\<@37\>Ailey Series

\<@33\>\<i\>*Depth class:*\<p\> Very deep

\<@33\>\<i\>*Drainage class:*\<p\> Well drained

\<@33\>\<i\>*Permeability:*\<p\> Slow

\<@33\>\<i\>*Parent material:*\<p\> Sandy and loamy marine sediments

\<@33\>\<i\>*Landscape:*\<p\> Coastal Plain

\<@33\>\<i\>*Landform:*\<p\> Uplands

\<@33\>\<i\>*Landform position:*\<p\> Narrow ridges; side slopes

\<@33\>\<i\>*Slope:*\<p\> 2 to 25 percent

\<@33\>\<i\>*Taxonomic class:*\<p\> Loamy, kaolinitic, thermic Arenic
Kanhapludults

\<@27\>Commonly Associated Soils

\<@30\>Cowarts, Lakeland, Maubila, Nankin, and Troup soils are commonly
associated with the Ailey series.

-   \<@49\>The Cowarts soils are in positions similar to those of the
    Ailey soils; do not have thick, sandy surface and subsurface layers;
    and have a solum that ranges from 20 to 40 inches in thickness.

-   \<@29\>The Lakeland soils are in the slightly higher positions, are
    excessively drained, and are sandy throughout.

-   \<@29\>The Maubila soils are in positions similar to those of Ailey
    soils; are moderately well drained; and have a fine control section.

-   \<@29\>The Nankin soils are in positions similar to those of the
    Ailey soils or slightly lower; do not have thick, sandy surface and
    subsurface layers; and have a fine control section.

-   \<@29\>The Troup soils are in the slightly higher positions, are
    somewhat excessively drained, and have sandy surface and subsurface
    layers with a combined thickness of 40 to 80 inches.

\<@27\>Typical Pedon

\<@30\>Ailey loamy sand, 5 to 8 percent slopes; about 2,500 feet north
of County Road 152, on a side slope adjacent to Collins Mill Creek;
Randolph County, Georgia; USGS Brooksville topographic quadrangle; lat.
31 degrees 51 minutes 2 seconds N. and long. 84 degrees 41 minutes 55
seconds W., NAD27.

\<@23\>Ap---0 to 3 inches; brown (10YR 4/3) loamy sand; weak fine
granular structure; very friable; many fine and medium roots and few
coarse roots; about 5 percent, by volume, angular ironstone; moderately
acid; abrupt wavy boundary.

\<@33\>E1---3 to 14 inches; light yellowish brown (10YR 6/4) loamy sand;
weak coarse subangular blocky structure; very friable; many fine and
medium and few coarse roots; about 5 percent, by volume, angular
ironstone; moderately acid; gradual wavy boundary.

\<@33\>E2---14 to 23 inches; yellowish brown (10YR 5/6) loamy sand; weak
coarse subangular blocky structure; very friable; many fine and medium
and few coarse roots; about 5 percent, by volume, angular ironstone;
strongly acid; gradual wavy boundary.

\<@33\>Bt1---23 to 30 inches; strong brown (7.5YR 5/6) sandy loam; weak
medium subangular blocky structure; friable; common fine and medium
roots; common medium distinct pockets of very pale brown (10YR 7/3)
clean sand grains; about 10 percent, by volume, angular ironstone;
strongly acid; gradual wavy boundary.

\<@33\>Bt2---30 to 42 inches; strong brown (7.5YR 5/8) sandy clay loam;
moderate medium subangular blocky structure; friable; few fine and
medium roots; few medium distinct pockets of very pale brown (10YR 7/3)
clean sand grains; about 12 percent, by volume, angular ironstone;
strongly acid; gradual wavy boundary.

\<@33\>Btx---42 to 47 inches; strong brown (7.5YR 5/6) sandy clay loam;
about 80 percent moderate medium subangular blocky structure and 20
percent red (2.5YR 5/6) strong thick platy; firm when moist; platy peds
are hard and brittle when dry; few medium roots; few faint clay films on
faces of some peds; strongly acid; gradual wavy boundary.

\<@33\>2Cd---47 to 80 inches; strong brown (7.5YR 5/6) clay loam;
massive parting to strong thick platy structure; very firm; few medium
roots; few faint clay films on faces of some peds; common medium
distinct red (2.5YR 5/6) and pale brown (10YR 6/3) masses in which iron
has accumulated; light gray (10YR 7/1) areas from which iron has
depleted; strongly acid.

\<@27\>Range in Characteristics

\<@33\>\<i\>*Thickness of the solum:*\<p\> 42 to 60 inches

\<@33\>\<i\>*Thickness of the sandy epipedon:*\<p\> 20 to 40 inches

\<@33\>\<i\>*Reaction:*\<p\> Very strongly acid or strongly acid
throughout, except where the surface layer has been limed

\<@23\>\<i\>*A or Ap horizon:*\<p\>

\<@31\>Color---hue of 10YR, value of 3 to 5, and chroma of 2 or 3

\<@31\>Texture---loamy sand or sand

\<@23\>\<i\>*E horizon:*\<p\>

\<@31\>Color---hue of 10YR, value of 5 or 6, and chroma of 4 to 6

\<@31\>Texture---loamy sand or sand

\<@23\>\<i\>*BE horizon (where present):*\<p\>

\<@31\>Color---hue of 7.5YR or 10YR, value of 5 or 6, and chroma of 6 to
8

\<@31\>Texture---loamy sand or sandy loam

\<@23\>\<i\>*Bt horizon:*\<p\>

\<@31\>Color---hue of 7.5YR or 10YR, value of 5 or 6, and chroma of 6 to
8

\<@31\>Redoximorphic features---no, few, or common iron accumulations in
shades of brown and red

\<@31\>Texture---sandy loam or sandy clay loam

\<@23\>\<i\>*Btx horizon:*\<p\>

\<@31\>Color---hue of 7.5YR or 10YR, value of 5 or 6, and chroma of 6 to
8; or no dominant color and multicolored in shades of red, yellow,
brown, and gray

\<@31\>Redoximorphic features---few or common iron or clay depletions in
shades of gray and iron accumulations in shades of brown, red, and
yellow

\<@31\>Texture---sandy clay loam

\<@31\>Other features---brittle and hard bodies, commonly red, make up
10 to 40 percent, by volume, of the horizon.

\<@23\>\<i\>*Cd or 2Cd horizon:*\<p\>

\<@31\>Color---hue of 5YR to 10YR, value of 4 to 7, and chroma of 4 to
8; or no dominant color and multicolored in shades of red, yellow,
brown, and gray

\<@31\>Redoximorphic features---common or many iron or clay depletions
in shades of gray and iron accumulations in shades of red, brown, or
yellow

\<@31\>Texture---sandy loam, sandy clay loam, or clay loam

\<@37\>Benevolence Series

\<@33\>\<i\>*Depth class:*\<p\> Very deep

\<@33\>\<i\>*Drainage class:*\<p\> Well drained

\<@33\>\<i\>*Permeability:*\<p\> Moderate or moderately rapid

\<@33\>\<i\>*Parent material:*\<p\> Sandy and loamy marine sediments

\<@33\>\<i\>*Landscape:*\<p\> Coastal Plain

\<@33\>\<i\>*Landform:*\<p\> Uplands

\<@33\>\<i\>*Landform position:*\<p\> Broad ridges; side slopes

\<@33\>\<i\>*Slope:*\<p\> 0 to 5 percent

\<@33\>\<i\>*Taxonomic class:*\<p\> Coarse-loamy, kaolinitic, thermic
Typic Kandiudults

\<@27\>Commonly Associated Soils

\<@30\>Lakeland, Lucy, Orangeburg, Red Bay, and Troup soils are commonly
associated with the Benevolence series.

-   \<@49\>The Lakeland soils are in the higher positions, are
    excessively drained, and are sandy throughout.

-   \<@29\>The Lucy soils are in positions similar to those of the
    Benevolence soils and have sandy surface and subsurface layers with
    a combined thickness of 20 to 40 inches.

-   \<@29\>The Orangeburg soils are in positions similar to those of the
    Benevolence soils and have a fine-loamy control section.

-   \<@29\>The Red Bay soils are in positions similar to those of the
    Benevolence soils or slightly higher, have red hues, and have a
    fine-loamy control section.

-   \<@29\>The Troup soils are in positions similar to those of the
    Benevolence soils or slightly higher, are somewhat excessively
    drained, and have sandy surface and subsurface layers with a
    combined thickness of 40 to 80 inches.

\<@27\>Typical Pedon

\<@30\>Benevolence loamy sand, 0 to 5 percent slopes; in a pine
plantation about 3 miles northeast of Benevolence; Randolph County,
Georgia; USGS Cuthbert topographic quadrangle; lat. 31 degrees 54
minutes 33 seconds N. and long. 84 degrees 41 minutes 47 seconds W.,
NAD27.

\<@23\>Ap---0 to 12 inches; brown (7.5YR 4/4) loamy sand; weak fine
granular structure; very friable; many fine roots; moderately acid;
clear smooth boundary.

\<@33\>Bt1---12 to 37 inches; yellowish red (5YR 5/6) sandy loam; weak
coarse subangular blocky structure; friable; many fine and medium roots;
sand grains coated and bridged with clay; moderately acid; gradual wavy
boundary.

\<@33\>Bt2---37 to 47 inches; red (2.5YR 4/8) sandy loam; weak medium
subangular blocky structure; very friable; common fine and medium roots;
most sand grains coated and bridged with clay; moderately acid; gradual
wavy boundary.

\<@33\>Bt3---47 to 80 inches; red (2.5YR 5/6) sandy clay loam; moderate
medium subangular blocky structure; friable; few fine roots; few faint
discontinuous clay films on faces of peds; strongly acid.

\<@27\>Range in Characteristics

\<@33\>\<i\>*Thickness of the solum:*\<p\> More than 80 inches

\<@33\>\<i\>*Reaction:*\<p\> Very strongly acid to moderately acid
throughout, except where the surface layer has been limed

\<@23\>\<i\>*Ap or A horizon:*\<p\>

\<@31\>Color---hue of 7.5YR or 10YR, value of 3 or 4, and chroma of 3 or
4

\<@31\>Texture---loamy fine sand or loamy sand

\<@23\>\<i\>*E horizon (where present):*\<p\>

\<@31\>Color---hue of 10YR, value of 5 or 6, and chroma of 4

\<@31\>Texture---loamy fine sand or loamy sand

\<@23\>\<i\>*EB horizon (where present):*\<p\>

\<@31\>Color---hue of 7.5YR, value of 5 or 6, and chroma of 5 or 6

\<@31\>Texture---loamy fine sand or loamy sand

\<@23\>\<i\>*BE horizon (where present):*\<p\>

\<@31\>Color---hue of 5YR or 7.5YR, value of 4 to 6, and chroma of 4 to
8

\<@31\>Texture---sandy loam

\<@23\>\<i\>*Bt horizon:*\<p\>

\<@31\>Color---hue of 2.5YR or 5YR, value of 4 or 5, and chroma of 6 to
8

\<@31\>Texture---fine sandy loam or sandy loam in the upper part; sandy
loam or sandy clay loam in the lower part

\<@37\>Bibb Series

\<@33\>\<i\>*Depth class:*\<p\> Very deep

\<@33\>\<i\>*Drainage class:*\<p\> Poorly drained

\<@33\>\<i\>*Permeability:*\<p\> Moderate

\<@33\>\<i\>*Parent material:*\<p\> Stratified loamy and sandy alluvium

\<@33\>\<i\>*Landscape:*\<p\> Coastal Plain

\<@33\>\<i\>*Landform:*\<p\> Flood plains

\<@33\>\<i\>*Landform position:*\<p\> Planer or slightly concave areas

\<@33\>\<i\>*Slope:*\<p\> 0 to 2 percent

\<@33\>\<i\>*Taxonomic class:*\<p\> Coarse-loamy, siliceous, active,
acid, thermic Typic Fluvaquents

\<@27\>Commonly Associated Soils

\<@30\>Cowarts, Kinston, Lakeland, Lucy, Nankin, and Troup soils are
commonly associated with the Bibb series.

-   \<@49\>The Cowarts soils are on side slopes on uplands and are well
    drained.

-   \<@29\>The Kinston soils are in positions similar to those of the
    Bibb soils and have a fine-loamy control section.

-   \<@29\>The Lakeland soils are on uplands, are excessively drained,
    and are sandy throughout.

-   \<@29\>The Lucy soils are on uplands, are well drained, and have a
    sandy epipedon that ranges from 20 to 40 inches in thickness.

-   \<@29\>The Nankin soils are on side slopes on uplands, are well
    drained, and have a fine control section.

-   \<@29\>The Troup soils are on uplands, are somewhat excessively
    drained, and have sandy surface and subsurface layers with a
    combined thickness of 40 to 80 inches.

\<@27\>Typical Pedon

\<@30\>Bibb fine sandy loam in an area of Kinston and Bibb soils, 0 to 1
percent slopes, frequently flooded; about 3,800 feet west of the
Randolph and Terrell County line on County Road 155 and 300 feet north
in the Ichawaynochaway Creek flood plain; Randolph County, Georgia; USGS
Parrot topographic quadrangle; lat. 31 degrees 54 minutes 3 seconds N.
and long. 84 degrees 36 minutes 48 seconds W., NAD27.

\<@23\>A---0 to 5 inches; very dark gray (10YR 3/1) fine sandy loam;
weak fine granular structure; very friable; many fine and medium and
common coarse roots; strongly acid; clear wavy boundary.

\<@33\>Cg1---5 to 8 inches; dark gray (10YR 4/1) loam; massive; very
friable; common fine, medium, and coarse roots; few fine distinct strong
brown (7.5YR 5/6) masses in which iron has accumulated; strongly acid;
clear wavy boundary.

\<@33\>Cg2---8 to 13 inches; dark gray (10YR 4/1) sandy loam; massive;
friable; few fine and medium and common coarse roots; common medium
distinct strong brown (7.5YR 5/6) masses in which iron has accumulated
and which have diffuse boundaries; common medium distinct light brownish
gray (10YR 6/2) areas from which iron has depleted and which have
diffuse boundaries; strongly acid; clear wavy boundary.

\<@33\>Cg3---13 to 21 inches; light brownish gray (10YR 6/2) sandy loam;
massive; friable; few medium and common coarse roots; common medium
distinct pale brown (10YR 6/3), light yellowish brown (10YR 6/4), and
brownish yellow (10YR 6/6) masses in which iron has accumulated and
which have diffuse boundaries; very strongly acid; clear wavy boundary.

\<@33\>Cg4---21 to 27 inches; gray (10YR 5/1) sandy loam; massive;
friable; few coarse roots; common medium distinct light yellowish brown
(10YR 6/4) masses in which iron has accumulated and which have diffuse
boundaries; very strongly acid; clear wavy boundary.

\<@33\>Ab---27 to 45 inches; very dark gray (10YR 3/1) sandy loam;
massive; firm; very strongly acid; clear wavy boundary.

\<@33\>C´g1---45 to 63 inches; very dark gray (10YR 3/1) sandy loam;
massive; friable; common medium distinct pockets and strata of light
brownish gray (10YR 6/2) clean sand grains; strongly acid; clear wavy
boundary.

\<@33\>C´g2---63 to 80 inches; dark gray (10YR 4/1) loamy sand; massive;
very friable; very strongly acid.

\<@27\>Range in Characteristics

\<@33\>\<i\>*Reaction:*\<p\> Very strongly acid or strongly acid
throughout, except where the surface layer has been limed

\<@33\>\<i\>*Other features:*\<p\> The buried surface and substratum
horizons have the same range in colors and textures as the Ag and Cg
horizons.

\<@23\>\<i\>*A or Ap horizon:*\<p\>

\<@31\>Color---hue of 7.5YR or 10YR, value of 2 to 5, and chroma of 1 to
3

\<@31\>Redoximorphic features---no, few, or common iron or clay
depletions in shades of gray and iron accumulations in shades of brown

\<@31\>Texture---loamy sand, loamy fine sand, sandy loam, fine sandy
loam, or silt loam

\<@23\>\<i\>*Ag horizon (where present):*\<p\>

\<@31\>Color---hue of 10YR or 2.5Y, value of 3 to 7, and chroma of 2 or
less; or neutral in hue and value of 3 to 7

\<@31\>Redoximorphic features---no, few, or common iron accumulations in
shades of yellow and brown

\<@31\>Texture---loamy sand, loamy fine sand, sandy loam, fine sandy
loam, or silt loam

\<@23\>\<i\>*Cg horizon:*\<p\>

\<@31\>Color---hue of 10YR to 5BG, value of 3 to 7, and chroma of 2 or
less; or neutral in hue and value of 3 to 7

\<@31\>Redoximorphic features---few to many iron or clay depletions in
shades of gray and iron accumulations in shades of brown, yellow, and
red

\<@31\>Texture---upper part: sandy loam, fine sandy loam, or loam or
stratified in these textures; lower part: sand, loamy sand, loamy fine
sand, sandy loam, fine sandy loam, or loam or stratified in these
textures

\<@37\>Bonneau Series

\<@33\>\<i\>*Depth class:*\<p\> Very deep

\<@33\>\<i\>*Drainage class:*\<p\> Well drained

\<@33\>\<i\>*Permeability:*\<p\> Moderate

\<@33\>\<i\>*Parent material:*\<p\> Loamy marine sediments

\<@33\>\<i\>*Landscape:*\<p\> Coastal Plain

\<@33\>\<i\>*Landform:*\<p\> Uplands

\<@33\>\<i\>*Landform position:*\<p\> Ridges and side slopes

\<@33\>\<i\>*Slope:*\<p\> 0 to 8 percent

\<@33\>\<i\>*Taxonomic class:*\<p\> Loamy, siliceous, subactive, thermic
Arenic Paleudults

\<@27\>Commonly Associated Soils

\<@30\>Norfolk, Orangeburg, and Troup soils are commonly associated with
the Bonneau series.

