                          I         I         I         I                              I           I          I       I        I            I
           November  ---  1  68.6   1  42.4   1  55.5   1      84              22      1    188    1   2.13   1  1.001    3.101       4     1     .0
                          I         I         I         I                              I           I          I       I        I            I
           December---I      60.4   1  35.7   1  48.1   1      80       1      15      1    101    1   3.19   1  1.771    4.431       6     1     .1


           Yearly:
               Average--I    75.3   1  52.2   1  63.8   1      ---
                          I         I
               Extreme--I     --- 1                            10,      1      13      1    ---    I     ---  I  ---  I   --- I      ---    I    ---
               Total----                                                                  5 666      50.03 1    40.9811  58.651       80    1     .6

                   A growing degree day       is a unit of heat available for plant growth. It can be calculated by adding the
           maximum and minimum daily temperatures, dividing the sum bg 2, and subtracting the temperature below which
           growth is minimal for the principal crops in the area (50 F).








      Dorchester County, South Carolina                                                                                      103




                                            TABLE 2.--FREEZE DATES IN SPRING AND FALL

                                                [Data recorded in the period 1951-81
                                                   at Summerville, South Carolinal


                                                                         Temperature


                                     Probability                0           28 OF          32 OF
                                                             24 F
                                                          or lower        or lower       or lower



                                   Last freezing
                                     temperature
                                     in spring:

                                      1 year in  10
                                       later than--         March 12       April     I    April     16

                                      2 years in 10
                                       later than--         March    4     March 23       April      9

                                      5 years in 10
                                       later than--      February 17       March     7    March     27


                                   First freezing
                                     temperature
                                     in fall:


                                      I year  in 10
                                       earlier than--    November 16     November 1      October 24


                                      2 years in 10
                                       earlier than--    November 22     November 7      October 29

                                      5 years in 10
                                       earlier than--    December 3      November 17    November     7





                                                      TABLE 3.--GROWING SEASON

                                                  rData recorded in the period 1951-81
                                                     at Summerville, South Carolina]


                                                              Daily minimum temperature
                                                                during growing season


                                         Probability       Higher       Higher       Higher
                                                            than         than          than
                                                                0
                                                            24 F         28 OF         32 OF

                                                            Days         Days          Days

                                        9 years in 10   1    256          223          198

                                        8 years in 10        267          234          207

                                        .5 years in 10       288          255          224

                                        2 years in 10        309          275          241

                                        1 year in 10         320          286          250








          104                                                                                                             Soil Survey




                                        TABLE 4.--ACREAGE AND PROPORTIONATE EXTENT OF THE SOILS

           Map                                             Soil name                                          I   Acres    IPercent
          sy boll


          AbA     Albany fine sand, 0 to 2 percent slopes    --------------------------------------------           7 '500     2.1
          ApB     Alpin fine sand, 0 to 6 percent slopes    ---------------------------------------------           11200      0.3
          BIA     Blanton fine sand, 1) to 2 percent slopes   -------------------------------------------           3 ,000     0.8
                                                              -------------------------------------------                      0.7
          BIB     Blanton fine sand, :2 to 6 percent slopes                                                         2 500
          BoA     Bonneau fine sand, 1) to 2 percent slopes   -------------------------------------------           6 700      1 8
          BoB     Bonneau fine sand, '2 to 6 percent slopes   ------------------------------------                  2'200      0*6
          Br      Brockman clay loam, frequently flooded    ----------------------------------------------         20:500      5:6
          Ca      Capers silty clay loam  -------------------------------------------------------------             1,100      0.3
          ChA     Chipley sand, 0 to 2 percent slopes     -----------------------------------------   I-------      8,000      2.2
          CoB     Chisolm fine sand, D to 6 percent slopes    -------------------------------------------           2 000      0.6
          Cs      Coosaw loamy fine sand  -------------------------------------------------------------             61000      1.6
          Cx      Coxville loam  ----------------------------------------------------------------------             4 ,100     1.1
          Da      IDaleville silt loam  ----------------------------------------------------------------           11,000      3.0
          Ec      lEchaw fine sand  --------------------------------------------------------------------            5,100      1.4
          E0      iElloree loamy fine sand, occasionally flooded     --------------------------------------         3,800      1.0
          EpB     I
                  ,Emporia loamy fine sand, 2 to 6 percent slopes    -------------------------------------          3,000      0.8
          EuA     Eulonia. fine sandy loam, 0 to 2 percent slopes    -------------------------------------          2,100      0.6
          EuB     Eulonia fine sandy loam, 2 to 6 percent slopes     -------------------------------------          1,000      0.3
          FoA     Foreston loamy fine sand, 0 to 2 percent slopes      ------------------------------------         1,500      0.4
          FxB     Foxworth fine sand, 0 to 6 percent slopes    ------------------------------------------           1,800      0.5
          GoA     Goldsboro loamy sand, 0 to 2 percent slopes    ----------------------------------------          31,400      8.6
          Gr      Grifton fine sandy loam, frequently flooded    ----------------------------------------          24,200      6.7
          Hb      Handsboro muck  ---------------------------------------------------------------------               200      0.1
          HP      Haplaquents, loamy  -------------------------------------------------      -----------------      2,300      0.6
          IzA     Izagora silt loam, 0 to 2 percent slopes    -------------------------------------------           8,700      2.4
          TzB     Izagora silt loam, 2 to 6 percent slopes    ---------------------------------                       200      0.1
          Jd      Jedburg loam --------------------------------------------------------------                      15,300      4.2
          JoA     Johns loamy sand, 0 to 2 percent slopes    --------------------------------------------           1,700      0.5
          Le      ILeon sand  ---------------------------------------------------------------------------           2,300      0- 6
          Lm      ILumbee fine sandy loam, occasionally flooded   ---------------------------------------           4,500      1 2
          Ln      ILynchburq loamy sand -----------------------------------------------------------         --1    23,300      6'5
          Ly      Fynn Haven fine sand  ---------------------------------------------------------------             1,000      0'.3
          Mo      Mouzon fine sandy loam, occasionally flooded    ----------------------------                     45,800      12.6
          Na      Nakina fine sandy loam  -------------------------------------------------------------             2,500      0.7
          NoA     Noboco loamy sand, 0 to 2 percent slopes    --------------------------------------------         15,400      4.2
          OcA     Ocilla sand, 0 to 2 percent slopes    --------------------------------------------------          6,400      1.8
          Og      Ogeecbee fine sandy loam  ------------------------------------------------------------            7,000      1.9
          Os      Osier loamy fine sand, frequently flooded    -------------------------------------------         11,600      3.2
          Pa      Pantego sandy loam  ------------------------------------------------------------------            5,600      1.5
          Pe      Pelham sand  --------------------------------------------------------------------------           7,300      2.0
          PM      Plummer loamy sand  -------------------------------------------------------------------           2,200      0.6
          Ra      Rains sandy loam   ---------------------------------------------------------------------         23,400      6.5
          Ru      Rutlege loamy fine sand, frequently flooded    ----------------------------------------           4,100      1.1
          Se      Seagate sand ------------------------------------------------------------------------             1,500      0.4
          Wa      lWahee fine sandy loam  -------------------------------------------------------     I-------      8 700      2 4
          YaA     IYauhannah loamy fine sand, 0 to 2 percent slopes     -----------------------------------         3'400      0:9
          Ye      IYemassee fine sandy loam -----------------------------------------------------------             7'400      2.0
                  1 Water  -----------------------------------------------------------------------------      I..... 2:500_1   0.7
                  1                                                                                           1     -----  I-------
                  I    Total  -------------------------------------------------------------------------            364,000    100.0









        Dorchester County, South Carolina                                                                                              105




                             TABLE 5.--LAND CAPABILITY CLASSES AND YIELDS PER ACRE OF CROPS AND PASTURE

        [Yields are those that can be expected         under a high level of management. Absence of a yield indicates that the
             soil is not suited to the crop or         the crop generally is not     grown on the soil]


                           I            I              I             I             I             I              I             I
         Map symbol and    I    Land    I              I             I             I             1              11              Improved
            soil name      11capabilityl     Corn       Soybeans        Tobacco    I   Wheat     I    Oats      iBahiagrass   I bermuda-
                           I            I                                          I             I              I             I   grass
                                                Bu           Bu           Lbs           Bu              Bu           AUM3V          AUM*

        AbA -------------       ITIw            65            25         2,100                                       6.5            7.0
         Albany

        ApB -------------       IVs                                                                                  7.0            8.0
         Alpin

        BIA, BlB --------       Ills            60            25         2,000                                       6.5            8.0
         Blanton


        BoA, BoB --------       Hs              85            25         2,600                                       8.0            8.5
         Bonneau


        Br --------------       vi,
         Brookmar


        Ca --------------      VIIIW
         Capers

        ChA -------------       Ills            50            20                                                     7.5            8.0
         Chipley                                                         2,000

        CoB -------------       ITs             85     1      25                                         50          8.0          10.0
         Chisolm


        Cs --------------       TTTw            90            30                                         60          8.0          10.0
         Coosaw


        Cx --------------       IIIw            100           35
                                                                                          50     1       70          8.0            9.0
         Coxville


        Da --------------       IITw            100           35                                                     8.0            8.0
         Daleville


        Ec --------------       Ills            70            30                                                     7.5            7.5
         Ecbaw


        E0 --------------       VIw                                                                                  7.5            7.5
         Elloree

        EpB -------------       Ile             100           35     1   2,900            50                         9.0            9.0
         Emporia

        EuA -------------       IN              100           40                                         75
                                                                                                                     9.5            9.5
         Eulonia


        EuB -------------       Ile             90            35                                         70          9.0          10.0
         Eulonia


        FoA -------------       ITw             100           35
                                                                                                                     9.0            9.0
         Foreston


        FxB -------------       Ills            45            20                                                     7.5            7.0
         Foxwortb


        GoA -------------       TIw             125           45         3,000            60                         9.0            9.0
         Goldsboro



            See footnote at end of table.









         106                                                                                                        Soil Survey




                      TABLE S.--LAND CAPABILITY CLASSES AND YIELDS PER ACRE OF CROPS     AND PASTURE--Continued


          Map symbol and      Land                                                                                  Tmproved
             soil name    Icapabilityl     Corn    ISoybeans   I  Tobacco   I   Wheat    I  Oats     lBahiagrass    bermuda-
                          I           I            I           I            I            I           I            I
                                                                                                                      qrass
                          I           I     BU         Eu            Lbs         ju           @u          AUM*
         Gr --------------    VIw
          Grifton


         Hb --------------    VITIw
          Handsboro

         Hp--                 VIw
          Haplacruents

         TzA  -------------   IN            110          45                                               9.0          9.0
          Izaqora

         IzB  -------------   Ile           90           30                                               8.0          9.0
          Izaqora

         Jd --------------    IN            100          50        2,800          30                      10.0
          Jedburg

         JoA  -------------   IN            110          40        2,700          50                      9.0          9.0
          Johns


         Le --------------    IVw           50                                                            7.5          7.0
          Leon


         LM --------------    VIw                                                                         8.0          8.0
          Lumbee

         In --------------    Ilw           115          45       2,800                        75         10.0
          Lynchburg

         Ly --------------    TVw                                                                         7.5
          Lynn Haven

         Mo --------------    VIw
          MOU207)


         Na --------------    VIw
          Nakina


         NoA  -------------    1            115          45       3,000           60                      9.0          9.0
          Noboco
         OcA --- ;---------   I11w          75           30       2,600                                   7.5          8.5
          Ocill


         Oq --------------    I11w          100          45                                               9.0
          Ogeecbee

         Os --------------      Vw
          Osier


         Pa --------------    VIw
          Panteqo

         Pe --------------    IIIw          75           30                                               7.0          7.0
          Pelham


         PM --------------      Vw
          Plummer



             See footnote at end of table.









      Dorchester County, South Carolina                                                                                  107




                  TABLE 5.--LAND CAPABUITY CLASSES AND YTELDS PER ACRE OF CROPS      AND PASTITRE-Continued



      Map symbol and       Land                                                                                  Tmproved
          soil name    Icapabilityl    Corn    I Soybeans   I  Tobacco   I   Wheat    11  Oats     IBahiaqrass I bermuda-
                       I                                                                                           grass
                                        Bu          Bu           Lbs          Bu           Bu           AUMII       AUM*


     Ra --------------     TTTw         110          40         2,300                                   10.0
                                                                                            70
      Rains


     R---------------      VTw
      Rutlege

     Se --------------     TTTw           75         25         1.1800                                  8.0          8.0
      Seagate

     Wa --------------     TTw          110          45                                     70          8.0          8.5
      Wahee


     YaA  -------------    Tlw          125          45                                                 9.0           11
      Yauhannah


     ye --------------     IN                        45                                                11.0           12
                                        120
      Yemassee



            Animal-unit-montb: The amount of    forage or feed required   to feed one animal unit   (one cow, one
     horse, one mule, five sheep, or five goats for 30 days.







         108                                                                                                           Soil Survey



                                             TABLE 6.--CAPABILITY CLASSES AND SUBCLASSES


                                        (Miscellaneous areas are excluded. Absence of an
                                             entry indicates no acreage)


                                                                                 cerns (Subclass7
                                                            Major manaa    nt con
                                         Class     TotaI    1                        1    Soil
                                                  acreage     Erosion      Wetness       problem
                                                                 (e)         (w)            (s)
                                                            +              Acres           Acres

                                          1          15,4001      ---   I       ---  I      ---
                                          TI    1   118,6001     4,200  1  103,500   1    10,900
                                                1           1           1            1
                                          111        94,6001      ---   1    74,200       20,400
                                          IV    1     4,5001      ---   1     3,300  1     1,200
                                          V          13,800,                 13,800  1      ---
                                          VI    1   113,3001      ---   1  113,300   1      ---

                                          VII
                                          Vill  1     1,3001      ---   1     1,300  1      ---








       Dorchester County, South Carolina                                                                                              109



                                                  TABLE 7.--WOODLAND MANAGEMENT AND PRODUCTIVITY

           [Only the soils suitable for production of commercial trees are listed. Absence of an entry indicates
               that information was not available]


                               I          anagemen concerns                     Potential productivity
             Map symbol and    1          1, Equip- I          I                                  I      I
               soil name       lErosion     ment ISeedlingl     Plan          Common trees        Site IProduc-I     Trees to
                               Ihazard    I I           -tal   I  p i                             I
                                            imita-Imo'r        Icom e                             indexitivity    I   plant
                                                                 t                                       I
                                            tion I itz             io                                    class*   I
           AbA -------------   ISlight    IModerate ModezratelModeratelLoblolly pine::-:::-I         95  1  129   jLoblolly pine.
             Albany            I          I                    I          ILongleaf pine             80     100
                               I          I                    I          I                                       I
           ApB -------------   19light    IModeratelModerate!Slight       Loblolly pine  -------  1  85  1  114   Itoblolly pine,
             Alpin             I                                          Longleaf pine  -------  1  70     _86     longleaf pine.
                               I                               I          ITurkey oak ----------  I ---
                               I                               I          IPost oak ------------  I ---  I  ---   I
                               I                               I          IBIackjack oak ------ :1
                                                               I          IBluejack oak -------   I
                                                               I          I                       I
           BIA, BIB  --------  ISlight    IModeratelModeratelModerate Loblolly pine      ---  ---    80  1  114   ILoblolly pine,
             Blanton           I          I                               Longleaf pine  --- --- -   70     _86     longleaf pine.
                               I          I                               IBlue'lack oak---   --- I  -_      -_
                               I          I                               ITurkey oak ----- :---- I
                               I          I                               ISouthern red oak ----  i
                               I          I         I          I          ILive oak ------               I  ---   I
           BoA, BoB-- ---- 'Sliqbt        !ModeratelModeratelModeratelLoblolly pine      ----        86  1  129   ILoblolly pine,
             Bonneau                                                      ILongleaf pine -------  1  75  1   86   1 longleaf pine.
                                                                          lWhite oak -------- -1    ---  I  ---   I
                                                               I          lHickory ------------
                                                               I
           Br  ----------m  --- ISlight   ISevere   ISevere    ISevere    ISwamp tupelo ------       55  1   71   1Sweetgum, water
             Brookman          I                                                                                    tupelo.
                               I
           ChA-m  -----------  ISlight    IModeratelSlight     IModerate Loblolly pine   -------     90  1  129   ILoblolly pine.
             Cbipley           I          I         I          I          ILongleaf pine -------  1 -80  1  100
                               I          I         I                     IPost oak ------------  I
                               I          I         I                     ITurkey oak -------
                                                                          IBlackjack oak -------  I
                                                                          I                       I
           CoB -----------   m-ISlight    I.ModeratelModeratelModerateIL-oblolly pine:    ------  1  90  1  129   ILongleaf pine.
             Cbisolm           I          I         I          I          ILongleaf pine  ------    _78     100   1
                               I          I         I          I          ISouthern red oak ----            -     I
                               I          I         I          I          IHickory -------------  I --- I   ---   I
                               I          I         I          I          I                       I      I        I
           Cs  --------------  ISligbt    IModerate IModemratelModerateiLoblolly pine:    ---- :-1   79  1  114   ILoblolly pine.
             Coosaw            I          I         I          I          ILongleaf pine_--          68  1  _71   1
                                                                          IWater oak ---- m-         --  I   --   I
                                                                          IBIackgum ---------- D
           Cx  --------------- ISliqht    ISevere   IModeratelSevere      Loblolly pine  -----       90     129   iLoblolly pine.
             Coxville          I          I'        I                     ILong3eaf pine -----                    I
                               I          I         I                     ISweetgum ---------- -  I ---     ---   I
                               I          I         I                     Blackqum--m   -------D    ---     ---   I
                               I          I         I                     Water oak -----------   I
                               I          I         I                     IWillow oak ----------  I
                               I          I         I                     lWater tupelo --------  I
                               I          I         I                     Gm  ------m----------   I
                               I          I         I
                                                                          IUickory ------------
                                                                          I
           Da  --------------- iSlight    ISevere   iSevere    lModeratelLoblolly pine   -------  1  95     129   ILoblolly pine,
             Daleville         I          I         I          I          ISweptgum ------           go     100   1 sweetgum.
                               I          I         I          I          IWater oak ----            85
                               I          I         I          I          lWillow oak-         --1   80


                See footnote at end of table.









           110                                                                                                                   Soil Survey




                                            TABLE 7.--WOODLAND MANAGEMENT AND PRODUCTTVITY--Continued

                                            Managemen     oncerns                 poti7ntial productivity
               Map symbol and                Equip- I            I                                  I      I        I
                  soil name      IErosion     ment ISeedling,     Plant -1      Common trees        ISite Produc--l    Trees to
                                 Ihazard     limita-Imortal- competi I                              lindexitivity   I   plant
                                              tion I ity         I         I                        I      !class*
                                                                   tion

               Fr --------------- ISlight   IModeratelSligbt     IModeratelLongleaf pine   -------  1 68   1   71   ILongleaf pine,
               Ecbaw             I                                         ILoblolly pine  -------  1 85   1 114    1 loblolly pine.
               Eo -------------- jSlight    ISevere   ISevere    ISevere   ILoblolly pine  -------  1 90   1 129    ILoblolly pine,
               Elloree                      I         I          I         ISweetgum ------------   I---   I ---    I sweetgum,
                                 I                    I          I         IYellow poplar  ----- :-I ---   I ---    I yellow poplar.
                                 I                    I                    1,Red maple --------- -  I
                                 I                    I                    Water oak  -----------   I
                                 I                    I                                             I
               EpB ------------- ISlight    IS]fght   lModeratelModeratelLoblolly pine              1 75   1 100    ILoblolly pine,
               Emporia           I          I         I          I         ISouthern red              70   1   57     sweetgum.
               EuA, EuB -------- !Slight    IModeratelModerate ModeratelLoblolly pine      -------  1 90     129    Loblolly pine,
                                                                 I         IWater oak -----------   I go   1,         American
               Eulonia                                                     I                                 ---
                                                                 I         Sweetqum  -------------  1 90   1 100      sycamorer
                                                                 I         IBlackcrum ------------  I---   I ---    I sweetgum,
                                                                 I                                         I        I
                                                                           ISouthern red oak  ----  I---   I ---    I yellow poplar.
                                                                 I         ILongleaf pine  -------  1 85     114
                                                                 1         IHickory  -------------  I --- I  ---    I
                                                                 I    -    I                        I      I        I
                                                                                                           f
               FoA ------------- ISlight    iMode-ratel,Slight   IModeratelLoblolly pine   -------  1 90   1 129    ILoblolly pine.
               Foreston                                          I         IT-,ongleaf pine ------- 1 75   1   86   1
               FxB ------------- ISlight    IModeratelModeratelModerate Longleaf pine      -----    1_65   1 _71    ILongleaf pine.
               Foxworth          I          I         I          I         Turkey oak   -------- D --      I   --   I
                                 I          I                              ILive oak ------------   I---   I ---    I
                                 I          I                              IPost oak ------------   I---   I ---    I
                                 I          I                              IBluejack oak   -------- I---   I ---    I
                                                      I                    lFlowering dogwood---I    ---   I ---    I
                                                      I                    I                        I      I        I
               GoA ------------- ISlight    IModeratelSlight     IModerate Loblolly pine   -------    90     129    Loblolly pine,
               Goldsboro         I          I         I          I         Lonqleaf pine   -------    77     100    1 yellow poplar,
                                 I          I         I          I         Sweetgum  ------------     90     100    1 American
                                 I          I         I          I         ISouthern red oak  ----           ---    I sycamorel
                                 I          I         I                    IWhite oak -----------   I---   I ---    I sweetgum.
                                 I          I         I                    IWater oak ------- :-:-I  ---   I ---    I
                                 I          I         I                    IRed maple ------- - -   I---   I ---    I
                                 I          I         I                    I                        I      I        I
               Gr -------------- ISlight    ISevere   iSevere    ISevere   ILoblolly pine  -------  1 89   1 129    ILoblolly pine,
               Grifton                                                                                                sweetgum,
                                                                                                                      water tupelo,
                                                                                                                      American
                                                                                                                      sycamore,
                                                                                                                      water oak.
               IzA, IzB -------- ISlight    IModeratelSlight     IModeratelLoblolly pine   -------  1 90   1 129    ILoblolly pine,
               Izaqora                                                     ISweetgum ------------   1 90   1 100    1 sweetgum,
                                                                           iYellow poplar  -------  1100   1 114    1 yellow poplar,
                                 I          I         I          I         IWater oak -----------   I go   I ---    I water oak.
                                 I          II        I          I         I                        I      I        I
                                            I
                                            I























               Jd -------------- ISlight    ISevere ISlight      ISevere Loblolly pine     -------  1_90   1 129    ILoblolly pipe.
               Jedburg           I          I                              ISweetgum ------------   I --   I ---    I
                                 I          I                              I                        I      I        I
               JoA ------------- ISlight.   IModeratelSlight     IModeratelLoblolly pine   ----  ::-1 86   1 12     ILdblolly pine.
                                 I          I         I          I                                         I log    I
               Johns                                                       ISweetgum ---------     -1 90
                                 I          I         I          I         I                        I      I        I

                  See footnote at end of     table.









