LOCATION KOBASE             MT
Established Series
Rev. GFB-CJH-JAL
10/1999

KOBASE SERIES


The Kobase series consists of very deep, well drained soils that formed in alluvium derived from semiconsolidated shale and sandstone, or glaciofluvial or glaciolacustrine deposits. They are on till plains, lake plains, stream terraces, alluvial fans, drainageways, sedimentary plains, and hills. Slopes are 0 to 40 percent. Mean annual precipitation is about 12 inches. Mean annual air temperature is about 43 degrees F.

TAXONOMIC CLASS: Fine, smectitic, frigid Torrertic Haplustepts

TYPICAL PEDON: Kobase silty clay loam, in cropland (colors are for dry soil unless otherwise noted).

Ap--0 to 7 inches; grayish brown (2.5Y 5/2) silty clay loam, dark grayish brown (2.5Y 4/2) moist; moderate very fine granular structure in upper 3 inches grading to weak medium and fine subangular blocky in the lower part; hard, very friable, sticky and plastic; many fine and very fine roots; many fine and very fine pores; slightly effervescent; neutral (pH 7.3); abrupt wavy boundary. (5 to 8 inches thick)

Bw--7 to 15 inches; light brownish gray (2.5Y 6/2) silty clay loam, dark grayish brown (2.5Y 4/2) moist; moderate medium prismatic structure parting to moderate medium and fine angular blocky; very hard, friable, sticky and plastic; many fine and very fine roots; many fine and very fine pores; disseminated lime; strongly effervescent; moderately alkaline (pH 8.4); gradual wavy boundary. (6 to 15 inches thick)

Bk1--15 to 20 inches; light brownish gray (2.5Y 6/2) silty clay loam, dark grayish brown (2.5Y 4/2) moist; moderate medium prismatic structure parting to weak medium and coarse subangular blocky; extremely hard, firm, sticky and plastic; common fine and very fine roots; many fine and very fine pores; few fine masses of lime; strongly effervescent; strongly alkaline (pH 8.8); gradual wavy boundary.

Bk2--20 to 31 inches; light brownish gray (2.5Y 6/2) clay loam, dark grayish brown (2.5Y 4/2) moist; weak medium and coarse angular blocky structure; extremely hard, friable, sticky and plastic; common fine and very fine roots; many fine and very fine pores; few fine masses of lime; strongly effervescent; strongly alkaline (pH 8.8); gradual wavy boundary. (Combined Bk horizons 8 to 38 inches thick)

Bky--31 to 60 inches; light brownish gray (2.5Y 6/2) clay loam, dark grayish brown (2.5Y 4/2) moist; weak coarse angular blocky structure; hard, friable, sticky and plastic; few fine and very fine roots; many very fine pores; common fine masses of lime; common fine threads of gypsum and other salts; strongly effervescent; strongly alkaline (pH 8.8). (0 to 30 inches thick.)

TYPE LOCATION: Fergus County, Montana; 800 feet east and 1,350 feet north of the southwest corner of sec. 9, T. 18 N., R. 26 E.

RANGE IN CHARACTERISTICS:

Soil temperature - 42 to 47 degrees F.

Moisture control section - between 4 and 12 inches; dry in all parts between four-tenths and five-tenths of the cumulative days per year when the soil temperature at 20 inches is 41 degrees F or higher.

Depth to Bk horizon - 12 to 17 inches.

The one chromas are lithochromic in the B horizons, a C horizon is allowed.

Soil phases - moist, saline.

Ap horizon - Hue: 10YR or 2.5Y

Value: 5 or 6 dry; 4 or 5 moist

Chroma: 2 or 3

Texture: silty clay loam, silty clay, clay, or clay loam

Clay content: 27 to 45 percent

Rock fragments: 0 to 5 percent pebbles

EC: 0 to 4 mmhos/cm (saline phase 2 to 4 mmhos/cm)

