LOCATION WEDOWEE            AL+GA NC SC VA
Established Series
Rev. WBP:PGM:DTA
07/2007

WEDOWEE SERIES


The Wedowee series consists of very deep, well drained, moderately permeable soils that formed in residuum weathered from felsic igneous and metamorphic rocks of the Piedmont uplands. These soils are on narrow ridges and on side slopes of uplands. Slope is dominantly between 6 and 25 percent but ranges from 0 to 60 percent. Near the type location, the average annual temperature is about 63 degrees F. and average annual precipitation is about 53 inches.

TAXONOMIC CLASS: Fine, kaolinitic, thermic Typic Kanhapludults

TYPICAL PEDON: Wedowee sandy loam, in a field. (Colors are for moist soil.)

A--0 to 4 inches; dark grayish brown (10YR 4/2) sandy loam; moderate fine granular structure; very friable; strongly acid; abrupt smooth boundary. (1 to 8 inches thick)

E--4 to 7 inches; brownish yellow (10YR 6/6) coarse sandy loam; weak fine granular structure; very friable; very strongly acid; clear smooth boundary. (0 to 6 inches thick)

Bt--7 to 23 inches; strong brown (7.5YR 5/6) clay; few fine distinct brownish yellow (10YR 6/6) and red (2.5YR 4/6) mottles; moderate medium subangular blocky structure; firm; slightly sticky, slightly plastic; few faint clay films on faces of peds; very strongly acid; gradual wavy boundary. (10 to 24 inches thick)

BC--23 to 35 inches; strong brown (7.5YR 5/6) clay loam; many fine distinct red (2.5YR 4/6) and common fine distinct brownish yellow (10YR 6/6) mottles; weak medium subangular blocky structure; friable; slightly sticky, nonplastic; very strongly acid; gradual wavy boundary. (0 to 12 inches thick)

C--35 to 80 inches; mottled strong brown (7.5YR 5/6), brownish yellow (10YR 6/6), yellowish red (5YR 5/8), and white (10YR 8/1) sandy clay loam saprolite; massive; very friable; very strongly acid.

TYPE LOCATION: Granville County, North Carolina; about 2.5 miles east of Wilton on North Carolina Highway 56, about 1.5 miles northeast on Secondary Road 1625, about 1,000 feet north of the intersection with Secondary Road 1628, in a field; Wilton USGS topographic quadrangle; lat. 36 degrees 08 minutes 33 seconds N. and long. 78 degrees 31 minutes 18 secinds W.

RANGE IN CHARACTERISTICS: The Bt horizon is at least 10 to 24 inches thick and extends to a depth of 18 to 30 inches. Depth to rock is more than 60 inches. Reaction ranges from extremely acid to strongly acid throughout except where lime has been added. Flakes of mica range from none to few in the A horizon and the upper part of the B horizon and from none to common in the lower part of the B and C horizon.

The A horizon has hue of 7.5YR to 2.5Y, value of 3 to 6 and chroma of 2 to 8. It is coarse loamy sand, coarse sandy loam, sandy loam, fine sandy loam, loam; or their gravelly analogues. In eroded areas, the A horizon is sandy clay loam or clay loam ,or their gravelly analogues. Content of coarse fragments, dominantly gravel size, range from 0 to 35 percent by volume.

The E horizon has hue of 7.5YR to 2.5Y, value of 4 to 7, and chroma of 3 to 8. It is coarse loamy sand, coarse sandy loam, sandy loam, fine sandy loam, loam; or their gravelly analogues.

The BE horizon, where present, has hue of 5YR to 10YR, value of 4 to 7 and chroma of 3 to 8. It is loam, fine sandy loam, sandy loam, sandy clay loam or clay loam.

The Bt horizon has hue of 7.5YR or 10YR, value of 4 to 6 and chroma of 6 to 8, but includes hue of 5YR with the same range in value and chroma. Mottles in shades of brown, yellow, and red may be in some pedons. Texture of the Bt horizon is sandy clay loam, clay loam, sandy clay, or clay. Clay content of the particle-size control section averages 35 to 60 percent.

The BC horizon has hue of 2.5YR to 10YR, value of 5 to 7 and chroma of 4 to 8. Mottles in shades of red, brown, and yellow range from none to common. It is sandy clay loam, clay loam, loam, or fine sandy loam.

The C horizon is multicolored sandy clay loam, loam, fine sandy loam, or sandy loam saprolite.

COMPETING SERIES: These include the Appling, Bethlehem, Cecil, Georgeville, Herndon, Madison, Nanford, Nankin, Pacolet, Saw, and Tarrus series in the same family. Appling and Cecil soils have thicker Bt horizons. Additionally, Cecil soils have dominant hue of 5YR or redder throughout the Bt horizon. Bethlehem soils have a paralithic contact within 20 to 40 inches of the surface. Georgeville, Herndon, Nanford, and Tarrus soils formed from Carolina slate and have more than 30 percent silt. Madison soils have dominant hue of 5YR or redder in the Bt horizon and contain more mica. Nankin soils formed from marine sediments. Pacolet soils have Bt horizons with hue of 2.5YR or redder. Saw soils have a lithic contact within 20 to 40 inches of the surface.

GEOGRAPHIC SETTING: Wedowee soils are on sloping to steep uplands of the Southern Piedmont MLRA. Slopes are mainly 6 to 25 percent, but range from 0 to 60 percent. The soils have formed in residuum from weathered felsic igneous and metamorphic rocks. Near the type location, the mean annual precipitation ranges from 42 to 56 inches and the mean annual temperature ranges from 58 to 65 degrees F.