        Dorchester County, South Carolina




                                           TABLE 7.--WOODLAND MANAGEMENT AND PRODUCTIVITY--Continued

                                           Managemen concerns                     Potentlal productivi y
              Map symbol and               I Equip-             I                                   I      Tt
                 soil name      lErosion   I ment lSeedlingl       Plant        common trees        Site 1Produc-1     Trees to
                                1hazard    I limita-imortal-'Icompeti-I                             lindexitivity   I   plant
                                I          I tion       ity         tion                                   class*   I
                                I
            Le --------------   ISliqht    lModeratelModeratelModeratelLongleaf pine      -------   1 65   1   71   'Loblo3ly pine.
              Leon              I          I         I          I          I                        I      I        I
                                I          I         I          I          I                        I      I        I
            L ---------------   ISlight    ISevere   ISevere    kevere     ILoblolly pine -------   1 94   1 129    ILoblolly pine,
              Lumbee                       I                    I          IPond pine -----------   I---   I          water tupelo,
                                           I                    I          lWater tupelo --------   I---   I          sweetcrum.
                                           I                    I          ISweetgum -------------  I---   I ---    I
                                                                I          lWhite oak -----------   I---   I ---    I
            Ln --------------   ISlight    IModeratelSlight     ISevere    Loblolly pine  -------     86     129    ILoblolly pine
              Lynchburq         I          I         I          I          Longleaf pine  -------     74       86     American
                                I          I         I          I          IYellow poplar -------     92       86     sycamore,
                                I          I                               ISweetqum ------------   1 90   1 100    1 sweetgum.
                                I          I                               1coutbern red oak  ----  I---   I ---    I
                                I          I                               1"ite oak  ---:-------   I---   I ---    I
                                I          I                               IBlackgum ---- -------   I---   I ---    I
                                I          I                               I                        I      I        I
            Ly --------------   1Sliqht    iModeratelModeratelModeratelLoblolly pine      -------   1 80   1 114    ILoblolly pine.
              Lynn Haven        I          I         I          I          ILongleaf pine -------   1 70   1 _86    1
                                                                           IPord pine -----------     70
                                                                           I
            Mo --------------   ISlight    ISevere   ISevere    ISevere    lSweetqum ------------   1100   1 143    ISweetgum.
              Mouzon            I          I         I          I          lBaldcypress-: -------   I---   I ---    I
                                I          I         I          I          ISwamp tupelo  -------   I---   I ---    I
                                I          I         I          i          I                        I      I        I
            Na --------------   ISlight    ISevere   ISevere    ISevere    ISweetclum ----:-------  1_90   1 100    ISweetgum.
              Nakina            I          I         I          I          lWater oak --- -------   I -    I ---    I
                                I          I         I          I          I                        I   -  I        I
            NoA -------------   ISlight    ISlight   ISlight    lModeratelLoblolly pine   -------   1 90   1 129    ILoblolly pine,
              Noboco            I          I         I          I          ILongleaf pine -------   1 80.1   100    1 American
                                I                    I          I          ISoutbern red oak  ----  I---   I ---    I sycamore,
                                                     I          I          ISweetgum ------------   I---   I ---    I sweetqum.
                                                     I          I          I                        I      I        I
            OcA -------------   ISlight    IModeratelModeratelModeratelLoblolly pine      -------     85   1 114    ILoblolly pine.
              Ocilla            I          I         I          I          ILongleaf pine -------     77     100    1
                                I          I         I          I          I                                        I
            Og --------------   ISlight    Severe    lModeratelModeratelLoblolly pine     --- :---1   90   1 129    lLoblolly pine,
              Ogeechee          I                    I          I          IPond pine ------- ---     70              sweetgum.
                                I                    I          i          I
            Os --------------   ISlight    ISevere   ISevere    ISevere    lqweetqum-               1-90   1 100    ISweetgum,
              Osier             I          I         I          I          lWater tupelo: -------   I --   I ---      water oak.
                                I          I         I          I          lBaldcypress ---------   I --- I
                                1          11        1          1          1                        1      1
            Pa --------------   ISlight    ISevere   ISevere    ISevere    Loblolly pine  -------     98     129    Loblolly pine,
              Pantego           I          I         I          I          IPond pire --- :-------  1 73   1 ---      sweetgum,
                                I          I         I          I          lBaldcypress - -------   I --   I ---    i American
                                I          I         i          I          Nater tupelo:--:   ----  I                 sycamorer
                                I          I         I          I          lWater oak --- -- ----   I                 water tupelo.
            Pe --------------   ISlight    ISevere   ISevere    ISevere    Loblolly pine  -------     90     129    ILoblolly pine.
              Pelham            I          I         I          I          ILongleaf pine -------   1 80   1 100    1
                                I          I         I          I          lgweetqum ------------   1 80   1   86   1
                                                     i          I          IBlackgum ---- -------   1 80   1 114    1
                                                     I          I          lWater oak --- -------   1 80   1 -      I
                                                     I          I          I                        I      i   __   I
            Pm --------------   ISlight    ISevere   ISevere    ISevere    IPond pine --- -------   1_60       39
              Plummer           I          I         I          I          lBaldcypress - -------   I
                                I          I         I          I          lFwamp tupelo --------   I --- I  ---    I
                                I          I         I          I    -     I                        I      I        I

                 See footnote at end of table.








          1  12                                                                                                                     Soil Survey




                                             TABLE 7.--WOODLAND MANAGEMENT AND PRODUCTIVITY--Continued

                                             Manacement concerns                     Potential productivity
               Map symbol and                  Equip-              I                                   I      I
                   soil name      iErosior   I ment     Seedling     Plant         common trees        Site IProduc-I     Trees to
                                  Ihazard    I limita-I                                                I
                                                        mortal-    1competi-I                          indexitivity     I  plant
                                  I          I tion        ity     I ti"                                      class*
                                  I          I                     I
              R---------------    ISlight    ISevere    ISevere    ISevere    ILoblol)y pine  -------  1  94  1  129    ILoblolly pine,
               Rains              I                                           1Sweetgum ------------   1  90  1  100    1 sweetgum,
                                                                                                                         American
                                                                                                                         sycamore.
              Ru --------------   I'Slight   ISevere    ISevere    ISevere    ISweetgum ------------      90  1  100    ISweetqum,
               Rutlege                                  I          I          1Pin oak -------------      85  1   57    1 baldcvpress.
                                                        I          I          I                               I         I
              Se --------------   ISlight    114oderatelModeratelModeratelLoblolly pine       -----    1  80  1  114    ILoblolly pine.
               Seagate            I          I          I          I          ILongleaf pine  ----- :--1  70  1   86    1
                                  1          1          1          1          1                        1      1         1
              Wa --------------   ISlight    IModeratelModeratelSevere        Loblolly pine--             86     129    Loblolly pine,
               Wahee              I          I          I          I          Sweetgum  -------           90     100    1sweetgum,
                                                                              Blackgum  ------------   I --      ---    IAmerican
                                                                              lWater oak -----------   I---   I  ---    Isycamore,
                                                                              ISwamp chestnut oak--I          I  ---    Iwater oak.
                                                                              ?Willow oak  -------- :-I       I  ---    I
                                  I          I          I          I          ISoutbern red oak-- -1    ---   I  ---    I
                                  I          I          I          I          I                        I      I         I
              YaA  -------------  ISlight    lModerateiSlight      !Moderate!Loblolly pine    -------     go     129    Loblolly pine,
               Yauhannah          I          I          I                     Sweetgum  ------------      90     100    1yellow poplar,
                                  I                     I                     ISouthern red oak  ----     80      57     sweetgum,
                                  I                     I          I          IWhite oak ------ :----  1  80  1   57    1American
                                  I                     I          I          IYellow poplar  -- ----  1100      114     sycamore.
                                                                              ILonqleaf pine  -------  1  80      00
              Ye --------------   ISliqht    IModerate  Slight     iSevere    Loblolly pine   -------     90     129    Loblolly pine.
               Yemassee           I          I                     I          Sweetgum  ------------      95     114     American
                                  I                                           Southern red oak   ----   ---      ---     sycamore,
                                                                              White oak  -----------                     yellow poplar.
                                             I                     I          IYellow poplar  -------  1100   1  114.   1
                                                                              ILoriqleaf pine -------  1  80     loci   I
                                                                              IBlackgum ------------   I
                                             I          I          I          lHickory -------------   I---   I


                     Productivity class      is the yield in cubic feet       per acre per year calculated     at the age of
             culmination of mean annual increment f0T fully stocked natural stands.
                                                                              I
                                                                              I








       Dorchester County, South Carolina                                                                                                   113



                                                     TABLE 8.--RECREATTONAL DEVELOPMENT

         [Some terms that describe restrictive soil features are               defined in the Glossary. See text for definitions
               of "slight," "moderate," and "severe." Absence of               an entry indicates that the soil was not rated]



              Map symbol and
                  soil name              Camp areas          Picnic areas          Playgrounds      jPaths and trailsi     Golf fairways


         AbA  -------------------     ISevere:             ISevere:            Severe:              Isevere:             Severe:
                                      I                                                             I
           Albany                      wetness.            I too sandy.          too sandy,           too sandy.           droughty.
                                      I                    I                   I wetness.           I
         ApB  -------------------     Severe:              ISevere:            ISevere:             ISevere:             ISevere:
           Alpin                      I too sandy.         I'too sandy.        I too sandy.         I too sandy.           droughty.
                                      I                    I                   I                    I
         BIA  -------------------     ISevere:             iSevere:            ISlight  ----------  ISevere:             ISevere:
           Blanton                    I too sandy.         I too sandy.        I                      too sandy.         I droughty.
                                      I                    I                   I                                         I
         BIB  -------------------     ISevere:             ISevere:            IModerate:           ISevere:             ISevere:
           Blanton                    I too sandy.         I too sandy.        I slope.             I too sandy.         I droughty.
                                      I                    I                   I                    I                    I
         FoA, BoB  --------------     ISevere:             ISevere:            ISevere:             ISevere:             IModerate!
           Bonneau                     too sandy.           too sandy.           too sandy.         I too sandy.         I droughty.
                                                                                                    I                    I
         Br   --------------------    !Severe:             1,Severe:           I.Severe:            IlSevere:            !Severe:
           Brookman                    flooding,            wetness.             wetness,             wetness.             wetness,
                                       wetness.                                  flooding.                                 flooding.
         Ca   ---------------- I----  ISevere-             ISevere:            ISevere!             ISevere:             ISevere:
           Capers                     Iflooding,           I pondinq,          I pondinq,             pondinq.           I excess salt,
                                      I                    I excess salt.        flooding.                               I excess sulfur,
                                       pondinq,
                                      Ipercs slowly.                                                                       ponding.
                                      I
         ChA  -------------------     ISevere:             ISevere:            ISevere:             ISevere:             ISevere:
           Chipley                    I too sandy.         I too sandy.        1, too sandy.          too sandy.         I droughty.
         CoR  -------------------     ISevere:             !Severe:            I'Severe:            ISevere:             !Moderate:
           Chisolm                     too sandy.           too sandy.           too sandy.           too sandy.           droughty.
         Cs   --------------------    IModerate:           IModerate:          IModerate:           Slight   ----------- IModerate:
           Coosaw                     I wetness.            wetness.           .1 wetness.                               I droughty.
                                      I
         Cx   --------------------    ISevere:             ISevere:            ISevere:             ISevere:             ISevere:
           Coxville                   I wetness.           I wetness.            wetness.           I wetness.           I wetness.
                                      I                    I                                        I                    I
         Da   --------------------    IlSevere!            iSevere:            ISevere:             ISevere!             ISevere:
           Daleville                   wetness.            I wetness.          I wetness.             wetness.             wetness.
         PC   --------------------    Severe:              Severe:             ISevere:             ISevere:             IModerate:
           Echaw                       too sandy.           too sandy.           too sandy.         I too sandy.         1 droughty.
         Eo   --------------------    ISevere:             ISevere:            ISevere:             ISevere:             ISevere:
           Elloree                    I flooding,          1, wetness.         I wetness.           I wetness.           I wetness.
                                      I
                                       wetness.
         EpB  -------------------     IModerate:           !Moderate:          IModerate:           ISliqht  ----------  IModerate:
           Emporia                    I percs slowly.       percs slowly.        Slope,             I                    I droughty.
                                      I                                          small stones       I                    I
                                      I
                                                                                 percs slowly.      I
                                      I                                                             I
         EuA  -------------------     IModerate:           IModerate-          IModerate-           IModerate:           IModerate:
           Eulonia                    1, percs slowly,     I wetness'          I percs slowly,        wetness.             wetness.
                                                                     r
                                       wetness.                      lowly.    I wetness.
                                                            percs s            I








              114                                                                                                                                Soil Survey



                                                     TABLE 8.--RECREATTONAL DEVELOPMENT-Continued



                   Map symbol and
                                                Camp areas           Picnic areas           Playgrounds      IPaths and trailsi        Golf fairways
                       soil name



              FuB -------------------       IModerate:           !Moderate:             IModerate:           IModerate:             iModerate:
                Eulonia                     Ipercs slowly,         wetness,             I slope,             I wetness.              wetness.
                                            I                                           I                    I
                                             Vretness.             percs slowly.         wetness,
                                                                                         percs slowly.
              FoA -------------------       I'Sliqht ----------  'Slight   ----------   ISlight  ----------  iSlight------------IModerate-
                Foreston                                                                I                                           I
                                                                                                                                     droughty-
              FXB -------------------       iSeveret             ISevere:               iSevere:             ISevere:               IlModerate:
                Foxworth                     too sandy.          i too sandy.           I too sandy.         I too sandy.            droughty,
                                                                 I                      I                    I
                                                                                                                                     too sandy.
                                                                 I                      I                    I
              GoA -------------------       IModerate:           iModerate:             IModerate:           ISliqht   -----------  !Slight.
                Goldsboro                    ifetness.           I wetness.             I wetness.           I
              Gr  --------------------      !Severe:             ISevere:               Severe:              !severe:               Severe:
                Grifton                      'Flooding,          I wetness.              wetness.              wetness   .           wetness.
                                             wetness.            I
                                                                 I
              Hb  --------------------      iSevere:             IlSevere:              IlSevere:            ISevere:               IlSevere-
                Handsboro                    flooding,             pondinq,              excess   humus,       pondinq,              excess salt,
                                             pondinq,              excess humu4          ponding,              excess humus.         excess sulfur,
                                             excess humus.         excess   salt..       flooding.                                   pondina.

              Hp.
                Haplaquents
              IzA --------------------      IModerate:           IModerate:             IModerate:           ISevere:               ISlight.
                Tzaqora                     I wetness.           I wetness.             I wetness.           I erodes    easily.    I
                                            I                    I                      I                    i                      i
              IzB -------------------       IModerate:           IModerate:             IModerate:           ISevere:               'Slight.
                Izaqora                      wetness.              wetness.              slope,                erodes    easily.
                                                                                         wetness.
              Jd  --------------------      iSevere:             ISevere:               ISevere:             ISevere:               ISevere:
                Jedburq                     I wetness.           I wetness.             I wetness.             wetness.             I wetness.
                                            i                    I                      I                                           i
              JoA -------------------       ISevere:             IModerate:             IModerate:           IModerate:             IModerate:
                Johns                       I"flooding.          I wetness.             I wetness.           I wetness.              wetness,
                                            I                    I                      I                    I                       droughty.
                                            I
              Le  --------------------      locevere:            ISevere:               ISevere:             ISevere:               Severe:
                Leon                         wetness,            I wetness,             I                    I
                                                                                        I too sandy,           wetness,              wetness,
                                                                   too sandy.            wetness.            I too sandy.            droughty.
                                             too sandy.
              Lm  --------------------      ISevere:             ISevere:               ISevere:             ISevere:               ISevere:
                Lumbee                       flooding,           I wetness.              wetness.            I wetness.             I wetness.
                                             wetness.            I                                           I                      I
              Ln  ----------                Severe:              ISevere:               Severe:              iSevere:               ISevere:
                Lynchburg                    wetness.              wetness.              wetness.            I wetness.              wetness.
                                                                                                             I
              Ly  --------------------      I'levere:            ISevere:               ISevere:             ISevere:               ISevere:
                Lynn Haven                   wetness,              wetness,              too sandy,            wetness,             I wetness,
                                            I too sandy.           too sandy.            wetness.              too sandy.           I droughty.
                                            I                                                                                       I
              Mo  --------------------      ISevere:             ISevere:               ISevere:             ISevere:               ISevere:
                Mouzon                      I wetness,           I wetness.             I wetness,           I wetness.             I wetness,
                                            I flooding.          I                       flooding.           I                       flooding.









      Dorchester County, South Carolina                                                                                                   115




                                            TABLE 8.--RECREATIONAL DFVELOPMFNT--Continued



            Map symbol and
                soil name              Camp areas          Picnic areas          Playgrounds      IPatbs and trailsl      Golf fairways
                                                                                                  I

        Na --------------------     ISevere:            ISevere:             ISevere:             ISevere:             ISevere:
         Nakina                     I wetness.          I wetness.           I wetness.             wetness.           I wetness.
                                    I                   I                    I                                         I
                                    I                   1                    11                                        1
        NoA -------------------     ISligbt  ---------- ISligbt  ----------  ISliqht  ----------  ISligbt  ----------  !Moderate:
         Noboco                     I                   I                    I                    I                      droughty.
                                    I                   I                    I                    I
        OcA -------------------     ISevere:            IlSevere:            ISevere:             IlSevere:            IModerate:
         Ocilla                     I too sandy.          too sandy.         I too sandy.           too sandy.         I wetness,
                                    I                                        I                                         I drouabty,
                                    I                                        I                                         I too sandy.
                                    I                                        I                                         I
        Og --------------------     ISevere:            ISevere:             ISevere:             ISevere:             ISevere:
         Ogeechee                   I flooding,         I                    I                    I                    I wetness.
                                                        I wetness.             wetness.             wetness.
                                    Iwetness.
                                    I
        Os --------------------     ISevere:            ISevere:             Isevere:             ISevere:             ISevere:
         Osier                      I wetness,            wetness.           I wetness.           I wetness.           I wetness,
                                    I ponding.                               I                    I                    I droughty.
                                    I                                        1                    11                   1
        Pa --------------------     ISevere:            ISevere:             IlSevere:            !Severe:             Severe:
         Pantego                    I                   1                                         11                   i
                                     wetness.             wetness.             wetness.             wetness.             wetness.
                                                        1                                         11
        Pe --------------------     ISevere:            ISevere:             iSevere:             Severe:              IlSevere:
         Pelham                     I wetness,          I wetness,           I too sandy,           wetness,             wetness.
                                     too sandy.           too sandy.           wetness.             too sandy.
        Pm --------------------     ISevere:            ISevere:             IlSevere:            !Severe:             ISevere:
         Plummer                    I wetness.          I wetness.             wetness.             wetness.           I wetness,
                                    I                   I                                                                droughty.
                                    I                   I
        Ra --------------------     ISevere:            ISevere:             ISevere:             ISevere:             ISevere:
         Rains                      I wetness.          I wetness.           I wetness.           I wetness.           I wetness.
                                    I                   I                    I                    I                    I
        Ru --------------------     ISevere:            ISevere:             ISevere:             ISevere:             iSevere:
         Rutlege                    I flooding,         I wetness.             wetness,             wetness.             wetness,
                                     wetness.                                  flooding.                                 droughty,
                                                                                                                         flooding.
        Se --------------------     ISevere:            'Severe-             ISevere:             ISevere:             ISevere:
         Seagate                    I too sandy.        I too sa*ndy.        I too sandy.         I too sandy.           droughty.
                                    I                   I                    I                    I
        Wa --------------------     iSevere:            ISevere:             ISevere:             ISevere:             ISevere:
         Wahee                      I wetness.            wetness.           I wetness.           I wetness.           I wetness.
                                    I                                        I                    I                    I
        YaA -------------------     IModerate:          IModerate:           IModerate:           IModerate:           IModerate:
         Yauhannab                  I wetness.          I wetness.           I wetness.             wetness.           I wetness,
                                    I                                                                                    droughty.
                                    I
        Ye --------------------     ISevere:            IModerate:           'Severe:             Moderate-            IModerate:
         Yemassee                   I wetness.            wetness.           i wetness.             wetness.           I wetness.
                                    I                                        I                                         I








               116                                                                                                                                    Soil Survey




                                                                       TABLE 9.--WILDLTFE HABITAT

                fSee text for definitions of "qood," "fair," "poor," and "very poor." Absence of an entry indicates that the
                      soil was not ratedl.