SAR: 0 to 4

Calcium carbonate equivalent: 0 to 5 percent

Reaction: pH 6.6 to 8.4

Bw horizon - Hue: 10YR, 2.5Y, or 5Y

Value: 5 or 6 dry; 4 or 5 moist

Chroma: 1, 2, 3, or 4

Texture: clay loam, silty clay loam, silty clay, or clay

Clay content: 35 to 45 percent

Rock fragments: 0 to 5 percent pebbles

Calcium carbonate equivalent: 0 to 10 percent

EC: 0 to 2 mmhos/cm

SAR: 0 to 4

Reaction: pH 7.4 to 8.4

Bk1 horizon - Hue: 10YR, 2.5Y, or 5Y

Value: 5, 6, or 7 dry; 4, 5, or 6 moist

Chroma: 1, 2, 3, or 4

Texture: clay loam, silty clay loam, silty clay, or clay

Clay content: 35 to 45 percent

Rock fragments: 0 to 5 percent pebbles

Calcium carbonate equivalent: 5 to 15 percent

SAR: 0 to 10

EC: 0 to 2 mmhos/cm

Reaction: pH 7.4 to 9.0

Bk2 horizon - Hue: 10YR, 2.5Y, or 5Y

Value: 5, 6, or 7 dry; 4, 5, or 6 moist

Chroma: 2, 3, or 4

Texture: clay loam, silty clay loam, silty clay, or clay

Clay content: 35 to 45 percent

Rock fragments: 0 to 5 percent pebbles

Calcium carbonate equivalent: 5 to 15 percent

SAR: 0 to 10

EC: 0 to 4 mmhos/cm

Reaction: 7.9 to 9.0

Bky horizon - Hue: 10YR, 2.5Y, or 5Y

Value: 5, 6, or 7 dry; 4, 5, or 6 moist

Chroma: 1, 2, 3, or 4

Texture: clay loam, silty clay loam, silty clay, or clay

Clay content: 35 to 45 percent

Rock fragments: 0 to 5 percent pebbles

Calcium carbonate equivalent: 5 to 15 percent

SAR: 1 to 20

EC: 0 to 8 mmhos/cm

Gypsum: 1 to 5 percent

Reaction: pH 7.9 to 9.0

Some pedons have thin strata of silt loam or loam below depths of 40 inches and a BCy or Byz horizon.

COMPETING SERIES:

Alzada (MT) - has a lithological discontinuity within depths of 40 inches.

Brunelda (MT) - has a gypsic horizon; does not have a cambic horizon.

Megonot (MT) - has a paralithic contact above a depth of 40 inches.

Nunemaker (MT) - has a discontinuity of till that has a bulk density of 1.65 g/cc and greater.

Teigen (MT) - is noncalcareous throughout the profile; has very strongly acid to medium acid reaction in the surface and cambic horizons.

Zatoville (MT) - has a gypsic horizon; has a paralithic contact at depths between 40 and 60 inches.

GEOGRAPHIC SETTING:

Landform - till plains; stream terraces; alluvial fans; sedimentary plains; drainageways; lake plains; hills.

Elevation - 2,200 to 5,200 feet.

Slope- 0 to 40 percent.

Parent material - alluvium derived from semiconsolidated shale and sandstone, glacial meltwater deposits, and glaciofluvial or glaciolacustrine deposits.

Climate - long, cold winters; moist springs; warm summers.

Mean annual precipitation - 10 to 14 inches, most of which fall during the spring and the early part of summer.

Mean annual temperature - 39 to 45 degrees F.

Frost-free period - 90 to 135 days.

DRAINAGE AND PERMEABILITY: Well drained, slow permeability.

USE AND VEGETATION: Kobase soils are used for irrigated and nonirrigated cropland and for rangeland. The potential native vegetation is green needlegrass, bluebunch wheatgrass, western wheatgrass, forbs, and shrubs.

DISTRIBUTION AND EXTENT: The Kobase series is extensive in the plains area of Montana, in adjacent states, and in Colorado.

MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Denver, Colorado

SERIES ESTABLISHED: Hill County, Montana, 1994. Kobase is a coined name.

REMARKS: Soil interpretations records: MT0106, MT0892.

Diagnostic horizons and features recognized in this pedon are: ochric epipedon - from the soil surface to 7 inches (Ap horizon); cambic horizon - from 7 to 15 inches (Bw horizon); accumulations of lime - from 15 to 60 inches (Bk1, Bk2, Bky horizons); particle-size control section - from 10 to 40 inches (Bw, Bk1, Bk2, Bky horizons). Kobase soils have a frigid temperature regime and an ustic moisture regime bordering on aridic.


National Cooperative Soil Survey
U.S.A.