LOCATION IVANELL            MT
Established Series
Rev. JMS-JAL
11/98

IVANELL SERIES


The Ivanell series consists of moderately deep, well drained soils that formed in material derived from semiconsolidated shale. These soils are on side slopes on uplands. Slopes are 0 to 15 percent. Mean annual precipitation is about 10 inches, and mean annual temperature is about 42 degrees F.

TAXONOMIC CLASS: Fine-silty, mixed, superactive, frigid Aridic Haplustalfs

TYPICAL PEDON: Ivanell clay loam in grassland (colors are for dry soil unless otherwise noted).

E--0 to 3 inches; light brownish gray (2.5Y 6/2) loam, dark grayish brown (2.5Y 4/2) moist; moderate very thin platy structure; slightly hard, very friable, slightly sticky and slightly plastic; many very fine roots; slightly alkaline (pH 7.6); abrupt smooth boundary. (2 to 5 inches thick)

Bt--3 to 7 inches; grayish brown (2.5Y 5/2) clay loam, dark grayish brown (2.5Y 4/2) moist; moderate medium prismatic structure parting to moderate medium and fine angular blocky; hard, friable, sticky and plastic; many very fine roots; common very fine tubular pores; continuous faint thin clay films on faces of peds and in pores; slightly alkaline (pH 7.8); clear smooth boundary. (4 to 9 inches thick)

Btk--7 to 9 inches; light brownish gray silty clay loam (2.5Y 6/2) light yellowish brown (2.5Y 5/4) moist; moderate medium prismatic structure parting to moderate medium subangular blocky; very hard, friable, sticky and plastic; common very fine roots; many very fine tubular pores; common faint clay films on faces of peds; strongly effervescent; few fine masses of lime; moderately alkaline (pH 8.0); clear smooth boundary. (0 to 4 inches thick)

Bk--9 to 22 inches; light brownish gray (2.5Y 6/2) silty clay loam, grayish brown (2.5Y 5/2) moist; moderate coarse prismatic structure; very hard, friable, sticky and plastic; common very fine roots; many very fine tubular pores; strongly effervescent; common fine masses of lime; strongly alkaline (pH 8.6); clear smooth boundary. (5 to 21 inches thick)

BC--22 to 37 inches; light brownish gray (2.5Y 6/2) clay loam, dark grayish brown (2.5Y 4/2) moist; massive; hard, friable, sticky and plastic; common very fine roots; many very fine pores; slightly effervescent; strongly alkaline (pH 8.6); gradual smooth boundary. (0 to 20 inches thick)

Cr--37 to 60 inches; semiconsolidated shale that crushes to silty clay loam; few very fine roots in cracks; common fine masses of gypsum; moderately alkaline (pH 8.0).

TYPE LOCATION: Rosebud County, Montana; 1,500 feet east and 1,000 feet south of the NW corner of sec. 32, T. 9 N., R. 38 E.

RANGE IN CHARACTERISTICS:

Soil temperature - 41 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 a depth of 20 inches is 41 degrees F or higher.

Depth to Bk horizon - 6 to 12 inches.

Depth to Cr horizon - 20 to 40 inches, mainly 25 to 40 inches.

A Bz horizon is allowed.

E horizon - Hue: 2.5Y or 10YR

Value: 5, 6, or 7 dry; 3, 4, or 5 moist

Texture: loam or silt loam, mixed to 7 inches it is a clay loam

Clay content: 18 to 25 percent

Reaction: pH 6.6 to 7.8

Bt horizon - Hue: 2.5Y or 10YR

Value: 5 or 6 dry; 4 or 5 moist

Chroma: 2, 3, or 4

Texture: silty clay loam or clay loam

Clay content: 27 to 35 percent

Reaction: pH 7.4 to 8.4

Bk or Btk horizon - Hue: 2.5Y or 10YR

Value: 5 or 6 dry; 4 or 5 moist

Chroma: 2, 3, or 4

Texture: silty clay loam or clay loam

Clay content: 27 to 35 percent

Calcium carbonate equivalent: 5 to 15 percent

Electrical conductivity: 0 to 4 mmhos/cm

SAR: 5 to 15

Reaction: pH 7.9 to 9.0

BC horizon - Hue: 2.5Y or 10YR

Value: 5 or 6 dry; 4 or 5 moist

Chroma: 2 or 4

Texture: silty clay loam or clay loam

Clay content: 27 to 35 percent

Calcium carbonate equivalent: 5 to 15 percent

Electrical conductivity: 8 to 16 mmhos/cm

SAR: 10 to 25

Reaction: pH 7.4 to 9.0

Cr horizon - semiconsolidated shale that crushed to silty clay loam or clay loam

Estimated electrical conductivity: 8 to 16 mmhos/cm

Estimated sodium absorption ratio: 10 to 25

Reaction: pH 7.4 to 8.4

COMPETING SERIES:

Davidell (MT) - does not have a paralithic contact of semiconsolidated shale at depths of 20 to 40 inches.

Debs (MN) - does not have a paralithic contact of semiconsolidated shale at depths of 20 to 40 inches.

Virkula (SD) - does not have a paralithic contact of semiconsolidated shale at depths of 20 to 40 inches.

Winterridge (UT) - does not have a paralithic contact of semiconsolidated shale at depths of 20 to 40 inches.

GEOGRAPHIC SETTING:

Landform - sedimentary plains.

Elevation - 2,200 to 3,500 feet.

Slope- 0 to 15 percent.

Parent material - semiconsolidated shale or semiconsolidated interbedded shale and siltstone.

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

Mean annual precipitation - 10 to 14 inches.

Mean annual temperature - 39 to 45 degrees F.

Frost-free period - 100 to 135 days.

DRAINAGE AND PERMEABILITY: Well drained; moderately slow permeability.

USE AND VEGETATION: Ivanell soils are used mainly for range. The potential native vegetation is western wheatgrass, needleandthread, forbs, and shrubs.

DISTRIBUTION AND EXTENT: Ivanell soils are of moderate extent in southeastern Montana.

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

SERIES ESTABLISHED: Rosebud County, Montana, 1985.

REMARKS: Soil interpretation record: MT0589. Diagnostic horizons and features recognized in this pedon are: an ochric epipedon from the soil surface to 3 inches (E horizon); an argillic horizon from 3 to 7 inches (Bt horizon); accumulations of secondary calcium carbonate from 7 to 22 inches (Btk, Bk horizons); a paralithic contact of semiconsolidated shale at 37 inches (Cr horizon). Ivanell soils have a frigid temperature regime and an ustic moisture regime bordering on aridic.


National Cooperative Soil Survey
U.S.A.