                                          I                     Potential    for habitat elements                                  ntial as habitat for--
                   Map symbol and         I-         I              Wild     '           I           I            I           I    ------T- I
                     soil name             Grain ilGraqses          herba-   lHardwo(,. Conif-       lWetland     ISballow OpenlandlWoodlandlWetland
                                                                             I trees                              11                                  1
                                          and see-d' an           I ceous                   erous    I plants      water      lwildlifelwildlife wildlife
                                                                                                                                          I           I
                                           crops     1,legrumes     plants                 plants    I            Iareas      I
               AbA ----------------       jFair      lFair        iFair      lFair       lFair       lFair        Poor        lFair       lFair       'Poor.
                Albanv
               ApB ----------------       IPoor      lFair        Fair       IPoor       lFair       lVery        lVery       'Fair       ',Fair      lVery
                Alpin                     I          I                       I           I           I poor.      I poor.                              poor.
                                          I          I                       I           I           i            I
               BIA, BIB   -----------     1,Poor     lFair        1,Fair     1,Fair      1,Fair      1,Very       1,Very      lFair       ,Fair       Very
                Blanton                                                                                poor.       poor.                               poor.
               BoA, BoB   -----------     !Good      !Good        lGood      lGood       lGood       )Poor        IPoor       lGood       'Good       IPoor.
                Bonneau
               Br  -----------------      lVery      iPoor        lFair      IPoor       1,Poor      lGood        lGood       I.Poor      lFair       lGood.
                Brookman                  Ipoor      I            I          I           I           I            I           I           I           I
                                                                                         I           It           i           I           I           i
               Ca  -----------------                                         I  ---      I  ---      IG,,d        I.Good      I  ---      1  ---      lGo,d.
                Capers                                                                                                                                i
               CbA ----------------       IPoor      1,Fair       IFair      IFair       IFair       !,Very       lVery       IFair       IFair       1,Very
                Cbipley                   I                       I          I           I                 Dr      poor       I           I
                                                                                                       pol                                             poor.
               CoB -----------------      lGood      lGood        Good       I                       lVery        lVer        Good        !Good       lVery
                                                                             Good        Good        I            I    y
                Chisolm                                                                                poor.       poor.                               poor.
               CS  -----------------      11Poor     !Fair        lGood      1Poor       lGood       IPoor        !Poor       11Fair      lGood       1,Poor.
                Coosaw
               Cx  -----------------      1,Good     iGood        iGood      lGood       lGood       IPoor        Fair        lGood       lGood       IPoor.
                Coxville
               Da  -----------------      iPoor      lFair        lFair      lGood       lFair       lGood        lGood       lFair       lGood       iGood.
                Daleville                 I          I            I          I
                                          I          I            I          I
               Ec  -----------------      11poor     lFair        Good       lFair       lFair       IPoor        lVery       lFair       lFair       Very
                Ecbaw                                                                                              poor.                               poor.
               Eo  ------------------     poor       iFair        lFair      lFair       lFair       lGood        lGood       lFair       lFair       lGood.
                Elloree                   I          I            I          I           I           I            I           I           I           I
                                          I          I            I          I           i           i            I           I           I           I
               EpR ----------------       'Good      lGood        11Good     lGood       !Good       IPoor        iVery       iGood       lGood       lVery
                                          I                                  I                       I            I                       I           I
                Emporia                                                                                            poor.                               poor.
               EuA, EuB----               Good       Good         lGood      lGood       Good        IPoor        1,Poor      lGood       lGood       IPoor.
                Eulonia
               FoA ----------------       1,Good     'Good        lGood      ')Good      Good        Poor         Poor        Good        lGood       1,Poor.
                Foreston
               FxB ----------------       1,Fair     Fair         ',Fair     !Fair       lFair       lVery        lVery       lFair       lFair       lVery
                Foxworth                                                                               poor.      I poor.                              poor.
               GoA ----------------       jGood      I.Good       lGood      1,Good      'Good       ,Poor        Poor        lGood       Good        !Poor.
                Goldsboro
               Gr  -----------------      1Poc-r     lFair        lFair      lFair       Fair        lGood        lFair       lFair       11Fair      lFair.
                Grifton









      Dorchester County, South Carolina                                                                                         117




                                              TABLE 9.--WILDLTFE HABITAT--Continued

                                               -Potential   for habitat elements                    Potential as habitat for-:@
          Map symbol and                            Wild    I         I         I                             I          I
            soil name         Grain IGrasses      I herba-  IHardwoodl Conif-   IWetland Shallow    10penlandIlWoodlandiWetland
                             and seedl and        l ceous   I trees   I erous   I plants  I water   lvildlifelwildlifelwildlife
                               crops    1legoes     21ants             plants                areas

       Hb -----------------  IVery      IVery     IVery     IVery     IVery     IPoor     IVery     lVery     lVery      IPoor.
          Handsboro          I poor.    I poor.   I poor.   I poor.   I poor.   I         I poor.   I poor.   I poor.    I

       Hp.
          Haplaquents
       IzA ----------------  IGood      lGood     iGood     IGood     IGood     IPoor     IPoor     iGood     IGood      IPoor.
          Izagora
       IzB ----------------  lGood      IGood     lGood     lGood     IGood     IPoor     IVery     IGood     lGood      lVery
          Tzagora            i          I         I         I         I         I         I poor.   I         I          I poor.
                             I          I         I         I         I         I         I         I         I          I
       Jd -----------------  IGood      lGood     IGood     IGood     lGood     IFair     IFair     lGood     lGood      IFair.
          Jedburg            I          I         I         I         I         I         I         I         I          I
                             I          I         I         I         i         I         I         I         I          I
       JoA ----------------  IFair      lGood     IGood     lGood     IGood     IPoor     lVery     lGood     lGood      IVery
          Johns              I                                                              poor.   I         I            poor.
                             I                                                                      I         I
       Le -----------------  IPoor      lFair     IGood     IPoor     IFair     IFair     IPoor     lFair     IFair      IPoor.
          Leon               I          I         I         I         I         I         I         I         I          I
                             I          I         I         I         I         I         I         I         I          I
       Lm -----------------  IPoor      IFair     IFair     IFair     IFair     IGood     IFair     IFair     IFair      IFair.
          Lumbee             I          I         I         I         I         I         I         I         I          I
                             I          I         I         I         I         I         I         I         I          I
       Ln -----------------  IFair      lGood     lGood     IGood     IGood     lFair     IFair     lGood     IGood      IFair.
          Lynchburq          I          I         I         I         I         I         I         I         I          I
                             1          11        1         1         1         1         1         1         1          1
       Ly -----------------  IPoor      IFair     IFair     IPoor     IPoor     IFair     IFair     IFair     IPoor      IFair.
          Lynn Haven         I          I         I         I         I         I         I         I         I          I
                             I          I         I         I         I         I         I         I         I          I
       Mo -----------------  IVery      IVery     IVery     IFair     IFair     IGood     lGood     lVery     IPoor      IGood.
          Mouzon             I poor.    I poor.   I poor.   I         I         I         I         I poor.   I          I
                             I          I         I         I         I         I         I         I         I          I
       Na -----------------  IFair      IFair     IFair     IGood     IGood     lGood     lGood     IFair     lGood      IGood.
          I
          Nakina             I          I         I         I         I         I         I         I         I          I
                             I          I         I         I         I         I         I         I         I          I
       NoA ----------------  IGood      Good      Good      IGood     lGood     IPoor     IVery     lGood     IGood      IVery
          Noboco             I                              I         I         I         I poor.   I         I          I poor.
                             I                              I         I         I         I         I         I          I
       OcA ----------------  IFair      IFair     lGood     IFair     lGood     IFair     IFair     IFair     IGood      IFair.
          Ocilla             I          I         I         I         I         I         I         I
                             I          I         I         I         I         I         I         I
       Og -----------------  IPoor      IFair     IFair     IFair     IFair     IGood     IGood     lFair     IFair      IGood.
          Ogeechee           I          I         I         I         I         I         I         I         I          I
                             I          I         I         I         I         I         I         I         I          I
       Os -----------------  IVery      IPoor     IFair     lFair     IFair     IFair     IGood     IPoor     IFair      IFair.
          Osier              I poor.    I         I         I         I         I         I         I         I          I
                             I          I         I         I         I         I         I         I         I          I
       Pa -----------------  lVery      IPoor     IPoor     IPoor     IPoor     lGood     IFair     IPoor     IPoor      IFair.
          Pantego               poor.   I         I         I         I         I         I         I         I          I
                                        I         I         I         I         I         I         I         I          I
       Pe -----------------  IPoor      IFair     lFair     lFair     IFair     IFair     IFair     lFair     IFair      IFair.
          Pelham             I          I         I         I         I         I         I         I         I
                             I          I         I         I         I         I         I         I         I
       Pm -----------------  IVery      iPoor     IPoor     IPoor     IPoor     lGood     IGood     IPoor     IPoor      IGood.
          Plummer            I poor.
                             I
       Ra -----------------  IFair      IFair     IFair     lGood     lGood     IGood     IGood     lFair     IGood      IGood.
          Rains









           118                                                                                                               Soil Survey




                                                   TABLE 9.--WILDLIFE HABITAT--Conttnued

                                                     Potential  for habitat elements                          tial as habiFat -for--
               Map symbol and                           Wild
                 soil name         Grain    Grasses   I herba-  Hardwoodl  Conif -  Wetland   khallow   10penlandIWoodlandIWetland
                                  and seedi, and      l ceous   I         I er                                     wildlifelwildlife
                                                                 trees         ous  I plants   water    1wildlifel
                                                                          I                                        I         I
                                                   s  I         I         I
                                   crops llequmie       plants             plants   I           areas   I                    i

           Ru  ------------       Very      IPoor     IPoor     IPoor     iPoor     IFair     Good      IPoor      IPoor     IFair.
            Rutleqe                poor.    I         I         I         I         I                   I          I         I
                                            I         I         I         I         I                   i          1         11
           Se  -----------------  Poor      IPoor     I.Fair    IPoor     IPoor     Poor      IPoor     IPoor      Poor      !Poor.
            Seaqate
           TAa -----------------  Good      Good      IGood     IGood     lGood     IPoor     IPoor     lGood      IGood     IPoor.
            Wahee
           YaA ----------------   !Good     !Good     !Good     lGood     IGood     IPoor     IPoor     lGood      IGood     IPoor.
            Yauhannah             I         I         I         I         I         I         I         I          I
                                  I         I         I         i         I         I         I         I          I
           Ye  -----------------  IFair     IGood     lGood     lGood     lGood     IFair     IFair     lGood      IGood     IFair.
            Yerriassee








       Dorchester County, South Carolina                                                                                                      119




                                                      TABLE 1O.--BUILDING SITE DEVELOPMENT

       fSone terms that describe restrictive soil features are defined in the Glossary. See text for definitions of
            11sliqbt," "moderate," and "severe." Absence of an entry indicates that the soil was not rated. The
            information in     this table indicates the dominant soil condition; it does not                 eliminate the need for onsite
            investigationj


                             I                    I                  I                   I                   I                   I
          Map symbol and     I     Shallow        J  Dwellings       I   Dwellings       I       Small       I  Local roads      I   Lawns and
            soil name           excavations           without                with           commercial          and streets         landscaping
                                                     basements           basements           buildings


       AbA ---------------   ISevere:             ISevere-           ISevere:            iSevere:            IModerate:          ISevere:
       Albany                I cutbanks cavej wetne;s.                 wetness.          I wetness.          I wetness.            droughty.
                             I wetness.           I                                      I                   I
                             i                    i                                      I                   I
       ApB ---------------   ISevere:             ISligbt ---------  ISliqht  ---------  ISlight  ---------  1Sliqht  ---------  ISevere:
       Alpin                 I cutbanks   cave.1                     I                   I                   I                   I droughty.
                             I                    I                  I                   I                   1                   11
       BIA ---------------   ISevere:             ISliqbt ---------  IModerate-          ISlight  ---------  klight   ---------  ISevere:
       Blanton               I cutbanks   cave.1                       wetness.          I                                         droughty.
                             I                    I                                      I
       BIB ---------------   ISevere:             Iqlight ---------  IModerate:          IModerate:          ISlight  ---------  ISevere:
       Blanton               I cutbanks   cave.1                     I wetness.          I slope.            I                   I droughty.
                             I                    I                  I
       .BoA ---------------  ISevere:             ISliabt ---------  IModerate:          ISligbt  ---------  ISligbt  ---------  IModerate:
       Bonneau               I cutbanks   cavP.11                      wetness.          I                   I                   I droughty.
       BoB ---------------   'Severe:             ISliabt ---------  iModerate-          IModerate:          Slight   ---------- IModerate,
       Bonneau               I cutbanks   cave.1                       wetness.          I slope.                                  drouqhty'-
                             I                    I                                      I
       Br ----------------   ISevere:             ISevere:           ISevere:            Severe:             !Severe:            ISevere:
       Brookman              I wetness.            flooding,           floodingo,          flooding,           flooding,         I wetness,
                             I                     wetness.            wetness.            wetness.            wetness,          1 flooding.
                             I                                                                                 low strength.
                             I
       Ca ----------------   ISevere:             Severe:            'Severe-            'Severe-            ISevere-            ISevere-
       Capers                I ponding.            flooding,         I flooding,         I flooding,         I low st*renqt.hl   1, exces's salt,
                             I                     pondinq,          I ponding,          I ponding,          I pondinq,            excess sulfur,
                             I                     shrink-swell.       shrink-swell.     I shrink-swell      I flooding.         I
                             I                                                           I                .  I                   I ponding.
       ChA ---------------   ISevere:             IModerate-         ISevere:            IModerate:          IModerate:          ISevere:
       Chipley               I cutbanks cavej wetness'.              I wetness.            wetness.          I wetness.          I droughty.
                             I wetness.           I                  I                                       I                   I
                             I                    I                  I                                       I                   I
       CoB ---------------   ISevere:             ISlight ---------  IModerate:          iSligbt  ---------  ISlight  ---------  lModerate:
       Chisolm               11 cutbanks  cave.1                     I wetness.          I                                         droughty.

       C
       's -----------------  ISevere-             IModerate-         ISevere:            IModerate:          IModerate:          IModerate:
       Coosaw                I cutban'ks  cavej wetness.*            I wetness.          I wetness.          I wetness.          I droughty.
                             I wetness.           I
                             I                    I
       Cx ------             ISevere:             ISevere:           ISevere:            ISevere:            ISevere:            ISevere-
       Coxvill;   ---------  I wetness.           I wetness.         I wetness.          I wetness.          I low strength,     I wetness.
                             I                    I                  I                   I                   I wetness.
                             I                    I                  I                   I                   I
       Da ----------------   ISevere:             ISevere:           ISevere:            ISevere:            ISevere:            ISevere-
       Daleville             I wetness.           I wetness.           wetness.          I wetness.          I low strength,     I wetnes's.
                             I                    I                                      I                   I wetness.          I
       Ec ----------------   iSevere:             ISliqht ---------  IModerate:          lSliqbt  ---------  ISlight  ---------  IModerate:
       Echaw                 I cutbanks caveJ                        I wetness.          I                   I                   I droughty.
                             I                    I                  I                   I                   I                   I
       Eo ----------------   ISevere:             ISevere:           ISevere:            ISevere:            ISevere:            !Severe:
       Elloree               I wetness.           I flooding,          flooding,           flooding,         I wetness,            wetness.
                             I                    I wetness.           wetness.            wetness.          I flooding.









             120                                                                                                                             Soil Survey




                                                   TABLE 1O.--BUILDING SITE DEVELOPMENT--Continued


             Map symbol and           Shallow             Dwellings           Dwellings               Small          Local roads           Lawns and
                soil name           excavations            without               with            commercial           and streets         landscaping
                                                          basements           basements           buildings


         EpB ---------------     IModerate:          ISlight  ---------   IModerate:          IModerate-           IModerate:          IModerate-
                                                                          I                                        I low strength.     I drought'
             Emporia             I wetness.          I                    I wetness,          I slope                                              Y_
                                 I                   I                      shrink-swell.     I                    I                   I
                                 I                   I                                        I                    I                   I
         EuA ---------------     ISevere:            IModerate:           ISevere:            IModerate:           IModerate:          IModerate-
             Fulonia               wetness.          I wetness.           I wetness.          I wetness.           I low strength,     I wetness*.
                                                     I                    I                   I                    I wetness.          I
                                                     I                    I                   I                    I                   I
         EuB ---------------     ISevere:            IModerate:           ISevere:            IModerate:           IModerate:          IModerate-
             Eulonia             I wetness.          I wetness.           I wetness.          I wetness,           I low strength,     I wetness'.
                                 I                   I                    I                   I slope.             I wetness.
                                 I                   I                    I                   I                    I
         FoA ---------------     ISevere:            IModerate-           IModerate:          IModerate:           IModerate:          11-loderate:
             Foreston            I cutbanks cave.1 wetness.*              I wetness.          I wetness.           I wetness.          I droughty.
                                 I                   I                    I                   I                    I                   I
         FxB ---------------     ISevere:            ISlight  ---------   IModerate:          ISlight  ---------   ISlight  ---------- IModerate:
             Foxworth            I cutbanks cave.1                        I wetness.          I                    I                   I droughty,
                                                                                                                                         too sandy.
         GoA ---------------     ISevere:            IModerate:           ISevere:            IModerate:           IModerate:          ISlight.
             Goldsboro           I wetness.            wetness.           I wetness.          I wetness.           I wetness.          I
                                 I                                        I                   I                    I                   I
         Gr  ----------------    ISevere:            ISevere:             iSevere:            ISevere:             ISevere-            ISevere:
             Grifton               wetness.          I flooding,          I flooding,         I flooding,          I flooding,           wetness.
                                                     I wetness.           I wetness.          I wetness.'          I wetness.
         Hb  ----------------    ISevere:            iSevere-             ISevere:            ISevere-             ISevere:            ISevere:
             Handsboro           I excess   humus,   I flooding,          I flooding,         I flooding           I ponding           I excess salt,
                                 I                   I                    I Pondino           I ponding"                               I
                                   ponding.          I ponding,                                                    I floodincr.          excess sulfur,
                                 I                     low strength.      I low str;ngth.     I low strength.      I                   I ponding.

         Hp.
             Haplaquents
         IzA ---------------     ISevere:            IModerate:           ISevere:            111oderate:          ISevere:            !Slight.
             Izagora               wetness.            wetness.             wetness.            wetness.             low strength.
         IzB ---------------     ISevere:            IModerate:           ISevere:            IModerate:           ISevere:            ISlight.
             Izagora               wetness.            wetness.             wetness.            wetness,             low strength.
                                                                                                slope.
         Jd  ----------------    ISevere:            ISevere:             ISevere:            ISevere:             ISevere:            ISevere:
             Jedburg             I wetness.          I wetness.           I wetness.          I wetness.           I wetness.          I wetness.
                                 I                   I                    I                   I                    I                   I
         JoA ---------------     ISevere:            ISevere-             10evere:            ISevere:             IModerate:          IModerate:
                                 I                                        @-flooding,           flooding.                   -s,        I
             Johns                 cutbanks: cave,1 flooding                                                         wetnes              wetness,
                                   wetness.          I                    I wetness.                                 flooding.         I droughty.
                                                     I                    I                                                            I
         Le  ----------------    ISevere:            ISevere-             iSevere:            ISevere:             lSevere::           ISevere:
             Leon                I cutbanks   cave,i wetnes's.            I wetness.            wetness.           I wetness.            wetness,
                                 I wetness.,         I                    I                                        I                     droughty.
                                 I                   I                    1                                        11
                                                                          ISevere:            ISevere:             ISevere:            ISevere:
         Lm  ---------------     Severe:             ISevere-
             Lumbee              I cutbanks   cave,1 flooding,            I flooding,         I flooding,          I wetness.          I wetness.
                                 I                   I wetness.           I                   I                    I                   I
                                   wetness.                                 wetness.            wetness.
                                 I                   I                    I                   I                    I
         In  ----------------    ISevere:            ISevere:             ISevere:            ISevere:             iSevere::           ISevere:
             Lynchburg           I wetness.,         I wetness.             wetness.          I wetness.           I wetness.          I wetness.
         Ly  ----------------    ISevere:            ISevere-             ISevere:            ISevere:             ISevere:            ISevere:
             Lynn Haven          I cutbanks cavej wetnes's.                 wetness.          i wetness.           I wetness.          I wetness,
                                 i                                                                                                       droughty.
                                 I wetness.,









        Dorchester County, South Carolina                                                                                                   121




                                              TABLE 10.--BUILDING SITE DEVELOPMENT--Continued


         Map symbol and           Shallow           Dwellings           Dwellings              Small         Local roads          Lawns and
                                                     without               with           commercial
            soil name          excavations                                                                   and streets         landscaping
                                                    basements          basements           buildings


      Mo ----------------   ISevere:            19evere:            ISevere:           ISevere:            ISevere:            ISevere:
        Mouzon                wetness.          I wetness,          I wetness,         I wetness,          1. wetness,         I wetness,
                                                  flooding.         I flooding.        I flooding.          flooding.          I flooding.
                                                                    I                  I                                       I
      Na ----------------   ISevere:            Severe:             Severe:            ISevere:            ISevere:            ISevere:
        Nakina              I wetness.            wetness.           wetness.          I wetness.           wetness.           I wetness.
                            I                                                          I                                       I
      NoA ---------------   IModerate:          iSliqbt  ---------  IModerate:         islight  ---------  ISliqbt ---------   IModerate:
        Noboco              I wetness.          I                   I wetness.                                                  droughty.
                            I                   I                   I
      OcA ---------------   ISevere:            IModerate-          ISevere:           ISevere:            IModerate:          IModerate:
        Ocilla              I cutbanks   cave,1 wetness.*            wetness.          I wetness.          I wetness.           wetness,
                            I wetness.          I                                      I                   I                    droughty,
                                                                                                                                too sandy.
      Oq ----------------   ISevere:            ISevere:            ISevere:           IlSevere:           ISevere:            IlSevere:
        Ogeechee              flooding,         I flooding,         I flooding,          wetness.          I wetness.           wetness.
                              wetness.          I wetness.          I wetness.
                                                I                   I
      Os ----------------   ISevere:            IlSevere:           ISevere:           ISevere:            ISevere:            ISevere:
        Osier               I cutbanks   cave,    flooding,         I flooding,        I flooding,          wetness.            wetness,
                            I wetness.            wetness.          I wetness.         I wetness.                               droughty.
                            I                                       I                  I
      Pa ----------------   ISevere:            ISevere:            ISevere:           ISevere:            ISevere:            ISevere:
        Panteqo             I wetness.            wetness.          I wetness.         I wetness.          I wetness.          I wetness.
                            I                                       I                  I                   I                   I
      Pe ----------------   ISevere:            ISevere-            ISevere:           ISevere:            ISevere:            ISevere:
        Pelham              I cutbanks   cave.1 wetness.            I wetness.         I wetness.           wetness.           I wetness.
                            I wetness.          I                   I                  I                                       I
                            I                   I                   I                  I                                       I
      Pri ----------------  ISevere:            ISevere-            ISevere:           ISevere:            ISevere:            Severe:
        Plummer               cutbanks   cave,1 pondin*g.            pondinq.            ponding.           ponding.            ponding.
                            I ponding.
      Ra ----------------   ISevere:            ISevere:            ISevere:           ISevere:            ISevere:            ISevere:
        Rains               I wetness.          I wetness.          I wetness.           wetness.          I wetness.          I wetness.
                            I                   I                   I                                      I                   I
      Ru ----------------   ISevere:            IlSevere:           ISevere:           ISevere:            ISevere:            Severe:
        Rutlege             I cutbanks cave,      flooding,         I flooding,          flooding,         1, wetness,          wetness,
                              wetness.            wetness.           wetness.            wetness.           flooding.           droughty,
                            I                                       I                                                           flooding.
                            I                                       I
      Se ----------------   ISevere:            IModerate-          ISevere:           IModerate:          IModerate:          IModerate:
        Seagate               cutbanks   cave,1                                                            I                   I
        S                   .1                    wetness:          I wetness.         I wetness.           wetness.            wetness,
                              wetness.          I                   I                  I                   I                   Idroughty.
                                                I                   I                  I                   I                   I
      Ila ----------------  ISevere:            ISevere:            ISevere:           ISevere:            ISevere:            ISevere:
        Wahee               I wetness.          I wetness.          I wetness.         I wetness.          I low strength,      wetness.
                            I                   I                   I                  I                   I wetness.
                            I                   I                   I                  I                   I
      YaA ---------------   ISevere:            IModerate:          ISevere:           IModerate:          IModerate:          IModerate:
        Yauhannah           I wetness.          I wetness.          I wetness.         I wetness.          I wetness.          I wetness,
                            I                   I                   I                  I                   I                   I droughty.
                            I                   I                   I                  I                   I                   I
      Ne ----------------   ISevere:            ISevere:            iSevere:           iSevere:            IModerate:          IModerate:
        Yemassee            I wetness.            wetness.          I wetness.         I wetness.           wetness.            wetness.
                            I                                       I                  I   -









             122                                                                                                                                  Soil Survey




                                                                  TABLE II.--SANITARY FACILITIES

              [Some terms that describe restrictive soil features are defined in the Glossary. See text for definitions of
                    "slight," "good," and other terms.             Absence of an entry indicates that the soil was not rated. The
                    information in this table indicates the dominant soil condition; it does not eliminate                             the need for
                    onsite investigation]



                 Map symbol and              Septic tank           Sewage lagoon                Trench                  Area               Daily cover
                     soil name                absorption                                I
                                                                         areas                sanitary               sanitary             for landfill
                                                fields                                         landfill              landfill.-

              AbA -----------            Severe,.               fSevere:                fSevere:               ISevere:                IPoor:
              Albany                                            I seepage,              I wetness,             I seepage,                too sandy,
                                          wetness.              I wetness.              I too sandy.           I wetness.                wetness.
                                                                I                       I                      I
              ApB -----------------      ISlight -----------    ISevere:                ISevere:               ISevere:                IPoor:
              Alpin                      I                        seepage.              I seepage,               seepage.                too sandy,
                                         I                                              I too sandy.                                     seepage.
                                         I                                              I
              BIA, BIB  ------------     IModerate:             ISevere:                ISevere:               ISevere:                IPoor:
              Blanton                     wetness.                seepage.                too sandy.             seepage.                too sandy.
              BoA, BoB  ------------     ISevere:               ISevere:                ISevere:               ISevere:                lGood.
              Bonneau                    I wetness.             I seepage.              I wetness.             I seepage.              I
                                         I                      I                       i                      I                       I
              Br ------------------      ISevere:               I'Slight -----------    ISevere:               IlSevere:               IPoor:
              Brookman                   Iflooding,                                       flooding,              flooding,             I too clayey,
                                          wetness,                                        wetness,               wetness.              I hard to pack,
                                          percs slowly.                                   too clayey.                                  I wetness.
                                                                                                                                       I
              Ca ------------------      IlSevere:              ISevere-                ISevere:               ISevere:                IlPoor-
              Capers                      flooding,             I flooding,               flooding,            I flooding,               too clayey,
                                                                I                                              I
                                          pondinq,      ly.     I pondinq.                ponding,             I pondinq.                hard to pack,
                                          percs Slow            I                         too clayey.          I                         pondinq.
              ChA -----------------      ISeve-re:              ISevere:                ISevere:               ISevere:                IPoor:
              Chipley                    I wetness,               seepage,                seepage,               seepage,                too sandy,
                                         I poor filter.           wetness.                wetness,               wetness.                seepage.
                                         I                                                too sandy.
              CoB ----------------     @-IModerate-             ISevere:                !Severe:               iSevere:                !Good.
              Chisolm                    I wetness.               seepage.                seepage,             I seepage.
                                         I                                                wetness.             I
              Cs ------------------      ISevere:               ISevere:                !Severe:               iSevere:                IlFair:
              Coosaw                      weiness,                seepage,                wetness,               seepage,                wetness,
                                          poor filter.            wetness.                seepage.               wetness.                thir, layer.
              Cx ------------------      ISevere:               !Severe:                lSevere:               I.Severe:               IPoor:
              Coxville                   I wetness,               wetness.              I wetness,               wetness.              I wetness.
                                         I percs slowly.                                I too clayey.                                  I
                                         I                                              I                                              I
              Da ------------------      ISevere:               ISliqht  -----------    ISevere:               ISevere:                IPoor:
              Daleville                  I wetness,             I                       I wetness.               wetness.              I wetness.
                                         I percs slowly.        I                       I                                              I
                                         I                      I                       I                                              i
              Ec ------------------      ISevere:               ISevere:                iSevere:               ISevere:                iPoor:
              Echaw                      I wetness,             I seepage,              I seepage              I seepage,                too sandy.
                                         I poor filter.         I wetness.                wetness:             I wetness.
                                                                                          too sandy.           I
                                                                                                               I
              Eo ------------------      ISevere:               ISevere:                ISevere:               ISevere:                iPoor-
              Elloree                     flooding,               seepage,                seepage,               seepage,                wetness.
                                          wetness.                flooding,               flooding,              flooding,
                                                                  wetness.                wetness.'              wetness.