GEOGRAPHICALLY ASSOCIATED SOILS: In addition to the competing Appling, Bethlehem, Cecil, Madison, Pacolet, and Saw series, these are the Ashlar, Durham, Hard Labor, Helena, Lockhart, Louisburg, Rion, Rolesville, Vance, Wake, Wateree, and Worsham series. Ashlar soils are coarse-loamy and have a lithic contact within 20 to 40 inches. Durham soils are fine-loamy. Hard Labor soils have a perched water table at 2.5 to 5 feet. Helena and Vance soils have a mixed mineralogy and, in addition, Helena soils have a perched water table 1.5 to 2.5 feet. Lockhart soils have more than 35 percent rock fragments in the particle-size control section. Louisburg soils are coarse-loamy. Rion soils are fine-loamy. Rolesville soils are sandy throughout and have a lithic contact within 20 to 40 inches. Wake soils are sandy throughout and have a lithic contact within 20 inches. Wateree soils are coarse-loamy and have a paralthic contact within 20 to 40 inches. Worsham soils are poorly drained and are around the heads of drains.

DRAINAGE AND PERMEABILITY: Well drained. Runoff is medium to rapid and internal drainage is medium. Permeability is moderate.

USE AND VEGETATION: Most areas are wooded. Common trees include loblolly pine, Virginia pine, red oak, white oak, post oak, hickory, blackgum, maple, and dogwood. Cleared areas are used for cotton, corn, tobacco, small grain, hay, and pasture.

DISTRIBUTION AND EXTENT: The Piedmont of Alabama, Georgia, North Carolina, South Carolina and Virginia. The series is of moderate extent.

MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Raleigh, North Carolina

SERIES ESTABLISHED: Randolph County, Alabama; 1969.

REMARKS: Wedowee soils were formerly mapped as thin solum phases of the Appling series. The 5/90 revision changed the classification to Typic Kanhapludults in recognition of the low activity clay content of the argillic horizon. The December 2005 revision moved the type location from Randolph County, Alabama to a more representative site.

Revised: RLV 11/24/97; DTA 12/30/2005

Diagnostic horizons and features recognized in this pedon are:

Ochric epipedon - the zone from the surface of the soil to a depth of 7 inches (A and E horizons)
Argillic and kandic horizon - the zone from 7 to 23 inches (Bt horizon)

ADDITIONAL DATA:

TABULAR SERIES DATA:

SOI-5   Soil Name  Slope  Airtemp  FrFr/Seas  Precip  Elevation
AL0046  WEDOWEE    0-60   58-65    175-225    42-56   200-800
AL0138  WEDOWEE    0-60   58-65    175-225    42-56   200-800
AL0146  WEDOWEE    0-60   58-65    175-225    42-56   200-800 

SOI-5 FloodL FloodH Watertable Kind Months Bedrock Hardness AL0046 NONE >6.0 - >60 AL0138 NONE >6.0 - >60 AL0146 NONE >6.0 - >60

SOI-5 Depth Texture 3-Inch No-10 Clay% -CEC- AL0046 0-10 SL FSL L 0-0 80-100 5-20 2-8 AL0046 0-10 SCL CL 0-0 90-100 20-30 2-8 AL0046 10-14 L SCL 0-0 90-100 14-30 3-10 AL0046 14-32 SC CL C 0-0 95-100 35-60 3-10 AL0046 32-60 SCL CL SL 0-0 70-100 15-30 3-8

AL0138 0-10 BY-SL BY-L 10-20 70-90 5-20 2-8 AL0138 10-14 L SCL 0-5 90-100 14-30 3-10 AL0138 14-32 SC CL C 0-0 95-100 35-60 3-10 AL0138 32-60 SCL CL SL 0-0 70-100 15-30 3-8

AL0146 0-10 GR-SL GR-FSL GR-L 0-5 50-80 6-20 2-8 AL0146 0-10 GR-SCL GR-CL 0-5 50-80 20-30 2-8 AL0146 10-14 L SCL 0-0 90-100 14-30 3-10 AL0146 14-32 SC CL C 0-0 95-100 35-60 3-10 AL0146 32-60 SCL CL SL 0-0 70-100 15-30 3-8

SOI-5 Depth -pH- O.M. Salin Permeab Shnk-Swll AL0046 0-10 3.6- 5.5 .5-3. 0-0 2.0-6.0 LOW AL0046 0-10 3.6- 5.5 .5-3. 0-0 0.6-2.0 LOW AL0046 10-14 3.6- 5.5 0.-.5 0-0 0.6-2.0 LOW AL0046 14-32 3.6- 5.5 0.-.5 0-0 0.6-2.0 LOW AL0046 32-60 3.6- 5.5 0.-.5 0-0 0.6-2.0 LOW

AL0138 0-10 3.6- 5.5 0.-1. 0-0 2.0-6.0 LOW AL0138 10-14 3.6- 5.5 0.-.5 0-0 0.6-2.0 LOW AL0138 14-32 3.6- 5.5 0.-.5 0-0 0.6-2.0 LOW AL0138 32-60 3.6- 5.5 0.-.5 0-0 0.6-2.0 LOW

AL0146 0-10 3.6- 5.5 .5-3. 0-0 2.0-6.0 LOW AL0146 0-10 3.6- 5.5 .5-3. 0-0 0.6-2.0 LOW AL0146 10-14 3.6- 5.5 0.-.5 0-0 0.6-2.0 LOW AL0146 14-32 3.6- 5.5 0.-.5 0-0 0.6-2.0 LOW AL0146 32-60 3.6- 5.5 0.-.5 0-0 0.6-2.0 LOW


National Cooperative Soil Survey
U.S.A.