-   \<@49\>The Norfolk and Orangeburg soils are in positions similar to
    those of the Bonneau soils and do not have thick, sandy surface and
    subsurface horizons.

-   \<@29\>The Troup soils are in the slightly higher positions, are
    somewhat excessively drained, and have sandy surface and subsurface
    horizons with a combined thickness of 40 to 80 inches.

\<@27\>Typical Pedon

\<@30\>Bonneau loamy sand, 0 to 5 percent slopes; about 0.6 mile
northwest of Springvale on County Road 31 and 40 feet west of the road;
Randolph County, Georgia; USGS Morris topographic quadrangle; lat. 31
degrees 50 minutes 8 seconds N. and long. 84 degrees 53 minutes 43
seconds W., NAD27.

\<@23\>Ap---0 to 6 inches; dark grayish brown (10YR 4/2) loamy sand;
weak fine granular structure; very friable; many fine and medium and few
coarse roots; slightly acid; abrupt wavy boundary.

\<@33\>E1---6 to 12 inches; light yellowish brown (10YR 6/4) loamy sand;
weak fine granular structure; very friable; many fine and medium roots;
slightly acid; gradual wavy boundary.

\<@33\>E2---12 to 22 inches; yellowish brown (10YR 5/4) loamy sand; weak
fine granular structure; very friable; many fine and medium roots;
moderately acid; gradual wavy boundary.

\<@33\>E3---22 to 33 inches; yellowish brown (10YR 5/6) loamy sand; weak
fine granular structure; very friable; many fine and medium roots;
moderately acid; gradual wavy boundary.

\<@33\>Bt1---33 to 52 inches; yellowish brown (10YR 5/6) sandy loam;
weak medium subangular blocky structure; friable; common fine and medium
roots; about 3 percent, by volume, ironstone nodules; moderately acid;
gradual wavy boundary.

\<@33\>Bt2---52 to 65 inches; light yellowish brown (10YR 6/4) sandy
loam; moderate medium subangular blocky structure; friable; few fine and
medium roots; about 3 percent, by volume, ironstone nodules; common
medium distinct yellowish brown (10YR 5/6) masses in which iron has
accumulated; common medium distinct very pale brown (10YR 7/3) areas
from which iron has depleted; moderately acid; gradual wavy boundary.

\<@33\>BC---65 to 72 inches; multicolored, about 35 percent brownish
yellow (10YR 6/6), 35 percent light yellowish brown (10YR 6/4), and 30
percent light gray (5Y 7/2) sandy clay; weak medium subangular blocky
structure; friable; the areas of brownish yellow and light yellowish
brown are areas in which iron has accumulated; the areas of light gray
are areas from which iron has depleted; moderately acid.

\<@27\>Range in Characteristics

\<@33\>\<i\>*Thickness of the solum:*\<p\> 60 to more than 80 inches

\<@33\>\<i\>*Thickness of the sandy epipedon:*\<p\> 20 to 40 inches

\<@33\>\<i\>*Reaction:*\<p\> Very strongly acid to moderately acid
throughout, except where the surface layer has been limed

\<@23\>\<i\>*A or Ap horizon:*\<p\>

\<@31\>Color---hue of 10YR, value of 3 to 5, and chroma of 2 to 4

\<@31\>Texture---loamy sand

\<@23\>\<i\>*E horizon:*\<p\>

\<@31\>Color---hue of 10YR, value of 4 to 6, and chroma of 4 to 6

\<@31\>Texture---loamy sand

\<@23\>\<i\>*Bt horizon, upper part:*\<p\>

\<@31\>Color---hue of 7.5YR or 10YR, value of 5 to 7, and chroma of 6 to
8

\<@31\>Texture---sandy loam or sandy clay loam

\<@23\>\<i\>*Bt horizon, lower part:*\<p\>

\<@31\>Color---hue of 7.5YR or 10YR, value of 5 or 6, and chroma of 3 to
8; or multicolored in shades of red, brown, yellow, or gray

\<@31\>Redoximorphic features---no, few, or common iron accumulations in
shades of brown, red, and yellow; depletions with chroma of 2 or less
within a depth of 60 inches

\<@31\>Texture---sandy loam, sandy clay loam, or sandy clay

\<@23\>\<i\>*BC horizon (where present):*\<p\>

\<@31\>Color---hue of 7.5YR to 2.5Y, value of 5 to 7, and chroma of 3 to
8; or multicolored in shades of red, brown, yellow, or gray

\<@31\>Redoximorphic features---few to many iron or clay depletions in
shades of gray and few to many iron accumulations in shades of red and
brown

\<@31\>Texture---sandy loam, sandy clay loam, or sandy clay

\<@37\>Carnegie Series

\<@33\>\<i\>*Depth class:*\<p\> Very deep

\<@33\>\<i\>*Drainage class:*\<p\> Well drained

\<@33\>\<i\>*Permeability:*\<p\> Moderately slow

\<@33\>\<i\>*Parent material:*\<p\> Clayey marine sediments

\<@33\>\<i\>*Landscape:*\<p\> Coastal Plain

\<@33\>\<i\>*Landform:*\<p\> Uplands

\<@33\>\<i\>*Landform position:*\<p\> Side slopes and knolls

\<@33\>\<i\>*Slope:*\<p\> 2 to 12 percent

\<@33\>\<i\>*Taxonomic class:*\<p\> Fine, kaolinitic, thermic Plinthic
Kandiudults

\<@27\>Commonly Associated Soils

\<@30\>Cowarts, Faceville, Henderson, Nankin, and Norfolk soils are
commonly associated with the Carnegie series.

-   \<@49\>The Cowarts soils are in positions similar to those of the
    Carnegie soils or lower, have less than 5 percent plinthite, and
    have a fine-loamy control section.

-   \<@29\>The Faceville soils are in positions similar to those of the
    Carnegie soils or slightly higher and have less than 5 percent
    plinthite.

-   \<@29\>The Henderson soils are in positions similar to those of the
    Carnegie soils or slightly lower, have less than 5 percent
    plinthite, and have chert fragments throughout.

-   \<@29\>The Nankin soils are in positions similar to those of the
    Carnegie soils or slightly lower, have less than 5 percent
    plinthite, and have a solum that is less than 60 inches thick.

-   \<@29\>The Norfolk soils are in positions similar to those of the
    Carnegie soils or slightly lower, have less than 5 percent
    plinthite, and have a fine-loamy control section.

\<@27\>Typical Pedon

\<@30\>Carnegie sandy loam, 2 to 5 percent slopes, eroded; about 2.2
miles south of Shellman on County Road 44, about 400 feet west of the
roadway; Randolph County, Georgia; USGS Martins Crossroads topographic
quadrangle; lat. 31 degrees 42 minutes 51 seconds N. and long. 84
degrees 37 minutes 58 seconds W., NAD27.

\<@23\>Ap---0 to 5 inches; brown (7.5YR 4/3) sandy loam; weak fine
granular structure; very friable; many very fine and fine roots; about
10 percent, by volume, ironstone nodules; strongly acid; abrupt wavy
boundary.

\<@33\>Bt1---5 to 12 inches; yellowish red (5YR 4/6) sandy clay loam;
moderate medium subangular blocky structure; friable; many very fine and
fine roots; common distinct clay films on faces of peds; about 5
percent, by volume, ironstone nodules; strongly acid; gradual wavy
boundary.

\<@33\>Bt2---12 to 17 inches; yellowish red (5YR 4/6) clay; moderate
medium subangular blocky structure; firm; few fine roots; many distinct
clay films on faces of peds; about 4 percent, by volume, plinthite;
about 5 percent, by volume, ironstone nodules; strongly acid; gradual
wavy boundary.

\<@33\>Btv1---17 to 22 inches; yellowish red (5YR 4/6) clay; moderate
medium subangular blocky structure; firm; many distinct clay films on
faces of peds; about 10 percent, by volume, plinthite; very strongly
acid; gradual wavy boundary.

\<@33\>Btv2---22 to 38 inches; multicolored, about 40 percent red (2.5YR
4/6), 40 percent light reddish brown (2.5YR 6/4), and 20 percent pale
red (2.5YR 7/3) clay; moderate medium subangular blocky structure; firm;
common distinct clay films on faces of peds; about 10 percent, by
volume, plinthite; red and light reddish brown areas are relic iron
accumulations; pale red areas are relic iron depletions; very strongly
acid; gradual wavy boundary.

\<@33\>Btv3---38 to 72 inches; multicolored, about 25 percent red (2.5YR
4/6), 25 percent light reddish brown (2.5YR 6/4), 25 percent pale red
(2.5YR 7/3), and 25 percent light gray (5Y 7/1) clay in a variegated
pattern; weak medium subangular blocky structure; friable; about 6
percent, by volume, plinthite; red and light reddish brown areas are
relic iron accumulations; pale red and light gray areas are relic iron
depletions; very strongly acid.

\<@27\>Range in Characteristics

\<@33\>\<i\>*Thickness of the solum:*\<p\> More than 60 inches

\<@33\>\<i\>*Content of gravel:*\<p\> 5 to 25 percent, by volume,
ironstone nodules in the A or Ap horizon and 0 to 10 percent, by volume,
in the Bt horizons

\<@33\>\<i\>*Content of plinthite:*\<p\> More than 5 percent between
depths of about 20 and 50 inches

\<@33\>\<i\>*Reaction:*\<p\> Very strongly acid or strongly acid
throughout, except where the surface layer has been limed

\<@23\>\<i\>*A, Ap, or Apc horizon:*\<p\>

\<@31\>Color---hue of 7.5YR or 10YR, value of 3 to 5, and chroma of 2 to
6

\<@31\>Texture---sandy loam or gravelly sandy loam

\<@23\>\<i\>*Upper part of the Bt or Btc horizon:*\<p\>

\<@31\>Color---hue of 5YR to 10YR, value of 4 or 5, and chroma of 6 to 8

\<@31\>Relic redoximorphic features---no or few in shades of red or
yellow

\<@31\>Texture---sandy clay loam or sandy clay

\<@23\>\<i\>*Lower part of the Bt or B´t horizon (where present):*\<p\>

\<@31\>Color---multicolored in shades of red, brown, yellow, or gray

\<@31\>Relic redoximorphic features---few or common relict accumulations
in shades of red, brown, or yellow and relic depletions in shades of
gray

\<@31\>Texture---sandy clay or clay

\<@23\>\<i\>*Btv horizon:*\<p\>

\<@31\>Color---hue of 2.5YR to 10YR, value of 4 or 5, and chroma of 6 to
8; or multicolored in shades of red, brown, yellow, or gray

\<@31\>Relic redoximorphic features---few to many relict accumulations
in shades of red, brown, or yellow and depletions in shades of gray

\<@31\>Texture---sandy clay or clay

\<@23\>\<i\>*C horizon (where present):*\<p\>

\<@31\>Color---multicolored in shades similar to those in the lower part
of the Bt horizon

\<@31\>Texture---sandy clay or sandy clay loam

\<@37\>Clarendon Series

\<@33\>\<i\>*Depth class:*\<p\> Very deep

\<@33\>\<i\>*Drainage class:*\<p\> Moderately well drained

\<@33\>\<i\>*Permeability:*\<p\> Moderately slow

\<@33\>\<i\>*Parent material:*\<p\> Loamy marine sediments

\<@33\>\<i\>*Landscape:*\<p\> Coastal Plain

\<@33\>\<i\>*Landform:*\<p\> Uplands

\<@33\>\<i\>*Landform position:*\<p\> Concavities

\<@33\>\<i\>*Slope:*\<p\> 0 to 5 percent

\<@33\>\<i\>*Taxonomic class:*\<p\> Fine-loamy, siliceous, semiactive,
thermic Plinthaquic Paleudults

\<@27\>Commonly Associated Soils

\<@30\>Goldsboro, Grady, Marlboro, Norfolk, and Rains soils are commonly
associated with the Clarendon series.

-   \<@49\>The Goldsboro soils are in positions similar to those of the
    Clarendon soils or slightly higher and have less than 5 percent
    plinthite.

-   \<@29\>The Grady soils are in the lower positions, are poorly
    drained, and have a fine control section.

-   \<@29\>The Marlboro soils are in the higher positions, are well
    drained, and have a fine control section.

-   \<@29\>The Norfolk soils are in the higher positions and are well
    drained.

-   \<@29\>The Rains soils are in the lower positions and are poorly
    drained.

\<@27\>Typical Pedon

\<@30\>Clarendon sandy loam, 0 to 2 percent slopes; about 500 feet south
of the Shellman city limit on Georgia Highway 41, about 160 feet west of
the highway; Randolph County, Georgia; USGS Doverel topographic
quadrangle; lat. 31 degrees 44 minutes 27.2 seconds N. and long. 84
degrees 36 minutes 52.9 seconds W., NAD27.

\<@23\>Ap---0 to 8 inches; very dark grayish brown (10YR 3/2) sandy
loam; weak medium granular structure; very friable; common fine and
medium roots; about 8 percent, by volume, iron-manganese concretions;
moderately acid; abrupt smooth boundary.

\<@33\>Bt1---8 to 20 inches; yellowish brown (10YR 5/8) sandy clay loam;
weak fine subangular blocky structure; friable; common fine and medium
roots; few faint clay films on faces of peds; about 5 percent, by
volume, iron-manganese concretions; strongly acid; clear smooth
boundary.

\<@33\>Bt2---20 to 29 inches; yellowish brown (10YR 5/6) sandy clay
loam; weak medium subangular blocky structure; friable; common fine and
medium roots; few faint clay films on faces of peds; about 5 percent, by
volume, iron-manganese concretions; common fine distinct strong brown
(7.5YR 4/6) and common fine prominent red (2.5YR 4/8) masses in which
iron has accumulated; the masses have sharp boundaries and are within
the matrix; strongly acid; clear wavy boundary.

\<@33\>Bt3---29 to 34 inches; yellowish brown (10YR 5/6) sandy clay
loam; moderate medium subangular blocky structure; friable; few fine
roots; common faint clay films on faces of peds; about 3 percent, by
volume, plinthite; about 4 percent, by volume, iron-manganese
concretions; common medium distinct strong brown (7.5YR 4/6) and common
medium prominent red (2.5YR 4/8) masses in which iron has accumulated;
common medium distinct light brownish gray (10YR 6/2) areas from which
iron has depleted; strongly acid; clear wavy boundary.

\<@33\>Btv1---34 to 42 inches; yellowish brown (10YR 5/6) sandy clay
loam; moderate medium subangular blocky structure; friable; few fine
roots; common distinct clay films on faces of peds; about 10 percent, by
volume, plinthite; 2 percent, by volume, iron-manganese concretions;
common medium distinct light brownish gray (10YR 6/2) areas from which
iron has depleted; strongly acid; gradual wavy boundary.

\<@33\>Btv2---42 to 50 inches; pale brown (10YR 6/3) sandy clay loam;
moderate medium subangular blocky structure; friable; few fine roots;
common distinct clay films on faces of peds; about 5 percent, by volume,
plinthite; about 2 percent, by volume, iron-manganese concretions;
common medium distinct strong brown (7.5YR 5/6) and common medium
prominent red (2.5YR 4/8) masses in which iron has accumulated; strongly
acid; gradual wavy boundary.

\<@33\>Btv3---50 to 72 inches; pale brown (10YR 6/3) sandy clay loam;
moderate medium subangular blocky structure; friable; common distinct
continuous clay films on faces of peds; about 5 percent, by volume,
plinthite; about 2 percent, by volume, iron-manganese concretions; many
medium distinct strong brown (7.5YR 5/6) and many medium prominent red
(2.5YR 4/8) masses in which iron has accumulated and which have sharp
boundaries; strongly acid.

\<@33\>\<@27\>Range in Characteristics

\<@33\>\<i\>*Thickness of the solum:*\<p\> More than 60 inches

\<@33\>\<i\>*Content of gravel:*\<p\> 0 to 10 percent, by volume, in the
A and E horizons and the upper part of the Bt horizon; 0 to 2 percent in
the lower part of the Bt horizon

\<@33\>\<i\>*Content of plinthite:*\<p\> 5 percent or more beginning at
a depth of 20 to 58 inches

\<@33\>\<i\>*Reaction:*\<p\> Very strongly acid to moderately acid in
the upper part of the solum and very strongly acid to strongly acid in
the lower part, except where the surface layer has been limed

\<@23\>\<i\>*A or Ap horizon:*\<p\>

\<@31\>Color---hue of 10YR, value of 3 to 6, and chroma of 1 or 2

\<@31\>Texture---loamy sand or sandy loam

\<@23\>\<i\>*Bt horizon:*\<p\>

\<@31\>Color---hue of 10YR or 2.5Y, value of 5 or 6, and chroma of 4 to
8

\<@31\>Redoximorphic features---few or common in shades of gray, red,
and brown

\<@31\>Texture---sandy clay loam

\<@23\>\<i\>*Btv horizon:*\<p\>

\<@31\>Color---hue of 10YR or 2.5Y, value of 5 to 7, and chroma of 3 to
6

\<@31\>Redoximorphic features---few to many in shades of gray, red, and
brown

\<@31\>Texture---sandy clay loam

\<@37\>Cowarts Series

\<@33\>\<i\>*Depth class:*\<p\> Very deep

\<@33\>\<i\>*Drainage class:*\<p\> Well drained and moderately well
drained

\<@33\>\<i\>*Permeability:*\<p\> Moderately slow or slow

\<@33\>\<i\>*Parent material:*\<p\> Loamy marine sediments

\<@33\>\<i\>*Landscape:*\<p\> Coastal Plain

\<@33\>\<i\>*Landform:*\<p\> Uplands

\<@33\>\<i\>*Landform position:*\<p\> Narrow ridges; side slopes

\<@33\>\<i\>*Slope:*\<p\> 2 to 25 percent

\<@33\>\<i\>*Taxonomic class:*\<p\> Fine-loamy, kaolinitic, thermic
Typic Kanhapludults

\<@27\>Commonly Associated Soils

\<@30\>Ailey, Bibb, Carnegie, Kinston, Lakeland, Lucy, Maubila, Nankin,
Ocilla, and Troup soils are commonly associated with the Cowarts series.