      Dorchester County, South Carolina                                                                                                    123




                                                 TABLE   ll.--SANITAPY FACILITIES--Continued


           Map symbol and           Septic tank          Sewage lagoon              Trench                 Area              Daily cover
              soil name              absorption               areas                sanitary             sanitary            for landfill
                                       fields                                      landfill             landfill

       EpE -----------------     ISevere:              ISevere:              IModerate:            ISlight  -----------  lFair:
         Emporia                  wetness,             I seepage,              wetness,                                    too clayey,
                                  percs slowly.          wetness.              too clayey.                                 wetness.
       EuA, EuB  ------------    ISevere:              ISevere-              ISevere:              ISevere:              IPoor:
         Eulonia                 I percs slowly,       I wetnes's.           I wetness,            I wetness.            I too clayey.
                                 I wetness.            I                     I too clayey.         I                     I
                                 I                     I                     I                     I                     I
       FoA -----------------     ISevere:              ISevere:              ISevere:              ISevere:              IPoor:
                                                                             I                     I                     I
         Foreston                I wetness.              seepage,              wetness.              seepage,              thin layer.
                                 I                       wetness.            I                       wetness.
                                 I                                           I
       FxB -----------------     IModerate:            ISevere:              ISevere:              ISevere:              IPoor:
         Foxwortb                I wetness,              seepage.            I seepage,            I seepage.              seepage,
                                 I poor filter.                                wetness,            I                       too sandy.
                                 I                                             too sandy.          I
                                 I                                                                 I
       GoA -----------------     ISevere:              ISevere:              ISevere:              ISevere:              lFair:
         Goldsboro               I wetness.            I wetness.              wetness.            I wetness.            I wetness.
                                 I                     I                                           I                     I
       Gr  ------------------    ISevere:              ISevere:              IlSevere:             ISevere:              'Poor:
         Grifton                 I wetness,              wetness,              flooding,           I wetness,            I wetness.
                                 I flooding.             seepage,              wetness.            I flooding,
                                 I                       flooding.                                   seepage.
                                 I
       Hb  ------------------    ISevere:              ISevere:              iSevere-              ISevere:              IPoor:
         Handsboro               Iflooding,              flooding,             flooding,             flooding,             ponding,
                                 Ipondinq.               excess humus,         pondinq,              pondinq.              excess humus,
                                 I                       ponding.              excess humus.                               excess salt.
                                 I
       Hp.
         Haplaquents
       TzA, TzB  ------------    ISevere:              ISevere-              ISevere:              ISevere:              lFair:
         Tzaqora                 I wetness,            I wetness.            I wetness.            I seepage,            I too clayey,
                                 I percs slowly.       I                     I                       wetness.            I wetness,
                                 I                     I                     I                                           I thin layer.
                                 I                     I                     I                                           I
       Jd  ------------------    ISevere:              ISevere:              ISevere:              ISevere:              IPoor:
         Jedburg                 I wetness.            I wetness.            I wetness.              wetness.            I wetness.
                                 I                     I                     I                                           I
       JoA -----------------     ISevere:              ISevere:              ISevere:              ISevere:              jPoor:
         Johns                    wetness.             I seepage,            I seepager              seepage,              seepage,
                                                       I flooding,           I wetness,              wetness.              too sandy.
                                                       I wetness.            I too sandy.
                                                       I                     I
       Le  ------------------    ISevere:              iSevere:              ISevere:              ISevere:              IPoor:
         Leon                    I wetness,            I seepage,            I seepagel            I seepagel            I seepage,
                                 I poor filter.        I wetness.            I wetness,            I wetness.            I too sandy,
                                 I                     I                     I too sandy.          I                     I wetness.
                                 I                     I                     I                     I                     I
       Lm  ------------------    ISevere:              ISevere:              ISevere:              ISevere:              IPoor:
         Lumbee                  I wetness.            I seepage,            I seepage,            I seepage,            I wetness.
                                 I                     I flooding,           I wetness.            ! wetness.
                                 I                     I wetness.            I                     f
                                 I                     I                     I                     I
       In  ------------------    ISevere:              ISevere:              ISevere:              ISevere:              IPoor:
         Lynchburg               I wetness.            I wetness.            I wetness.              wetness.            I wetness.









              124                                                                                                                             Soil Survey




                                                          TABLE  11.--SANITARY FACILITIES--Continued


                 Map symbol and             Septic tank           Sewage lagoon              Trench                  Area              Daily cover
                                             absorption                areas               sanitary
                      so13 name                                                                                   sanitary            for landfill
                                               fields                                      landfill               landfill

              Ly ------------------     ISevere:               ISevere:               ISevere:               ISevere:               IPoor:
                Lynn Haven              I wet-ness,            I seepage,             I seepage,              seepage,              I seepage,
                                        I poor filter.         I wetness.             I wetness,              wetness.              I too sandy,
                                        I                      I                      Itoo sandy.                                   I wetness.
                                        I                      I                      I                                             I
              Mo ------------------     iSevere:               ISevere-               ISevere:               ISevere:               IPoor:
                Mouzon                  I flooding,            I flooding,             flooding,             I flooding,            I wetness.
                                        I wetness,             I wetness.              wetness.              I wetness.             I
                                        I percs slowly.        I                                             I                      I
                                        I                      I                                             i                      I
              Na ------------------     ISevere:               ISevere:               ISevere:               ISevere:               IPoor:
                Nakina                  I wetness.             I wetness.             I seepagel             I seepage,             I wetness,
                                        I                      I                      I wetness.             I wetness.              thin layer.
                                        I                      I                      I                      I
              NoA -----------------     ISevere:               iSevere:               iSevere:               ISevere:               lFair:
                Noboco                  I wetness.             I seepage,             I wetness.             I wetness.             I too clayey,
                                        I                      I wetness.             I                      I                      I wetness.
                                        I                      I                      I                      I                      I
              OcA -----------------     ISevere:               ISevere:               ISevere:               ISevere:               lFair:
                Ocilla                   wetness.              I seepage,             I wetness.             I seepage,              wetness.
                                                               I wetness.             I                      I wetness.
                                                               1                      11                     1
              Og -----------            Severe:                Severe:                ISevere:               ISevere:               IPoor:
                Ogeechee                 wei-ness.             I flooding,            I wetness.             I wetness.             I wetness.
                                                               I wetness.             I                      I                      I
              Os ------------------     ISevere:               ISevere:               ISevere:               iSevere:               Poor:
                Osier                   I wetness,             I seepage,             I seepage,             I seepage,              seepage,
                                        I po.,.)r filter.      I wetness.             I wetness,             I wetness.              too sandy,
                                        I                                              too sandy.            I                       wetness.
                                        I                                                                    I
              Pa ------------------     ISevere:               ISevere:               ISevere:               ISevere:               IPoor:
                Panteqo                 I wetness.             I seepage,             I wetness.              wetness.               wetness.
                                                                 wetness.             I
              Pe ------------------     ISevere:               ISevere:               Severe:                !Severe:               'Poor:
                Pelham                   wetness.                seepage,              wetness.               wetness,               wetness.
                                                                 wetness.                                     seepage.
              Pm ------------------     ISevere-               ISevere:               ISevere:               ISevere:               jPoor:
                Plummer                 I ponding,             I pondinq,             I pondinq,             I seepage,              seepage,
                                        I poor filter.           seepage.              too sandy.             ponding.               too sandy,
                                        I
                                        I                                                                                            ponding.
              Ra ------------------     ISevere:               ISevere:               ISevere:               ISevere:               IPoor:
                Rains                    wetness.                wetness.             I wetness.              wetness,               wetness.
                                                                                      I                       seepage.
                                                                                      I
              Ru ------------------     ISevere:               ISevere:               ISevere:               ISevere:               IPoor:
                Rutleqe                 I flooding,            I seepage,             I flooding,            I flooding,            I seepage,
                                        I wetness,             I flooding,            I seepage,              seepage,               too sandy,
                                        I poor filter.         I wetness.             I wetness.              wetness.               wetness.
              Se -------------------    'Severe'.              Ievere:                ISevere:               ISevere:               lFair-
                Seagate                 I wetnes"s             I seepage,             I wetness.             I seepage,             I wetness,
                                        I poor filter.         I wetness.             I                      I wetness.             I too clayey.
                                        i                      I                      i                      I                      I
              Wa ------------------     ISevere:               'Severe:               iSevere:               ISevere:               IPoor:
                Wahee                   I wetness,               wetness.             I wetness,             I wetness.             i too clayey,
                                        I percs slowly.                               I too clayey.                                  bard to pack,
                                        I                                             I                                              wetness.









     Dorchester County, South Carolina                                                                                     125




                                            TABLE II.--SAITITARY FACILITIES--Continued


         Map symbol and         Septic tank        Sewage lagoon          Trench               Area            Daily cover
             soil name          absorption             areas             sanitarv            sanitary         for landfill
                                   fields                                landfill            landfill


      YaA  ----------------- ISevere:            ISevere:           ISevere:            ISevere:            lFair:
       Yauhannah             I wetness.          I seepage,         I seepage,          I wetness.          I wetness.
                             I                   I wetness.         I wetness.          I                   I
                             I                   I                  I                   I                   i
      Ye  ------------------ ISevere:            Severe:            ISevere:            ISevere:            Poor:
       Yemassee              I wetness.            seepage,         I wetness.          I seepage,           wetness.
                             I                     wetness.         I                    wetness.









            126                                                                                                                   Soil Survey




                                                         TABLE 12.--CONSTRUCTION MATERIALS

             [Some terms that describe restrictive soil features are defined in the Glossary. See text. for definitions of
                   "good," "fair," and other terms. Absence of an entry indicates that the soil was not rated. The
                   information in this table indicates the dominant soil condition; it does not             eliminate the need for
                   onsite investigation]



                 Map symbol and
                    soil name                      Roadfill                            Sand                            Topsoil


            AbA --------------------   lFair:                           lImprobable-                       IPoor:
             Albany                    I wetness.                         thin layer.                       too sandy.
                                       I
            ApB -------------------    lGood ------------------------   lProbable --------------------     IPoor:
             Alpin                                                                                          too sandy.
            131A, BIB --------------   lGood ------------------------   lProbable --------------------     IPoor:
             Blanton                   I                                I                                  I too sandy.
                                       I                                I                                  I
            BoA, BoB  --------------   lGood ------------------------   ITmprobable:                       IPoor:
             Bonneau                   I                                I excess fires.                    I too sandy.
                                       I                                I                                  i
            Br  --------------------   1Poor:                           lImprobable:                       IPoor:
             Brookman                  I low strength,                    excess fines.                     too clayey,
                                       I wetness.                                                           wetness.
                                       I
            Ca. --------------------   IPoor:                           JImprobable-                       Poor-
             Capers                     low strength,                     excess fines.                     too clayey,
                                        wetness,                                                            excess salt,
                                        shrink-swell.                                                       wetness.
            ChA -------------------    lFair:                           lProbable --------------------     IPoor:
             Chipley                   I wetness.                       I                                  I too sardy.
                                       I                                I                                  I
            CoB -------------------    lGood ------------------------   lProbable --------------------     Poor:
             Chisolm                   I                                I                                   too sardy.
                                       I                                I
            Cs  --------------------   lFair:                           lProbable --------------------     lFair:
             Coosaw                    I 'wetness.                      I                                  I too sandy.
                                       I                                I                                  I
            Cx  --------------------   IPoor:                           lImprobable:                       IPoor-
             Coxville                   wetness,                        I excess fines.                    I thin layer,
                                        low strength.                   I                                   wetness.
                                                                        I
            Da  --------------------   IPoor:                           lImprobable:                       IPoor:
             Daleville                  low strength,                     excess fines.                     wetness.
                                        wetness.
            Ec  --------------------   lFair:                           lProbable --------------------     IPoor:
             Echaw                     I wetness.                       I                                  I too sandy.
                                       I                                I                                  I
            EO  --------------------   Ir-loor:                         lImprobable:                       IPoor:
             Elloree                   I wetness.                       I excess fines.                    I thin layer,
                                       I                                I                                  I wetness.
                                       I                                I                                  I
            EpB -------------------    lFair:                           lImprobable:                       lFair:
             Emporia                    shrink-swell.                   1, excess fines.                    too sandy,
                                                                                                            small :stones.
            EuA, EuB  --------------   lFair:                           iImprobable:                       lPoor::
             Eulonia                    wetness.                          excess fines.                     thin layer.
            FoA -------------------    111air:                          ITmprobable:                       lFair:
             Foreston                   wetness.                        I excess fines.                    I too sandy.









       Dorchester County, South Carolina                                                                                           127




                                             TABLE 12.--CONSTRUCTION MATERTALS-Continued


             Map symbol and
                soil name                     Roadfill                            Sand                           Topsoil


        FxB -------------------   lGood  ------------------------   lProbable --------------------   IPoor:
          Foxworth                I                                 I                                I too sandy.
                                  I                                 1                                11
        GoA -------------------   lFair:                            lImprobable:                     lFair:
          Goldsboro                 wetness.                         excess fines.                     too sandy.
        Gr  --------------------  IPoor:                            lImprobable:                     IPoor:
          Grifton                 I wetness.                        I excess fines.                  I wetness.
                                  I                                 I                                I
        Hb  --------------------  iPoor:                            lImprobable:                     IPoor:
          Handsboro               I wetness.                        Iexcess fines.                   I excess humus,
                                                                                                       excess salt,
                                                                                                       wetness.


        Hp.
          Haplaquents
        IzA, IzB  --------------  IPoor:                            limprobable:                     lGood.
          Izagora                   low strength.                    excess fines.
        Jd  --------------------  !Poor:                            ',Improbable:                    !Poor:
          Jedburq                   wetness.                         excess fines.                     wetness.
        JoA -------------------   lFair:                            lProbable --------------------   lFair:
          Johns                     wetness.                                                           too sandy,
                                                                                                       thin layer.
        Le  --------------------  IPoor-                            lProbable --------------------   IPoor:
          Leon                    I wetness.                        I                                I too sandy,
                                  I                                 I                                I wetness.
                                  I                                 I                                I
        Lm  --------------------  IPoor:                            lProbable --------------------   IPoor:
          Lumbee                    wetness.                                                           wetness.
        In  --------------------  IPoor:                            lImprobable:                     Poor:
          Lynchburg               I
                                    wetness.                         excess fines.                     wetness.
        Ly  --------------------  IPoor:                            lProbable --------------------   IPoor:
          Lynn Haven              I wetness.                        I                                I too sandy,
                                  I                                 I                                I wetness.
                                  I                                 I                                I
        Mo  --------------------  IPoor:                            Improbable:                      IPoor:
          Mouzon                  I wetness.                         excess fines.                   I thin layer,
                                  I                                                                  I wetness.
                                  I                                                                  I
        Na  --------------------  IPoor:                            lImprobable:                     IPoor:
          Nakina                    wetness.                         excess fines.                     wetness.
        NoA -------------------   lFair:                            llmprobable:                     lFair:
          Noboco                  I wetness.                         excess fines.                     too clayey.
                                  I
        OcA -------------------   lFair:                            lImprobable:                     IPoor:
          Ocilla                    wetness.                         excess fines.                     too sandy.
        Oq  --------------------  IPoor:                            Improbable:                      IPoor:
          Oqeechee                I wetness.                         excess fines.                   I wetness.
        Os  --------------------  IPoor:                            lProbable --------------------   IPoor:
          Osier                     wetness.                        I                                I wetness.








          128                                                                                                                 Soil Survey




                                                TABLE 12.-CONSTRUCTION MATERIALS-Continued



                Map symbol and
                   soil name                     Roadfill                            Sand                           Topsoil


           Pa --------------------   IPoor:                            Improbable:                      11Poor:
            Pantego                    wetness.                         excess fines.                     wetness.
           Pe --------------------   IPoor:                            Improbable:                      IPoor:
            Pelham                     wetness.                         excess fines.                   I too sandy,
                                                                                                        I wetness.
                                                                                                        I
           Pm --------------------   1Poor:                            Probable ---------------------   IPoor-
            Plummer                  I wetness.                                                         I too*sandjr,
                                     I                                                                  I wetness.
                                     I                                                                  I
           Ra --------------------   IPoor:                            Improbable:                      1,Poor:
            Rains                      wetness.                         excess fines.                     wetness.
           Ru --------------------   IPoor:                            lProbable --------------------   IPoor:
            Rutleqe                  I wetness.                        I                                I wetness.
                                     I                                 I                                I
           Se --------------------   iFair:                            lImprobable:                     IPoor:
            Seagate                    VE!tneSS.                       I excess fines.                  I too sand-v.
                                                                       I                                I
           Wa --------------------   1Poor:                            lImprobable:                     IPoor:
            Wabee                    I low strength,                   I excess fines.                  I thin layer,
                                     I wetness.                        I                                I wetness.
                                     I                                 I                                I
           YaA  -------------------  iFaJ.r:                           lProbable --------------------   lFair:
            Yauhannab                I wetness.                        I                                I too sandy.
                                     I                                 I                                I
           Ye --------------------   lFair:                            lImprobable:                     IPoor:
            Yemassee                 I wetness.                        I excess fines.                   thin layer.








           Dorchester County, South Carolina                                                                                                 129




                                                             TABLE 13.--WATER MANAGEMENT

           [Some terms that describe restrictive soil features are defined in the Glossary. See text for definitions of
             "slight," "moderate," and "severe." Absence of an entry indicates that the soil was not evaluated. The
             information in     this table indicates the dominant soil condition; it does not eliminate the need for onsite
             investigation]


                              I                   Limitations for--                                        Features affectin
           Map symbol and             Pond           Embankments,        Aquifer-fed                          I                  9T   Grassed
             Soil name            reservoir          dikes, and           excavated          Drainage           Irrigation       I
                                                                                                                                     waterways
                                     areas             levees               ponds

           AbA --------------- ISevere:           iSevere:            ISevere:           'Cutbanks cave       Wetness,           Wetness,
           Albany               seepage.             seepage,          cutbanks cave.1                         droughty,           droughty.
                                                     piping,                                                   fast intake.
                                                     wetness.
           ApB --------------- ISevere:           ISevere:            iSevere:           iDeep to water       IDroughty,         IDroughty.
           Alpin              I seepage.          I seepage,          I no water.        I                    I soil blowing.
                              I                   I piping.           I                  I                    I
                              I                   I                   I                  I                    I
           BIA, BIB ---------- ISevere:           ISevere:            ISevere:           IDeep, to water      IDroughty,         1,Drouqhty.
           Blanton            I seepage.          I seepage.          I no water.        I                    I fast intake
                              I                   I                   I                  I                    I soil blowing'-
                              I                   I                   I                  i                    I
           BoA, BoB ---------- ISevere:           ISevere:            ISevere:           IDeep to water       IDroughty,         IDrouqhty.
           Bonneau              seepage.             thin layer.      I cutbanks cave.1                       I fast intake      I
                                                                      I                  I                     soil blowin;.     I
           Br ---------------- 1,Moderate:        ISevere:            IModerate-         lFlooding  -------   IFlooding,         lWetness.
           Brookman             seepage.          I hard to pack,     I slow ref*ill.    I                    I wetness,         I
                                                  I wetness.          I                  I                     percs slowly.     I
                                                  I                   I                  I                                       i
           Ca ---------------- 1Sliqht ---------  ISevere:            ISevere-           IPondinq,            lPondina,          Netness,
           Capers                                    hard to pack,    I slow r*efill,    I percs slowly,      I flooding,        i
                                                                      I                                        excess salt.       excess salt,
                                                     pondinq,          salty water.      I flood'ing.         I                   percs slowly.
                                                     excess salt.     I                  I                    I
                                                                      I                  I                    I
           ChA --------------- 1,Severe:          ISevere:            ISevere:           lCutbanks cave       lWetness,          IDroughty.
           Chipley              seepage.          I seepage.          I cutbanks cave.1                       I droughty,        I
                                                  I                   I                  I                    I fast intake.
                                                  I                   I                  1                    11
           CoB --------------- ISevere:           ISevere:            ISevere:           IDeep to water       IDroughty,         IDroughty.
           Chisolm            I seepage.          I seepace,          I cutbanks cave.1                       1, fast intake,    I
                              I                   I piping.           I                                        slope.            I
                              I                   I                   i                                                          I
           Cs ---------------- ISevere:           ISevere:            ISevere:           lFavorable   ------  lWetness,          IDroughty.
           Coosaw               seepage.             piping.          I cutbanks cave.1                        droughty,
                                                                                                               fast intake.
           Cx ---------------- ISliqht ---------  ISevere:            ISevere:           lFavorable   ------  lWetness --------  lWetness.
           Coxville           I                   I wetness.          I slow refill.     I                    I                  I
                              I                   I                   I                  I                    I                  i
           Da ---------------- 1Sliqbt ---------  ISevere:            ISevere:           IPercs slowly    --- !Wetness,          lWetness
           Daleville          I                   I wetness.          I slow refill.     I                     percs slowly.     I erodes'easily,
                              I                   I                   I                  I                                       I percs slowly.
                              I                   I                   I                  1                                       1
           Ec ---------------- iSevere:           ISevere:            ISevere:           lCutbanks cave       Wetness,           IDroughty.
           Echaw              i seepage.          I seepager            cutbanks caveJ                         droughty,         I
                              I                   I piping.                              I                     fast intake.      I
           Eo ---------------- ISevere:           ISevere:            ISevere:           Irlooding  -------   lWetness,          lWetness,
           Elloree            I seepage.             wetness,         I cutbanks cave.1                       1, fast intake,    I droughty.
                              I                      seepage,         I                  I                     droughty.         I
                              1                                       1                  1                    i                  I
                              I                      piping.







