LOCATION BLANEY             SC+GA NC
Established Series
Rev. JAK
12/2005

BLANEY SERIES


MLRA(s): 133A-Southern Coastal Plain, 137-Carolina and Georgia Sand Hills
MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Raleigh, North Carolina
Depth Class: Very deep
Drainage Class (Agricultural): Well drained
Internal Free Water Occurrence: Very deep
Flooding Frequency and Duration: None
Ponding Frequency and Duration: None
Index Surface Runoff: Negligible to high
Permeability: Moderately slow (Saturated Hydraulic Conductivity: Moderately high
Shrink-swell Potential: Low
Landscape: Upper coastal plain, sandhills
Landform: Marine terrace, hills, flats
Geomorphic Component: Treads, risers, interfluves, side slopes, talfs
Hillslope Profile Position: Summit, shoulder, backslope
Parent Material: Marine deposits, fluviomarine deposits
Slope: 0 to 25 percent
Elevation (type location): Unknown
Frost Free Period (type location): 217 days
Mean Annual Air Temperature (type location): 64 degrees F.
Mean Annual Precipitation (type location): 44 inches

TAXONOMIC CLASS: Loamy, siliceous, semiactive, thermic Arenic Hapludults

TYPICAL PEDON: Blaney sand--forested (Colors are for moist soil, unless otherwise indicated.)

A--0 to 3 inches; very dark gray (10YR 3/1) sand, dark grayish brown (10YR 4/2) dry; weak fine granular structure; very friable; many fine and medium roots; very strongly acid; abrupt smooth boundary. (0 to 5 inches thick)

E1--3 to 9 inches; dark grayish brown (2.5Y 4/2) sand; single grain; loose; many fine roots; mostly uncoated sand grains; very strongly acid; clear smooth boundary.

E2--9 to 25 inches; pale brown (10YR 6/3) sand; single grain; loose; many fine roots; mostly uncoated sand grains; very strongly acid; clear smooth boundary. (Combined thickness of the E horizon is 15 to 39 inches.)

Bt1--25 to 38 inches; light brown (7.5YR 6/4) sandy clay loam; weak medium subangular blocky structure; friable; brittle in 20 percent of the mass, dense and compact; many medium and fine pores; few faint clay films on faces of peds; few medium faint very pale brown (10YR 7/4) iron depletions; strongly acid; gradual wavy boundary.

Bt2--38 to 50 inches; light brown (7.5YR 6/4) sandy clay loam; weak medium subangular blocky structure; hard and compact; friable; brittle in 20 percent of the mass; common faint clay films on faces of peds; common coarse distinct reddish yellow (7.5YR 7/6) masses of oxidized iron; strongly acid; gradual wavy boundary. (Combined thickness of the Bt horizon is 10 to 40 inches.)

BCt--50 to 65 inches; reddish brown (7.5YR 6/6) sandy loam; weak medium subangular blocky structure; friable; brittle in 15 percent of the mass, dense and compact; many clay bridging between sand grains; strongly acid.

TYPE LOCATION: Lexington County, South Carolina; about 20 feet south of Dogwood Road; 300 feet west of Fish Hatchery Road, and 2.6 miles southwest of U.S. Highway 21.

RANGE IN CHARACTERISTICS:
Thickness of the sandy surface and subsurface horizons: 20 to 39 inches
Depth to top of argillic horizon: 20 to 39 inches
Depth to base of argillic horizon: 40 to 60 inches or more
Depth to bedrock: Greater than 80 inches
Depth to seasonal high water table: Greater than 72 inches (Water may be perched above the dense, compact layer for brief periods after heavy rains.)
Depth to lithologic discontinuity (abrupt textural change): Greater than 60 inches
Depth to fragic soil properties: 20 to 39 inches
Fragic soil properties content: 10 to 30 percent, by volume in the B horizon
Rock fragment content: 0 to 10 percent, by volume throughout; mostly quartz pebbles
Soil Reaction: Extremely acid to strongly acid throughout, unless limed

RANGE OF INDIVIDUAL HORIZONS:
A horizon or Ap horizon (where present):
Color--hue of 10YR or 2.5Y, value of 2 to 6, chroma of 1 or 2, or is neutral with value of 2 to 4. Where the value is less than 3.5, the A horizon is less than 6 inches thick.
Texture--sand, coarse sand, loamy sand, or loamy coarse sand

E horizon
Color--hue of 10YR or 2.5Y, value of 4 to 6, chroma of 2 to 4
Texture--sand, coarse sand, loamy sand, or loamy coarse sand

BE or EB horizon (where present)
Color--hue of 7.5YR or 2.5Y, value of 4 to 6, chroma of 3 or 4
Texture--sandy loam or coarse sandy loam

Bt or Btx horizon:
Color--hue of 5YR to 10YR, value of 5 to 7, chroma of 3 to 8
Texture--sandy clay loam or sandy loam, ranging to sandy clay in the lower part
Redoximorphic features (where present)--masses of oxidized iron in shades of red, brown, or yellow

BCt or BC horizon:
Color--hue of 5YR to 10YR, value of 5 to 7, chroma of 3 to 8
Texture--sandy loam or sandy clay loam
Redoximorphic features (where present)--masses of oxidized iron in shades of red, brown, or yellow

