LOCATION COBB               TX+OK
Established Series
Rev. RFG-CRC-ACT-CLN-WJG
02/2007

COBB SERIES


The Cobb series consists of moderately deep, well drained, moderately permeable soils that formed in residuum derived from sandstone. These nearly level to moderately sloping soils are on ridges. Slope ranges from 0 to 8 percent. Mean annual temperature is about 63 degrees F., and mean annual precipitation is about 23 inches.

TAXONOMIC CLASS: Fine-loamy, mixed, active, thermic Typic Haplustalfs

TYPICAL PEDON: Cobb fine sandy loam, in a cultivated field. (Colors are for dry soil unless otherwise stated.)

Ap--0 to 8 inches; reddish brown (5YR 4/3) fine sandy loam, dark reddish brown (5YR 3/3) moist; weak fine subangular blocky structure; hard, very friable; few fine roots; slightly acid; gradual smooth boundary. (3 to 12 inches thick)

Bt1--8 to 22 inches; reddish brown (5YR 4/4) sandy clay loam, dark reddish brown (5YR 3/4) moist; weak coarse prismatic structure parting to weak medium subangular blocky; very hard, friable; few fine roots; few fine pores; slightly acid; clear wavy boundary. (8 to 18 inches thick)

Bt2--22 to 30 inches; reddish brown (5YR 5/4) sandy clay loam, reddish brown (5YR 4/4) moist; weak coarse prismatic structure parting to weak medium subangular blocky; very hard, friable; neutral; abrupt irregular boundary. (6 to 18 inches thick)

Cr--30 to 60 inches; weakly cemented reddish sandstone with common distinct coatings of calcium carbonate in the fissures or crevices; neutral.

