LOCATION BILLMAN            MT
Established Series
Rev. GAR-EWC-JAL
12/1999

BILLMAN SERIES


The Billman series consists of moderately deep, well drained soils that formed in interbedded shale and sandstone residuum. These soils are on sedimentary plains and hills. Slopes are 2 to 60 percent. Mean annual precipitation is about 20 inches and the mean annual temperature is about 39 degrees F.

TAXONOMIC CLASS: Fine, mixed, superactive, frigid Typic Argiustolls

TYPICAL PEDON: Billman clay loam, in hayland (Colors are for dry soil unless otherwise noted).

A--0 to 7 inches; dark grayish brown (10YR 4/2) clay loam, very dark brown (10YR 2/2) moist; moderate medium granular structure; slightly hard, firm, moderately sticky and moderately plastic; common very fine and fine roots; 5 percent pebbles; neutral (pH 7.0); clear wavy boundary. (6 to 10 inches thick)

Bt1--7 to 15 inches; brown (7.5YR 4/2) clay, dark brown (7.5YR 3/2) moist; moderate medium prismatic structure; very hard, firm, moderately sticky and moderately plastic; common fine and very fine roots, few medium roots; common distinct clay films on faces of peds and lining pores; 5 percent pebbles; neutral (pH 7.0); clear wavy boundary.

Bt2--15 to 23 inches; brown (7.5YR 5/2) clay, dark brown (7.5YR 4/2) moist; strong medium subangular blocky structure; very hard, firm, moderately sticky and moderately plastic; few fine and very fine roots; common distinct clay films on faces of peds and lining pores; 5 percent pebbles; neutral (pH 7.0); clear wavy boundary. (Combined thickness of Bt1 and Bt2 horizons is 14 to 30 inches).

Cr1--23 to 38 inches; brown (7.5YR 4/2) moist; semi-consolidated shale that textures to silty clay loam; neutral (pH 7.0).

Cr2--38 to 60 inches; dark gray (5YR 4/1) moist; semiconsolidated shale.

TYPE LOCATION: Gallatin County, Montana; 2200 feet north and 2200 feet west of the southeast corner of sec. 11, T.2S., R.6E.

RANGE IN CHARACTERISTICS:

Soil temperature - 39 to 43 degrees F.
Moisture control section - between 4 and 12 inches.
Mollic epipedon thickness - 8 to 16 inches and may include part of the Bt horizon.
Depth to Cr horizon - 20 to 40 inches.

A horizon - Hue: 2.5Y, 5YR, 7.5YR or 10YR
Value: 2 or 3 moist
Chroma: 1 or 2
Clay content: 27 to 35 percent
Rock fragments: 0 to 30 percent--0 to 15 percent pebbles, 0 to 10 percent cobbles; 0 to 5 percent stones.
Reaction: pH 6.1 to 7.3

Bt1 horizon - Hue: 7.5YR, 5YR or 10YR
Value: 4 or 5 dry; 3 or 4 moist
Chroma: 2, 3 or 4
Texture: clay loam, clay, silty clay loam, silty clay
Clay content: 35 to 50 percent
Rock fragments: 0 to 15 percent-- 0 to 10 percent pebbles, 0 to 5 percent cobbles or flagstones
Reaction: pH 6.6 to 7.3

Bt2 horizon - Hue: 5YR, 7.5YR or 10YR
Value: 5 or 6 dry; 4 or 5 moist
Chroma: 2, 3 or 4
Texture: clay loam, clay, silty clay loam, silty clay
Clay content: 35 to 50 percent
Rock fragments: 0 to 15 percent-- 0 to 10 percent pebbles,
0 to 5 percent cobbles
Reaction: pH 6.6 to 7.3

Note: Some pedons contain lime in the Cr horizon.

COMPETING SERIES:

Alder (MT) - has horizon of secondary carbonate accumulation.

Bacbuster (MT) - has horizons of secondary carbonate accumulation.

Bigbear (MT) - is very deep.

Charo (NM) - has a lithic contact of basalt at 20 to 40 inches.

Darret (MT) - has horizon of secondary carbonate accumulation.

Durston (MT) - is very deep.

Mishakal (MT) - formed in residuum from argillite.

Microy (NM) - has a lithic contact of basalt at 20 to 40 inches.

Pino (NM) - has a lithic contact at 20 to 40 inches.

Terrad (MT) - has a paralithic contact at 40 to 60 inches; has horizons of secondary carbonate accumulation.

Wilcoxson (NM) - has a lithic contact of limestone at 40 inches or more; has horizon of secondary carbonate accumulation.

GEOGRAPHIC SETTING:

Landform - sedimentary plains and hills.
Elevation - 5,300 to 6,400 feet.
Slope - 2 to 60 percent.
Parent material - interbedded shale and sandstone residuum.
Climate - long cold winters; moist springs; warm summers.
Mean annual precipitation - 17 to 22 inches.
Mean annual air temperature - 37 to 41 degrees F.
Frost-free period - 80 to 100 days.

DRAINAGE AND PERMEABILITY: Well drained; slow permeability.

USE AND VEGETATION: Billman soils are used mainly for hayland and rangeland. Potential native vegetation may include subalpine needlegrasses, Idaho fescue, bluebunch wheatgrass, sedges, lupine, sticky geranium, rose and big sagebrush as well as other grasses, forbs and woody shrubs.

DISTRIBUTION AND EXTENT: Billman soils are of small extent in southwestern Montana.

MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Bozeman, Montana

SERIES ESTABLISHED: Gallatin County, Montana, 1997.

REMARKS: Soil interpretation record: MT1421. Diagnostic horizons and features recognized in this pedon are: a mollic epipedon from the soil surface 15 inches (A, Bt1 horizon); an argillic horizon which is also the particle-size control section from 7 to 23 inches (Bt1, Bt2 horizons); a paralithic contact at 23 inches (Cr horizon). Billman soils have a frigid temperature regime and an ustic moisture regime.


National Cooperative Soil Survey
U.S.A.