           130                                                                                                                      Soil Survey



                                                      TABLE 13.--WATER MANAGEMENT--Continued

                                                   Limitations for--                     r           --Features affecting--
             Map symbol and             Pond         Embankments          Aquifer-fed
                soil name           reservoir         dikes, and'          excavated         Drainage           Irrigation          Grassed
                                                        levees              ponds                                                  waterways
                                        areas


         EpB ---------------    IModerate:         IModerate:         ISevere:           iDeep to water     IFast intake,       IDroughty,
           Emporia              I seepage,         I thin layer,      I no water.        I                  I soil blowing,     I percs slowly.
                                I slope.             piping.          I                  I                  I slope.            I
                                I                                     I                  I                  I                   I
         EuA ----------------   Moderate:          Moderate:          IModerate-         lFavorable  ------ IWetnes! ---------  IFavorable.
           Eulonia              I                                                water   I                  I                   I
                                 seepage.            wetness.           deep to
                                I
         EuB-                   -IModerate-        IModerate:         IModerate,:        ISlope ----------  IWetness,           IFavorable.
              -7   -----------  I                  I                                                        I                   I
           Eulonia               seepage.            wetness.         I deep to water.1                       soil ])lowing,
                                I                  I                  I                  I
                                                                                                              slope.
                                I                  I                  I                  I
         FoA ----------------   ISevere-           !Severe:           ISevere:           lFavorable  ------ IWetness,           IDrouqbty.
           Foreston             I seepage.           seepage,         I cutbanks cave.11                    I droughty,         I
                                I                                     I                                       fast intake       I
                                I                    piping.
         FxB ---------------    ISevere:           ISevere:           ISovere:           IDeep to water     IDrouqbty,          IDroughty.
           Foxworth             I seepage.         I seepage.         I cutbanks cave.1                     I fast intake       i
                                I                  I                  I                  I                  I soil blowin;.
         GoA ---------------    IModerate:         IModerate:         IMaderate:         'Favorable  ------ 1,WPtness           lFavorable.
                                                   I                                     I
           Goldsboro            I seepage.           piping,            slow refill                         I fast intake.
                                I                  I                                  '  I
                                                     wetness.           cutbanks cave.
         Gr ----------------    IModerate:         ISevere:           IModerate:         IFlooding  ------- IWetness,           IWetness.
           Grifton               seepage.          I wetness.         I slow refill.                          floodincf.        I
         Ub -----------------   'Slight ---------- ISevere:           ISovere-           'Pondinq           IPonding,           Wetness,
           Handsboro            I                  I                  I s
                                                     excess  humus,      alty water.     I  flooding,         floodincf,         excess salt.
                                I                  I pondinq,         I                  I excess salt.       excess salt.      I
                                                     excess salt.
         HP ----------------    lSligbt ---------  ISevere:           ISevere:           !Percs slowly --- IVIetness,           i,Wetness,
           Haplaquents                               wetness,           slow refill                           percs slowly-      percs slowly.
                                                     piping.
         IzA ---------------    IModerate:         IModerate:         ISevere:           IFavorable  ------ IWetness,           lErodes easily.
           Izagora               seepage.            piping,            slow refill.                          percs slowly.
                                                     wetness.
         IzB ---------------    IModerate:         IModerate:         'Severe:           ISlope ----------  IWetness,           !Erodes easily.
           Izagora               seepage,            piping,            slow refill.                          percs slowly,
                                 slope.              wetness.                                                 slope.
         Jd ----------------    ISliqbt ---------  ISevere:           ISevere:           IFavorable  ------ IWetness,           IWetness.
           Jedburg              I                  I wetness.         I slow refill.                          soil blowing.
                                I                  I                  I
         JoA ---------------    iSevere:           ISevere:           iSevere:           lCutbanks cave     IWetness,           IDrouqbty.
           Johns                 seepage.            seepage,         I cutbanks cave.1                     1, droughty,        I
                                                     piping,                                                  fast intake.      I
                                                     wetness.                                                                   I
                                                                                                                                I
         Le ----------------    ISevere:           ISevere:           ISevere:           ICutbanks cave     IWetness,           IWetness,
           Leon                 I seepage.         I seepage,         I cutbanks cave.1                     I droughty,           droughty.
                                I                  I piping,          I                                       fast intake.
                                                     wetness.         I
                                                                      I
         Lm ----------------    ISevere:           iSevere:           ISlight  --------- lCutbanks cave     IWetness ---------  IWetness.
           Lumbee               I seepage.           wetness.         I                  I                  I                   I









          Dorchester County, South Carolina                                                                                                131




                                                    TABLE 13.--WATER MANAGEMENT--Continued

                                                 Limitations for--                                       Features affecting--
           Map symbol and            Pond         ftbankments           Aquifer-fed                                                Grassed
             Soil name            reservoir         dikes, and'          excavated         Drainage           Irrigation      i
                                                                                                                                  waterways
                                    areas             levees               ponds

       Ln ----------------     IlModerate:       ISevere:           IModerate:          lFavorable ------  lWetness,          ketness.
        Lynchburg              seepage.           piping,           I slow refill.      I                  I fast intake.
                                                  wetness.          I                   I                  I
                                                                    I                   I                  I
       Ly ----------------     ISevere:          ISevere:           ISevere:            lCutbanks cave     lWetness,          lWetness,
        Lynn Haven             I seepage.        I seepage,         I cutbanks cave.1                      I droughty,        I droughty.
                               I                 Ipiping,           I                   I                  I fast intake.     I
                               I                 Iwetness.          I                   I                  I                  I
                               I                 I                  I                   I                  I                  I
       Mo ----------------     IModerate:        ISevere:           ISevere-            IPercs slowly,     lWetness           lWetness.
        Mouzon                 I seepage.        I hard to pack,      slow r*efill.     I flooding.        I percs ;lowly.    I percs slowly.
                               I                 I wetness.                             I                  I                  I
                               I                 I                                      I                  I                  I
       Na ----------------     ISevere:          iSevere:           ISli.cFht --------- lFavorable ------  lWetness --------  lWetness.
        Nakina                 seepage.          I wetness.         I                   I                  I                  I
       NoA ---------------     IModerate:        Moderate:          ISevere:            lFavorable ------  lWetness,          IDroughty,
                               I                                    I slow refill       I                  I droughty.        I rooting depth.
        Noboco                 Iseepage.          piping,           I              ive  I
                                                  wetness.            cutbanks cz
                               I                                    I
       OcA ---------------     ISevere:          ISevere:           ISevere:            lFavorable ------  lWetness,          Droughty.
        Ocilla                 I seepage.        I piping,          I cutbanks cave.1                      1, droughty,       I
                               I                 I wetness.         I                   I                   fast intake.
                               I                 I                  I                   I
       Og ----------------     IModerate:        ISevere:           lFavorable ------   lFavorable ------  lWetness --------  lWetness.
        Oqeecbee               I seepage.        I wetness.         I                   I                  I                  I
                               I                 I                  I                   I                  I                  I
       Os ----------------     ISevere:          ISevere:           ISevere:            lCutbanks cave     lWetness,          lWetness,
        Osier                  I seepage.         seepage,          I cutbanks cave.!                       droughty,         I droughty.
                               I                  piping,           I                                       fast intake.      I
                                                  wetness.          I                                                         I
                                                                    I                                                         I
       Pa ----------------     IModerate:        ISevere:           IModerate:          lFavorable ------  lWetness --------  1,Wetness.
        Pantego                I seepage.        I wetness.         I slow refill.      I                  I
              ------------     I-                I                  I                   I                  i
       Pe----                  Severe:           ISevere:           ISevere:            IFavorable ------- lFast intake,      lWetness.
        Pelham                 seepage.           piping,           I cutbanks cave.,                      I wetness.         I
                                                  wetness.
       Pm ----------------     ISevere:          Severe:            ISevere:            IPondinq           IPondina           lWetness,
        Plummer                I seepage.         seepage,          I cutbanks cave.1 cutbank's cave.1 cutban'k's caveJ droughty.
                                                  piping,
                                                  pondinq.
       Ra ----------------     IModerate:        ISevere:           IModerate:          lFavorable ------  lWetness --------  lWetness.
        Rains                  I seepage.        I piping,          I slow refill.      I                  I                  I
                               I                 I wetness.         I                   I                                     I
                               I                 i                  I                   I                  I                  I
       Ru ----------------     ISevere:          ISevere:           ISevere:            lFlooding          lWetness,          lWetness,
                               I                 I                  I                   I
        Rutlege                seepage.           seepage,          I cutbanks cave.    Icutbanks cave.1 droughty,            I droughty.
                               I                  piping,                                                  I fast intake.     I
                               I                  wetness.          I                   I                  I                  I
                               I                                    I                   i                  I                  I
       Se ----------------     ISevere:          ISevere:           ISevere:            lCutbanks cave     lWetness,          IDroughty.
        Seagate                I seepage.        I wetness.         I cutbanks cave.1                      I fast intake      I
                               I                 I                  I                   I                  I droughty.        I
                               I                 I                  I                   I                  I                  I
       Va ----------------     ISlight  --------- ISevere:          ISevere:            IPercs slowly --- lWetness,           lWetness,
        Wahee                  I                 I wetness.           slow refill.      I                   soil blowing,       percs slowly.
                               I                 I                                      I
                               I                 I                                      I                   percs slowly.








        132                                                                                                                   Soil Survey




                                                 TABLE 13.--WATER MANAGEMENT--Continued


                                               Limitati                            I
                                                       ons for--                                    Features affectinq-
          Map symbol and           Pond         Embankments,        Aquifer-fed                       I                 I    Grassed
             soil name          reservoir        dikes, and          excavated         Drainage          Irrigation     I
                                                                                                                            waterways
                                  areas             levees             ponds

       YaA  --------------- !Moderate:         ISevere:          ISevere:          IFavorable ------  IWetness,         IDroughty.
        Yaubannah              seepage.        I piping,         I cutbarks cave.1                      fast intake,    I
                                               I wetness.        I                 I                    drougbty.       I
                                               I
                                                                 I                 I                                    I
       Ye  ---------------- IModerate:         ISevere:          IModerate:        1,Favorable ------ IWetness,         IWetness
        Yemassee               seepage.        I piping,           slow refill.                         soil blowing.   1.
                                               I wetness.
                                               I









          Dorchester County, South Carolina                                                                                                 133




                                                       TABLE 14.--ENGINEMING INDEX PROPERTIES

            Me symbol < means less than. Absence of an entry indicates that                  data were not estimated. Some soils may
                 have Unified classifications and USDA textures in addition to               those shown. In general, the dominant
                  classifications and      textures are shown]


                                 I         1                     1,   Classification             Percentage passing
                Map symbol and     Depth     USDA texture                     I                     sieve   number--         Liquid    IPlas-
                soil name                                        IUnified     I  AASHTO             I       I        I         limit   Iticity
                                                                 I            1               4        10      40     200              lindex
                                                                              I
                                                                 I            I                                              I
            AbA --------------      0-54   IFine sand  --------  ISM SP-SM    IA-2-4, A-31   100    1100    175-90   110-20  1         1 NP
             Albany                54-59   !Sandy loam -------   ISM'         IA-2-4       1 100    1100    175-92   122-30  1  ---    I NP
                                   59-75   jSandy clay loam, ISC,     SM,     1A-2-4 I A-4197-100195-100!70-100120-50        1  <40    INP-17
                                             sandy loam, finel SM-SC            A-6        I        I
                                           I sandy loam.         I                         I        I
            ApB --------------   1  0-7    IFine sand  --------  ISP-SM  SM   IA-3   A-2-4195-100190-100160-1001      5-20   1           NP
                                      -5   IFine sand, sand ISP SM,           IA-3,
             Alpin               1  7 4                                            1 A-2-4195-100190-100160-1001      5-20   1         1 NP
                                 1 54-85   IFine sand, sand ISP-SM,      SM   IA-2-4       195-100190-100160-100111-20       1  ---    I NP
                                 I         I                     I            I            I        I       I        I       I         I
            BIA, BIB ---------   1  0-44   IFine sand  --------  ISP-SMr SM A-3, A-2-4       100    190-100165-1001 5-20     1  ---    I NP
             Blanton             1 44-80   ISandy clay loam ISC SM-SC,IA-4                 1 100    195-100169-96    125-50  1 16-45   13-22
                                             sandy loam, fin'el SA            I A 2F-4#    1        1
                                             sandy loam.         I            I A-2-6,     I        I
                                                                 I            I A' 6
            BoA, BoB ---------   1  0-27   IFine sand  --------  ISM  SP-SM   IA-2   A-3   1 100    1100    160-95   1B-20   1  ---    I NP
             Bonneau             1 27-80   ISandy loam, sandyl,SCI    SM-SC   IA-2'  A-61  11 100    100    160-100130-50    1 21-40   14-21
                                             clay loam, fine                  I A-4'                        I        I       I         I
                                             sandy loam.         I            I            I                I        I       I         I
            Br  ---------------  1  0-8    IC1ay loam  --------  11CLI MLI    11A-6, A-4   1 100    195-100175-100151-81     1 25-40   14-19
             Brookman            I         I                      CL-ML                    I        I       I        I       I         I
                                 1  8-49   ISandy clay, clay,ICH, CL          IA-71  A-6   1 100    198-100185-100155-91     1 37-65   118-41
                                 1         1 clay loam.          I            I            I        I       I        I       I         I
                                 1 49-76   iSandy clay,   claydCLI CHI SCiIA-6,      A-7   1 100    190-100170-100143-90     1 25-55   111-35
                                             sandy clay   loam.                            I        I       I        I       I         I
                                                                 I
            Ca  ---------------  I                               ly
                                    0-21   jSilty clay loam       H           IA-7-5       1 100    1100    180-100170-1001    50-81   115-40
             Capers                21-80 Clay, silty clay        IIMH         IA-7-5       1 100    1100    185-100175-1001    52-80   16-40
            ChA --------------   1  0-7    ISand ----------      ISP-SM       IA-3 A-2-41    100    1100    180-1001  6-12   1  ---    I NP
             Chipley             1  7-75   ISand, coarse s;nd-ISP-SM          IA-3:  A-2-41  100    1100    170-1001  6-12   1         1 NP
                                 I         I                     I            I            I        I       I        I       1         11
            CoR --------------      0-30 Fine sand     --------  ISP-SM SM    iA-2-4 A-31    100    198-100175-98    19-27   1         1 NP
             Chisolm               30-58 Sandy clay loam, ISM-SC' SC          IA-4 @-6     1 100    198-100175-98    136-55  1 20-35   14-15
                                             sandy loam, finel CL, C'L-ML'I                I        I       I        I       I         I
                                           I sandy loam          I            I            I        I       I        I       I         I
                                 1 58-80   iSandy loam,'fine ISM, SM-SC,IA-2, A-4f         1 100    198-100165-98    125-50  1 16-35   12-15
                                           1 sandy loam,         I SC         I A-6        I        I       I        I       I         I
                                           I sandy clay loam.1                I            I        I       I        I       I         I
                                           I                     I            I            I        I       I        I       I         I
            Cs  ---------------  1  0-26   ILoamy fine sand ISM               IA-2-4       1 100    1 100 190-100115-30      1  ---    I NP
             Coosaw              1 26-78   iSandy clay loam ISM SC            IA-2-6 I A-41  100    195-100180-100125-50     1 16-39   12-17
                                           1 fine sandy loam',I SM'-SC'       I A-6        I        I       I        I       I
                                           I sandy loam.         I            I            I        I       I        I       I
                                           I                     I            I            I        I       I        I       I
            Cx  ---------------  i  0-11   ILoam -------------   ISM, ML#     IA-4, A-61   1 100    1100    185-97   146-75  1 20-46   13-15
             Coxville            I         I                     ICL-ML,    CLI A-7        I        I       I        I       I         I
                                 1 11-80   lClay loam, sandy IFL, CH          IA-6, A-7    1 100    1100    185-98   150-85  1 30-55   112-35
                                             clay, clay.                      I            I        I       I        I       I         I
                                                                 I            I            I        I       I        I       I         I
            Da  ---------------     0-26   ISilt loam  --------  IML CL-ML    IA-4         1 100    1100    185-100160-90    1 <30     INP-7
             Daleville             26-80   lClay loam, loam, ICL'             IA-6         1 100    1100    190-100170-80    1 28-38   111-20
                                             silty clay loam.1                I            I        I       I        I       I         I








           134                                                                                                                                   Soil Survey




                                                  TABLE 14.--ENGINEERING INDEX PROPERTIES--Continued
                                                                      i     Classification                Percentage passincF_
              Map symbol and         Deptb       USDA te,t,re                                                sieve number--             !Liquid    jPlas-
                 soil name                                              Unified         AASHTO                                  1     -11  limit   11ticitv
                                                                                                      4          10      40       200   1          jindex
                                                                                                                                            P't
           EC ---------------         0-7       1,11in, sand -------- ISP, SP-SM     IA-3            100     1100     !50-80    1 4'[-101          1  NP
             Echaw                    7-45      jLoamy sand, fine ISM                IA-2-4, A-3!    100      100     1150-75   1 5-30                NP
                                                sand, loamy finel                    I
                                                sand.                 I              I
                                   1 45-80      11ine sand, loamy ISM, SP-SM         IA-2, A-3      1100      100     150-70    1 5-20  1          1  lip
                                                sand, loamy fine!                    I              I
                                                sand.
           Eo ---------------      1  0-20      1Loamy fine sand      ISM            fA-. 2         1100     198-100170-90      115-35  1   <25    INP-4
             Elloree               1 20-23      ISand, fine sand,     ISP-SM' SM     IA-2, A-3      1100     198-100 65-90      1 9-27  1   ---    I NP
                                   I            I                     I              I              I        I        I         I
                                   I            , loamy sand.
                                   1, 23-72     ISandy loam, sandyISM, SM-SC         iA-2           11 100   198-100160-90      115-35  i   <30    INP-12
                                                i clay loam.          I SC           I              I        I        I         I       I
                                     72-80 Loamy      sand,   sandyls@,     SM-SC IA-2,    A-4,     1100     198-100160-90      '115-45 1   <40    INP-18
                                                I loam, sandy clayl SC             'I A-6                                       I       I          I
                                                I loam.               I              I                                          I       I          I
           EpB --------------         0-14      Loamy fine sand       ISM,  SM-SC    IA-2  A-1      190-100180-100140-85        15-4D   1   <18    INP-7
             Emporia                                                  I              I A-@
                                     14-41      ISandy clay loam,     11SC, CL       IA-2, A-4      90-100180-100145-95         125-70  1  20-50   1 8-30
                                                sandy loam, clay                      A-6     A-@            I        I         I       I          I
                                                108m'
                                     41-54      iSandy clay loam,     IfSCY CL, CH A-2,    A-4,     190-100180-100145-95        130-80     25-55     8-30
                                                clay  loam, sandy                     A-6  ,  A-7
                                                clay,
                                     54-75 Stratified sandy           ISM   SC       1A-1  A-2      170-100155-100130-90        120-60  1   <40    1NP-25
                                                loam to clay            ML, CL        A-4, A-6
                                                loam.
           EuA, EuB   ---------    1  0-11      IT'ine sandy loam     SM SC          IA-2 A-4       1100     195-100160-98      130-50  1   <30    INP-10
             Fulonia               I            I                     I S@-Sc'
                                                                      1
                                     11-27 Sandy clay, clay',SC, CL                  A-61  A-71     11 100   195-100170-99      145-80  11 25-45     8-20
                                                1 sandy clay loam                     A-4                    I        I         I
                                                I C.
                                     27-49      roandy clay loam,'ISC, SM,           IA-2  A-4r     1100     190-100160-100118-50       1  16-35     3-15
                                                sandy loam.             SM-SC        I A-I;
                                     49-80      Illariable ---------      ---                                                               ---      ---
                                   I            I                     I                                                                            I
           FoA --------------         0-13 Loamy fine sand ISM                       IA-2            100     1100     160-100115-301    1   ---    I NP
             Foreston                13-32 Sandy loam, fine           SM             IA-2           1100     1100     170-10011EI-35    1   <25    INP-4
                                                sandy loam.           I              I              I        I        I         I       1          1
                                     32-53 Loamy fine sand            ISP-SMP SM     IA-2, A-3      1100     1100     150-98    11 6-25 1   ---    I NP
                                                I loamy sand,
                                   I                             finel               I              I        I
                                   I            I                     I              I              I        I
                                                sand.
                                   1 53-80      IFine sandy loam      isc SM-SC,'IA-2 A-4,           100     1100     155-90    125-49      <45    INP-25
                                   I            I sandy clay lo;;.1, S@               A-9, A-7               I        I         I                  I
                                   I            I                                    I                       I        I         I                  I
           FxB --------------      1  0-14      ITine sand --------   ISP-SM         IA-3 A-2-41     100     1100     160-1001 5-12     1   ---    I  NP
             Foxworth              1 14-85      ISand, fine sand ISP, SP-SM          IA-31' A-2-41   100     1100     150-1001 1-12     1   ---    I  NP
                                   I            I'                    I              I              I        I        I         I       I          I
           GoA --------------      1  0-14      ILoamy sand  -------  ISM            jA-2           195-100195-100150-95 113-30         1   <20    1  NP
             Goldsboro             1 14-62      !Sandy clay loam, ISM-SC, Sc       F A-2, A-4,      198-100195-100160-100125-55         1  16-37   1 4-18
                                                sandy loam.           11 CL-MLI CL! A-6
                                     62-80      11'ariable ---------
           Gr ---------------         0-10      Fine sandy loam ISM SM-SC            IA-2, A-4      1 100 195-100160-100120-45          1   <30    INP-7
             Grifton               1 10-61      Il'ine sandy loam,    IISC" CL       @A-4, A-6      198-100195-100160-100131-601        1  20-35   1 8-15
                                                sandy clay loam,
                                                clay loam.
                                     61-80      krariable ---------









       Dorchester County, South Carolina                                                                                                  135




                                           TABLE 14.--ENGINEERIITG INDEX PROPERTIES--Continued

                                                              I   Classification              Percentage passing
            Map symbol and     Depth      USDA texture        I            I                     sieve   number--         Ir,iquid Plas-
             soil name                                        Unified      I  AASHTO                                        limit  Iticity
                                                                                           4        10      40     200             lindex
                                 In

        Hb  ---------------      0-48   IMuck -------------   IPT
         Handsboro            148-80    IStratified sapricIPT
                                          and mineral
                                          material.