-   \<@49\>The Ailey soils are in positions similar to those of the
    Cowarts soils and have sandy surface and subsurface layers with a
    combined thickness of 20 to 40 inches over dense, brittle layers.

-   \<@29\>The Bibb soils are on flood plains, have a coarse-loamy
    control section, and are poorly drained.

-   \<@29\>The Carnegie soils are in positions similar to those of the
    Cowarts soils or slightly higher, have a fine control section, and
    have more than 5 percent plinthite, by volume.

-   \<@29\>The Kinston soils are on flood plains and are poorly drained.

-   \<@29\>The Lakeland soils are in the higher positions, are
    excessively drained, and are sandy throughout.

-   \<@29\>The Lucy soils are in positions similar to those of the
    Cowarts soils or slightly higher and have sandy surface and
    subsurface layers with a combined thickness of 20 to 40 inches.

-   \<@29\>The Maubila soils are in positions similar to those of the
    Cowarts soils or higher, are moderately well drained, and have a
    fine control section.

-   \<@29\>The Nankin soils are in positions similar to those of the
    Cowarts soils, have a solum that is less than 60 inches thick, and
    have a fine control section.

-   \<@29\>The Ocilla soils are adjacent to the Cowarts soils in lower
    positions, have sandy surface and subsurface layers with a combined
    thickness of 20 to 40 inches, and are somewhat poorly drained.

-   \<@29\>The Troup soils are in the higher positions, are somewhat
    excessively drained, and have surface and subsurface layers with a
    combined thickness of 40 to 80 inches.

\<@27\>Typical Pedon

\<@30\>Cowarts loamy sand in an area of Nankin-Cowarts complex, 15 to 35
percent slopes; about 0.6 mile north of Sharon Church, 2,960 feet south
of the Stewart County line, and 3,200 feet west of County Road 28;
Randolph County, Georgia; USGS Sanford topographic quadrangle; lat. 31
degrees 54 minutes 58 seconds N. and long. 84 degrees 53 minutes 30
seconds W., NAD27.

\<@23\>Ap1---0 to 3 inches; dark grayish brown (10YR 4/2) loamy sand;
weak fine granular structure; very friable; many fine and medium roots;
strongly acid; clear smooth boundary.

\<@33\>Ap2---3 to 7 inches; brown (10YR 4/3) loamy sand; weak fine
granular structure; very friable; many fine and medium roots; strongly
acid; clear wavy boundary.

\<@33\>Bt1---7 to 15 inches; yellowish brown (10YR 5/6) sandy loam; weak
coarse subangular blocky structure; very friable; many fine and medium
roots; sand grains coated and bridged with clay; strongly acid; gradual
wavy boundary.

\<@33\>Bt2---15 to 22 inches; brownish yellow (10YR 6/8) sandy clay
loam; weak medium subangular blocky structure; friable; common fine and
medium roots; few distinct clay films on faces of peds; strongly acid;
gradual wavy boundary.

\<@33\>Bt3---22 to 31 inches; brownish yellow (10YR 6/8) sandy clay
loam; moderate medium subangular blocky structure; firm; common medium
roots and few fine roots; few distinct clay films on faces of peds;
common medium distinct yellowish red (5YR 5/8) masses in which iron has
accumulated; the masses have sharp boundaries and are within the matrix;
strongly acid; gradual wavy boundary.

\<@33\>BC---31 to 40 inches; brownish yellow (10YR 6/8) sandy clay loam;
weak medium subangular blocky structure; friable; few medium roots; few
distinct clay films on faces of peds; common medium distinct yellowish
red (5YR 5/6) and strong brown (7.5YR 5/6) masses in which iron has
accumulated; the masses have sharp boundaries and are within the matrix;
strongly acid; gradual wavy boundary.

\<@33\>C1---40 to 48 inches; brownish yellow (10YR 6/8) sandy loam; weak
coarse subangular blocky structure parting to weak fine granular;
friable; few fine distinct yellowish red (5YR 5/6) and reddish yellow
(5YR 6/6) masses in which iron has accumulated; very strongly acid;
gradual wavy boundary.

\<@33\>C2---48 to 59 inches; brownish yellow (10YR 6/6) sandy loam;
massive parting to weak thin platy structure; firm, brittle; common thin
strata of yellowish red (5YR 5/6) sandy clay loam; few fine distinct
pale brown (10YR 6/3) areas from which iron has depleted; very strongly
acid; gradual wavy boundary.

\<@33\>C3---59 to 80 inches; multicolored, about 50 percent brownish
yellow (10YR 6/6), 30 percent light yellowish brown (10YR 6/4), and 20
percent yellowish red (5YR 5/6) stratified loamy sand; massive structure
parting to loose single grained; firm in place, very friable if
disturbed; the areas of brownish yellow and yellowish red are areas in
which iron has accumulated; the areas of light yellowish brown are areas
from which iron has depleted; very strongly acid.

\<@27\>Range in Characteristics

\<@33\>\<i\>*Thickness of the solum:*\<p\> 20 to 40 inches

\<@33\>\<i\>*Reaction:*\<p\> Very strongly acid or strongly acid
throughout, except where the surface layer has been limed

\<@23\>\<i\>*A or Ap horizon:*\<p\>

\<@31\>Color---hue of 10YR, value of 4 or 5, and chroma of 2 to 4

\<@31\>Texture---loamy sand or sandy loam

\<@23\>\<i\>*E horizon (where present):*\<p\>

\<@31\>Color---hue of 10YR, value of 5 or 6, and chroma of 4 to 6

\<@31\>Texture---loamy sand or sandy loam

\<@23\>\<i\>*BE horizon (where present):*\<p\>

\<@31\>Color---hue of 10YR, value of 5 or 6, and chroma of 4 to 8

\<@31\>Texture---sandy loam

\<@23\>\<i\>*Bt horizon:*\<p\>

\<@31\>Color---hue of 5YR to 10YR, value of 5 or 6, and chroma of 4 to 8

\<@31\>Redoximorphic features---no, few, or common iron accumulations in
shades of red, yellow, and brown

\<@31\>Texture---sandy loam or sandy clay loam

\<@23\>\<i\>*BC horizon (where present):*\<p\>

\<@31\>Color---hue of 2.5YR to 10YR, value of 4 to 6, and chroma of 4 to
8; or multicolored in shades of red, yellow, brown, and gray

\<@31\>Redoximorphic features---few to many iron or clay depletions in
shades of gray and iron accumulations in shades of red, brown, and
yellow

\<@31\>Texture---sandy loam or sandy clay loam

\<@23\>\<i\>*C horizon:*\<p\>

\<@31\>Color---hue of 2.5YR to 10YR, value of 4 to 6, and chroma of 4 to
8; or multicolored in shades of red, yellow, brown, and gray

\<@31\>Redoximorphic features---few to many iron or clay depletions in
shades of gray and few to many iron accumulations in shades of red,
brown, and yellow

\<@31\>Texture---loamy sand, sandy loam, or sandy clay loam or
stratified in these textures

\<@37\>Faceville Series

\<@33\>\<i\>*Depth class:*\<p\> Very deep

\<@33\>\<i\>*Drainage class:*\<p\> Well drained

\<@33\>\<i\>*Permeability:*\<p\> Moderate

\<@33\>\<i\>*Parent material:*\<p\> Clayey marine sediments

\<@33\>\<i\>*Landscape:*\<p\> Coastal Plain

\<@33\>\<i\>*Landform:*\<p\> Uplands

\<@33\>\<i\>*Landform position:*\<p\> Broad ridges; side slopes

\<@33\>\<i\>*Slope:*\<p\> 0 to 10 percent

\<@33\>\<i\>*Taxonomic class:*\<p\> Fine, kaolinitic, thermic Typic
Kandiudults

\<@27\>Commonly Associated Soils

\<@30\>Carnegie, Greenville, Marlboro, Norfolk, Orangeburg, Rains, and
Red Bay soils are commonly associated with the Faceville series.

-   \<@49\>The Carnegie soils are in positions similar to those of the
    Faceville soils or slightly lower and have more than 5 percent
    plinthite, by volume.

-   \<@29\>The Greenville soils are in positions similar to those of the
    Faceville soils and have redder hues.

-   \<@29\>The Marlboro soils are in positions similar to those of the
    Faceville soils or slightly lower and have hues that are more
    yellow.

-   \<@29\>The Norfolk soils are in positions similar to those of the
    Faceville soils or slightly lower, have hues that are more yellow,
    and have a fine-loamy control section.

-   \<@29\>The Orangeburg soils are in positions similar to those of the
    Faceville soils or slightly lower and have a fine-loamy control
    section.

-   \<@29\>The Rains soils are in the lower positions, are poorly
    drained, and have a fine-loamy control section.

-   \<@29\>The Red Bay soils are in positions similar to those of the
    Faceville soils, have redder hues, and have a fine-loamy control
    section.

\<@27\>Typical Pedon

\<@30\>Faceville sandy loam, 0 to 2 percent slopes; about 1.8 miles
north of the Quitman and Clay County line on Georgia Highway 39 and 700
feet west of the highway; Quitman County, Georgia; USGS Hatcher
topographic quadrangle; lat. 31 degrees 48 minutes 19 seconds N. and
long. 85 degrees 5 minutes 42 seconds W., NAD27.

\<@23\>Ap---0 to 10 inches; reddish brown (5YR 4/4) sandy loam; weak
fine granular structure; very friable; many fine roots; moderately acid;
abrupt smooth boundary.

\<@33\>Bt1---10 to 30 inches; red (2.5YR 4/6) sandy clay; moderate
medium subangular blocky structure; firm; few fine roots; few fine
pores; common distinct clay films on faces of peds; strongly acid;
gradual wavy boundary.

\<@33\>Bt2---30 to 72 inches; red (2.5YR 4/6) sandy clay; moderate fine
subangular blocky structure; firm; common fine pores; common distinct
clay films on faces of peds; strongly acid; gradual wavy boundary.

\<@33\>Bt3---72 to 80 inches; red (2.5YR 5/6) sandy clay; moderate fine
subangular blocky structure; firm; common fine pores; common distinct
clay films on faces of peds; few fine prominent strong brown (7.5YR 5/6)
masses in which iron has accumulated; strongly acid.

\<@27\>Range in Characteristics

\<@33\>\<i\>*Thickness of the solum:*\<p\> More than 65 inches

\<@33\>\<i\>*Reaction:*\<p\> Very strongly acid or strongly acid
throughout, except where the surface layer has been limed

\<@23\>\<i\>*A or Ap horizon:*\<p\>

\<@31\>Color---hue of 5YR to 10YR, value of 4 or 5, and chroma of 2 to 6

\<@31\>Texture---sandy loam

\<@23\>\<i\>*Bt horizon:*\<p\>

\<@31\>Color---hue of 2.5YR or 5YR, value of 4 or 5, and chroma of 4 to
8

\<@31\>Texture---clay loam, sandy clay, or clay

\<@23\>\<i\>*BC horizon (where present):*\<p\>

\<@31\>Color---hue of 2.5YR or 5YR, value of 4 or 5, and chroma of 4 to
8; or multicolored in shades of red, brown, and yellow

\<@31\>Redoximorphic features---no, few, or common iron accumulations in
shades of red, brown, and yellow

\<@31\>Texture---sandy clay loam or sandy clay

\<@37\>Goldsboro Series

\<@33\>\<i\>*Depth class:*\<p\> Very deep

\<@33\>\<i\>*Drainage class:*\<p\> Moderately well drained

\<@33\>\<i\>*Permeability:*\<p\> Moderate

\<@33\>\<i\>*Parent material:*\<p\> Loamy marine sediments

\<@33\>\<i\>*Landscape:*\<p\> Coastal Plain

\<@33\>\<i\>*Landform:*\<p\> Uplands

\<@33\>\<i\>*Landform position:*\<p\> Interstream divides

\<@33\>\<i\>*Slope:*\<p\> 0 to 5 percent

\<@33\>\<i\>*Taxonomic class:*\<p\> Fine-loamy, siliceous, subactive,
thermic Aquic Paleudults

\<@27\>Commonly Associated Soils

\<@30\>Clarendon and Norfolk soils are commonly associated with the
Goldsboro series.

-   \<@49\>The Clarendon soils are in positions similar to those of the
    Goldsboro soils or slightly lower and have more than 5 percent
    plinthite, by volume.

-   \<@29\>The Norfolk soils are in the higher positions and are well
    drained.

\<@27\>Typical Pedon

\<@30\>Goldsboro loamy sand, 0 to 2 percent slopes; about 1.8 miles
south of the Quitman and Clay County line on Georgia Highway 39 and 200
feet south of the highway; Clay County, Georgia; USGS Hatcher
topographic quadrangle; lat. 31 degrees 45 minutes 30 seconds N. and
long. 85 degrees 4 minutes 6 seconds W., NAD27.

\<@23\>Ap---0 to 10 inches; brown (10YR 5/3) loamy sand; weak fine
granular structure; very friable; moderately acid; clear smooth
boundary.

\<@33\>Bt1---10 to 18 inches; light yellowish brown (10YR 6/4) sandy
loam; weak fine subangular blocky structure; friable; sand grains coated
and bridged with clay; few faint discontinuous clay films on faces of
peds; moderately acid; clear smooth boundary.

\<@33\>Bt2---18 to 33 inches; light yellowish brown (10YR 6/4) sandy
clay loam; moderate medium subangular blocky structure; friable; sand
grains coated and bridged with clay; few faint clay films on faces of
peds; many medium distinct yellowish brown (10YR 5/8) masses in which
iron has accumulated; common medium distinct light gray (10YR 7/2) areas
from which iron or clay has depleted; strongly acid; clear smooth
boundary.

\<@33\>Btg1---33 to 60 inches; light gray (10YR 7/2) sandy clay loam;
moderate medium subangular blocky structure; friable; sand grains coated
and bridged with clay; few faint clay films on faces of peds; few
5-millimeter pockets of clean sand grains in the lower part; common
medium prominent red (2.5YR 4/8) and yellowish brown (10YR 5/8) masses
in which iron has accumulated; common medium faint light gray (10YR 7/1)
areas from which iron or clay has depleted; strongly acid; clear smooth
boundary.

\<@33\>Btg2---60 to 80 inches; light gray (10YR 7/1) sandy clay loam;
moderate medium subangular blocky structure; friable; sand grains coated
and bridged with clay; few faint clay films on faces of peds; few
5-millimeter pockets of clean sand grains; common medium prominent red
(2.5YR 4/8) and yellowish brown (10YR 5/8) masses in which iron has
accumulated; common medium faint light gray (10YR 7/2) areas from which
iron or clay has depleted; strongly acid.

\<@27\>Range in Characteristics

\<@33\>\<i\>*Thickness of the solum:*\<p\> More than 60 inches

\<@33\>\<i\>*Reaction:*\<p\> Very strongly acid or strongly acid
throughout, except where the surface layer has been limed

\<@23\>\<i\>*A or Ap horizon:*\<p\>

\<@31\>Color---hue of 10YR or 2.5Y, value of 4 or 5, and chroma of 1 to
4

\<@31\>Texture---loamy sand or sandy loam

\<@23\>\<i\>*E horizon (where present):*\<p\>

\<@31\>Color---hue of 10YR or 2.5YR, value of 5 to 7, and chroma of 2 to
6

\<@31\>Texture---loamy sand or sandy loam

\<@23\>\<i\>*Bt horizon, upper part:*\<p\>

\<@31\>Color---hue of 10YR, value of 5 to 7, and chroma of 4 to 6

\<@31\>Texture---sandy loam or sandy clay loam

\<@23\>\<i\>*Bt horizon, lower part:*\<p\>

\<@31\>Color---hue of 10YR or 2.5Y, value of 5 to 7, and chroma of 3 to
6

\<@31\>Redoximorphic features---few or common iron or clay depletions
and accumulations in shades of gray, red, yellow, and brown

\<@31\>Texture---sandy loam or sandy clay loam

\<@23\>\<i\>*Btg horizon (where present):*\<p\>

\<@31\>Color---hue of 10YR or 2.5Y, value of 5 to 7, and chroma of 1 or
2

\<@31\>Redoximorphic features---common or many iron or clay
accumulations in shades of red, yellow, and brown and depletions in
shades of gray

\<@31\>Texture---sandy loam or sandy clay loam

\<@37\>Grady Series

\<@33\>\<i\>*Depth class:*\<p\> Very deep

\<@33\>\<i\>*Drainage class:*\<p\> Poorly drained

\<@33\>\<i\>*Permeability:*\<p\> Slow

\<@33\>\<i\>*Parent material:*\<p\> Clayey marine sediments

\<@33\>\<i\>*Landscape:*\<p\> Coastal Plain

\<@33\>\<i\>*Landform:*\<p\> Depressions

\<@33\>\<i\>*Landform position:*\<p\> Concavities

\<@33\>\<i\>*Slope:*\<p\> 0 to 2 percent

\<@33\>\<i\>*Taxonomic class:*\<p\> Fine, kaolinitic, thermic Typic
Paleaquults

\<@27\>Commonly Associated Soils

\<@30\>Clarendon, Marlboro, and Rains soils are commonly associated with
the Grady series.

-   \<@49\>The Clarendon soils are in the higher positions, are
    moderately well drained, and have a fine-loamy control section.

-   \<@29\>The Marlboro soils are in the higher positions and are well
    drained.