TYPE LOCATION: Foard County, Texas; from the intersection of Texas Highway 6 and U.S. Highway 70 in Crowell; 1.5 miles west on U.S. Highway 70; 0.3 mile north on county road; 0.2 mile west in cropland. (Latitude: 33N, 59, 28; Longitude: 99W, 45, 15); ? topographic quadrangle; NAD 83.
RANGE IN CHARACTERISTICS:
Particle-size control section (weighted average)
Clay content: 18 to 35 percent
CEC/clay ratio: 0.4 to 0.6
Soil Moisture: A typic-ustic soil moisture regime.
Depth to paralithic contact: 20 to 40 inches
Thickness of the solum, 20 to 40 inches
Base saturation ranges from 75 to 100 percent throughout the argillic horizon.
A Horizon
Hue: 5YR or 7.5YR
Value: 4 to 6 (3 to 5 moist)
Chroma: 4 to 6 (3 to 5 moist)
Texture: Fine sandy loam or loamy fine sand
Clay content: 6 to 18 percent
EC (dS/m): 0 to 2
Effervescence: Noneffervescent
Reaction: Slightly acid or neutral
Bt Horizon
Hue: 2.5YR or 5YR
Value: 4 to 6 (3 to 5 moist)
Chroma: 4 or 6
Texture: Typically sandy clay loam or clay loam, but includes fine sandy loam in the lower part.
Clay content: 18 to 35 percent
Coarse fragments: Sandstone fragments less than 3 inches in diameter ranges from 0 to 10 percent
Base saturation: 75 to 100 percent
Calcium carbonate equivalent: 0 to 5 percent
EC (dS/m): 0 to 2
Effervescence: Noneffervescent to slightly effervescent
Reaction: Slightly acid to moderately alkaline
BC Horizon (where present)
Hue: 2.5YR or 5YR
Value: 4 to 6 (3 to 5 moist)
Chroma: 4 or 6
Texture: Fine sandy loam, sandy clay loam, or clay loam
Clay content: 10 to 35 percent
Coarse fragments: Sandstone fragments less than 3 inches in diameter ranges from 0 to 10 percent
Calcium carbonate equivalent: 0 to 5 percent
EC (dS/m): 0 to 2
Effervescence: Noneffervescent to slightly effervescent
Reaction: Slightly acid to moderately alkaline
Cr Horizon
Hue: 2.5YR to 10YR
Value: 4 or 5 (3 or 4 moist)
Chroma: 2 to 6
Texture: Extremely weakly to moderately cemented sandstone bedrock
Moist bulk density (g/cc): 1.85 to 2.35
Excavation difficulty: Moderate to high
Identifiable secondary carbonate: Thin coatings of calcium carbonate are in fissures or crevices of most pedons.
Effervescence: Noneffervescent to slightly effervescent
Reaction: Slightly acid to moderately alkaline
COMPETING SERIES: These are the Arnett, Decobb, Grandfield, Grandmore, Honeycreek, Hye, Lou, McKnight, Menard, and Rochelle series.
Arnett, Decobb, Grandfield, and Grandmore series: These soils have solum more than 60 inches thick.
Honeycreek series: These soils are 40 to 60 inches to schist bedrock.
Hye series: These soils have base saturation between 40 and 75 percent in the argillic horizon.
Lou series: These soils have granite bedrock in the upper 10 inches of the paralithic contact.
McKnight series: These soils have a lithologic discontinuity between 20 and 40 inches and depth to bedrock is 40 to 60 inches.
Menard and Rochelle series: These soils have solum more than 60 inches to bedrock. In addition, Rochelle soils have a very gravelly substratum.
GEOGRAPHIC SETTING:
Parent material: Residuum derived from sandstone, mainly of the San Angelo Formation of Permian age.
Landform: Convex ridges and side slopes of ridges.
Slope: 0 to 8 percent
Mean annual air temperature range: 60 to 64 degrees F.
Mean annual precipitation range: 22 to 28 inches
Frost-free period: 200 to 230 days
Elevation: 1000 to 2200 feet
Thornthwaite annual P-E indices: 32 to 44
GEOGRAPHICALLY ASSOCIATED SOILS: These are the Abilene, Bluegrove, Cosh, Decobb, Grandfield, Miles, Rochelle, Spade, Spikebox, Tillman, Tilvern, Vernon, and Westill series.
Abilene series: These soils have a mollic epipedon and are on lower alluvial or footslope positions.
Cosh and Spikebox series: These soils are shallow to sandstone bedrock and are on slightly convex positions higher in the landscape.
Decobb series: These soils are very deep to sandstone and are slightly lower in the landscape.
Grandfield and Miles series: These soils are on slightly lower positions and have developed in loamy, Pleistocene age alluvial sediments.
Rochelle series: These soils are on stream terraces and have gravelly substratum.
Spade series: These soils are in similar positions on the landscape, have a cambic horizon, and are calcareous to the surface.
Tillman and Westill series: These soils have a mollic epipedon, are on slightly lower positions and have developed in red alluvium.
Bluegrove, Tilvern and Vernon series: These soils occupy similar to slightly lower landscape positions and have a fine particle-size control section.
DRAINAGE AND PERMEABILITY: Well drained. Permeability is moderate. Runoff is negligible on slopes less than 1 percent, low on 1 to 5 percent slopes and medium on 5 to 8 percent slopes.
USE AND VEGETATION: Used mainly for rangeland. Native vegetation is mainly grasses such as sideoats grama, blue grama, little bluestem, dropseed, threeawn, Arizona cottontop, and buffalograss. Mesquite trees are the dominant woody plants. A small acreage is farmed. Grain sorghum, cotton, and wheat are the major crops.
DISTRIBUTION AND EXTENT: Central Rolling Red Plains of north and northwestern Texas and southwestern Oklahoma. LRR H; MLRA 78C; large extent
MLRA OFFICE RESPONSIBLE: Temple, Texas
SERIES ESTABLISHED: Washita County, Oklahoma; 1935.
REMARKS:
Diagnostic horizons and features recognized in this pedon are:
Ochric epipedon--0 to 8 inches (A horizon)
Argillic horizon--8 to 30 inches (Bt1 and Bt2 horizons)
Paralithic contact: The contact with 30 at inches. (Cr horizon)
Range Site: Sandy Loam Prairie PE 31-44 (078CY110TX).
Soil Interpretation Record Number: TX0125
Taxonomic version: Soil Taxonomy, Second Edition, 1999
ADDITIONAL DATA: NSSL characterization data from Young County, Texas; S92TX-503-005.


National Cooperative Soil Survey
U.S.A.