        Hp.
         Haplaquents
        IzA, IzB  ---------   1  0-13   ISilt loam   -------- CL, CL-ML, A-4            195-100195-100185-100160-90       1 <30    INP-10
         Izaqora              I         I                     I ML         I            I        I       I       I        I        I
                              113-41    ILoam, clay loam      ICL          IA-4, A-6f   195-100195-100185-100160-95       1 25-45  1 8-25
                              1         1 silty clay loam'    I            I A-7        I        I       I       I        I        I
                              141-80    IClay loam, silty'ICL,    CH       IA-6, A-7    195-100195-100190-100170-95       1 35-60  120-40
                              1         1 clay.               I            I            I        I       I       I'       I        I
                              I         I                     I            I            I        I       I       I        I        I
        Jd  ---------------   1  0-15 Loam   -------------    ism SM-SC    IA-4         1 100    195-100160-95   140-75   1 <30    1 0-10
         Jedburg              115-75    ILoav, silt loam, ICL'             IA-4  ,A-6     100    195-100185-100170-95     1 25-40  1 9-20
                              1         1 clay loam.          I            I                     I       I       I        I        I
                              175-80    IClay loam, sandy     ISC, CL      IA-61 A-7-61   100    195-100180-100140-80     1 30-50  110-25
                                          clay loam.          I            I            I        I       I       I        I        I
        JoA --------------       0-6    Loamy sand   -------  SM           A-2,  A-4    1 100    195-100160-90   115-45   1  ---   I NP
         Johns                1    -31  1                     ISC SM-SC    IA--2 A-4 ,  1 100    195-100160-98   130-65   1 20-45  1 5-25
                              1  6      1Sandy clay loamf I I         -M'I A-@   , A-7  I        I       I       I        I        I
                                          sandy loam           CLF CL L
                              131-80    ISand,'Ioamy*sand,ISM     SP-SMIIIA-2. A-3      195-100195-100151-90     1 4-25   1  ---   I  NP
                              I         I coarse sand.        I S@                      I        I       I       I        I
                              I         I                     I            I            I        I       I       I        I
        Le  ---------------   1  0-17   ISand -------------   ISP SP-SM IA-3     A-2-41   100    1100    180-1001  2-12   1  ---   I  NP
         Leon                  17-65    ISand, coarse         ISM" SP-SMIIIA-3,' A-2-41   100    1100    170-1001  3-20   1  ---   I  NP
                                        I sand, loamy sandl SP                          I        I
                                                              I P
                              165-80    ISand, coarse sandS .     SP-SM    IA-3, A-2-41   100    1100    170-1001  2-12   1  ---   I  NP
                              I         I                                  I            I        I       I       I        I        I
        Lm  ---------------   1  0-5    Fine sandy loam ISM       SM-SC    IA-2  A:4    1 100    185-100165-98   115-45   1  <20   INP-7
                              1  5-37 Sandy clay loam, ISC:       CL       IA-4,        1 10     190-100165-98   136-60   1 19-45  1 7-25
         Lumbee               I         I                     I                  ,A 6   1    0
                                          sandy loam, clay                 I A 7
                                          loam.               I            I            I
                              137-70    ILoamy sand, sand,ISP,_SM,         !A-2, A-3    190-100185-100150-90     1 4-25   1  ---   I  NP
                              I         I coarse sand.        I SP SM
                              I         I                     I
        Ln  ---------------   1  0-7    ILoamy sand  -------  ISM SP-SM    IA-2         192-100190-100160-100112-35       1  <25   INP-4
         Lynchburg            1  7-80   ISandy clay loam, ISM'SC SC        IA-2  A-41   192-100190-100170-100125-67       1 16-40  1 4-18
                              I         I sandy loam, clayl CL, C'L-MLI A-6'
                              I           loam.
                              I
        Ly  ---------------   1  0-19   IFine sand   -------- SP, SP-SM,IA-3,    A-2-41   100     100    180-1001  2-14   1  ---   I  NP
         Lynn Haven           I         I                     I SM         I            I                I       I        I        I
                              119-49    ISand, fine sand, ISM     SP-SM IA-3,    A-2-41   100    1100    170-1001  5-20   1  ---   I  NP
                              I         I loamv fine sand     I
                                        Sand, -fine sand *ISP,    SP
                              149-75    1                            -SM IA-3    A-2-41   100     100    180-1001  2-12   1  ---   I  NP
                              I         I                     I                         I                I       I        I        I
        Mo  ---------------   1  0-8    IFine sandy loam      ISM, SM-SC,IA-4           1 100    190-100165-90   140-70      <32   INP-7
         Mouzon               I         I                     I ML         i            I        I       I       I                 I
                                 8-61 Sandy clay loam,        1SC, CL      IA-6           100    190-100170-90   130-75   1 30-40  1 7-21
                                        1 clay loam           I            I                     I       I       I        I        I
                              161-68    ISandy loam: sandylCL-ML, SCIIA-41 A-6          1 100    190-1.00160-85  135-50   1 20-40  1 3-21
                              1         1 clay loam.          I SM___
                              168-80    lVariable ---------   I
        Na  ---------------   1  0-18   IFine sandy loam ISM ML            IA-2-4       1 100    1100    185-100120-60    1 <30    INP-7
         Nakina               118-61    ISandy clay loan, ISMf             IA-4 A 6,    1 100    1100    190-100128-45    1 28-40  1 9-18
                              I         I fine sandy loam I                I A-2'__
                              161-80    IVariable -------- :I    ---       I








               136                                                                                                                                             Soil Survey




                                                         TABLE 14.--ENGINEERING INDEX PROPERTIES--Continued

                                                                                    Classification                   PerceR-aqe passing
                  Map symbol and          Depth        USDA texture           I               I                         sieve number--                Liquid     IP]as-
                     soil name                                                I Urified       I AASHTO                  I        I          -_         lirlit ticitv
                                                                              I               1                 4           10      40          0                index'
                                                                              I                                                             _L2
                                            In                                I                                                                       I @@'      I
               NoA --------------       1   0-14    ILoamy sand     -------   ISM             IA-2           195-100192-100150-95           113-30    1 <20      1 NP
                Noboco                  1 14-80     ISandy loam, sandyISM-SC, SC              IA-2 A-4       195-100195-100170-96           130-63    120-38     1 4-15
                                                                                           ri      F      r  I          I        I          I         I          I
                                                      clay loam, clay I CL, CL-ML A-6
                                                      loam.                   I               I              I          I        I          I         I          I
                                                                              I               I              I          I        I          I         I          I
               OcA --------------       1   0-23    ISand -------------       ISM SP-SM       IA-2   A-3     1 100      195-100170-1001      8-35     1  ---     I  NP
                                        1     -80   ISandy loam, sandy1SM_'                   IA-2'  A-4  ,  1     0    195-lOOl8O-lOOi2O--55         1  0-4     INP-18
                Ocilla                    23        1                         1     ,CL,                     1 30       1        1          1          2     0
                                                      clay loam.                sc  , ML      I A-6'
                                                    I                         I               I              I          I        I          I
               Og ---------------       1   0-12    IFine sandy loam          ISM             IA-2           1 100      195-100148-70       115-25    1  <30     INP-5
                Ogeechee                1 12-57     ISandy clay loam,         iSC,  CL        IA-6           1 100      195-100165-85       140-55    132-40     116-23
                                                      clay loam.
                                          57-65     jSandy clay loam,         IISC            IA-6, A-2      1 100      190-100150-65       125-45    130-40     115-25
                                                      sandy loam.                             I
                                                    I                         I               I
               Os ------------     w---I    0-3     ILoamy fine sand          ISM             IA-2           1 100      198-100170-90       113-25    1  ---     I  NP
                Osier                   1   3-80    lCoarse sand,             ISP   'SP-SM    iA-1-6 A-31      100      190-100140-60       1 2-10    1  ---     I  NP
                                                    I sand, fine sand.1                       I A-2-4        I          I
                                        1                                                            4                           1
                                        I           I                         I               I              I          I        I
               Pa ---------------       1   0-18    ISandy loam     -------   ism, SM_-SCj1A-201     A-4     1 100      195-100160-95       125-75    1  <35     iNP-10
                                        I           I                                                        I          I        I
                Pantego                             I                         , CL, ML                       1
                                          18-37 Sandy clay loan, SC, CL                       IA-4   A-61      "LOO     195-100180-100130-80          120-40     1 4-16
                                                      sandy loam, clayl SM-SC:                I A-2'
                                                      loam                    i CL-ML         I
                                        1 37-80     ISandy*loam, sandylCL, SC                 IA-6,  A-7     1 100      195-100190-1001136-80         125-49     111-24
                                                    1 clay, sandy clayl                       I              I          I        I          I         I          I
                                                    I loam.                   I               I              I          I        I
                                                    I                         I               I              I          I        I
               Pe -------------      --1    0-35    !Sand -------------       ism, SP-sm      IA-2           1 100      195-100175-90       110-25    1          1 NP
                                        1 35-80     ISandy clay loi
                Pelham                                                 Im, ISM SC             IA-21 A-4,     1 100      195-100165-90       127-50    116-30     1 2-12
                                                      sandy loam.             I SA-SC'        I A-6          I          I        I
                                                                              I               I              I          I        I
               Pm ---------------           0-9     Loamy sand      -------   ISM SP-SM       IA-2-4 A-31      100      1100     175-96     15-26     1  ---     I  NP
                Pluminer                    9-58 Sand'. fine sand, Sm" Sp-sm                  IA-2-41' A-31    100      1100     175-96     15-26     1  ---     I  NP
                                                    I loamy sand.             I               I              I          I        I
                                        1 58-75     ISardy loam, sandyism, SC,                IA-2-4, A-41     100      197-100176-96       120-48    1  <30     INP-10
                                        I           I clay loam, fine I SM-SC
                                        I           I sandy loam.             I
                                        I           I                         I
               Ra ---------------       1   0-9     ISandy loam     -------   SM, ML          A-2,   A-4       100      195-100150-85       125-56    1  <35     INP-10
                Rains                       9-42    !Sandy clay loam, Isc sm-SC               IA-2   A-4     1 100      195-100155-98       130-70    118-40     1 4-20
                                                    1                                      '1 A '                       I        I          I         I          I
                                                      clay loam.              I CL CL-ML          -6
                                          42-56 Sandy clay loam               ISC 'SM-SCPIA-4        A-6     1 100      19S-100160-98       136-72    118-45     1 4-28
                                                      clay loam, san@yj CL, CL-MLI A-7'
                                                    I clay.                                   I
                                        1 56-80     ISandy loam, sandylsm, SC,                IA-2j, A-41    1 100      195-100160-95       130-60    116-40     1 3-18
                                                      clay loam, sandy          ML, CL        I A-6          I          I        I          I         I          I
                                                      clay.                   I               I              I          I
                                                                              I               I              I          I
               Ru ---------------       1   0-21    ILoamy fine sand          ISM, SP-SM      IA-2   A-3     195-100195-100150-80           115-35    1  <25     1  NP
                Rutleqe                 1 21-75     ISand, loamy sand,I,SP-SM, SPIIA-2'              A-3     195-100195-100150-80           12-25     1  <20     1  NP
                                        I           I fine sand.                Sm            I              I          I        I          I         I          I
                                        I           I                         I               I              I          I        I          I         I          I
               Se ---------------       1   0-14 Sand     -------------       ISM   SP SM     iA-2   A-3     1 100      1100     190-1001    15-20    1  --      I  NP
                                                                              I
                Seagate                   14-18     Fine sand, loamy          ism:  SP-SM     IA-2'          1 100      1100     190-100116-25        1             NP
                                        I           I                                         I              I          I        I          I         I
                                                                                                                                                      I
                                                                                                                                                      I





























































                                                      sand, sand.
                                          18-32     IFine sand, sand          ISM   SP-SM     IA-2   A-3     1 100      1100     190-10CII   15-20    1  ---     I  NP
                                          32-79     iFine sandy loam,         Ism"  SM-SC     IA-2:  A-4     1 100      1100     185-100120-45        1  <30     INP-7
                                                    I sandy clay loam.
                                                    I
               Wa ---------------       1   0-10    IFine sandy loam          ISM   SM-SC     IA-2   A-4     1 100      195-100150-98 130-50          1  <28     INP-7
                Wahee                   1 10-80     IClay, clay loam.         iCL:  CH        IA-6:  A-7     1 100      1 100 185-10CII51-90          1 38-70    118-42
                                        1           1                         1               1              1          1        1          1         1          1








      Dorchester County, South Carolina                                                                                                  137




                                           TABLE 14.--ENGINEERING INDEX PROPERTTES-Continued


                                                             I               ation           Percentage passinq
                                                                  Classific
          Map symbol and       Depth      USDA texture
                                                                                       I        sieve number-            IlLiquid  Plas
             soil name                                        Unified        AASHTO                              I         limit   Iticity
                                                                                          4     1,  10  1, 40.    200              i,d,,
                                In                                                                                          Pct
        YaA  --------------     0-18 Loamy fine sand         ISM          !A-2-4       1. 100   1100    175-100115-35    1  <25    INP-4
         Yaubannab             18-52 Sandy clay loam,        jSCr CLf     IA-2 A-4     1 100    195-100175-100125-55     1  <35    INP-16
                                         clay loam, fine      SM-SC,      I A-@        I        I       I
                                                             I            I            I        I       I
                                         sandy loam.          CL-ML
                               52-76 Fine sandy loam,                     IA-2, A-4    1 100    195-100175-lOOi25-50     1 25-50   INP-25
                                                             ISM, SM Scri
                                         sandy loam,         I Sc
                             I         I sandy clay loam.1
                             1 76-80   ISandy loam, loamyISM      SM-SC   IA-2, A-4    1 100    1100    175-100110-45    1  <28    INP-6
                             I         I fine sand,    fine  I SP'-SM
                             I         I sand.               I
                             I         I                     I
        Ye  ---------------  1   0-15  lFine sandy   loam    SM           ]A-2, A-4    1 100     100    175-100125-50    1  <30    INP-7
         Yemassee            1 15-48   ISandy clay   loam    CL ,  Sc,    !A-2 A-4   , 1 100     100    175-100130-70    1  16-38  j 4-18
                                         clay loam, fine      CL-ML         k-9
                                       I sandy loam.         I            I
                                       I                     ,SM-Sc       I            I                I        I       I         I
                               48-80   jSandy clay loam,     ISc, SMI     IA-2 A-4     1 100     100    175-100125-55    1  <35    INP-15
                                         sandy loam,          CL-ML        A-@
                                         sandy clay.          SM_SC'








              138                                                                                                                                          Soil Survey




                                                    TABLE 15.--PHYSICAL AND CHEMICAL PROPERTIES OF THE SOILS

              [The symbol < means less than; > means more than. Entries under "Erosion factors--T" apply to the entire
                    profile. Entries under "Wind erodibility group" and "Organic matter" apply only to the surface layer.
                   Absence of an entry indicates that data were not available or were not estimated]


                                                                                                                                         T-frosion Wind
               Map symbol and         IDeptblClay        I Moist      Permea-      'Availablel Soil 1,Salinityl.           Shrink-       _j:actors erodi-'Orqanic
                  soil name                              bulk       I bility       I water Ireaction                        swell          --F- bility         I  matter
                                                                                     pacity                               potential      I K     T group
                                                         density                   ica
                                       Ln       Pct      G/cc           In/hr        In/in                                                                        Pct
              AbA --------------      10-541    1-10111.40-1.551      6.0-20       10.02-0.0414 5-6 5       1    <2       JLow -------   10 101  5   1  1         1-2
                                                                                     08-0 1014 5-E                        Low -------    10,         I
              Albany                  154-591   1-20,11 50-1 701      2.0-6.0      10.             : i'O    1    <2       1                :,201,
                                      159-75113-35 1:55-1:65          0.6-2.0      iO.10-0.*1614.5-6:0      Ij   Q        ILow -------   10.241      1         1
                                      I       I          I          I                            I                        I              I     I     I         I
              'ApB --------------      0-7 i    1-1211 35-1.551       2.0-6 0      10 05-0 1014.5-6 5       1    <2       ILOW -------   10.101  5   1  2      1  0-2
              Alpin                    7-54      -7 11:40-1 551       6 0-26 010'03-0:0914.5-6:5            1    <2       ILow -------   10 101      1         1
                                            51  1
                                        -8      5-8      11.45-1 651  2 0-6   .         -0.0914.5-6     . 5 1    <2           -------    !0" 01      1         1
                                      54                                           10*.06                                 Low
                                      I
              BIA, BIB  ---------     10-441    1-7      111.30-1.601 6.0-20       10.03-0 0714 5-6 0       1    <2       ILow -------   10,101  5   1  2      1  .5-1
              Blanton                 144-80112-30       1.60-1.701   0.6-2.0      10.10-0:1514'5-5*5       11   <2       ILow -------   10'201      1         1
                                      1       1                                                  1 ,                      I              I " I       I         I
              BoA, BoB  ---------     1 0-271 2-8 11 30-1 701         6 0-20       10.04-0 0814 5-6 0       1    <2       !Low -------   10 151  5   1  1      1  .5-2
              Bonneau                 127-80118-3511:40-1:601         0:6-2.0      10.10-0:1514:5-5:5       1    <2       1Low -------   10':201     1         1
                                      I       I          I          I              I             I          I             I              I , I       I         I
              Br ---------------      1 0-8 11 5-3011 20-1 451        0.6-2.0      10.15-0.2014.5-6.5       1    <2       ILow --------  10 241  4   1  5         3-10
              Brookman                18-49 35-55il:30-1:501          0.6-2.0      10 18-0:2214.5-6.5       1    <2       jModerat, 10*281           1
                                      149-76120-5511.45-1.6510.06-0.2              1 *                                      )derate 10'24
                                                                                   0.12-0 16     15.1-7.8   1    <2       1M(            I
              Ca ---------------      11 0-21135-501        ---     10.06-0 2      10 01-0 0315 6-7 8       1    >16      lHigh -------  10 281  5   1  ---    I  ---
              Capprs                  121-80140-701         ---     1 <0.06*       10'01-0:0316:6-8:4       1    >16      IHiqh -------              I         I
                                      I       I          I          I              I I           I          I             I              I     1     11        1
              ChA --------------      1 0-7 1 1-5 11     35-1 451     6 0-20       10 05-0.1014.5-6 0       1    <2       iLow --------  10 101  5   1  2      1  2-5
              Chipley                 17-751    1-7      11:45-1:601  6:0-20       10:03-0.0814.5-6:5       1    <2       ILow --------  10:101'     1         1
                                      I       I          I          I              I             I          I             I              I     I     I         I
              CoB --------------      10-301    2-1011 40-1.701       6.0-20       10 03-0 0514 5-6.0       1    <2       ILow --------  10.101  5   1  1      1  <1
              Chisolm                 130-58118-3511'30-1 501         0 6-2 0      10'10-0*1514'5-6 0       1    <2       ILow --------  10 151      1         1
                                      158-80!15-3511:30-1:501         0:6-6:0      10:08-0:1514:5-6:0       1    <2       ILow --------  !0:151      1         1
              CS ---------------      10-261    5-1211 40-1 701       6 0-20       10.06-0.1114.5-6 0       1    <2       ILow --------  in 151  5   1  2      1  .5-2
              Coosaw                  126-78118-3511*30-1:501         0:6-2.0      10.08-0.16    4.5-5:5    1    <2       ILo  --------- 16*241      1         1
                                      I       I          I ,        I              I                        I             I              I , I       I         I
              Cx ---------------       0-111 5-27,11 45-1 651         0 6-2 0      10.12-0.1713 6-5 5       1    <2       ILow --------  10 241  5   1  ---    1  2-4
              Coxville                11-80135-60 1:25-1:451          0:2-0:6      10.14-0.1813:6-5:5       1    <2       jMod,rat, 10*321           1
                                              I          I          I              I             I          I             I              I * I       I
              Da ---------------      1 0-261110-2011.40-1 50"        0.6-2 0      10 18-0.20!4.5-6.5       1    <2       ILow --------  10 321  5   1  ---    1  .5-2
              Daleville               1                  1 40-l'.50110.06-0:6      10'16-0.2014.5-5.5       11   <2       IModerate !0:371           1         11
                                      I
                                      26-80112C,-3511!..,                          I
              Ec ---------------      1 0-7   1 1-8 11.40-1 60      1 2 0-20       10.03-0.0814 5-6 0       1    <2           ---------  10 10i  5   '1'1         <1
              Echaw                   17-451    2-1011 40-1:60,         :                   10i .       .   I             Low --------   10,101
                                                                    , 6 0-20       0.05-0. 4.5-6 0               <2       LOW              . 1
                                      145-801'  21-1011'50-1 70i      2.0-20       10.03-0.0814.5-6:0            <2       11,ow -------- 10.10 1     1
              Eo ---------------      1 0-201   2-8 11 40-1.601       6.0-20       10.06-0.1114.5-6 5       1    <2       ILow --------  10 151  5   1 ---     1  2-8
              Elloree                 120-231   1-6      11:50-1 701  6 0-20       10 02-0 1015 1-7:3       1    <2       'Low --------  10:10,      1
                                      123-721   S@-2511 30-1*601      2:0-6.0      10:10-0:1515:1-8 4       1    <2       ILow --------  10 151      1
                                      172-601   !;-2511'30-1*501      0.6-6.0      10.10-0 . 1715  .1-8:4   1    <2       ILow --------  10:171      1         1
                                      I       I          I *   , I                 I             I          I             1              1     1     1         1
              EpB --------------      1 0-141   5-1011 30-1 40"       6.0-20       10 05-0 1014 5-6 0       1    <2       ILow --------  In 281  4   1  2      1  .5-3
              Emporia                 114-411 1 EI-3511*35-1'45i      0 2-2 0      10'10-0*1814:5-6*0       1    <2       ILow --------  16*281      1         1
                                                1-40 1*
                                      141-5412           1 .45-1 6010   66-0'6     10:10-0'1614 5-6'0       1    <2       IModerate 10 2 1           1
                                                                   0,                                                                         0
                                      154-751 5-4011.45-1:6 0:06-2:0               10.08-0'1814:5-6*0       1    <2       IModerate 10'201           1         1
                                      I       1          11         1              1             1          1             1              1 *   I     I         I
              EuA, EuB  ---------     1 0-111   ei-2011 40-1 601      2.0-6 0      10.08-0.1214 5-6.5       1    <2       ILow --------  10 241  5   1  3      1  .5-2
              Eulonia                 111-27135-4511*50-1501          0.2-0:6      !0.12-0 1614:5-6 0       1    <2       ILow --------  10'241      1         1
                                      1 -491 5-3511:50-1:701          0.6-2 0      10 10-0 1414    .5-6 0   1             ILow ----- :--10 201       1         1
                                      27      1                                                                  <2
                                      149-801,                                                                            -------- --    I_:__I      I         I









       Dorchester County, South Carolina                                                                                                            139




                                  TABLE 15.--PHYSICAL AND CHE24TCAL PROPERTIES OF THE SOILS--Continued


                                     I       I            I            I            I           I           f             I Erosion'Wind
          Map symbol and     IDeplth Clay    I Moist      I   Permea-  lAvailable   I Soil ISalinity, Sbrink-               fac-torslerodi-IOrganic
          Soil name          I                  bulk      I bility     I water Ireactioni                                 -----r-lbil ity I      matter
                                                                                                I           I  swell                        .  I
                                                density                !Capacity ,              I           potential       K       T Igoup,
                               in      Pct      G/cc -        janE -   ' In/in 1         LH     iMMboS/CM   i                         I        I -
       FoA --------------    1 0-131   5-1211.20-1 401        6 0-20   10 05-0 1014 5-6 5       1    <2     ILow -------  10 151    5 1     2  1 .5-2
       Foreston              113-32110-1811.20-1:401          2:0-6 0  10'09-0*1314:5-6:0       1    <2     ILow -------  10-101      1        1
                             132-531 4-1211 30-1 601          6 0-2;   10*03-0:1014 5:6 0       1    <2     ILow -------  10'101      1        1
                             153-80110-3511:35-1:601          0:6-2.0  10:12-0.1614:5 6:0       1    <2     ILow -------  10'201      1        1
                             1       1       1            1            1            1           1           1             1 * I       I        I
       ?xB --------------    1 0:141   1-8 11 25-1 551        >20      10 02-0 1014 5-6 0       1    <2     Low -------   10 101    5 1     2  1   <1
                             114 851   1-6   11 40-1 601               10 02-0 OSi4:5-6:0       I           ILow -------  10 101      1        1
       Foxworth              I       I       I  :      :  1   >20      1 :       :  1           1    <2     1             1 :    I    I        I
       GoA --------------    1 0:1411  2-8   11 55-1 751      60-20.010 06-0 1114 5-6 0         1    <2     Low -------   10.171    5 1 ---    1 .5-2
                             114       8-3011'30-1'501        06-2.0             ' 14:5-5:5     1    <2     ILow -----  :JO.24I       I        I
       Goldsboro                 _6211                                 10*.11-0.15
                             162 801 --- I                I   ---      I   ---      I   ---     I    --     I-------- -   I- D        I        I
                             I       I       I            I            I            I           I           I             I      I    I        I
       Gr ---------------    1 0-101   7-1811 45-1 651        20-6 0   10 10-0 1414 5-6 5       1    <2     Low -------   10 201    5 1  ---   1   2-4
       Grifton               110-61118-3511:35-1:451          0:6-2:0  10:12-0:1715:6-8:4       1    <2     ILow -------  10*241      1        1
                             161-801   ---   I    ---     I   ---      I   ---      I   ---     I    --     I----------   I_:__I      I        I
                             I       I       I            I            I            I           I           I             I      I    1        1
                                  481  ---   10 75-1 401      ---      I   ---      16 6:8 4    1   >16
       Handsboro   -------   11408:801 ---   10-75-1 401      ---      I   ---      16 6 8 4    1   ---
       Hb