-   \<@29\>The Rains soils are in positions similar to those of the
    Grady soils and have a fine-loamy control section.

\<@27\>Typical Pedon

\<@30\>Grady clay loam, ponded; about 0.4 mile south of Five Points and
250 feet west of County Road 154; Randolph County, Georgia; USGS Doverel
topographic quadrangle; lat. 31 degrees 41 minutes 42 seconds N. and
long. 84 degrees 33 minutes 35 seconds W., NAD27.

\<@23\>Ap---0 to 5 inches; very dark grayish brown (10YR 3/2) clay loam;
moderate medium granular structure; friable; many fine roots; very
strongly acid; clear smooth boundary.

\<@33\>Btg1---5 to 10 inches; gray (10YR 5/1) clay; moderate medium
subangular blocky structure; very firm; common fine roots; common
distinct clay films on faces of peds; very strongly acid; gradual smooth
boundary.

\<@33\>Btg2---10 to 30 inches; light brownish gray (10YR 6/2) clay;
moderate medium subangular blocky structure; very firm; few fine roots;
common distinct clay films on faces of peds; very strongly acid; gradual
smooth boundary.

\<@33\>Btg3---30 to 65 inches; light brownish gray (10YR 6/2) clay;
moderate medium subangular blocky structure; very firm; common distinct
clay films on faces of peds; common medium distinct yellowish brown
(10YR 5/8) and common medium prominent yellowish red (5YR 4/6) masses in
which iron has accumulated; very strongly acid.

\<@27\>Range in Characteristics

\<@33\>\<i\>*Thickness of the solum:*\<p\> More than 60 inches

\<@33\>\<i\>*Reaction:*\<p\> Extremely acid to strongly acid throughout,
except where the surface layer has been limed

\<@23\>\<i\>*A or Ap horizon:*\<p\>

\<@31\>Color---hue of 10YR, value of 2 or 3, and chroma of 1 or 2

\<@31\>Texture---loam or clay loam

\<@23\>\<i\>*Btg horizon:*\<p\>

\<@31\>Color---hue of 10YR to 5Y, value of 5 or 6, and chroma of 1 or 2

\<@31\>Redoximorphic features---no, few, or common iron or clay
depletions in shades of gray and iron accumulations in shades of yellow,
brown, and red

\<@31\>Texture---sandy clay or clay in the upper part and clay in the
lower part

\<@37\>Greenville Series

\<@33\>\<i\>*Depth class:*\<p\> Very deep

\<@33\>\<i\>*Drainage class:*\<p\> Well drained

\<@33\>\<i\>*Permeability:*\<p\> Moderate

\<@33\>\<i\>*Parent material:*\<p\> Clayey marine sediments

\<@33\>\<i\>*Landscape:*\<p\> Coastal Plain

\<@33\>\<i\>*Landform:*\<p\> Uplands

\<@33\>\<i\>*Landform position:*\<p\> Broad ridges; side slopes

\<@33\>\<i\>*Slope:*\<p\> 0 to 18 percent

\<@33\>\<i\>*Taxonomic class:*\<p\> Fine, kaolinitic, thermic Rhodic
Kandiudults

\<@27\>Commonly Associated Soils

\<@30\>Faceville, Henderson, Orangeburg, and Red Bay soils are commonly
associated with the Greenville series.

-   \<@49\>The Faceville soils are in positions similar to those of the
    Greenville soils and have hues that are more yellow.

-   \<@29\>The Henderson soils are in the slightly lower positions, have
    hues that are more yellow, and have chert fragments throughout.

-   \<@29\>The Orangeburg soils are in positions similar to those of the
    Greenville soils or slightly lower, have hues that are more yellow,
    and have a fine-loamy control section.

-   \<@29\>The Red Bay soils are in positions similar to those of the
    Greenville soils or slightly lower and have a fine-loamy control
    section.

\<@27\>Typical Pedon

\<@30\>Greenville sandy clay loam, 0 to 2 percent slopes; about 0.5 mile
east of Carter Creek on County Road 22, about 0.8 mile north on County
Road 73, and 150 feet west; Randolph County, Georgia; USGS Martins
Crossroads topographic quadrangle; lat. 31 degrees 39 minutes 16 seconds
N. and long. 84 degrees 42 minutes 47 seconds W., NAD27.

\<@23\>Ap---0 to 8 inches; dark reddish brown (5YR 3/3) sandy clay loam;
weak medium granular structure; very friable; few fine roots; strongly
acid; abrupt smooth boundary.

\<@33\>Bt1---8 to 45 inches; dark red (10R 3/6) sandy clay; moderate
medium subangular blocky structure; firm; common fine pores; common
distinct clay films on faces of peds; strongly acid; gradual wavy
boundary.

\<@33\>Bt2---45 to 80 inches; dark red (2.5YR 3/6) sandy clay; moderate
medium subangular blocky structure; firm; few fine pores; common
distinct clay films on faces of peds; strongly acid.

\<@27\>Range in Characteristics

\<@33\>\<i\>*Thickness of the solum:*\<p\> More than 60 inches

\<@33\>\<i\>*Reaction:*\<p\> Very strongly acid to moderately acid
throughout, except where the surface layer has been limed

\<@23\>\<i\>*A or Ap horizon:*\<p\>

\<@31\>Color---hue of 2.5YR or 5YR, value of 3 or 4, and chroma of 2 to
6

\<@31\>Texture---sandy clay loam

\<@23\>\<i\>*Bt horizon:*\<p\>

\<@31\>Color---hue of 10R or 2.5YR, value of 2 or 3, and chroma of 2 to
6

\<@31\>Texture---clay loam, sandy clay, or clay

\<@37\>Henderson Series

\<@33\>\<i\>*Depth class:*\<p\> Very deep

\<@33\>\<i\>*Drainage class:*\<p\> Well drained

\<@33\>\<i\>*Permeability:*\<p\> Slow

\<@33\>\<i\>*Parent material:*\<p\> Clayey marine sediments and impure
limestone

\<@33\>\<i\>*Landscape:*\<p\> Coastal Plain

\<@33\>\<i\>*Landform:*\<p\> Uplands

\<@33\>\<i\>*Landform position:*\<p\> Ridge, knolls, and side slopes

\<@33\>\<i\>*Slope:*\<p\> 2 to 20 percent

\<@33\>\<i\>*Taxonomic class:*\<p\> Fine, kaolinitic, thermic Typic
Paleudults

\<@27\>Commonly Associated Soils

\<@30\>Carnegie, Greenville, Marlboro, and Nankin soils are commonly
associated with the Henderson series.

-   \<@49\>The Carnegie soils are in positions similar to those of the
    Henderson soils or slightly higher, do not have chert fragments, and
    contain more than 5 percent plinthite, by volume.

-   \<@29\>The Greenville soils are in the slightly higher positions, do
    not have chert fragments, and have redder hues.

-   \<@29\>The Marlboro soils are in positions similar to those of the
    Henderson soils or slightly higher and do not have chert fragments.

-   \<@29\>The Nankin soils are in positions similar to those of the
    Henderson soils or slightly lower, do not have chert fragments, and
    have a solum that is less than 60 inches thick.

\<@27\>Typical Pedon

\<@30\>Henderson gravelly sandy loam, 2 to 8 percent slopes; about 2.7
miles south of the intersection of U.S. Highway 82 and Georgia Highway
266 and about 30 feet west of Georgia Highway 266; Randolph County,
Georgia; USGS Carnegie topographic quadrangle; lat. 31 degrees 43
minutes 20 seconds N. and long. 84 degrees 51 minutes 31 seconds W.,
NAD27.

\<@23\>Ap---0 to 4 inches; very dark grayish brown (10YR 3/2) gravelly
sandy loam; weak fine granular structure; very friable; many fine roots;
about 20 percent chert pebbles and 3 percent chert stones; strongly
acid; clear wavy boundary.

\<@33\>E---4 to 13 inches; yellowish brown (10YR 5/4) gravelly sandy
loam; weak fine granular structure; very friable; common medium roots;
about 20 percent chert pebbles; strongly acid; abrupt irregular
boundary.

\<@33\>Bt1---13 to 18 inches; strong brown (7.5YR 5/6) gravelly sandy
clay; moderate fine subangular blocky structure; friable; common medium
roots; about 20 percent chert pebbles and 5 percent chert stones; very
strongly acid; abrupt irregular boundary.

\<@33\>Bt2---18 to 33 inches; strong brown (7.5YR 5/6) gravelly clay;
strong medium subangular blocky structure; firm; common distinct clay
films on faces of peds; few large roots; about 20 percent chert pebbles
and 5 percent chert stones; common medium distinct yellowish red (5YR
5/6) and reddish brown (2.5YR 4/4) masses in which iron has accumulated;
very strongly acid; gradual irregular boundary.

\<@33\>Bt3---33 to 49 inches; strong brown (7.5YR 5/6) gravelly clay;
moderate medium subangular blocky structure; firm; common distinct clay
films on faces of peds; about 20 percent chert pebbles, 2 percent chert
cobbles, and 3 percent chert stones; common fine distinct yellowish red
(5YR 5/6) and reddish brown (2.5YR 4/4) masses in which iron has
accumulated; very strongly acid; gradual irregular boundary.

\<@33\>Bt4---49 to 65 inches; multicolored, about 40 percent yellowish
brown (10YR 5/6), 35 percent light gray (2.5Y 7/2), and 25 percent
reddish brown (2.5YR 4/4) gravelly clay; moderate medium and coarse
subangular blocky structure; very firm; many pebbles and fragments of
chert, few stones; the areas of yellowish brown and reddish brown are
areas in which iron has accumulated; the areas of light gray are areas
from which iron or clay has depleted; very strongly acid.

\<@27\>Range in Characteristics

\<@33\>\<i\>*Thickness of the solum:*\<p\> More than 65 inches

\<@33\>\<i\>*Reaction:*\<p\> Very strongly acid or strongly acid
throughout, except where the surface layer has been limed

\<@23\>\<i\>*A or Ap horizon:*\<p\>

\<@31\>Color---hue of 10YR or 2.5Y, value of 3 or 4, and chroma of 2 or
3

\<@31\>Texture---gravelly sandy loam or gravelly loam

\<@23\>\<i\>*E horizon (where present):*\<p\>

\<@31\>Color---hue of 10YR or 2.5Y, value of 5, and chroma of 3 to 6

\<@31\>Texture---gravelly sandy loam or gravelly loam

\<@23\>\<i\>*Bt horizon, upper part:*\<p\>

\<@31\>Color---hue of 2.5YR to 10YR, value of 4 or 5, and chroma of 6 to
8

\<@31\>Texture---gravelly sandy clay loam or gravelly sandy clay

\<@23\>\<i\>*Bt horizon, lower part:*\<p\>

\<@31\>Color---hue of 2.5YR to 10YR, value of 4 or 5, and chroma of 6 to
8; or multicolored in shades of red, brown, yellow, and, below a depth
of 40 inches, gray

\<@31\>Redoximorphic features---common or many iron or clay depletions
in shades of gray and iron accumulations in shades of red, brown, or
yellow; the gray depletions are below a depth of 40 inches.

\<@31\>Texture---gravelly sandy clay or gravelly clay

\<@37\>Kinston Series

\<@33\>\<i\>*Depth class:*\<p\> Very deep

\<@33\>\<i\>*Drainage class:*\<p\> Poorly drained

\<@33\>\<i\>*Permeability:*\<p\> Moderate

\<@33\>\<i\>*Parent material:*\<p\> Stratified loamy and sandy alluvium

\<@33\>\<i\>*Landscape:*\<p\> Coastal Plain

\<@33\>\<i\>*Landform:*\<p\> Flood plains

\<@33\>\<i\>*Landform position:*\<p\> Planer to concave slopes

\<@33\>\<i\>*Slope:*\<p\> 0 to 2 percent

\<@33\>\<i\>*Taxonomic class:*\<p\> Fine-loamy, siliceous, semiactive,
acid, thermic Typic Fluvaquents

\<@27\>Commonly Associated Soils

\<@30\>Bibb, Cowarts, Lakeland, Lucy, Nankin, and Troup soils are
commonly associated with the Kinston series.

-   \<@49\>The Bibb soils are in positions similar to those of the
    Kinston soils and have a coarse-loamy control section.

-   \<@29\>The Cowarts soils are on side slopes on uplands and are well
    drained.

-   \<@29\>The Lakeland soils are on uplands, are excessively drained,
    and are sandy throughout.

-   \<@29\>The Lucy soils are on uplands, are well drained, and have
    sandy surface and subsurface layers with a combined thickness of 20
    to 40 inches.

-   \<@29\>The Nankin soils are on side slopes on uplands, are well
    drained, and have a fine control section.

-   \<@29\>The Troup soils are on uplands, are somewhat excessively
    drained, and have sandy surface and subsurface layers with a
    combined thickness of 40 to 80 inches.

\<@27\>Typical Pedon

\<@30\>Kinston loam, in an area of Kinston and Bibb soils, 0 to 1
percent slopes, frequently flooded; about 3,800 feet west of the
Randolph and Terrell County line on County Road 155 and 400 feet north
in the flood plain along Ichawaynochaway Creek; Randolph County,
Georgia; USGS Parrot topographic quadrangle; lat. 31 degrees 54 minutes
5 seconds N. and long. 84 degrees 36 minutes 53 seconds W., NAD27.

\<@23\>A1---0 to 3 inches; dark gray (10YR 4/1) loam; weak fine
subangular blocky structure; friable; many fine and medium and common
coarse roots; many faint yellowish red (5YR 5/6) coatings on faces of
peds; strongly acid; clear wavy boundary.

\<@33\>A2---3 to 8 inches; very dark gray (10YR 3/1) silt loam; weak
fine subangular blocky structure; friable; many medium and common fine
and coarse roots; common faint yellowish red (5YR 5/6) clay films on
faces of peds; strongly acid; clear wavy boundary.

\<@33\>Bg---8 to 15 inches; dark gray (2.5Y 4/1) clay loam; weak medium
subangular blocky structure; firm; few fine and common medium and coarse
roots; strongly acid; clear wavy boundary.

\<@33\>Ab---15 to 33 inches; very dark gray (10YR 3/1) sandy loam;
massive parting to weak fine subangular structure; friable; common
medium and coarse roots; common medium distinct pale brown (10YR 6/3)
areas in which iron has accumulated and common medium distinct light
brownish gray (10YR 6/2) areas from which iron has depleted; very
strongly acid; clear wavy boundary.

\<@33\>Cg1---33 to 52 inches; dark gray (10YR 4/1) sandy clay loam;
massive; firm; few coarse roots; common fine and medium distinct dark
yellowish brown (10YR 4/4) areas in which iron has accumulated; very
strongly acid; gradual wavy boundary.

\<@33\>Cg2---52 to 80 inches; dark gray (10YR 4/1) loamy sand; massive;
friable; very strongly acid.

\<@27\>Range in Characteristics

\<@33\>\<i\>*Reaction:*\<p\> Very strongly acid or strongly acid
throughout, except where the surface layer has been limed

\<@23\>\<i\>*A or Ap horizon:*\<p\>

\<@31\>Color---hue of 10YR, value of 2 to 5, and chroma of 1 to 3; or
neutral in hue and value of 5

\<@31\>Redoximorphic features---no, few, or common iron or clay
depletions in shades of gray and iron accumulations or stains in shades
of brown, yellow, and red

\<@31\>Texture---loamy sand, sandy loam, fine sandy loam, silt loam, or
loam

\<@23\>\<i\>*Ab horizon (where present):*\<p\>

\<@31\>Color---hue of 10YR, value of 3, and chroma of 1 or 2

\<@31\>Redoximorphic features---none to common in shades of brown,
yellow, and gray

\<@31\>Texture---sandy loam, fine sandy loam, loam, or sandy clay loam

\<@23\>\<i\>*Ag horizon (where present):*

\<@31\>Color---hue of 10YR, value of 5, and chroma of 1; or neutral in
hue and value of 5

\<@31\>Texture---same range as that of the A or Ap horizon

\<@23\>\<i\>*Bg horizon:*\<p\>

\<@31\>Color---hue of 10YR to 5Y, value of 3 to 7, and chroma of 1 or 2;
hue of 5GY to 5BG, value of 6, and chroma of 1; or neutral in hue and
value of 4 to 6

\<@31\>Redoximorphic features---few or common iron accumulations in
shades of yellow, brown, and red

\<@31\>Texture---sandy loam, fine sandy loam, loam, sandy clay loam, or
clay loam

\<@23\>\<i\>*Cg or C´g horizon:*\<p\>

\<@31\>Color---hue of 10YR to 5Y, value of 3 to 7, and chroma of 1 or 2;
hue of 5GY to 5BG, value of 6, and chroma of 1; or neutral in hue and
value of 4 to 6

\<@31\>Redoximorphic features---few or common iron accumulations in
shades of yellow, brown, and red

\<@31\>Texture---sandy loam, sandy clay loam, clay loam, or, below a
depth of 40 inches, loamy sand or loamy fine sand

\<@37\>Kolomoki Series

\<@33\>\<i\>*Depth class:*\<p\> Very deep

\<@33\>\<i\>*Drainage class:*\<p\> Well drained

\<@33\>\<i\>*Permeability:*\<p\> Moderate

\<@33\>\<i\>*Parent material:*\<p\> Clayey and sandy alluvial sediments

\<@33\>\<i\>*Landscape:*\<p\> Coastal Plain

\<@33\>\<i\>*Landform:*\<p\> River terraces

\<@33\>\<i\>*Landform position:*\<p\> Knolls

\<@33\>\<i\>*Slope:*\<p\> 0 to 2 percent

\<@33\>\<i\>*Taxonomic class:*\<p\> Fine, kaolinitic, thermic Typic
Hapludults

\<@27\>Commonly Associated Soils

\<@30\>Lakeland, Meggett, and Wahee soils are commonly associated with
the Kolomoki series.

