LOCATION BILLARD            KS
Tentative Series
SAG, BCE
09/2006

BILLARD SERIES


The Billard series consists of very deep, well drained soils that formed in alluvium on flood plains. Permeability is rapid. Slopes range from 1 to 4 percent. Mean annual precipitation is about 36 inches and the mean annual temperature is about 55 degrees F.

TAXONOMIC CLASS: Coarse-loamy, mixed, superactive, mesic Cumulic Hapludolls

TYPICAL PEDON: Billard sandy loam , 1 to 4 percent slope. (Colors are for moist soil unless otherwise noted.)

Ap--0 to 6 inches; dark brown (10YR 3/3) sandy loam, brown (10YR 5/3) dry; weak fine granular structure; soft, friable, slightly sticky and slightly plastic; neutral abrupt smooth boundary.

A--6 to 11 inches; dark brown (10YR 3/3) sandy loam, brown (10YR 5/3) dry; weak fine subangular blocky structure; soft, friable, slightly sticky and slightly plastic; neutral; clear smooth boundary.. (10 to 20 inches thick)

Bw1--11 to 16 inches; dark brown (10YR 3/3) sandy loam, brown (10YR 5/3) dry; weak fine and medium subangular blocky structure; soft, friable, slightly sticky and slightly plastic; slightly acid; clear smooth boundary

Bw2--16 to 31 inches; brown (10YR 4/3) sandy loam, pale brown (10YR 6/3) dry; weak medium subangular blocky structure; soft, friable, slightly sticky and slightly plastic; slightly acid; clear smooth boundary. . (10 to 30 inches thick)

BC--31 to 51 inches; brown (10YR 5/3) loamy sand, very pale brown (10YR 7/3) dry; weak coarse subangular blocky structure; soft, friable, slightly sticky and slightly plastic; slightly acid; clear smooth boundary. (3 to 10 inches thick)

Ab--51 to 71 inches; very dark brown (10YR 2/2) loam, dark grayish brown (10YR 4/2) dry; moderate fine subangular blocky structure; slightly hard, friable, moderately sticky and moderately plastic; slightly acid.

TYPE LOCATION: Shawnee County, Kansas; about .5 mile north and .5 mile east of Silverlake; located about 1200 feet north and 1950 feet east of the northwest corner of sec. 10, T. 11 S., R. 14 E.; USGS Silverlake topographic quad; lat. 39 degrees 6 minutes 49 seconds N. and long. 95 degrees 50 minutes 42 seconds W.

RANGE IN CHARACTERISTICS:
Mean annual soil temperature: 52 to 57 degrees F
Mean summer soil temperature: 72 to 77 degrees F
Depth to cambic horizon: 10 to 15 inches
Depth to redox concentrations: 40 to 60 inches
Particle-size control section (weighted average): 5 to 18 percent
Clay content: 5 to 18 percent
Sand content: 10 to 50 percent

A horizon:
Hue: 10YR
Value: 2 or 3 moist; 4 or 5 dry
Chroma: 2 or 3
Texture: sandy loam, fine sandy loam, loamy sand, loam
Clay content: 10 to 18 percent
Reaction: 5.1 to 7.3

Bw horizon:
Hue: 10YR
Value: 3 or 4 moist; 4 to 6 dry
Chroma: 2 to 4
Texture: sandy loam, fine sandy loam, loam
Clay content: 10 to 18 percent
Reaction: 5.1 to 7.8

BC horizon:
Hue: 10YR
Value: 4 or 5 moist; 5 to 7 dry
Chroma: 2 to 4
Texture: sandy loam, loamy sand; loam, fine sandy loam
Clay content: 5 to 18 percent
Reaction: 5.1 to 7.8

Ab horizon:
Hue: 10YR
Value: 2 or 3 moist; 4 or 5 dry
Chroma: 1 to 3
Texture: loam, clay loam
Clay content: 10 to 27 percent
Reaction: 5.6 to 8.4

COMPETING SERIES: There are no competing series.

GEOGRAPHIC SETTING:
Parent material: coarse loamy material derived from colluvium
Landform: alluvial fans and footslopes
Slopes: 1 to 4 percent
Mean annual temperature: 52 to 57 degrees F
Mean annual precipitation: 34 to 40 inches
Frost-free period: 170 to 190 days.

GEOGRAPHICALLY ASSOCIATED SOILS: These are the Gymer, Konawa, Menoken(T), Morrill, Olmitz, Pawnee, Shelby series. The Gymer soils are red and occur on terraces. The Konawa soils are red and have a sandier surface. The Morrill soils formed in glacio-fluvial outwash and sit higher on the landscape. The Olmitz soils are fine-loamy and are on similar positions on the landscape. The Pawnee soils formed in clay till and are on higher positions on the landscape. The Shelby soils formed in fine-loamy till and are on higher positions on the landscape. The Menoken (T) soils are sandy and sit somewhat higher on the landscape.

DRAINAGE AND PERMEABILITY: Well drained. Surface runoff is low. Permeability is moderate.

USE AND VEGETATION: Native vegetation are woods and grasses. Now the soils are mainly cropped to corn, small grains, and soybeans.

DISTRIBUTION AND EXTENT: Northeastern Kansas, MLRA 106, Kansas River subset; Very limited extent.

MLRA OFFICE RESPONSIBLE: Salina, Kansas

SERIES PROPOSED: Shawnee County, Kansas, MLRA 106 soil survey area.

REMARKS: These soils were formerly mapped as Eudora sandy loam, sandy variant in Shawnee County, Kansas. Pedon used is 95KS177175. Lab data was run at the Kansas State University Pedology Laboratory in Manhattan, Kansas. Lab samples were SS958-963.
Diagnostic horizons and features recognized in this pedon are: mollic epipedon - the zone from the surface to a depth of 16 inches (Ap, A, Bw1 horizons); cambic horizon - the zone from 11 to 31 inches (Bw1, Bw2 horizons); Udic moisture regime-
Particle-size control section: The zone from 10 to 40 inches. ( A, Bw1, Bw2, BC horizons)
Mollic epipedon: The zone from 20 to 30 inches. (Ap, A horizons)
Cambic horizon: The zone from10 to 30 inches. (Bw1, Bw2 horizons)


National Cooperative Soil Survey
U.S.A.