       Hp.
       Haplaqueants
       TzA, IzB  ---------   1 0-13110-2011 40-1 601          2 0-6.0  10 16-0 2213 6-6 0       1    <2     ILow -------  10 371    5            .5-2
       Izagora               113-41118-3011*40:1*601          0*6-2 0  10:12-0:2013:6-5:5       1    <2     ILow -------  10*321
                             141-80135-5511:30 1:6010.66-0:2           10. 16-0  .2013.6-5.5    1    <2     lModerate--10:321         I        I
                             I       I       I            I            I            I           I           I             I      I    I        I
       Jd ----------------   1 0-15110-1811.40-1.501          2.0-6 0  10.11-0 1714 5-6 0       1    <2     ILow -------  10 321    5 1     3  1   1-3
       Jedburg               115-75118-3011 30-1 401          0 2-0:6  10 15-0*2214:5-6*0       1    <2     ILow -------  10*281      1        1
                             175-80120-4011:20-1:401          0:2-0.6  10:12-0:2014.5-6:0       1    <2     ILow -------  10:281
                             I       I       I            I            I            I           I           I             I      I
       JoA ---------------   1 0-6 1 4-1211.60-1 751          2'0-6 0  10 06-0 11 4 5-5.5       1    <2     Low -------   10 151    5 1 ---    1 .5-2
       Jobns                 1 6-31118-3511 40-1*601          0 6-2*0  10'12-0'1514:5-5 5       1    <2     ILow -------  10*241      1        1
                             131-801   2-1011:60-1:751        6:0-26   10:03-0:0614   . 5-5:5   1    <2     ILow -------  10:101      1        1
                             I       I       I            I            I            I           I           I             I      I    I        I
       Le ---------------    1 0-171   1-6 11 40-1 651        6 0-20   10 02-0.0513 6-5     *5  1    <2     ILow -------  10 101    5 1     2  1 .5-4
       1,eon                 1.17-651  2-8   11:50-1:701      0:6-6 0  10*05-0 1013'6-5 5       1    <2     ILow -------  10-151      1        1
                             165-801   1-6   11.40-1.651      0.6-6:0  10:02-0:0513:6-5:5       1    <2     ILow -------  10:101      1        1
                             I       I       I            I            I            I           I           I             I      I    I        I
          ---------------    1 0-5 1   4-1811 55-1 701        2 0-6 0  10 08-0 1214 5-5 5       1    <2     Low -------   10 241    5 1 ---    1   2-4
       Lumbee                1 5-37118:3511:30-1:451          0:6-2*0  10'12-0'1614*5-5:5       1    <2     ILow -------  10*321      1        1
                             137-701 1 1011     .60-1  .751   6.0-26   10:03-0:0614:5-5.5       1    <2     ILow -------  10:101      1        1
                             I       I       I            I            I            I           I           I             I      I    I        I
       Ln ----------------   1 0-7 1   2-1011 40-1 701        6 0-20   10 07-0 1013.6-5 5       1    <2     Low -------   10 151    5 1     2    .5-5
       Lynchburq             1 7-80118-3511:30-1:501          0:6-2.0  10:12-0:1613.6-5:5       1    <2     iLov -------  10:201      1
       Ly ----------------   1 0-191 1-4 11 35-1 601          6 0-20   10 05-0 1013 6-5 5       1    <2     ILow -------  10 101    5 1     2  1   1-4
       Lynn Haven            119-491   2-8   11:40-1:551      0:6-6,0  10'10:0'-013:6-5:5       1    <2     ILow -------  10-151      1        1
                             149-751   2-5   11 .50-1  .651   >20      10:01 0:08513.6-5.5      1    <2     ILow -------  10:10i      I        I
                             I       I       I            I            I            I           I           I             I      I    I        I
       No ---------------    1 0-8 110-2211 30:1.501          2 0-6 0  10 10-0 1514 5-6 5       1    <2     ILow-:-:--:10 201       5 1     2  1 .5-4
       Mouzon                1 8-61118-3511'30_1 5010 66-0'2           10*10-,0:1515:1-8:4      1    <2     1Low-_-_--_10:201         1        1
                             161-68112-3511'30_1:501          6.2-0:6  10:10:0   .1516. 1-8 .4  1    <2-    ILow-_-_--_10 201         1        1
                             168-801 --- I                I   ---      I   - -      I   ---     I    --     I---- - --    1-:--l      I        I
                             I       I       I            I            I            I           I           I             I      I    I        I
       Na ---------------    1 0-18110-1511 60:1 701          2 0-6 0  10 15-0 2014 5-6 5       1    <2     Low -------   10 201    5 1  ---   1   6-15
       Nakina                118-61118-3011'60_1:701          0:6:6'.0 10:12-0:1715:1-8:4       1    <2_    ILow -------  10'281      1        1
                             161-801 --- I                                                                  ----------    I_:__I      I        I
       NoA --------------    1 0-141 2-8 11 55-1 751          6 0-20   10 06-0 1114.5-6 0       1    <2     ILow -------  10 171    5 1  ---   1 .5-2
       Noboco                114-80118-3511:30-l.'451         0:6-2.0  10:10-0:2014.5-S'.5      1    <2     )Low -------  10:241      1        1
                             I       I       I            I            I            I           I           I             I      I    I        I









               140                                                                                                                                               Soil Survey




                                              TABLE 15.--PHYSICAL AND CHEMICAL PROPERTIES OF THE SOILS--Continued


                                                    I      I           I               I             I            I            I                                d
                                                                                       I                                       I               , Erosion Win
                  Map symbol and         IDeptblClay         moist     I  Permea-      'Available        Soil     fSalinity    I Shrink-       -Eactorsierodi- Organic
                     soil name           I          I      I bulk      I bility        I water       reactioni                 I swell         i     T-1bility       I matter
                                         I          I      I                           I                          I            1potential      I     I
                                                    I-     Idensity    1,              capacity      ,            j                               K    T   ,group.
                                          L
                                           n        I TR     G/cc      'I - -I-n=b r     In I-in     I -   H      I                            I
                                            _       j__      _                              _        I   p        Mmbos/cm     I               I           I
               OcA --------------        10-231     11-1011  45-1   651   2 -0-20      110 05-0 0714.5-5.5        11  <2       1,Low --------  10 101  5   1  2      1   1-2
                Ocilla                   123-801    15-3511*55-1 701      0.6-2.0      110:09-0:1214 5-5.5            <2       jLow --------   10:241      1         1
                                         1          1      1 *         I                             I "          i                            I     I     I         I
               Og ---------------        1 0-121 5-1011 35-1 451          0 6-2.0      10 10-0 1414 5-5 5         1   <2       1Lov------J0 101        5   1 ---     1   1-2
                Ogeecbee                 112-571,2)-3511*55-1*651         0*6-2 0      10:08-0:1414:5-5:5         1   <2       ILow --------   10:151      1         1
                                         1 7-65111(.-,          -1'651    0'6-2:0      110. 10-0 .1414 . 5-5  .5  i            ILow --------   10.151      1         1
                                         5          .5 -1011'55                                                       <2
                                         1                 i ,      , I     ,          I             I            I            I               I     I     I         I
               Os ---------------        10-3 IlO-1511.35-1 601           6.0-20       10.10-0.1513.6-6 0         1   <2       ILow --------   10 151  5   1  3      1   2-5
                Osier                    13-801 2-5        11.40-1:601      >20        10.02-0.0513.6-6:0         1   <2       ILow -------    10'051      1         1
                                         I
                                         I
                                         1  -18,1115-151'       -1 601    2 0-6.0      10.10-0.2013.6-5.5             <2       jLoi -------    10 151  5   1 ---     1   4-10
               Pa ---------------         0                L 40                                                                    or          I  *
                Panteqo                  118-37 8-351i*30-l'401           0 6-2.0      10 12-0 2013.6-5 5             <1       'Low -------    10 281                11
                                         137-8011:3-401 ,             01    :                                 :5  1   <2       ILow -------    10 :281     1         1
                                                           1.25-1.4       0 6-2.0      0 15-0 20 3.6-5
                                         1          1      11          1               1             1            1            1               1     1     1         1
               Pe ---------------        11 0-351 1-8      11 50-1 701    6 0-20       10.04-0 0714 15-5 5        1   <2       lVery low 10 101        5   1  2      1   1-2
                Pelham                   35-80115-3011:30-1:601           0:6-2.0      10.10-0:1314:'5-5:5        1,  <2       iLow -------    10'241      1         1
                                                    1      1           1               1             1            1            1               1 , I       I         I
               Pm ---------------        1 0-9 11 1-7 11.35-1 651         6 0-20 010 03-0.0813 6-5 5              1   <2       lVery low       10 101  5   1 ---     1   1-15
                Plummer                                                                              13:6-5 5     1   <2       lVery low       10*101      1         1
                                         19-581     1-7    11 35-1:651    6:0-20'010.03-0.20
                                         18-7 1     5-3    11   -1  .701  0 .6-2.'     1     -0.1513.6-5      .5  1   <2       lVery low       10'151      1         1
                                         15    5    11 0   1:50                   0    0.07
               Ra ---------------        1 0-9 15-2011 30-1 60         1  2 0-6   0    10.10-0.1414.5-6.5         1   <2                               5   11 3          1-6
                Rains                    19-421 8-35 1:30-1:501           0:6-2:0      0.11-0.15 4.5-5.5              <2       Low --------    0.24
                                         142-56118-4011 30-1 501          0 .6-2 0     10 10-0 1514.5-5 5         1   <2       ILOW --------   113.281     1
                                         156-80115-4511:30-1:601          0 .6-2:0     10:10-0:1514.5-5:5         1   <2
                                         I          I      I           I               I             i            I
               Ru ---------------        1 0-211    <10    i   ---     1  6.0-20       110.04-0 1013 6-5 5        1   <2       !Low --------   10 171  5   11            3-15
                Rutlege                  121-75!    <10    I   ---     1  6.0-20       10.04-0:0813:6-5.'5        1   <2       jLow------J0*l71            I
                                         I          I      I           I                             I            I                            I , I       I
               Se ---------------        1 0-141    0-3    11 60-1 701    6 0-20    0'0 03-0.0613.6-6.0           1   <2       ILow --------   10 101  5   1  ---    1   <.5
                                         14-181     3      11 60-1 701                                                                                               1
                Seagate                  11         -10 :                 6:0-20*010.05-0.1213.6-6.0              1   <2       ILow--------10 151          1
                                         118-321    1-5 11 60:1 701       2 0-6 6      10 03-0 0613 6-6 0         1   <2       1Low-----..-10:1O1          1         1
                                         132-7911.0-3511:40 1:501         0:6-2:0      10:12-0:2013:6-6:0         1   <2       1Low-----..-1O.281          I         I
                                         I          I      I           I               I             I            I            i               I     I     I         I
               Wa ---------------        I 0-101 5-20,11 30-1 601         0 6-2 0      110*10-0:1514 15-6 0       1   <2       fLow --------   10 241  5   1, 3      1  .5-5
                                                    5-55 1 40-1                                        .6-                     IMod,rate 10:281            1         1
                Wabee                    110-8013                   :6010.66-0:2       0.12-0 20 3" -5:5              <2
               YaA --------------        1 0-181 5-1511 40-1.601          6 0-20       10 06-0 1113 6-6 5         1   <2       ILow --------   10 171  5   1  2      1  .5-4
                                         1                                             1                                                                             1
                Yauhannah                18-521.LS-3511*30-1 501          0:6-2 0      0:11-0:1613:6-610          1   <2       ILow --------   10'241      1
                                         152-761-10-3011:30-1'50!         2 .0-6:0     10 10-0   .1513 6-6    .0  1   <2       jLow --------   10 -241     1         1
                                         176-801''5-1511.30-1:601         2.0-20       10:06-0.1213:6-6.0         1   <2       jLow -------    10 171      1         1
                                         1          1      1                                         1            1                            1 , I       I         i
               Ye ---------------        1 0-151'0-2011.30-1.601          2.0-6 0      10.10-0.1513 6-6.0         1   <2       ILow -------    10.201  5   1  3      1  .5-4
                Yemassee                 115-481'8-3511 30:1.501          0.6-2:0      110.11-0.1813:6-5.5            <2       1,Low -------   10 201      1         1
                                         148-801                    501   0.6-2.0      0.11-0.1713.6-5.5              <2                .___1 * I          1         1
                                                    2-4011 30 1.                       1                                       Low----         10.20









     Dorchester County, South Carolina                                                                                                      141




                                                       TABLE 16.--SOIL AND WATER FEATURES

        ["Flooding" and "water table" and terms such as "rare," "brief," "apparent," and "perched" are explained in
              the text. The symbol > means more than. Absence               of an entry indicates that the feature is not a
              concern or that data were       not estimated]


                               I            _r               Flooding                        High water table            Risk of corrosion
          Map symbol and       1Hydroloqicl                  I                                 ---T-         I                       I
            soil name             group       Frequency       Duration        Months      Depth      Kind IMontbs       IlUncoated   IConcrete
                                                                                                                          steel


        AbA ---------------    I    C        INone --------  I   ---       I   ---      11.0-2.5iApparentiDec-MariHigb       -----   iHigh.
         Albany                I             I               I             I            I         I          I          I            I
                               i             1               11            11           1         1          1          1            1
        ApB ---------------    I    A        iNone --------  I   ---       I   ---        @6.0    1  ---     I ---      Low ------   IHigh
         Alpin
        BIA, BIB  ----------   I    A        INone --------  I   ---       I   ---      15.0-6.01Percbed     IDec-MarIHigh   -----   1,Hiqh.
         Blanton               I             I
                               1             11
        BOA, BOB  ----------   I    A        INone --------                I   ---      13.5-5.OlApparentiDec-MarILow       ------   IHiqb.
         Bonneau               I             I                                          I         I          I          I            I
                               I             I                             I            I         I          I          I            i
        Br ----------------    I    D        IFrequent ----  ILong ------  1Nov-Apr     I  0-I.OlApparentINov-MaylModerate           IModerate.
         Brookman              I             I               I             I
                               I             I               I             i
        Ca ----------------    I    D        IFrequent ----  IVery bried    Jan-Dec     I  +1-1.OlApparentiJan-DeclHigh-----IHigh.
         Capers                I             I               I             I            I         I          I          I            I
                               I             I               I             I            I         I          I          I            I
        ChA ---------------    I    C        INone --------  I   ---       I   ---      12.0-3.OlApparentIDec-AprILow       ------   IHiqb.
         Chipley               I             I               I             I            I         I          I          I            I
                               1             11              1             1            1         1          1          11           1
        COB ---------------    I    A        114one -------- I   ---       I   ---      13.5-5.OlApparentiJan-MarILow       ------   lHigh.
         Chisolm               I             I               I             I            I         I          I          I            I
                               I             It              I             I            I         I          I          I            i
        CS ----------------    1    D        INone --------  I   ---       I   ---      12.0-3.OlApparent Dec-Mar Moderate           IHiqh.
         Coosaw
        Cx ----------------    I    D        iNone --------                             1  0-l.51ApparentINov-AprIHiqb       -----   lHigh.
         Coxville              I             I                                          I         I          I          I            I
                               I             I                                          I         I          I          I            I
        Da ----------------    I    D        INone --------                             I  0-1.01APparentiNov-MaylHigh       -----   IHiqh.
         Daleville             I
                               I
        Ec ----------------    I    B        INone --------  I             I   ---      12.5-5.OlApparentINov-AprILow       ------   lHigh.
         Echaw
        Eo ----------------    I    D        10ccasional     !Long ------  IDec-Apr     I  0-l.0IApparentINov-AprjHigb       -----   Moderate.
         Elloree               I             I
                               I             I
        EpB ---------------    I    C        iNone --------  I   ---       1   ---      13.0-4.5iPercbed lNov-AprIModerate           lHigh.
         Emporia               I             I               I             I            I         I          I          I            I
                               I             i               1             11           1         1          1          1            11
        FuA, EuB  ----------   I    C        INone --------  I   ---       I   ---      11.5-3.51APparentiDec-MaylModerate           IHigb.
         Eulonia               I             I               I             I            I         I          I          I            I
                               I             I               I             I            I         I          I          I            I
        FoA ---------------    I    C        INone --------  I   ---       i   ---      12.0-3.5lApparentIDec-ApriModerate           iHigb.
         Foreston              I             I               I             I            I         I          I          I            I
                               I             I               I             I            I         I          I          I            I
        FxB ---------------    I    A        INone --------  I   ---       I   ---      13.5-6.OiApparentIJun-OctiLow       ------   IHiqb.
         Foxworth              I             I               I             I            I         I          I          I            I
                               I             I               I             I            I         I          I          I            I
        GOA ---------------    I    B        INone --------  I   ---       I   ---      12.0-3.OlApparentiDec-AprIModerate IHiqh.
         Goldsboro             I             I               I             I            I         I          I          I            I
                               I             I               I             I            I         I          I          I            I
        Gr ----------------    I    D        lFrequent ----  IBrief  ----- IDec-May     10.5-I.OlApparentiDec-MayiHigh       -----   Low.
         Grifton









            142                                                                                                               Soil Survey



                                                 TABLE 16.--SOTL AND WATER FE&TURES--Continued
                                                                     9                          __Te__r_f_ab7F_ _r`_@Riso@fc
                                                             Floodin                       High wa                ___orrosion
                Map symbol and    lHydrologici
                 soil name           grot                     Duration       Months   IDepth   I Kind    IMoDths  !Uncoated   IConcrete
                                         Ip     Frequency                                                                     I
                                                                                                                    steel

             Hb ----------------  I   D       lFrequent ---- ILong ------I Jan-Dec    I +3-O.51AppareDtIJan-DecIHiqb   -----  IHigb.
              Handsboro


             lip.
              Haplaquents
             TzA, IzB ----------  1   C       INone -------- I               ---      11.5-2.5lApparentIDec-11.4ariModerate   IHigt.
              Izagora
             Jd ----------------  I   C       INone -------- I   ---         ---      10.5-1.5lApparentiNov-.Rpy'lHigh-----IHigh.
              Jedburg             I
                                  I
             JoA ---------------  I   C       ?Rare -------- IBrief -----I   ---      11.5-3.OlApparentIDec-Api,lModerate     IHigh.
              Johns               I           I              I           I
                                  I           1              11          1
             Le ----------------  I  B/b      INone -------- I   ---                  I O-l.OIApparentIJun-FebIHigh    -----  iHigh.
              Leon                I           I              I                        I        I         I        I           I
                                  I           I              I                        I        I         I        I           I
             Lm ----------------  I  B/D      10ccasional    IBrief ----- I.Dec-Apr   I 0-1.5lApparentiNov-,Ap:rlHigb-----IHigh.
              Lumbee              I           I
                                  1           11
             Ln ----------------  I   C       ixone -------- I           I   ---      10.5-1.5lApparentiNov--AprIHigh-----IHigh.
              Lynchburg
             Ly ----------------  I  B/D      ?None --------                          I O-l.01ApparentIJun--F4bIHtqh   -----  IHiqh.
              Lynn Haven          I           I                                       I        I         I
                                  I           I                                       I        I         I
             Mo ----------------      D       10ccasional    ILong ------I Dec-Apr    I 0-I.OlApparentiNov--AprIHigh   -----  Imoderate.
              Mouzon                          I              I           I            I        I         I        I           I
                                              I              I           I            I        I         I        I           I
             Na ----------------  I  B/D      IRare -------- IBrief -----I Jan-Mar    I 0-1.01APparentlNov.-AprIHigh   -----  IModerate.
              Nakina
             NoA ---------------  I   B       INoe --------  I   ---     I   ---      12.5-4.01APparentiDec.-MairiModerate    IHiqb.
              Noboco              I
                                  I
             OcA ---------------  I   C_      IKo'e -------- I   ---     I   ---      11.0-2.51ApparentlDec-AprlHigh   -----  IModerate.
              Ocilla              I           I              I                        I        I         I        I           I
                                  I           I              I           I            1        11        1        1           1
             Og ----------------  I  BID      IRarp -------- IBrief-----I  Jan-Mar    I 0-0.51ApparentlDec-MaylHigh    -----  IHigh.
              Ogeechee            I           I              I           I            I        I         I        I           I
                                  I           I              i           I            I        I         I        1           11
             Os ----------------  I  A/D      lFrequent ---- IBrief-----I  Dec-Apr    I 0-1.01ApparentlNom-MarlHigh    -----  !High.
              Osier               I
             Pa ----------------  I  B/D      None --------  I                        I 0-1.51ApparentlDec-MaylHiqb    -----  IHigb.
              Pantego             I                          I                        I        I
                                  I                          i                        I        I
             Pe ----------------  I  B/D      INone -------- 1,  ---     I   ---      10.5-l.5IApparentIJan-kprIHigb   -----  IHigb.
              Pelham              I           I                          I            I        I         I        I           I
                                  I           I                          I            I        I         I        I           I
             Pm ----------------  I  E;/D     None --------              I   ---      I12-1.5lApparentIDec-JtillModerate IHiqh.
              Plummer             I           I                          I            I        I         I        I           I
                                  I           I                          I            I        I         I        I           I
             Ra ----------------  I  B/D      None --------              I   ---      I O_l.OIApparentINov-AprIHiqb    -----  IHigh.
              Rains               I           I                          I            I        I         I        I           I
                                  I           I                          I            I        I         I        I           I
             Ru ----------------  I  B/D      IFrequent ---- IBrief-----I  Dec-May    I 0-l.01ApparentIDc4::-Y:ayIHigb -----  IFiah.
              Rutlege             I









       Dorchester County, South Carolina                                                                                         143




                                             TABLE 16.--SOTL AND WATER FEATURES--Continued

                                                                                  I    High water table         RIsk of  corrosion
                                                         Flooding
           Map symbol and     Hydrolocicl-               I
             soil name                   @I Frequency     Duration
                                group-                                  Months     Depth I    Kind    Months  lUncoated  IConcrete
                                           I                                               I                     steel
                                                                                     Ft
         Se ----------------  I   A/D      I                         I   ---      I             rentiNov-Apr'Piah  ----- lHigh.
                                           None --------                           1.5-2.5lAppai      I
          Seagate
         Wa ----------------  I    D       INone --------I   ---     I   ---      10.5-1.5lApparentIDer-MariHiqh   ----- IHiqb.
          Wahee
         YaA  --------------- I    B       INone --------                                       -entIDec-MariModerate    !Hiah.
                                                                                  ,1.5-2.5lAppat
          Yaubannah
         Ye ----------------  I    C       None -------- I           I   ---      11.0-1.5lApparentiDec-MariFiqh   -----   High.
          Yemassee            I                          I           I            I        I          I       I