-   \<@49\>The Lakeland soils are in the higher positions, are sandy
    throughout, and are excessively drained.

-   \<@29\>The Meggett soils are in the lower positions and are poorly
    drained.

-   \<@29\>The Wahee soils are in the lower positions and are somewhat
    poorly drained.

\<@27\>Typical Pedon

\<@30\>Kolomoki fine sandy loam, 0 to 2 percent slopes, rarely flooded;
in a cultivated field about 0.5 mile south on Georgia Highway 39 from
the intersection of Georgia Highway 39 and Georgia Highway 37 and 0.9
mile southwest on a dirt road; Clay County, Georgia; USGS Fort Gaines
topographic quadrangle; lat. 31 degrees 36 minutes 42 seconds N. and
long. 85 degrees 3 minutes 27 seconds W., NAD27.

\<@23\>Ap---0 to 9 inches; brown (7.5YR 4/4) fine sandy loam; weak fine
granular structure; friable; common fine roots; moderately acid; abrupt
smooth boundary.

\<@33\>Bt1---9 to 13 inches; yellowish red (5YR 5/6) sandy clay loam;
weak fine subangular blocky structure; very friable; common fine roots;
few faint clay films on faces of peds; moderately acid; clear smooth
boundary.

\<@33\>Bt2---13 to 28 inches; red (2.5YR 4/6) sandy clay; moderate fine
subangular blocky structure; firm; few fine roots; few faint clay films
on faces of peds; strongly acid; gradual wavy boundary.

\<@33\>Bt3---28 to 41 inches; yellowish red (5YR 5/6) sandy clay; weak
fine subangular blocky structure; friable; few fine roots; few faint
clay films on faces of peds; strongly acid; gradual wavy boundary.

\<@33\>BC---41 to 48 inches; strong brown (7.5YR 5/8) sandy loam; weak
fine subangular blocky structure; friable; strongly acid; gradual wavy
boundary.

\<@33\>C---48 to 72 inches; strong brown (7.5YR 5/8) loamy coarse sand;
single grained; loose; strongly acid.

\<@27\>Range in Characteristics

\<@33\>\<i\>*Thickness of the solum:*\<p\> 30 to 55 inches

\<@33\>\<i\>*Reaction:*\<p\> Very strongly acid to moderately acid
throughout, except where the surface layer has been limed

\<@23\>\<i\>*A or Ap horizon:*\<p\>

\<@31\>Color---hue of 7.5YR or 10YR, value of 4 or 5, and chroma of 3 or
4

\<@31\>Texture---loamy sand, loamy fine sand, sandy loam, or fine sandy
loam

\<@23\>\<i\>*BA or BE horizon (where present):*\<p\>

\<@31\>Color---hue of 7.5YR, value of 4 or 5, and chroma of 4 to 6

\<@31\>Texture---sandy loam or sandy clay loam

\<@23\>\<i\>*Bt horizon:*\<p\>

\<@31\>Color---hue 2.5YR or 5YR, value of 4 or 5, and chroma of 6 to 8

\<@31\>Texture---sandy clay loam, sandy clay, clay loam, or clay

\<@31\>Redoximorphic features---no, few, or common iron masses in shades
of yellow or brown

\<@23\>\<i\>*BC horizon (where present):*\<p\>

\<@31\>Color---hue of 5YR to 10YR, value of 4 or 5, and chroma of 4 to 8

\<@31\>Texture---sandy loam or sandy clay loam

\<@31\>Redoximorphic features---no, few, or common iron masses in shades
of yellow or brown

\<@23\>\<i\>*C horizon:*\<p\>

\<@31\>Color---hue of 5YR to 10YR, value of 5 or 6, and chroma of 6 to 8

\<@31\>Texture---sandy loam or sandy clay loam, and, below a depth of 40
inches, loamy sand, loamy coarse sand, sand, or coarse sand; stratified
layers of contrasting textures in some pedons

\<@31\>Redoximorphic features---no, few, or common iron masses in shades
of yellow or brown

\<@37\>Lakeland Series

\<@33\>\<i\>*Depth class:*\<p\> Very deep

\<@33\>\<i\>*Drainage class:*\<p\> Excessively drained

\<@33\>\<i\>*Permeability:*\<p\> Rapid

\<@33\>\<i\>*Parent material:*\<p\> Sandy marine sediments

\<@33\>\<i\>*Landscape:*\<p\> Coastal Plain

\<@33\>\<i\>*Landform:*\<p\> Uplands

\<@33\>\<i\>*Landform position:*\<p\> Broad ridges; side slopes

\<@33\>\<i\>*Slope range:*\<p\> 0 to 15 percent

\<@33\>\<i\>*Taxonomic class:*\<p\> Thermic, coated Typic
Quartzipsamments

\<@27\>Commonly Associated Soils

\<@30\>Ailey, Benevolence, Bibb, Cowarts, Kinston, Kolomoki, and Troup
soils are commonly associated with the Lakeland series.

-   \<@49\>The Ailey soils are in the slightly lower positions and on
    adjacent side slopes and have sandy surface and subsurface layers
    with a combined thickness of 20 to 40 inches over a dense, brittle
    subsoil.

-   \<@29\>The Benevolence soils are in the lower positions, are well
    drained, do not have thick sandy surface and subsurface layers, and
    have a coarse-loamy control section.

-   \<@29\>The Bibb and Kinston soils are on flood plains and are poorly
    drained.

-   \<@29\>The Cowarts soils are in the lower positions, are well
    drained, and have a fine-loamy control section.

-   \<@29\>The Kolomoki soils are in the lower positions, are well
    drained, and have a fine control section.

-   \<@29\>The Troup soils are in positions similar to those of the
    Lakeland soils, are somewhat excessively drained, and have sandy
    surface and subsurface layers with a combined thickness of 40 to 80
    inches.

\<@27\>Typical Pedon

\<@30\>Lakeland sand, 0 to 8 percent slopes; about 0.7 mile north of
Cemochechobee Creek on Cemetery Road, 0.1 mile east on a field road, and
100 feet north of the road; Randolph County, Georgia; USGS Coleman
topographic quadrangle; lat. 31 degrees 38 minutes 45 seconds N. and
long. 84 degrees 55 minutes 2 seconds W., NAD27.

\<@23\>Ap---0 to 4 inches; dark yellowish brown (10YR 4/4) sand; single
grained; loose; common fine and medium roots; common uncoated sand
grains; strongly acid; clear wavy boundary.

\<@33\>C1---4 to 25 inches; yellowish brown (10YR 5/6) sand; single
grained; loose; common fine and medium roots; few uncoated sand grains;
strongly acid; gradual smooth boundary.

\<@33\>C2---25 to 60 inches; yellowish brown (10YR 5/8) sand; single
grained; loose; few fine roots; common uncoated sand grains; few coarse
sand grains; strongly acid; clear smooth boundary.

\<@33\>C3---60 to 80 inches; strong brown (7.5YR 5/8) sand; single
grained; loose; many uncoated sand grains; few coarse sand grains;
strongly acid.

\<@27\>Range in Characteristics

\<@33\>\<i\>*Thickness of the sandy epipedon:*\<p\> More than 80 inches

\<@33\>\<i\>*Reaction:*\<p\> Strongly acid to moderately acid
throughout, except where the surface layer has been limed

\<@23\>\<i\>*A or Ap horizon:*\<p\>

\<@31\>Color---hue of 10YR, value of 3 or 4, and chroma of 2 to 4

\<@31\>Texture---sand

\<@23\>\<i\>*C horizon:*\<p\>

\<@31\>Color---hue of 5YR to 10YR, value of 5 to 7, and chroma of 4 to 8

\<@31\>Texture---sand

\<@37\>Lucy Series

\<@33\>\<i\>*Depth class:*\<p\> Very deep

\<@33\>\<i\>*Drainage class:*\<p\> Well drained

\<@33\>\<i\>*Permeability:*\<p\> Moderate

\<@33\>\<i\>*Parent material:*\<p\> Sandy and loamy marine sediments

\<@33\>\<i\>*Landscape:*\<p\> Coastal Plain

\<@33\>\<i\>*Landform:*\<p\> Uplands

\<@33\>\<i\>*Landform position:*\<p\> Ridges and side slopes

\<@33\>\<i\>*Slope:*\<p\> 0 to 15 percent

\<@33\>\<i\>*Taxonomic class:*\<p\> Loamy, kaolinitic, thermic Arenic
Kandiudults

\<@27\>Commonly Associated Soils

\<@30\>Benevolence, Bibb, Cowarts, Kinston, Orangeburg, and Troup soils
are commonly associated with the Lucy series.

-   \<@49\>The Benevolence and Orangeburg soils are in positions similar
    to those of the Lucy soils and do not have thick, sandy surface and
    subsurface layers.

-   \<@29\>The Bibb and Kinston soils are on flood plains adjacent to
    the Lucy soils and are poorly drained.

-   \<@29\>The Cowarts soils are in the slightly lower positions and do
    not have thick, sandy surface and subsurface layers.

-   \<@29\>The Troup soils are in positions similar to those of the Lucy
    soils or slightly higher and have sandy surface and subsurface
    layers with a combined thickness of 40 to 80 inches.

\<@27\>Typical Pedon

\<@30\>Lucy loamy sand, 0 to 5 percent slopes; about 1.5 miles west of
Coleman on Georgia Highway 266 and 550 feet south of the highway;
Randolph County, Georgia; USGS Coleman topographic quadrangle; lat. 31
degrees 40 minutes 8 seconds N. and long. 84 degrees 54 minutes 38
seconds W., NAD27.

\<@23\>Ap---0 to 8 inches; grayish brown (10YR 5/2) loamy sand; weak
fine granular structure; very friable; many fine and medium roots;
moderately acid; clear smooth boundary.

\<@33\>E---8 to 24 inches; brown (7.5YR 5/4) loamy sand; weak fine
granular structure; very friable; many fine and medium roots; moderately
acid; gradual smooth boundary.

\<@33\>Bt1---24 to 48 inches; yellowish red (5YR 5/8) sandy loam; weak
fine subangular blocky structure; very friable; common fine and medium
roots; strongly acid; gradual wavy boundary.

\<@33\>Bt2---48 to 72 inches; red (2.5YR 4/8) sandy clay loam; weak
medium subangular blocky structure; friable; common fine and medium
roots; strongly acid.

\<@27\>Range in Characteristics

\<@33\>\<i\>*Thickness of the solum:*\<p\> More than 60 inches

\<@33\>\<i\>*Thickness of the sandy epipedon:*\<p\> 20 to 40 inches

\<@33\>\<i\>*Reaction:*\<p\> Very strongly acid to moderately acid in
the A and E horizons and very strongly acid or strongly acid in the Bt
horizon, except where the surface layer has been limed

\<@23\>\<i\>*A or Ap horizon:*\<p\>

\<@31\>Color---hue of 7.5YR or 10YR, value of 3 to 5, and chroma of 2 to
4

\<@31\>Texture---loamy sand or loamy fine sand

\<@23\>\<i\>*E horizon:*\<p\>

\<@31\>Color---hue of 5YR to 10YR, value of 4 to 6, and chroma of 4 to 6

\<@31\>Texture---loamy sand or loamy fine sand

\<@23\>\<i\>*BE horizon (where present):*\<p\>

\<@31\>Color---hue of 2.5YR to 7.5YR, value of 4 to 6, and chroma of 6
to 8

\<@31\>Texture---loamy sand, loamy fine sand, or sandy loam

\<@23\>\<i\>*Bt horizon:*\<p\>

\<@31\>Color---dominantly hue of 2.5YR or 5YR, value of 4 to 6, and
chroma of 6 to 8; the upper 10 inches or less, however, has hue of 7.5YR
or 10YR in some pedons.

\<@31\>Redoximorphic features---no, few, or common iron accumulations in
shades of brown, red, and yellow below a depth of 40 inches

\<@31\>Texture---sandy loam, sandy clay loam, or, below a depth of 50
inches, sandy clay

\<@37\>Marlboro Series

\<@33\>\<i\>*Depth class:*\<p\> Very deep

\<@33\>\<i\>*Drainage class:*\<p\> Well drained

\<@33\>\<i\>*Permeability:*\<p\> Moderate

\<@33\>\<i\>*Parent material:*\<p\> Clayey marine sediments

\<@33\>\<i\>*Landscape:*\<p\> Coastal Plain

\<@33\>\<i\>*Landform:*\<p\> Uplands

\<@33\>\<i\>*Landform position:*\<p\> Broad ridges; side slopes

\<@33\>\<i\>*Slope:*\<p\> 0 to 8 percent

\<@33\>\<i\>*Taxonomic class:*\<p\> Fine, kaolinitic, thermic Typic
Paleudults

\<@27\>Commonly Associated Soils

\<@30\>Clarendon, Faceville, Grady, Henderson, and Nankin soils are
commonly associated with the Marlboro series.

-   \<@49\>The Clarendon soils are in the lower positions, are
    moderately well drained, and have a fine-loamy control section.

-   \<@29\>The Faceville soils are in positions similar to those of the
    Marlboro soils or slightly higher and have redder hues.

-   \<@29\>The Grady soils are in the lower, depressional positions and
    are poorly drained.

-   \<@29\>The Henderson soils are in positions similar to those of the
    Marlboro soils or slightly lower and have chert fragments
    throughout.

-   \<@29\>The Nankin soils are in the slightly lower positions and have
    a solum that is less than 60 inches thick.

\<@27\>Typical Pedon

\<@30\>Marlboro sandy loam, 0 to 2 percent slopes; about 1.8 miles south
of the Clay and Quitman County line on Georgia Highway 39, northeast 0.4
mile on County Road 129, north 0.2 mile on a field road, and 400 feet
west of the road; Clay County, Georgia; USGS Hatcher topographic
quadrangle; lat. 31 degrees 45 minutes 19 seconds N. and long. 85
degrees 4 minutes 19 seconds W., NAD27.

\<@23\>Ap---0 to 8 inches; brown (10YR 4/3) sandy loam; weak fine
granular structure; very friable; few fine and medium roots; moderately
acid; clear smooth boundary.

\<@33\>Bt1---8 to 13 inches; yellowish brown (10YR 5/8) sandy clay loam;
weak medium subangular blocky structure; friable; few fine roots; few
distinct clay films on faces of peds; moderately acid; clear smooth
boundary.

\<@33\>Bt2---13 to 36 inches; yellowish brown (10YR 5/8) clay loam;
moderate medium subangular blocky structure; firm; few fine roots;
common distinct clay films on faces of peds; few fine distinct strong
brown (7.5YR 5/8) masses in which iron has accumulated; strongly acid;
clear smooth boundary.

\<@33\>Bt3---36 to 70 inches; yellowish brown (10YR 5/8) clay loam;
moderate medium subangular blocky structure; firm; few very fine roots;
many distinct continuous clay films on faces of peds; few medium
prominent yellowish red (5YR 5/8), common medium distinct strong brown
(7.5YR 5/8), and few fine distinct yellow (10YR 7/8) masses in which
iron has accumulated; about 1 percent, by volume, ironstone nodules;
strongly acid; clear smooth boundary.

\<@33\>BC---70 to 80 inches; brownish yellow (10YR 6/8) sandy clay loam;
weak medium subangular blocky structure; friable; few very fine roots;
few faint clay films on faces of peds; few medium prominent red (2.5YR
4/6), common medium prominent yellowish red (5YR 5/8), common fine
distinct strong brown (7.5YR 5/8), and common fine faint yellow (10YR
7/8) masses in which iron has accumulated; strongly acid.

\<@27\>Range in Characteristics

\<@33\>\<i\>*Thickness of the solum:*\<p\> More than 60 inches

\<@33\>\<i\>*Reaction:*\<p\> Very strongly acid to moderately acid
throughout, except where the surface layer has been limed

\<@23\>\<i\>*A or Ap horizon:*\<p\>

\<@31\>Color---hue of 10YR, value of 4 or 5, and chroma of 1 to 4

\<@31\>Texture---loamy sand, loamy fine sand, or sandy loam

\<@23\>\<i\>*E horizon (where present):*\<p\>

\<@31\>Color---hue of 10YR or 2.5Y, value of 5 to 7, and chroma of 3 to
5

\<@31\>Texture---loamy sand, loamy fine sand, or sandy loam

\<@23\>\<i\>*Bt horizon:*\<p\>

\<@31\>Color---hue of 7.5YR or 10YR, value of 5 or 6, and chroma of 4 to
8

\<@31\>Redoximorphic features---iron accumulations in shades of red,
brown, and yellow in the middle and lower parts; no, few, or common iron
or clay depletions in shades of gray below a depth of 40 inches

\<@31\>Texture---dominantly clay loam, sandy clay, or clay; a thin layer
of sandy clay loam in the upper part of the horizon in some pedons

\<@23\>\<i\>*BC horizon (where present):*\<p\>

\<@31\>Color---hue of 7.5YR or 10YR, value of 5 or 6, and chroma of 4 to
8

\<@31\>Redoximorphic features---few to many iron or clay depletions in
shades of gray and iron accumulations in shades of red, brown, or yellow

\<@31\>Texture---sandy loam or sandy clay loam

\<@37\>Maubila Series

\<@33\>\<i\>*Depth class:* Very deep\<p\>

\<@33\>\<i\>*Drainage class:* Moderately well drained

\<@33\>\<i\>*Permeability:*\<p\> Slow

\<@33\>\<i\>*Parent material:*\<p\> Clayey marine sediments

\<@33\>\<i\>*Landscape:*\<p\> Coastal Plain

\<@33\>\<i\>*Landform:*\<p\> Uplands

\<@33\>\<i\>*Landform position:*\<p\> Knolls, ridgetops, and side slopes

\<@33\>\<i\>*Slope range:*\<p\> 5 to 45 percent

\<@33\>\<i\>*Taxonomic class:*\<p\> Fine, mixed, subactive, thermic
Aquic Hapludults

\<@27\>Commonly Associated Soils

\<@30\>Ailey, Cowarts, and Nankin soils are commonly associated with the
Maubila series.