C horizon (where present):
Color--hue of 5YR to 10YR, value of 4 to 8, chroma of 3 to 8
Texture--sandy loam or sandy clay loam
Redoximorphic features (where present)--masses of oxidized iron in shades of red, brown, or yellow and iron depletions in shades of brown, yellow, or gray

2C horizon (where present:
Texture--sand coarse sand, loamy coarse sand, or loamy sand
Redoximorphic features (where present)--masses of oxidized iron in shades of red, brown, or yellow and iron depletions in shades of brown, yellow, or gray

COMPETING SERIES:
(Semiactive Family)
Baymeade soils--do not have a dense, compact subsoil and have a seasonal high water table at a depth of 48 to 60 inches
Chisolm soils--do not have a dense, compact subsoil and have a seasonal high water table at a depth of 36 to 60 inches
Gomery soils--formed in residuum from sandstone and have paralithic materials at a depth of 40 to 60 inches
Tenaha soils--formed in residuum from sandstone and shale
Valhalla soils--have underlying spodic horizons
(Subactive Family)
Remlik soils--do not have a dense, compact subsoil
Kenansville soils--do not have a dense, compact subsoil

GEOGRAPHIC SETTING:
Landscape: Upper coastal plain, sandhills
Landform: Marine terrace, hills
Geomorphic Component: Treads, risers, interfluves, side slopes, talfs
Hillslope Profile Position: Summit, shoulder, backslope
Parent Material: Marine deposits, fluviomarine deposits
Slope: 0 to 25 percent
Elevation: 250 to 450 feet
Frost Free Period: 190 to 245 days
Mean Annual Air Temperature: 57 to 70 degrees F.
Mean Annual Precipitation: 40 to 50 inches

GEOGRAPHICALLY ASSOCIATED SOILS:
Ailey soils--are underlain by densic materials
Blanton soils--have a sandy surface and subsurface layers more than 40 inches thick
Gilead soils--are fine-textured
Lakeland soils--are sandy throughout
Pelion soils--have sandy surface and subsurface layers less than 20 inches thick
Troup soils--have a sandy surface and subsurface layers more than 40 inches thick
Vaucluse soils--have sandy surface and subsurface layers less than 20 inches thick

DRAINAGE AND PERMEABILITY:
Depth Class: Very deep
Drainage Class (Agricultural): Well drained
Internal Free Water Occurrence: Very deep
Flooding Frequency and Duration: None
Ponding Frequency and Duration: None
Index Surface Runoff: Negligible to high
Permeability: Moderately slow (Saturated Hydraulic Conductivity: Moderately high
Shrink-swell Potential: Low

USE AND VEGETATION:
Major Uses: Cropland, woodland
Dominant vegetation: Where cultivated--corn, small grains, soybeans, or pasture. Where wooded--loblolly pine, longleaf pine, or slash pine.

DISTRIBUTION AND EXTENT:
Distribution: South Carolina, Georgia, and North Carolina.
Extent: Moderate

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

SERIES ESTABLISHED: Scotland County, North Carolina; 1965

REMARKS: Additional investigation of the Blaney soils are needed to better define the amount of fragic soil properties and the degree of clay activity. Blaney soils were initially established as Arenic Fragiudults and were reclassified (1979) to Arenic Hapludults. With 10 to 20 percent brittleness and friable moist consistence (Bt horizon of the type location) the 2005 series revision limited the range of the series to 10 to 30 percent brittleness to eliminate any potential conflict with Fragic Hapludults (30 to 60 percent fragic soil properties). The series range in characteristics of the B was modified to allow the x suffix designation to be used with the series where pedogenic brittleness, firmness, and root-restrictive character is observed in less than 30 percent of the mass. Diagnostic horizons and soil characteristics recognized in this pedon:
Ochric epipedon--the zone from 0 to 25 inches (A, E1, E2 horizons)
Albic horizon (materials)--the zone from 3 to 25 inches (E1, E2 horizons)
Argillic horizon--the zone from 25 to 65 inches (Bt, BCt horizons)
Fragic soil properties--the zone from 25 to 65 inches (Bt1, Bt2, Btx horizons)
Series control section--the zone from 0 to more than 65 inches

ADDITIONAL DATA:
Laboratory Data: No laboratory data available.

TABULAR SERIES DATA:

SOI-5   Soil Name   Slope  Airtemp  FrFr/Seas  Precip  Elevation
SC0063  BLANEY      0-25   57-70    190-245    40-50   250-450

SOI-5 FloodL FloodH Watertable Kind Months Bedrock Hardness SC0063 NONE >6.0 - - >80 -

SOI-5 Depth Texture 3-Inch No-10 Clay% -CEC- SC0063 0-25 S LS 0-0 95-100 2-10 0.5-1.5 SC0063 0-25 COS LCOS 0-0 92-100 2-10 0.5-1.5 SC0063 25-50 SCL SL 0-0 90-100 18-35 0.5-2.0 SC0063 50-65 SL SCL LS 0-0 90-100 10-25 0.5-2.0

SOI-5 Depth -pH- O.M. Salin Permeab Shnk-Swll SC0063 0-25 3.5-5.5 0.5-1.0 0-0 6.0-20 LOW SC0063 0-25 3.5-5.5 0.5-1.0 0-0 20-20 LOW SC0063 25-50 3.5-5.5 0.0-0.01 0-0 0.2-0.6 LOW SC0063 50-65 3.5-5.5 0.0-0.01 0-0 0.2-0.6 LOW


National Cooperative Soil Survey
U.S.A.