            144                                                                                                                                         Soil Survey




                                                               TABLE 17.--ENGINEERTNG TNDEX TEST DATA

                                                [Dashes indicate data not available. NP means nonplastic]

                      Soil name, report                Classification                     Grain-size distribution                       Li(paidlPlasti-
                      number, horizon, and                         I                                                                    I   mit,   city
                                                                             I          Percentage                  Percentage            li
                                     nches)            AASHTO      Unified         passing sieve--                               -_     I
                      depth (in i                                                                             i smaller than                        index
                                                                               No.      No.                  -1
                                                                                         0      No       No       02   11.005  1.002    1
                                                                                 4      1       40       206
                                                                                                                  mm      ME       mm



                     Albany: 1/
                      S81SCO-5-10
                        A - - - - - -         0-6   IA-2-4(0)      ISP-SM    I ---    1 100      92   1   12                9                        NP
                        El   - - - - -        6-23  IA-3(0)        ISP-SM    I ---    1 100      97   1   10                8                        NP
                        Bt   - - - - -     54-6,'r  IA-2-4(0)      ISM       1          100      97   1   28              25                         NP

                     Chisolm: 2/
                      S81SC0357-7
                        A - - - - - -         0-7   IA-2-4(0)      ISM       1          100      80       24              10                         NP
                        E2   - - - - -     13-22    IA-2-4(0)      ISM       1 100    1 10    1  S3   1   27  1        1  11   1 ---    I   ---  I   NP
                        Btl  - - - - -     22-41    IA-4(0)        ISC       I ---    I 10(o)    86   1   42              29                25         8

                     Coosaw: 3/
                      S81SCO33-13
                        Ap   - - - - -        0-7   IA-2-4(0)      ISM       I ---    1 100      89       21              13                         NP
                        E    - -   ._ _  _    7-26  IA-2-4(0)      ISM       I ---    1 100      89   1   18  1        1  10   1 ---    I   ---  I   NP
                        Bt   - - -- - -    26-43    IA-2-6(01)ISC            I        1 100   1  85   1   33  1 ---    1  29   1 ---    1   37   1   15
                        Btq  - - - - -     43-56    1A-6(02)       ISC       I        1 100      95       39              32                39       17
                     Echaw: 3/
                      S80SCO735-13
                        Ap - - -- -      -    0-7   IA-3(1)        ISP-SM    I ---    1 100      73        9                7                        NP
                        E2   - - -- - -    18-45    IA-2-4(0)      ISP-SM    I ---    1 100   1  87   1   12  1             9                        lip
                        Bh2  - - - - -     52-60    1A-3(l)        1SP-SM    1          100      75        9                7                        NP
                     Oster: 4/
                      S80SCO'55-24_
                        A - - - -       - 0-7       iA-I-b(l)      ISP-SM    I loo       97      19        7                4  1            ---      Mp
                        Cgi  - - - - -        7-1'8 IA-1-b(i)      ISp-SM    1 100       95      18        7                5                        NP
                        Cg2  - - - - -     18-62    IA-1-b(i)      ISP           99      80        4       1                                         Np

                     Yauhannah: 3/
                      SBOSCO35-2'5
                        A - - - - - -         0-1   'A-2-4(0)      ISM                  100      91       28              15                         NP
                        BE   - - -- - -    18-  :@4 IA-2-4(0)      ISM       1 100       99      94       33              20                         NP
                        Btl  - - - - -     24-  :38 IA-4(0)        ism                  100      94       39              28                         Np
                        BCq -              52-76    IA-2-7(02)ISC              100       99      69       32              28                46 1     21


                            1/ 13.0 miles southwest of Summerville at                   the   intersection of South         Carolina Highway        165
                     and County Road 317, about 4.5 miles east on County                      Road 317, and 500 feet north of road.
                            2/ 12.5 miles southwest of Summerville on South Carol1na Highway 165, 3.75 mi:[es northwest
                     On South Carolina Highway 84, 500 feet southwest on South Carolina Highway 163, and 150 feet
                     southeast of road.
                            3/ Sample site is the same as that of the series typical pedon given in "Soil Series and
                     Their Morphology."
                            4/ 2 miles southeast of Grover, 1.5 miles east of U.S. Highway 15, 4,000 feet south of
                     South7Carolina Higbway 280, and 3,200 feet north of the Edisto River. This soil is a taxadjunct
                     to the Oster series because the pedon has more coarse sand in the upper part of the profile than
                     is typcial for the series.









       Dorchester County, South Carolina                                                                                145




                                             TABLE 18.--CLASSIFICATION OF THE SOILS


                 Soil name                                      Family or higher taxonomic class



         Albany  -------------------- Loamy, siliceous, thermic Grossarenic Paleudults
         Alpin   --------------------- Thermic, coated Typic Quartzipsamnents
         Blanton -------------------  Loamy, siliceous, thermic Grossarepic Paleudults
         Bonneau -------------------  Loamy, siliceous, thermic Arenic Palaudults
         Brookman ------------------  Fine, mixed, thermic Typic Umbraqualfs
         Capers  -------------------- Fine, mixed, nonacid, tbermic Typic Sulfaquents
        *Chipley -------------------  Thermic, coated Aquic Quartzipsaminents
         Chisolm -------------------  Loamy, siliceous, thermic Arenic Hapludults
         Coosaw  -------------------- Loamy, siliceous, thermic Arenic Hapludults
         Coxville ------------------  Clayey, kaolinitic, thermic Typic Paleaquults
         Daleville -----------------  Fine-loamy, siliceous, thermic Typic Paleaquults
         Echaw   --------------------- Sandy, siliceous, thermic Entic Haplobumods
        *Elloree -------------------  Loamy, siliceous, thermic Arenic Ochraqualfs
         Emporia -------------------  Fine-loamy, siliceous, thermic Typic Hapludults
         Eulonia -------------------  Clayey, mixed, thermic Aquic Hapludults
         Foreston ------------------  Coarse-loamy, siliceous, thermic Aquic Paleudults
         Foxwortb ------------------  Thermic, coated Typic Puartzipsamnents
         Goldsboro -----------------  Fine-loamy, siliceous, tbermic Aquic Paleudults
         Grifton -------------------  Fine-loamy, siliceous, thermic Typic Ochraqualfs
        *Handsboro -----------------  Euic, thermic Typic Sulfihemists
         Haplaquents  --------------- Haplaquents
         Tzaqore -------------------  Fine-loamy, siliceous, thermic Aquic Paleudults
         Jedburg -------------------  Fine-loamy, siliceous, tbermic Aeric Paleaquults
         Johns   --------------------- Fine-loamy over sandy or sandy-skeletal, siliceous, thermic Aquic Hapludults
        *Leon    ---------------------- Sandy, siliceous, tbermic Aeric Haplaquods
         Lumbee  -------------------- Fine-loamy over sandy or sandy-skeletal, siliceous, thermic Typic Ochraquults
         Lynchburg -----------------  Fine-loamy, siliceous, thermic Aeric Palpaquults
         Lynn Haven  ---------------- Sandy, siliceous, thermic Typic Haplaquods
         Mouzon  -------------------- Fine-loamy, siliceous, thermic Typic Albaqualfs
         Nakina  -------------------- Fine-loamy, siliceous, thermic Typic Umbraqualfs
         Noboco  -------------------- Fine-loamy, siliceous, thermic Typic Paleudults
         Ocilla  -------------------- Loamy, siliceous, thermic Aquic Arenic Paleudults
         Ogeechee ------------------  Fine-loamy, siliceous, thermic Typic Ochraquults
         Osier   --------------------- Siliceous, thermic Typic Psammaquents
         Pantego -------------------  Fine-loamy, siliceous, thermic Umbric Paleaquults
         Pelham  -------------------- Loamy, siliceous, tbermic Arenic Paleaquults
         Plummer -------------------  Loamy, siliceous, thermic Grossarenic Paleaquults
         Rains   --------------------- Fine-loamy, siliceous, thermic Typic Paleaquults
         Rutlege -------------------  Sandy, siliceous, thermic Typic Humaquepts
        *Seagate ---------            Sandy over loamy, siliceoust thermic Ultic Haplohumods
         Wahee   -----------          Clayey, mixed, thermic Aeric Ochraquults
         Yauhannah -----------------  Fine-loamy, siliceous, thermic Aquic Hapludults
         Yemassee ------------------  Fine-loamy, siliceous, tbermic Aeric Ochraquults


                 The soil is a taxadjunct to the series. See text for description of those characteristics of the
         soil that are outside the range of the series.


                                                              * U.S. GOVERNMENT PRINTING OFFICE : 1990 0 - 205-534  QL 3











                                                                                                   80*30'





                                                                         CO          95


                                                                             178               15                            COO
                                                 80.40'                                                                              je
                                                     1                                                       26
                                           33*15-                                Rosinville                                   7

                                                                                                                     453

                                                                  5

                                                    78                                                                                              80*20'
                   0                            eevesville                                             arleyville
                                                                                                                                                        wa
                                                                                    St. George                             178
                                                                                                                                     4q
                                      5
                                                                                                                                             26
                                                     C-1


                                             7      19                                                                                                        27
                                                                                               Branch                                  urchest 1-
                                                                          15
                                                                           Grover                             z
                                                                                    5
                                                                                                                             3                       6
                                                                                                                                                              Ridgevill
                                                33*05'                                                      19
                                                                                        9                                            7                     27
                                                                                                               9
                                                                               River                                                                 tains  Uree      I
                                                             COLL                                                                                                                  78               80-10'
                                                                     PON


                                                                                                                                            61                      In  S                       165
                                                                                                                                         6                                            Surarn   Me

                                                                                                                                            Givhans                               6

                                                                                                                                 9                                                                              2




                                                                                                                                                                                                           Eagle    Cr


                                                                                                                                                                                                           64
                                                                                                                                              17


                                                                                                                        32*55'-                                                            A
                                                                                                                                                                                                           61               4
                                                                                                                                      13

                                                                                                                                                                                                                      10
                                                                                                                                                                         165
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               Each area outlined on this map consists of
               more than one kind of soil. The map is thus
               meant for general planning rather than a basis
               for decisions on the use of specific tracts.






                                                                                                                                                                                                                                                                                                                                                                                    SOUTH CAROLINA AGRICULTURAL EXPERIMENT STATION
         U.S. DEPARTMENT OF AGRICULTURE
         SOIL CONSERVATION SERVICE                                                                                                                                                                 DORCHESTER COUNTY, SOYTH CAROLINA                                                                                                                                 SOUTH CAROLINA LAND RESOURCES CONSERVATION COMMISSION
                                                                                                                                                                                                                                                        ea`@=
                                                                                                      SUL LESEHO                                                                                                                                                                                           CGHWENYWNAL AND SPE=L
                                                                                                                                                                                                                                                                                                                          SYMBOLS LEGEND

                                                                                 The map symbols recommended for publication are alphabetic. The
                                                                                 first capital letter is the initial one of the soil name. The second letter
                                                                                 is a tower rase and is used to identify mapping units that have the                                                                                            CULTURALFEATURES                                                                                                                                 SPEMAL SYMBOLS FOR
                                                                                 same initial capital letter. The third letter, if used, is a capital and
                                                                                 connotes slope class. Symbols without a slope letter are nearly level                                                                                  BOUNDARIES                                                                                                                                               SOL SURVEY
                                                                                 soils.                                                                                                                                                    National, late or province                                             MISCELLANEOUS CULTURAL FEATURES                                            SOIL DELINEATIONS AND SYMBOLS                        :A:bA@@ApB
                                                                                                                                                                                                                                           County or parish                                                          Farmstead, house                                                        ESCARPMENTS
                                                                                                                                                                                                                                                                                                                        (omit in urban areas)
                                                                                                                                                                                                                                           Minor civi   division                                                     Church                                                                     Bedrock
                                                                                                                                                                                                                                                                                                                                                                                                   (points down slope)
                                                                               SYMBOL                                       NAME                                                                                                           Reservati n (national forest or park,                                     School                                                                     Other than bedrock
                                                                                                                                                                                                                                                state I est or park,                                                                                                                               lpoints down slope)
                                                                                                                                                                                                                                                and lar a airport)                                                                                                             Indian
                                                                                   AbA                Albany fine sand, 0 to 2 percent slopes                                                                                                                                                                        Indian mound (label)                                      Mound         SHORT STEEP SLOPE                                    .............
                                                                                   APB                Alpin fine sand, 0 to 6 percent slopes                                                                                               Land gra I                                                                Located object (label)                                    0Tower        GULLY                                                -
                                                                                   BIA                Blanton fine sand, 0 to 2 percent slopes
                                                                                   BIB                Blanton fine sand, 2 to 6 percent slopes                                                                                             Limit of     survey (label)                                                                                                         Gas
                                                                                   BOA                Bonneau fine sand, 0 to 2 percent slopes                                                                                                                                                                       Tank (label)                                              0             DEPRESSION OR SINK                                           0
                                                                                   BOB                Bonneau fine sand, 2 to 6 percent slopes                                                                                                          amatchline and neatline
                                                                                   Br                 Brookman clay loam, frequently flooded                                                                                               Field sh                                                                  Wells, oil or gas                                                       SOIL SAMPLE                                                  0
                                                                                   Ca                 Capers silty clay loam                                                                                                            AD HOC BOJINDARY (label)                                                     Windmill                                                                      (normally not shown)
                                                                                   ChA                Chipley sand, 0 to 2 percent slopes                                                                                                               I                                                                                                                                    MISCELLANEOUS
                                                                                   COB                Chisolm fine sand, 0 to 6 percent slopes                                                                                             Small airp@rt, airfield, Park, oilfield,       fLo            @-F
                                                                                   Cs                 Coosaw loamy tine sand                                                                                                                    cemete@, or flood Pool                                               Kitchen midden                                                             Blowout                                                   %:1
                                                                                   Cx                 Coxville loam
                                                                                                                                                                                                                                        STATE   Coo DINATE TICK
                                                                                   Da                 Daleville silt loam                                                                                                                               I                                                                                                                                       Clay spot
                                                                                                                                                                                                                                        LAND DIVIS ON CORNER                              L -I-   + -7-L
                                                                                   Ec                 Echaw fine sand                                                                                                                      (sections 4 nd land grants)                                                                                                                          Gravelly spot
                                                                                   Eo                 Elloree loamy fine sand, occasionally flooded
                                                                                   EpB                Emporia loamy fine sand, 2 to 6 percent slopes                                                                                    ROADS                                                                             WATER FEATURES                                                        Gumbo, slick or scabby spot (sodic)                       0
                                                                                   EuA                Eulonia fine sandy loam, 0 to 2 percent slopes
                                                                                   EuB                Eulonia fine sandy loam, 2 to 6 percent slopes                                                                                       Divided (r iedian shown
                                                                                                                                                                                                                                                if scale ermits)                                                                                                                                Dumps and other similar
                                                                                   FoA                Foreston loamy fine sand, 0 to 2 percent slopes                                                                                                                                                             DRAINAGE                                                                         non soil areas
                                                                                   FxB                Foxworth fine sand, 0 to 6 percent slopes                                                                                            Other roa s
                                                                                   GOA                Goldsboro loamy sand, 0 to 2 percent slopes                                                                                          Trail                                                                     Perennial, double line                         ------                      Prominent hill or peak
                                                                                   Gr                 Grifton fine sandy loam, frequently flooded                                                                                                                                                                    Perennial, single line                                                     Rock outcrop
                                                                                   Hb                 Handsboro muck                                                                                                                    ROAD EMBLEM         DESIGNATIONS                                                                                                                           (includes sandstone and shale)
                                                                                   HP                 Haplaquents, loamy                                                                                                                                                                                             Intermittent                                                               Saline spot                                               +
                                                                                                                                                                                                                                           Interstate
                                                                                   IzA                Izagora silt loam, 0 to 2 percent slopes                                                                                                                                                                                                                                                  Sandy spot
                                                                                   IzB                Izagora silt loam, 2 to 6 percent slopes                                                                                             Federal                                                                   Drainage end
                                                                                   Jd                 Jedburg loam                                                                                                                                                                                                   Canals or ditches                                                          Severely eroded spot
                                                                                   JoA                Johns loamy sand, 0 to 2 percent slopes                                                                                              State                                                                                                                          CANAL                 Slide or slip (tips point upslope)
                                                                                   Le                 Leon sand                                                                                                                            County, ta   -m orranch                                                      Double-line (label)
                                                                                   Lm                 Lumbee fine sandy loam, occasionally flooded                                                                                                                                                                                                                                              Stony spot, very stony spot                               0 co
                                                                                   Ln                 Lynchburg loamy sand                                                                                                                                                                                              Drainage and/or irrigation
                                                                                   Ly                 Lynn Haven fine sand                                                                                                              RAILROAD                                                                  LAKES, PONDS AND RESERVOIRS                                                   Small dug pond                                            a)
                                                                                   MO                 Mouzon fine sandy loam, occasionally flooded                                                                                      POWERTR SMISSIO             IN                    ---------------
                                                                                   Na                 Nakina fine sandy loam                                                                                                               (normally of shown)                                                       Perennial                                                                  Small borrow areas
                                                                                   NoA                NobDco loamy sand, 0 to 2 percent slopes                                                                                          PIPE LINE
                                                                                                                                                                                                                                           (normally of shown)                                                       Intermittent                                     int
                                                                                                                                                                                                                                                                                                                                                                        '_1
                                                                                   OcA                Ocilla sand, 0 to 2 percent slopes                                                                                                FENCE
                                                                                   Og                 Ogeechee fine sandy loam                                                                                                             (normally of shown)                                                    MISCELLANEOUS WATER FEATURES
                                                                                   Os                 Osier loamy fine sand, frequently flooded                                                                                         LEVEES
                                                                                   Pa                 Pantego sandy loam                                                                                                                                                                                             Marsh or swamp
                                                                                   Pe                 Pelham sand                                                                                                                          Without rc ad
                                                                                   Prn                Plummer loamy sand                                                                                                                                                                                             Spring                                                    0-
                                                                                   Re                 Rains sandy loam                                                                                                                     With road                                                                 Well, artesian
                                                                                   Ru                 Rutlege loamy fine sand, frequently flooded                                                                                          With railroad                                      -11-1. 11111. *ffill 1. 11 .1 Well, irrigation                                   -0-
                                                                                   Se                 Seagate sand
                                                                                                                                                                                                                                        DAMS
                                                                                   Wa                 Wahee fine sandy loam                                                                                                                                                                                          Wet Spot                                                                                                                                            U
                                                                                   YaA                Yauhannah loamy fine sand, 0 to 2 percent slopes                                                                                     Large (to    le)

                                                                                   Ye                 Yernassee fine sandy loam                                                                                                            Modium       c Small                                         1-J
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                                                                                                   CORCHESITR COUNTY, SULFFK CARU'- INA w. i

                                                           This soil survey map was compiled by the U. S. Department of Agriculture, Soil Conservation Service,
                                                           and cooperating agencies. Base maps are prepa:-ed from 1979 aerial photography. Coordinate grid
                                                           ticks and land division corners, if shown, are approximately positioned.










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                                                                                                                                                                           DORCHESTER -COUNTY, SOUTH CAROLINA                                                              SHEET NUMBER 3
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                                                                                                                                  DORCHESTER COUNTY, SOUTH CAROLINA - SHEET NUMBER 5

                                                                                             1 2085000 FEET



                                                     Os                               1 2 115 000 FEET                                                                (Joins sheet 24)
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                                                                                                                                                                                         DORC!-:'E_S___._R COUNT!, SC'_)TX                                    CARC-NIA                                    NUMBER             8

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                                                            if                                (Joins sheet 15)





                                                                                                                                                                                                    DORCHESTER COUNTY, SOUTH CAROLINA                                                                          SHEET NUMBER 7


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                                                                                                            DORCI-:' STER COUNTY, SO@jTX CARC)L:NA                    S'EET NUMSER 10
       10                                                                  (joins inset, si)eet 3 7


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                                                                                                                                          DORCHESTER COUNTY, SOUTH CAROLINA - SHEET NUMBER 9
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                                                                                                   DORCHESTER COUNTY,           SOUTH CAROLINA            SHEET NUMBER li
                                                                                  I 2065000FEET


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                                                                                                             'ioins sheet 7;                                                          DORC14-:1ESTER COUNTY, SCU-',@H CAROLINA                                                          Sl-:EET          NUMOIER 14
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                                                                                                                                                                                DORCHESTER COUNTY, SOUTH CAROLINA - SHEET NUMBER 13
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                                                                                                                                                                    DOM.-I.ESTER COJNTY, SOU71-i CAROLINA                                                                                           15

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                                                                                                                                DORCHESTER COUNTY, SOUTH CAROLINA                                     SHEET NUMBER 16
                                                     11E]        (Joins A eef V)                    F78 I
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                                                                   (Joins sheet 22)





         IN                                                                                                                            S Co       Cl K I C.: I \A                M 3 12 7-18
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                                                                                                                                             DORCHESTER COUNTY, SOUTH CAROLINA                                              SHEET NUMBER 17
                                                                                        190 OLA,  1                                     (Joins shzt 10)
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                                                                                                                                                             DORCHESTER COUNTY,_-SOLITH CAROLINA                                                         SHEET NUMBER 19
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                                                                                                                                           DORCHESTER COUNTY, SOUTH CAROLINA                                            SHEET NUMBER 21
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                                                                                                                                                                                                                     T                    NITY,                                          N' A              S-         T IN U M K R 2 4
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                                                                                                                                    DORCHESTER COUNTY, SOUTH                            CAROLINA               SHEET NUMBER 23
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                                                                                                                                          DO.R"'-:'S-       R =;XXTY, SOUTH                  CARC-Nf-@                           IMWIK'          25
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                                                                                                                                           DORCHESTER COUNTY, SOUTH CAROLINA                                               SHEET NUMBER 25
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                                                                                                                              DORCHESTER COUNTY, SOUTH CAROLINA                                       SHEET NUMBER 27

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                                                                                                                                                                                                --DORCHESTER COUNTY, SOUTH CAROLINA                                                                            SHEET NUMBER 29
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                                                                                                                                     DORCHESTER COUNTY, SOUTH CAROLINA                                           SHEET NUMBER 31

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                                                                                                                                                           DORCHESTER COUNTY,                       ---SO-UTH CAROLINA                             SHEET NUMBER 39
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                                                                                                                                   DORCHESTER COUNTY, SOUTH                            CAROLINA               SHEET NUMBER 43
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                                                                                                                                    DORCHESTER COUNTY, SOUTH CAROLINA                                          SHEET NUMBER 45
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                                                                                                                                                                            DORCHESTER COUNTY, SOUTH CAROLINA                                                                SHEET NUMBER 47

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                                                                                     DORCHESTER COUNTY, SOUTH CAROLINA               SHEET NUMBER 53
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        Soil Survey of Dorchester County, South Carolina
                                                                                                                    11) U, k-L) (3)
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      Natural Resources Conservation Service
      5809 W. Jim Bilton Blvd.
      St. George, SC 29477
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                                                                                                                                  C
                                                    NOAA COASTAL SERVICES CTR. LIBRARY                                       Z--
                                                    2234 S. Hobson Ave.
                                                    Charleston, SC 29405-2413
                                                     Attn: Jill Konieczko