-   \<@49\>The Ailey soils are in positions similar to those of the
    Maubila soils, are well drained, and have sandy surface and
    subsurface layers with a combined thickness of 20 to 40 inches over
    dense, brittle layers.

-   \<@29\>The Cowarts soils are in positions similar to those of the
    Maubila soils or lower, are well drained, and have a fine-loamy
    control section.

-   \<@29\>The Nankin soils are in positions similar to those of the
    Maubila soils and are well drained.

\<@27\>Typical Pedon

\<@30\>Maubila flaggy sandy loam in an area of Cowarts-Maubila complex,
8 to 15 percent slopes; Barbour County, Alabama; USGS Clayton North
topographic quadrangle; lat. 31 degrees 56 minutes 24 seconds N. and
long. 85 degrees 29 minutes 5 seconds W., NAD27.

\<@23\>A---0 to 4 inches; brown (10YR 4/3) flaggy sandy loam; weak fine
granular structure; very friable; common fine and medium roots; about 25
percent, by volume, angular fragments of ironstone; very strongly acid;
clear smooth boundary.

\<@33\>Bt1---4 to 26 inches; strong brown (7.5YR 5/6) clay loam;
moderate medium subangular blocky structure; firm; common fine and
medium roots; about 10 percent, by volume, angular fragments of
ironstone; very strongly acid; clear wavy boundary.

\<@33\>Bt2---26 to 40 inches; yellowish brown (10YR 5/6) clay; strong
medium subangular blocky structure; very firm; few fine and medium
roots; about 10 percent, by volume, angular fragments of ironstone;
common medium distinct red (10R 4/6) masses in which iron has
accumulated; common medium distinct light brownish gray (10YR 6/2) areas
from which iron has depleted; very strongly acid; abrupt wavy boundary.

\<@33\>Bt3---40 to 52 inches; yellowish brown (10YR 5/6) clay; strong
coarse angular blocky structure; very firm; few fine roots; about 10
percent, by volume, angular fragments of ironstone; many fine and medium
distinct light red (10R 6/6) masses in which iron has accumulated; many
medium prominent gray (10YR 6/1) areas from which iron has depleted;
very strongly acid; clear irregular boundary.

\<@33\>BC---52 to 57 inches; 40 percent gray (10YR 6/1), 30 percent
yellowish brown (10YR 5/6), and 30 percent light red (10R 6/6) clay;
weak coarse angular blocky structure; very firm; about 5 percent, by
volume, angular fragments of ironstone; the areas of yellowish brown and
light red are areas in which iron has accumulated; the areas of gray are
areas from which iron has depleted; very strongly acid; gradual wavy
boundary.

\<@33\>C---57 to 72 inches; 40 percent gray (10YR 6/1), 30 percent
strong brown (7.5YR 5/8), and 30 percent red (2.5YR 5/8) clay; massive;
very firm; common discontinuous strata of ironstone; the areas of strong
brown and red are areas in which iron has accumulated; the areas of gray
are areas from which iron has depleted; very strongly acid.

\<@27\>Range in Characteristics

\<@33\>\<i\>*Thickness of the solum:*\<p\> 40 to 60 inches

\<@33\>\<i\>*Rock fragments:*\<p\> 5 to 35 percent, by volume, ironstone
fragments in the A and E horizons and less than 15 percent, by volume,
in the B and C horizons

\<@33\>\<i\>*Reaction:*\<p\> Extremely acid to strongly acid throughout,
except where the surface has been limed

\<@23\>\<i\>*A or Ap horizon:*\<p\>

\<@31\>Color---hue of 7.5YR or 10YR, value of 3 to 5, and chroma of 2 to
4

\<@31\>Texture---loamy sand, loamy fine sand, sandy loam, or loam in the
fine-earth fraction

\<@23\>\<i\>*E horizon (where present):*\<p\>

\<@31\>Color---hue of 10YR, value of 5 or 6, and chroma of 2 to 4

\<@31\>Texture---loamy sand, loamy fine sand, or sandy loam in the
fine-earth fraction

\<@23\>\<i\>*Bt horizon, upper part:*\<p\>

\<@31\>Color---hue of 7.5YR or 10YR, value of 4 to 6, and chroma of 6 to
8

\<@31\>Texture---clay loam or clay

\<@31\>Redoximorphic features---no, few, or common iron accumulations in
shades of red and brown and iron depletions in shades of gray

\<@23\>\<i\>*Bt horizon, lower part:*\<p\>

\<@31\>Color---hue of 7.5YR or 10YR, value of 4 to 6, and chroma of 6 to
8; or multicolored in shades of gray, yellow, red, and brown

\<@31\>Texture---clay loam, clay, or silty clay

\<@31\>Redoximorphic features---common or many iron accumulations in
shades of red and brown and iron depletions in shades of gray

\<@23\>\<i\>*BC horizon (where present):*\<p\>

\<@31\>Color---multicolored in shades of gray, yellow, red, and brown

\<@31\>Texture---silty clay, clay loam, or clay

\<@31\>Redoximorphic features---iron accumulations in shades of red,
yellow, and brown and iron depletions in shades of gray

\<@23\>\<i\>*C horizon:*\<p\>

\<@31\>Color---multicolored in shades of gray, yellow, red, and brown

\<@31\>Texture---silty clay, clay loam, or clay

\<@31\>Redoximorphic features---iron depletions in shades of gray and
iron accumulations in shades of red, yellow, and brown

\<@37\>Meggett Series

\<@33\>\<i\>*Depth class:*\<p\> Very deep

\<@33\>\<i\>*Drainage class:*\<p\> Poorly drained

\<@33\>\<i\>*Permeability:*\<p\> Slow

\<@33\>\<i\>*Parent material:*\<p\> Clayey alluvial sediments

\<@33\>\<i\>*Landscape:*\<p\> Coastal Plain

\<@33\>\<i\>*Landform:*\<p\> River terraces

\<@33\>\<i\>*Landform position:*\<p\> Flood plains

\<@33\>\<i\>*Slope:*\<p\> 0 to 2 percent

\<@33\>\<i\>*Taxonomic class:*\<p\> Fine, mixed, active, thermic Typic
Albaqualfs

\<@27\>Commonly Associated Soils

\<@30\>Kolomoki and Wahee soils are commonly associated with the Meggett
series.

-   \<@49\>The Kolomoki soils are in the higher positions and are well
    drained.

-   \<@29\>The Wahee soils are in the slightly higher positions and are
    somewhat poorly drained.

\<@27\>Typical Pedon

\<@30\>Meggett fine sandy loam, 0 to 2 percent slopes, occasionally
flooded; in a area of woodland about 0.5 mile south on Georgia Highway
39 from the intersection of Georgia Highway 39 and Georgia Highway 37
and 0.6 mile southwest on a dirt road; Clay County, Georgia; USGS Fort
Gaines topographic quadrangle; lat. 31 degrees 35 minutes 16 seconds N.
and long. 85 degrees 3 minutes 2 second W., NAD27.

\<@23\>A---0 to 4 inches; dark grayish brown (10YR 4/2) fine sandy loam;
weak fine granular structure; very friable; common fine roots;
moderately acid; clear smooth boundary.

\<@33\>E1---4 to 8 inches; grayish brown (10YR 5/2) fine sandy loam;
weak fine granular structure; very friable; common fine roots; common
fine distinct brown (7.5YR 5/4) masses in which iron has accumulated;
moderately acid; clear smooth boundary.

\<@33\>E2---8 to 15 inches; gray (10YR 6/1) fine sandy loam; weak fine
granular structure; very friable; common fine roots; common fine
prominent strong brown (7.5YR 5/6) masses in which iron has accumulated;
moderately acid; gradual wavy boundary.

\<@33\>Btg1---15 to 28 inches; gray (5Y 5/1) clay; moderate medium
subangular blocky structure; firm; few fine roots; few faint
discontinuous clay films on ped faces; common medium distinct yellowish
brown (10YR 5/6) masses in which iron has accumulated; moderately acid;
gradual wavy boundary.

\<@33\>Btg2---28 to 55 inches; gray (5Y 6/1) clay; moderate medium
subangular blocky structure; firm; few faint clay films on ped faces;
few or common medium distinct yellowish brown (10YR 5/6) and olive (5Y
5/4) masses in which iron has accumulated; slightly acid; gradual wavy
boundary.

\<@33\>BCg---55 to 65 inches; gray (5Y 6/1) sandy clay; weak medium
subangular blocky structure; firm; slightly acid.

\<@27\>Range in Characteristics

\<@33\>\<i\>*Thickness of the solum:*\<p\> 40 to more than 80 inches

\<@33\>\<i\>*Reaction:*\<p\> Very strongly acid to slightly acid in the
A and E horizons, strongly acid to moderately alkaline in the upper part
of the Btg horizon, and slightly acid to moderately alkaline in the
lower part of the Btg horizon and in the BCg and C horizons, except
where the surface layer has been limed

\<@23\>\<i\>*A or Ap horizon:*\<p\>

\<@31\>Color---hue of 10YR, value of 2 to 5, and chroma of 1 to 3

\<@31\>Texture---sandy loam, fine sandy loam, or clay loam

\<@23\>\<i\>*E horizon (where present):*\<p\>

\<@31\>Color---hue of 10YR, value of 4 to 6, and chroma of 1 or 2

\<@31\>Texture---sandy loam or fine sandy loam

\<@31\>Redoximorphic features---no, few, or common iron masses in shades
of red, yellow, or brown and iron depletions in shades of gray

\<@23\>\<i\>*Btg horizon:*\<p\>

\<@31\>Color---hue of 10YR to 5Y, value of 4 to 7, and chroma of 1 or 2;
or multicolored in shades of red, yellow, gray, or brown

\<@31\>Texture---sandy clay loam (in the upper part), sandy clay, clay
loam, or clay

\<@31\>Redoximorphic features---common or many iron masses in shades of
red, yellow, or brown

\<@23\>\<i\>*BCg horizon (where present):*\<p\>

\<@31\>Color---hue of 10YR to 5Y, value of 4 to 7, and chroma of 1 to 2;
or neutral in hue and value of 4 to 7

\<@31\>Texture---sandy clay loam, clay loam, or clay

\<@23\>\<i\>*Cg horizon (where present):*\<p\>

\<@31\>Color---hue of 10YR to 5Y, value of 4 to 7, and chroma of 1 to 2;
or neutral in hue and value of 4 to 7

\<@31\>Texture---variable or stratified with sand and clay

\<@37\>Nankin Series

\<@33\>\<i\>*Depth class:*\<p\> Very deep

\<@33\>\<i\>*Drainage class:*\<p\> Well drained

\<@33\>\<i\>*Permeability:*\<p\> Moderately slow

\<@33\>\<i\>*Parent material:*\<p\> Stratified loamy and clayey marine
sediments

\<@33\>\<i\>*Landscape:*\<p\> Coastal Plain

\<@33\>\<i\>*Landform:*\<p\> Uplands

\<@33\>\<i\>*Landform position:*\<p\> Narrow ridges; side slopes

\<@33\>\<i\>*Slope:*\<p\> 2 to 40 percent

\<@33\>\<i\>*Taxonomic class:*\<p\> Fine, kaolinitic, thermic Typic
Kanhapludults

\<@27\>Commonly Associated Soils

\<@30\>Ailey, Bibb, Carnegie, Cowarts, Henderson, Kinston, Marlboro,
Maubila, Norfolk, and Orangeburg soils are commonly associated with the
Nankin series.

-   \<@49\>The Ailey soils are in positions similar to those of the
    Nankin soils or slightly higher and have sandy surface and
    subsurface layers with a combined thickness of 20 to 40 inches over
    a dense, brittle subsoil.

-   \<@29\>The Bibb soils are on flood plains, are coarse-loamy, and are
    poorly drained.

-   \<@29\>The Carnegie soils are in positions similar to those of the
    Nankin soils or slightly higher; have more than 5 percent plinthite,
    by volume; and have a solum that is more than 60 inches thick.

-   \<@29\>The Cowarts soils are in positions similar to those of the
    Nankin soils, have a solum that ranges from 20 to 40 inches in
    thickness, and have a fine-loamy control section.

-   \<@29\>The Henderson soils are in positions similar to those of the
    Nankin soils or slightly higher, have a solum that is more than 60
    inches thick, and are cherty throughout.

-   \<@29\>The Kinston soils are on flood plains, are fine-loamy, and
    are poorly drained.

-   \<@29\>The Marlboro soils are in the slightly higher positions and
    have a solum that is more than 60 inches thick.

-   \<@29\>The Maubila soils are in positions similar to those of the
    Nankin soils and are moderately well drained.

-   \<@29\>The Norfolk and Orangeburg soils are in the higher positions,
    have a solum that is more than 60 inches thick, and have a
    fine-loamy control section.

\<@27\>Typical Pedon

\<@30\>Nankin loamy sand, in an area of Nankin-Cowarts complex, 15 to 35
percent slopes; about 0.6 mile north of Sharon Church, 2,800 feet west
of County Road 28, and 3,100 feet south of the Stewart County line;
Randolph County, Georgia; USGS Sanford topographic quadrangle; lat. 31
degrees 54 minutes 57 seconds N. and long. 84 degrees 53 minutes 28
seconds W., NAD27.

\<@23\>Ap---0 to 4 inches; very dark grayish brown (10YR 3/2) loamy
sand; weak fine granular structure; very friable; many fine and medium
roots; strongly acid; abrupt smooth boundary.

\<@33\>BA---4 to 10 inches; dark yellowish brown (10YR 4/4) sandy loam;
weak coarse subangular blocky structure; very friable; many fine and
medium roots; pockets of very dark grayish brown (10YR 3/2) loamy sand
in old root channels; strongly acid; gradual wavy boundary.

\<@33\>Bt1---10 to 16 inches; yellowish brown (10YR 5/8) sandy clay
loam; moderate coarse subangular blocky structure; friable; many fine
and medium roots; few faint clay films on faces of peds; few medium
distinct strong brown (7.5YR 5/8) masses in which iron has accumulated;
strongly acid; gradual wavy boundary.

\<@33\>Bt2---16 to 34 inches; yellowish red (5YR 5/8) sandy clay;
moderate medium subangular blocky structure; firm; common fine and
medium roots; common distinct clay films on faces of peds; strongly
acid; gradual wavy boundary.

\<@33\>Bt3---34 to 39 inches; yellowish red (5YR 5/8) sandy clay; weak
medium subangular blocky structure; friable; few medium roots; common
distinct clay films on faces of peds; common fine and medium distinct
red (2.5YR 5/8) masses in which iron has accumulated; the masses have
sharp boundaries and are within the matrix; strongly acid; gradual wavy
boundary.

\<@33\>BC---39 to 44 inches; strong brown (7.5YR 5/6) sandy clay loam;
weak fine subangular blocky structure; friable; few faint clay films on
faces of peds; common fine and medium distinct yellowish red (5YR 5/6)
masses in which iron has accumulated; very strongly acid; gradual wavy
boundary.

\<@33\>C1---44 to 48 inches; yellowish brown (10YR 5/6) sandy loam; weak
coarse subangular blocky structure parting to weak fine granular; very
friable; common medium prominent red (2.5YR 5/8) masses in which iron
has accumulated; strongly acid; gradual wavy boundary.

\<@33\>C2---48 to 55 inches; yellowish brown (10YR 5/6) sandy loam; weak
fine granular structure; very friable; about 3 percent, by volume,
ironstone fragments; common medium prominent red (2.5YR 5/8) masses in
which iron has accumulated; very strongly acid; gradual wavy boundary.

\<@33\>C3---55 to 80 inches; yellowish brown (10YR 5/6) sandy loam;
massive parting to weak thin platy structure; firm in place, friable
when disturbed, brittle in about 10 percent of the volume; about 15
percent, by volume, ironstone fragments; common medium prominent red
(2.5YR 5/8) masses in which iron has accumulated; few medium distinct
light brownish gray (10YR 6/2) areas from which iron has depleted; very
strongly acid.

\<@27\>Range in Characteristics

\<@33\>\<i\>*Thickness of the solum:*\<p\> 40 to 60 inches

\<@33\>\<i\>*Reaction:*\<p\> Very strongly acid or strongly acid
throughout, except where the surface layer has been limed

\<@23\>\<i\>*A or Ap horizon:*\<p\>

\<@31\>Color---hue of 10YR, value of 3 or 4, and chroma of 2 to 4

\<@31\>Texture---loamy sand or sandy loam

\<@23\>\<i\>*AB or BA horizon (where present):*\<p\>

\<@31\>Color---hue of 5YR to 10YR, value of 4 or 5, and chroma of 2 to 4

\<@31\>Texture---sandy loam

\<@23\>\<i\>*Bt horizon, upper part:*\<p\>

\<@31\>Color---hue of 2.5YR to 10YR, value of 4 or 5, and chroma of 6 to
8; or hue of 10YR, value of 5 or 6, and chroma of 4 to 8

\<@31\>Redoximorphic features---no, few, or common iron accumulations in
shades of red, brown, and yellow

\<@31\>Texture---dominantly sandy clay or clay loam; a thin Bt1 horizon
of sandy clay loam in some pedons

\<@23\>\<i\>*Bt horizon, lower part:*\<p\>

\<@31\>Color---hue of 2.5YR to 10YR, value of 4 or 5, and chroma of 6 to
8

\<@31\>Redoximorphic features---few to many iron accumulations in shades
of red, brown, and yellow

\<@31\>Texture---sandy clay, clay loam, or clay

\<@23\>\<i\>*BC horizon (where present):*\<p\>

\<@31\>Color---hue of 2.5YR to 10YR, value of 4 or 5, and chroma of 6 to
8; or no dominant color and multicolored in shades of yellow, brown,
red, and gray

\<@31\>Redoximorphic features---few to many iron or clay depletions in
shades of gray and iron accumulations in shades of red and brown

\<@31\>Texture---sandy clay loam

\<@23\>\<i\>*C horizon:*\<p\>

\<@31\>Color---hue of 2.5YR to 10YR, value of 4 or 5, and chroma of 6;
or no dominant color and multicolored in shades of yellow, brown, red,
and gray

\<@31\>Redoximorphic features---few to many iron or clay depletions in
shades of gray and iron accumulations in shades of red and brown

\<@31\>Texture---sandy loam or sandy clay loam

\<@37\>Norfolk Series

\<@33\>\<i\>*Depth class:*\<p\> Very deep

\<@33\>\<i\>*Drainage class:*\<p\> Well drained

\<@33\>\<i\>*Permeability:*\<p\> Moderate

\<@33\>\<i\>*Parent material:*\<p\> Loamy marine sediments

\<@33\>\<i\>*Landscape:*\<p\> Coastal Plain

\<@33\>\<i\>*Landform:*\<p\> Uplands

\<@33\>\<i\>*Landform position:*\<p\> Broad ridges

\<@33\>\<i\>*Slope:*\<p\> 0 to 5 percent

\<@33\>\<i\>*Taxonomic class:*\<p\> Fine-loamy, kaolinitic, thermic
Typic Kandiudults

\<@27\>Commonly Associated Soils

\<@30\>Bonneau, Carnegie, Clarendon, Faceville, Goldsboro, Nankin,
Ocilla, Orangeburg, Rains, and Red Bay soils are commonly associated
with the Norfolk series.

-   \<@49\>The Bonneau soils are in positions similar to those of the
    Norfolk soils or slightly higher and have sandy surface and
    subsurface layers with a combined thickness of 20 to 40 inches.

-   \<@29\>The Carnegie soils are in positions similar to those of the
    Norfolk soils or slightly higher; have more than 5 percent
    plinthite, by volume; and have a fine control section.

-   \<@29\>The Clarendon soils are in the lower, more concave positions;
    have more than 5 percent plinthite, by volume; and are moderately
    well drained.

-   \<@29\>The Faceville soils are in positions similar to those of the
    Norfolk soils or slightly higher and have a fine control section.

-   \<@29\>The Goldsboro soils are in the lower positions and are
    moderately well drained.

-   \<@29\>The Nankin soils are on adjacent, lower slopes; have a fine
    control section; and have a solum that is less than 60 inches thick.

-   \<@29\>The Ocilla soils are in the lower positions, have sandy
    surface and subsurface layers with a combined thickness of 20 to 40
    inches, and are somewhat poorly drained.

-   \<@29\>The Orangeburg and Red Bay soils are in positions similar to
    those of the Norfolk soils or slightly higher and have redder hues.

-   \<@29\>The Rains soils are in the lower positions and are poorly
    drained.

\<@27\>Typical Pedon

\<@30\>Norfolk loamy sand, 0 to 2 percent slopes; about 1.2 miles south
of Pataula Creek on Georgia Highway 39, west 0.4 mile along a field
border, and 85 feet north of a ditch; Clay County, Georgia; USGS Fort
Gaines NE topographic quadrangle; lat. 31 degrees 44 minutes 5 seconds
N. and long. 85 degrees 3 minutes 7 seconds W., NAD27.

\<@23\>Ap---0 to 6 inches; brown (10YR 4/3) loamy sand; weak fine
granular structure; very friable; common fine roots; moderately acid;
abrupt clear boundary.

\<@33\>Bt1---6 to 10 inches; brownish yellow (10YR 6/8) sandy loam; weak
medium subangular blocky structure; very friable; common fine roots;
sand grains coated and bridged with clay; strongly acid; clear smooth
boundary.

\<@33\>Bt2---10 to 30 inches; yellowish brown (10YR 5/6) sandy clay
loam; moderate medium subangular blocky structure; friable; few distinct
clay films on faces of peds; strongly acid; gradual wavy boundary.

\<@33\>Bt3---30 to 55 inches; brownish yellow (10YR 6/8) sandy clay
loam; moderate medium subangular blocky structure; friable; common
distinct clay films on faces of peds; strongly acid; gradual wavy
boundary.

\<@33\>Bt4---55 to 70 inches; brownish yellow (10YR 6/8) sandy clay
loam; weak medium subangular blocky structure; firm; about 1 percent, by
volume, nodular plinthite; few distinct clay films on faces of peds; few
medium prominent yellowish red (5YR 5/8) and few medium distinct strong
brown (7.5YR 4/6) masses in which iron has accumulated; few fine
prominent light brownish gray (10YR 6/2) areas from which iron has
depleted; strongly acid; gradual wavy boundary.

\<@33\>BC---70 to 80 inches; yellowish brown (10YR 5/8) sandy loam; weak
fine granular structure; very friable; about 3 percent, by volume,
nodular plinthite; few medium distinct red (2.5YR 4/8) and strong brown
(7.5YR 5/8) and few fine distinct brownish yellow (10YR 6/8) masses in
which iron has accumulated; strongly acid.

\<@27\>Range in Characteristics

\<@33\>\<i\>*Thickness of the solum:*\<p\> More than 60 inches

\<@33\>\<i\>*Reaction:*\<p\> Extremely acid to strongly acid throughout,
except where the surface layer has been limed

\<@23\>\<i\>*A or Ap horizon:*\<p\>

\<@31\>Color---hue of 10YR or 2.5Y, value of 4 to 7, and chroma of 2 to
4

\<@31\>Texture---loamy sand or sandy loam

\<@23\>\<i\>*E horizon (where present):*\<p\>

\<@31\>Color---hue of 10YR or 2.5Y, value of 4 to 7, and chroma of 2 to
6

\<@31\>Texture---loamy sand or sandy loam

\<@23\>\<i\>*Bt horizon:*\<p\>

\<@31\>Color---hue of 7.5YR to 2.5Y, value of 5 to 8, and chroma of 3 to
8

\<@31\>Redoximorphic features---below a depth of 48 inches no, few,
common, or many iron depletions in shades of gray and iron accumulations
in shades of red, brown, and yellow

\<@31\>Texture---sandy loam or sandy clay loam

\<@23\>\<i\>*BC horizon (where present):*\<p\>

\<@31\>Color---hue of 5YR to 2.5Y, value of 4 to 7, and chroma of 2 to
8; or no dominant color and multicolored in shades of yellow, brown,
red, and gray

\<@31\>Redoximorphic features---few to many iron or clay depletions in
shades of gray and iron accumulations in shades of red, brown, and
yellow

\<@31\>Texture---sandy loam or sandy clay loam

\<@37\>Ocilla Series

\<@33\>\<i\>*Depth class:*\<p\> Very deep

\<@33\>\<i\>*Drainage class:*\<p\> Somewhat poorly drained

\<@33\>\<i\>*Permeability:*\<p\> Moderate

\<@33\>\<i\>*Parent material:*\<p\> Sandy and loamy marine sediments

\<@33\>\<i\>*Landscape:*\<p\> Coastal Plain

\<@33\>\<i\>*Landform:*\<p\> Uplands

\<@33\>\<i\>*Landform position:*\<p\> Stream terraces

\<@33\>\<i\>*Slope:*\<p\> 0 to 2 percent

\<@33\>\<i\>*Taxonomic class:*\<p\> Loamy, siliceous, semiactive,
thermic Aquic Arenic Paleudults

\<@27\>Commonly Associated Soils

\<@30\>Cowarts, Norfolk, Orangeburg, and Rains soils are commonly
associated with the Ocilla series.

-   \<@49\>The Cowarts soils are in the higher positions and are well
    drained.

-   \<@29\>The Norfolk soils are in the higher positions and are well
    drained.

-   \<@29\>The Orangeburg soils are in the higher positions and are well
    drained.

-   \<@29\>The Rains soils are in the lower positions and are poorly
    drained.

\<@27\>Typical Pedon

\<@30\>Ocilla loamy sand, 0 to 2 percent slopes; in a cultivated field
about 1 mile south of the Stuart County line on Georgia Highway 39 and
100 feet west of the road; Quitman County, Georgia; USGS Georgetown
topographic quadrangle; lat. 31 degrees 59 minutes 8 seconds N. and
long. 85 degrees 3 minutes 12 seconds W., NAD27.

\<@23\>Ap---0 to 10 inches; grayish brown (10YR 5/2) loamy sand; weak
fine granular structure; very friable; common fine and medium roots;
moderately acid; abrupt smooth boundary.

\<@33\>E---10 to 24 inches; light brownish gray (10YR 6/2) loamy sand;
moderate medium granular structure; friable; strongly acid; gradual wavy
boundary.

\<@33\>Bt---24 to 32 inches; yellowish brown (10YR 5/8) sandy clay loam;
weak medium subangular blocky structure; friable; few faint clay films
on faces of peds; few fine distinct strong brown (7.5YR 5/8) masses in
which iron has accumulated and light brownish gray (10YR 6/2) areas from
which iron has depleted; strongly acid; gradual wavy boundary.

\<@33\>Btg1---32 to 40 inches; light brownish gray (10YR 6/2) sandy clay
loam; weak medium subangular blocky structure; friable; few faint clay
films on faces of peds; common medium distinct strong brown (7.5YR 5/8)
and common medium prominent yellowish red (5YR 5/8) masses in which iron
has accumulated; strongly acid; gradual wavy boundary.

\<@33\>Btg2---40 to 58 inches; light brownish gray (10YR 6/2) sandy clay
loam; moderate medium subangular blocky structure; friable; few faint
clay films on faces of peds; many coarse distinct strong brown (7.5YR
5/8) and many coarse prominent red (2.5YR 5/8) masses in which iron has
accumulated; strongly acid; gradual wavy boundary.

\<@33\>Btg3---58 to 72 inches; light brownish gray (10YR 6/2) sandy clay
loam; moderate medium subangular blocky structure; friable; few faint
clay films on faces of peds; many coarse distinct brownish yellow (10YR
6/6) masses in which iron has accumulated; strongly acid.

\<@27\>Range in Characteristics

\<@33\>\<i\>*Thickness of the solum:*\<p\> More than 60 inches

\<@33\>\<i\>*Depth to chroma of 2 or less:*\<p\> 12 to 30 inches

\<@33\>\<i\>*Reaction:*\<p\> Very strongly acid or strongly acid
throughout, except where the surface layer has been limed

\<@23\>\<i\>*A or Ap horizon:*\<p\>

\<@31\>Color---hue of 10YR or 2.5Y, value of 3 to 5, and chroma of 1 or
2

\<@31\>Texture---loamy sand or loamy fine sand

\<@23\>\<i\>*E horizon:*\<p\>

\<@31\>Color---hue of 10YR to 5Y, value of 4 to 7, and chroma of 1 to 4

\<@31\>Texture---loamy sand or loamy fine sand

\<@31\>Redoximorphic features---no, few, or common iron accumulations in
shades of brown or yellow or iron or clay depletions in shades of gray

\<@23\>\<i\>*Bt horizon, upper part:*\<p\>

\<@31\>Color---hue of 7.5YR to 2.5Y, value of 5 to 7, and chroma of 2 to
8

\<@31\>Texture---sandy loam or sandy clay loam

\<@31\>Redoximorphic features---no, few, common, or many iron
accumulations in shades of brown, red, or yellow or iron or clay
depletions in shades of gray

\<@23\>\<i\>*Bt horizon, lower part:*\<p\>

\<@31\>Color---multicolored in shades of gray, yellow, brown, and red;
hue of 10YR to 5Y, value of 5 to 8, and chroma of 1 to 8; or neutral in
hue and value of 7

\<@31\>Texture---sandy clay loam or sandy clay

\<@31\>Redoximorphic features---few to many iron accumulations in shades
of brown, red, or yellow or iron or clay depletions in shades of gray

\<@23\>\<i\>*Btg, BC, or BCg horizons (where present):*\<p\>

\<@31\>Color---comparable to lower part of the Bt horizon

\<@31\>Texture---comparable to lower part of the Bt horizon

\<@37\>Orangeburg Series

\<@33\>\<i\>*Depth class:*\<p\> Very deep

\<@33\>\<i\>*Drainage class:*\<p\> Well drained

\<@33\>\<i\>*Permeability:*\<p\> Moderate

\<@33\>\<i\>*Parent material:*\<p\> Loamy and clayey marine sediments

\<@33\>\<i\>*Landscape:*\<p\> Coastal Plain

\<@33\>\<i\>*Landform:*\<p\> Uplands

\<@33\>\<i\>*Landform position:*\<p\> Broad ridges; side slopes

\<@33\>\<i\>*Slope:*\<p\> 0 to 15 percent

\<@33\>\<i\>*Taxonomic class:*\<p\> Fine-loamy, kaolinitic, thermic
Typic Kandiudults

\<@27\>Commonly Associated Soils

\<@30\>Benevolence, Bonneau, Faceville, Greenville, Lucy, Nankin,
Norfolk, Ocilla, Rains, Red Bay, and Troup soils are commonly associated
with the Orangeburg series.

-   \<@49\>The Benevolence soils are in positions similar to those of
    the Orangeburg soils and have a coarse-loamy control section.

-   \<@29\>The Bonneau and Lucy soils are in positions similar to those
    of the Orangeburg soils and have sandy surface and subsurface layers
    with a combined thickness of 20 to 40 inches.

-   \<@29\>The Faceville soils are in positions similar to those of the
    Orangeburg soils or slightly higher and have a fine control section.

-   \<@29\>The Greenville soils are in positions similar to those of the
    Orangeburg soils or slightly higher, have a fine control section,
    and have redder hues.

-   \<@29\>The Nankin soils are on lower slopes adjacent to the
    Orangeburg soils and have a fine control section.

-   \<@29\>The Norfolk soils are in positions similar to those of the
    Orangeburg soils or slightly lower and have hues that are more
    yellow.

-   \<@29\>The Ocilla soils are in the lower positions, have sandy
    surface and subsurface layers with a combined thickness of 20 to 40
    inches, and are somewhat poorly drained.

-   \<@29\>The Rains soils are in the lower positions and are poorly
    drained.

-   \<@29\>The Red Bay soils are in positions similar to those of the
    Orangeburg soils or slightly higher and have redder hues.

-   \<@29\>The Troup soils are in the slightly higher positions, are
    somewhat excessively drained, and have sandy surface and subsurface
    layers with a combined thickness of 40 to 80 inches.

\<@27\>Typical Pedon

\<@30\>Orangeburg loamy sand, 0 to 2 percent slopes; about 0.3 mile
southeast of the Clay and Quitman County line on Georgia Highway 291 and
400 feet north of the highway; Clay County, Georgia; USGS Hatcher
topographic quadrangle; lat. 31 degrees 46 minutes 10 seconds N. and
long. 85 degrees 3 minutes 11 seconds W., NAD27.

\<@23\>Ap---0 to 7 inches; dark brown (10YR 3/3) loamy sand; weak fine
granular structure; very friable; many fine and medium roots; slightly
acid; abrupt smooth boundary.

\<@33\>BA---7 to 11 inches; yellowish red (5YR 4/6) sandy loam; weak
fine subangular blocky structure; friable; many fine and medium roots;
sand grains coated and bridged with clay; slightly acid; clear smooth
boundary.

\<@33\>Bt1---11 to 22 inches; red (2.5YR 4/8) sandy clay loam; moderate
medium subangular blocky structure; friable; common fine and medium
roots; common distinct clay films on faces of most peds; strongly acid;
gradual wavy boundary.

\<@33\>Bt2---22 to 80 inches; red (2.5YR 4/8) sandy clay loam; weak
medium subangular blocky structure; friable; few fine roots; common
distinct clay films on faces of most peds; strongly acid.

\<@27\>Range in Characteristics

\<@33\>\<i\>*Thickness of the solum:*\<p\> More than 70 inches

\<@33\>\<i\>*Reaction:*\<p\> Very strongly acid to moderately acid in
the upper part of the solum and very strongly acid or strongly acid in
the lower part, except where the surface layer has been limed

\<@23\>\<i\>*A or Ap horizon:*\<p\>

\<@31\>Color---hue of 7.5YR or 10YR, value of 3 to 5, and chroma of 2 to
4

\<@31\>Texture---loamy sand or sandy loam

\<@23\>\<i\>*E horizon (where present):*\<p\>

\<@31\>Color---hue of 7.5YR or 10YR, value of 5 or 6, and chroma of 3 or
4

\<@31\>Texture---loamy sand

\<@23\>\<i\>*BA horizon (where present):*\<p\>

\<@31\>Color---hue of 2.5YR to 7.5YR, value of 4 or 5, and chroma of 4
to 6

\<@31\>Texture---sandy loam

\<@23\>\<i\>*Bt horizon:*\<p\>

\<@31\>Color---hue of 2.5YR or 5YR, value of 4 or 5, and chroma of 6 to
8

\<@31\>Redoximorphic features---no, few, or common iron accumulations in
shades of brown in the part of the lower horizon

\<@31\>Texture---dominantly sandy clay loam; sandy clay in lower part of
the horizon in some pedons

\<@37\>Rains Series

\<@33\>\<i\>*Depth class:*\<p\> Very deep

\<@33\>\<i\>*Drainage class:*\<p\> Poorly drained

\<@33\>\<i\>*Permeability:*\<p\> Moderate

\<@33\>\<i\>*Parent material:*\<p\> Sandy loam marine sediments

\<@33\>\<i\>*Landscape:*\<p\> Coastal Plain

\<@33\>\<i\>*Landform:*\<p\> Broad upland flats

\<@33\>\<i\>*Landform position:*\<p\> Concave depressions

\<@33\>\<i\>*Slope:*\<p\> 0 to 2 percent

\<@33\>\<i\>*Taxonomic class:*\<p\> Fine-loamy, siliceous, semiactive,
thermic Typic Paleaquults

\<@27\>Commonly Associated Soils

\<@30\>Clarendon, Faceville, Grady, Norfolk, Ocilla, and Orangeburg
soils are commonly associated with the Rains series.

-   \<@49\>The Clarendon soils are in the slightly higher positions, are
    moderately well drained, and contain 5 percent or more plinthite, by
    volume.

-   \<@29\>The Faceville soils are in the higher, more convex positions,
    are well drained, and have a clayey control section.

-   \<@29\>The Grady soils are in the slightly lower positions and have
    a clayey control section.

-   \<@29\>The Norfolk soils are in the higher positions and are well
    drained.

-   \<@29\>The Ocilla soils are in the slightly higher positions, have
    sandy surface and subsurface layers with a combined thickness of 20
    to 40 inches, and are somewhat poorly drained.

-   \<@29\>The Orangeburg soils are in the higher positions and are well
    drained.

\<@27\>Typical Pedon

\<@30\>Rains sandy loam, 0 to 2 percent slopes; about 1.2 miles north of
the bridge over Pataula Creek on Georgia Highway 39 and 120 feet
southwest of the road; Clay County, Georgia; USGS Hatcher topographic
quadrangle; lat. 31 degrees 45 minutes 22 seconds N. and long. 85
degrees 4 minutes 1 second W., NAD27.

\<@23\>Ap---0 to 8 inches; very dark grayish brown (10YR 3/2) sandy
loam; weak fine granular structure; very friable; common fine and medium
roots; moderately acid; abrupt smooth boundary.

\<@33\>Btg1---8 to 26 inches; light gray (10YR 6/1) sandy clay loam;
moderate medium subangular blocky structure; friable; common fine and
medium roots; few faint discontinuous clay films on faces of peds;
moderately acid; clear wavy boundary.

\<@33\>Btg2---26 to 38 inches; light gray (10YR 6/1) sandy clay loam;
moderate medium subangular blocky structure; friable; few fine and
medium roots; few faint discontinuous clay films on faces of peds;
common medium distinct strong brown (7.5YR 5/8) and few fine prominent
yellowish red (5YR 5/6) masses in which iron has accumulated and which
have sharp boundaries within the matrix; strongly acid; gradual wavy
boundary.

\<@33\>Btg3---38 to 48 inches; light gray (10YR 6/1) sandy clay loam;
moderate medium subangular blocky structure; firm; few faint
discontinuous clay films on faces of peds; common medium distinct strong
brown (7.5YR 5/8) and common medium prominent yellowish red (5YR 5/6)
masses in which iron has accumulated and which have sharp boundaries
within the matrix; strongly acid; gradual wavy boundary.

\<@33\>Btg4---48 to 52 inches; light gray (10YR 6/1) sandy clay loam;
moderate medium subangular blocky structure; firm; few faint
discontinuous clay films on faces of peds; many coarse distinct strong
brown (7.5YR 5/8) and many coarse prominent yellowish red (5YR 5/6)
masses in which iron has accumulated and which have sharp boundaries
within the matrix; strongly acid; gradual wavy boundary.

\<@33\>Btg5---52 to 72 inches; light gray (10YR 6/1) sandy clay loam;
moderate medium subangular blocky structure; firm; few faint
discontinuous clay films on ped faces; strongly acid.

\<@27\>Range in Characteristics

\<@33\>\<i\>*Thickness of the solum:*\<p\> More than 60 inches

\<@33\>\<i\>*Depth to chroma of 2 or less:*\<p\> 0 to 12 inches

\<@33\>\<i\>*Reaction:*\<p\> Extremely acid to slightly acid, except
where the surface layer has been limed

\<@23\>\<i\>*A or Ap horizon:*\<p\>

\<@31\>Color---hue of 10YR or 2.5Y, value of 2 to 5, and chroma of 1 or
2; or neutral in hue and value of 2 to 5

\<@31\>Texture---sandy loam or loamy sand

\<@23\>\<i\>*Eg horizon (where present):*\<p\>

\<@31\>Color---hue of 10YR to 5Y, value of 4 to 7, and chroma of 1 or 2;
or neutral in hue and value of 4 to 7

\<@31\>Texture---sandy loam or loamy sand

\<@31\>Redoximorphic features---no, few, or common iron accumulations in
shades of brown or yellow and iron or clay depletions in shades of gray

\<@23\>\<i\>*Btg horizon:*\<p\>

\<@31\>Color---hue of 10YR to 5Y, value of 4 to 7, and chroma of 1 or 2;
or neutral in hue and value of 4 to 7

\<@31\>Texture---sandy loam, sandy clay loam, clay loam, or sandy clay,
ranging to sandy loam in the upper part and to sandy clay in the lower
part

\<@31\>Redoximorphic features---no, few, common, or many iron
accumulations in shades of brown, red, or yellow and iron or clay
depletions in shades of gray

\<@37\>Red Bay Series

\<@33\>\<i\>*Depth class:*\<p\> Very deep

\<@33\>\<i\>*Drainage class:*\<p\> Well drained

\<@33\>\<i\>*Permeability:*\<p\> Moderate

\<@33\>\<i\>*Parent material:*\<p\> Loamy marine sediments

\<@33\>\<i\>*Landscape:*\<p\> Coastal Plain

\<@33\>\<i\>*Landform:*\<p\> Uplands

\<@33\>\<i\>*Landform position:*\<p\> Broad ridges; side slopes

\<@33\>\<i\>*Slope:*\<p\> 0 to 15 percent

\<@33\>\<i\>*Taxonomic class:*\<p\> Fine-loamy, kaolinitic, thermic
Rhodic Kandiudults

\<@27\>Commonly Associated Soils

\<@30\>Benevolence, Faceville, Greenville, Norfolk, and Orangeburg soils
are commonly associated with the Red Bay series.

-   \<@49\>The Benevolence soils are in positions similar to those of
    the Red Bay soils or slightly lower, have hues that are more yellow,
    and have a coarse-loamy control section.

-   \<@29\>The Faceville soils are in positions similar to those of the
    Red Bay soils, have hues that are more yellow, and have a fine
    control section.

-   \<@29\>The Greenville soils are in positions similar to those of the
    Red Bay soils or slightly higher and have a fine control section.

-   \<@29\>The Norfolk soils are in the slightly lower positions and
    have hues that are more yellow.

-   \<@29\>The Orangeburg soils are in positions similar to those of the
    Red Bay soils or slightly lower and have hues that are more yellow.

\<@27\>Typical Pedon

\<@30\>Red Bay loamy sand, 2 to 5 percent slopes; about 0.3 mile east of
the intersection of Benevolence Road and County Road 105 and 200 feet
south of the county road; Randolph County, Georgia; USGS Benevolence
topographic quadrangle; lat. 31 degrees 51 minutes 4 seconds N. and
long. 84 degrees 44 minutes 49 seconds W., NAD27.

\<@23\>Ap---0 to 8 inches; dark reddish brown (2.5YR 3/3) loamy sand;
weak fine granular structure; very friable; common fine roots; slightly
acid; clear smooth boundary.

\<@33\>Bt1---8 to 40 inches; dark red (2.5YR 3/6) sandy loam; weak
medium subangular blocky structure; friable; few fine roots; sand grains
coated and bridged with clay; moderately acid; gradual smooth boundary.

\<@33\>Bt2---40 to 80 inches; dark red (10R 3/6) sandy clay loam;
moderate medium subangular blocky structure; friable; common faint clay
films on faces of peds; strongly acid.

\<@27\>Range in Characteristics

\<@33\>\<i\>*Thickness of the solum:*\<p\> More than 60 inches

\<@33\>\<i\>*Reaction:*\<p\> Very strongly acid to moderately acid in
the upper part of the solum and very strongly acid or strongly acid in
the lower part, except where the surface layer has been limed

\<@23\>\<i\>*A or Ap horizon:*\<p\>

\<@31\>Color---hue of 2.5YR or 5YR, value of 3 or 4, and chroma of 2 to
4

\<@31\>Texture---loamy sand or sandy loam

\<@23\>\<i\>*BA horizon (where present):*\<p\>

\<@31\>Color---hue of 10R to 5YR, value of 3 or 4, and chroma of 4 to 6

\<@31\>Texture---sandy loam or sandy clay loam

\<@31\>Other features---The horizon is less than 10 inches thick.

\<@23\>\<i\>*Bt horizon:*\<p\>

\<@31\>Color---hue of 10R or 2.5YR, value of 3, and chroma of 4 to 6

\<@31\>Texture---sandy loam or sandy clay loam

\<@37\>Troup Series

\<@33\>\<i\>*Depth class:*\<p\> Very deep

\<@33\>\<i\>*Drainage class:*\<p\> Somewhat excessively drained

\<@33\>\<i\>*Permeability:*\<p\> Moderate

\<@33\>\<i\>*Parent material:*\<p\> Sandy and loamy marine sediments

\<@33\>\<i\>*Landscape:*\<p\> Coastal Plain

\<@33\>\<i\>*Landform:*\<p\> Uplands

\<@33\>\<i\>*Landform position:*\<p\> Ridges and side slopes

\<@33\>\<i\>*Slope:*\<p\> 0 to 15 percent

\<@33\>\<i\>*Taxonomic class:*\<p\> Loamy, kaolinitic, thermic
Grossarenic Kandiudults

\<@27\>Commonly Associated Soils

\<@30\>Ailey, Bibb, Benevolence, Bonneau, Cowarts, Kinston, Lakeland,
Lucy, and Orangeburg soils are commonly associated with the Troup
series.

-   \<@49\>The Ailey soils are in the slightly lower positions, are well
    drained, and have sandy surface and subsurface layers with a
    combined thickness of 20 to 40 inches over a dense, brittle subsoil.

-   \<@29\>The Bibb and Kinston soils are on flood plains and are poorly
    drained.

-   \<@29\>The Benevolence soils are in the slightly lower positions,
    are well drained, and do not have thick, sandy surface and
    subsurface layers.

-   \<@29\>The Bonneau soils are in the slightly lower positions, are
    well drained, and have sandy surface and subsurface layers with a
    combined thickness of 20 to 40 inches.

-   \<@29\>The Cowarts soils are in the lower positions, are well
    drained, and do not have thick, sandy surface and subsurface layers.

-   \<@29\>The Lakeland soils are in positions similar to those of the
    Troup soils, are excessively drained, and are sandy throughout.

-   \<@29\>The Lucy soils are in positions similar to those of the Troup
    soils or slightly lower, are well drained, and have sandy surface
    and subsurface layers with a combined thickness of 20 to 40 inches.

-   \<@29\>The Orangeburg soils are in positions similar to those of the
    Troup soils or slightly lower, are well drained, and do not have
    thick, sandy surface and subsurface layers.

\<@27\>Typical Pedon

\<@30\>Troup loamy sand, 0 to 5 percent slopes; about 0.5 mile north of
Ichawaynochaway Creek on Georgia Highway 41 and 500 feet west in a
field; Randolph County, Georgia; USGS Benevolence topographic
quadrangle; lat. 31 degrees 53 minutes 55 seconds N. and long. 84
degrees 38 minutes 32 seconds W., NAD27.

\<@23\>Ap---0 to 9 inches; brown (7.5YR 4/3) loamy sand; weak fine
granular structure; very friable; few fine roots; slightly acid; clear
smooth boundary.

\<@33\>E1---9 to 50 inches; strong brown (7.5YR 5/6) loamy sand; weak
fine granular structure; very friable; few fine roots; moderately acid;
gradual smooth boundary.

\<@33\>E2---50 to 60 inches; yellowish red (5YR 5/6) loamy sand; weak
fine granular structure; very friable; strongly acid; gradual smooth
boundary.

\<@33\>Bt---60 to 80 inches; red (2.5YR 4/8) sandy loam; weak medium
subangular blocky structure; friable; very strongly acid.

\<@27\>Range in Characteristics

\<@33\>\<i\>*Thickness of the solum:*\<p\> More than 80 inches

\<@33\>\<i\>*Thickness of the sandy epipedon:*\<p\> 40 to 80 inches

\<@33\>\<i\>*Reaction:*\<p\> Very strongly acid or strongly acid
throughout, except where the surface layer has been limed

\<@23\>\<i\>*A or Ap horizon:*\<p\>

\<@31\>Color---hue of 7.5YR or 10YR, value of 3 to 6, and chroma of 2 to
4

\<@31\>Texture---sand or loamy sand

\<@23\>\<i\>*E horizon:*\<p\>

\<@31\>Color---hue of 5YR to 10YR, value of 5 to 7, and chroma of 4 to 8

\<@31\>Texture---sand or loamy sand

\<@23\>\<i\>*Bt horizon:*\<p\>

\<@31\>Color---hue of 10R to 5YR, value of 4 to 7, and chroma of 4 to 8

\<@31\>Texture---sandy loam or sandy clay loam

\<@37\>Wahee Series

\<@33\>\<i\>*Depth class:*\<p\> Very deep

\<@33\>\<i\>*Drainage class:*\<p\> Somewhat poorly drained

\<@33\>\<i\>*Permeability:*\<p\> Slow

\<@33\>\<i\>*Parent material:*\<p\> Clayey marine or fluvial sediments

\<@33\>\<i\>*Landscape:*\<p\> Coastal Plain

\<@33\>\<i\>*Landform:*\<p\> River terraces

\<@33\>\<i\>*Landform position:*\<p\> Shallow depressions

\<@33\>\<i\>*Slope:*\<p\> 0 to 2 percent

\<@33\>\<i\>*Taxonomic class:*\<p\> Fine, mixed, semiactive, thermic
Aeric Endoaquults

\<@27\>Commonly Associated Soils

\<@30\>Kolomoki and Meggett soils are commonly associated with the Wahee
series.

-   \<@49\>The Kolomoki soils are in the higher positions on terraces
    and are well drained.

-   \<@29\>The Meggett soils are in the lower positions and are poorly
    drained.

\<@27\>Typical Pedon

\<@30\>Wahee fine sandy loam, 0 to 2 percent slopes, rarely flooded; in
a cultivated field about 0.5 mile south on Georgia Highway 39 from the
intersection of Georgia Highway 39 and Georgia Highway 37 and 0.65 mile
southwest on a dirt road; Clay County, Georgia; USGS Fort Gaines
topographic quadrangle; lat. 31 degrees 35 minutes 23 seconds N. and
long. 85 degrees 3 minutes 9 second W., NAD27.

\<@23\>Ap---0 to 5 inches; gray (10YR 5/1) fine sandy loam; weak fine
granular structure; very friable; common fine roots; moderately acid;
abrupt smooth boundary.

\<@33\>E---5 to 18 inches; pale brown (10YR 6/3) fine sandy loam;
moderate medium granular structure; very friable; common fine roots;
moderately acid; clear smooth boundary.

\<@33\>Bt---18 to 24 inches; pale brown (10YR 6/3) sandy clay; moderate
medium subangular blocky structure; friable; few fine roots; few faint
clay films on faces of peds; common fine distinct yellowish brown (10YR
5/8) masses in which iron has accumulated and many distinct medium light
brownish gray (10YR 6/2) areas from which iron has depleted; strongly
acid; gradual wavy boundary.

\<@33\>Btg1---24 to 32 inches; grayish brown (10YR 5/2) sandy clay;
moderate medium subangular blocky structure; firm; few fine roots; few
faint clay films on faces of peds; common medium distinct yellowish
brown (10YR 5/8) and red (2.5YR 4/8) masses in which iron has
accumulated; strongly acid; gradual wavy boundary.

\<@33\>Btg2---32 to 72 inches; grayish brown (10YR 5/2) sandy clay;
moderate medium subangular blocky structure; firm; few faint clay films
on faces of peds; common fine distinct yellowish brown (10YR 5/8) masses
in which iron has accumulated; strongly acid.

\<@27\>Range in Characteristics

\<@33\>\<i\>*Thickness of the solum:*\<p\> 30 to more than 60 inches

\<@33\>\<i\>*Reaction:*\<p\> Very strongly acid to moderately acid in
the A and E horizons and extremely acid to strongly acid in the B and C
horizons, except where the surface layer has been limed

\<@23\>\<i\>*A or Ap horizon:*\<p\>

\<@31\>Color---hue of 10YR or 2.5Y, value of 2 to 5, and chroma of 3 or
less; or neutral in hue and value of 2 to 5

\<@31\>Texture---sandy loam or fine sandy loam

\<@23\>\<i\>*E horizon (where present):*\<p\>

\<@31\>Color---hue of 10YR to 5Y, value of 5 to 7, and chroma of 2 to 4

\<@31\>Texture---sandy loam or fine sandy loam

\<@23\>\<i\>*Bt horizon:*\<p\>

\<@31\>Color---hue of 10YR to 5Y, value of 5 to 7, and chroma of 3 to 8

\<@31\>Texture---sandy clay loam, sandy clay, clay loam, or clay

\<@31\>Redoximorphic features---few to many iron masses in shades of
red, yellow, or brown and iron depletions in shades of gray

\<@23\>\<i\>*Btg horizon:*\<p\>

\<@31\>Color---hue of 10YR to 5Y, value of 5 to 7, and chroma of 2 or
less; or neutral in hue and value of 5 to 7

\<@31\>Texture---sandy clay, clay loam, or clay

\<@31\>Redoximorphic features---few to many iron masses in shades of
red, yellow, or brown and iron depletions in shades of gray, olive, or
white

\<@23\>\<i\>*Cg horizon (where present):*\<p\>

\<@31\>Color---hue of 10YR to 5Y, value of 5 to 7, and chroma of 1 or 2

\<@31\>Texture---variable from sandy loam to clay

\<@31\>Redoximorphic features---few to many iron masses in shades of
red, yellow, or brown and iron depletions in shades of gray, olive, or
white