LOCATION GERDRUM            MT+SD
Established Series
Rev. GFB-CJH-JAL
10/1999

GERDRUM SERIES


The Gerdrum series consists of very deep, well drained soils that formed in alluvium or glacialfluvial deposits. These soils are on alluvial fans, stream terraces, drainageways, till plains, and sedimentary plains. Slopes are 0 to 25 percent. Mean annual precipitation is about 12 inches. Mean annual air temperature is about 43 degrees F.

TAXONOMIC CLASS: Fine, smectitic, frigid Torrertic Natrustalfs

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

A--0 to 2 inches; grayish brown (10YR 5/2) loam, dark brown (10YR 4/3) moist; weak thin platy structure parting to weak very fine granular; slightly hard, very friable, slightly sticky and nonplastic; common fine and very fine roots; many unstained silt and sand grains; soft very thin vesicular crust on surface; neutral (pH 7.3); clear smooth boundary. (0 to 2 inches thick)

E--2 to 4 inches; pale brown (10YR 6/3) silt loam, dark brown (10YR 4/3) moist; moderate thin platy structure; slightly hard, very friable, slightly sticky and nonplastic; common fine roots; many very fine vesicular pores; many unstained sand and silt grains, with light gray coats on plates; neutral (pH 7.3); abrupt wavy boundary. (Combined A and E horizons 2 to 4 inches thick)

Btn1--4 to 7 inches; brown (10YR 5/3) clay, dark brown (10YR 4/3) moist; strong fine and medium columnar structure parting to moderate medium and fine angular and subangular blocky; extremely hard, firm, sticky and plastic; few fine roots compressed along faces of peds and few very fine roots in matrix; few very fine tubular pores; light gray (10YR 7/2) coats of unstained sand and silt grains on tops of columns; dark grayish brown (10YR 4/2) coats on vertical faces of peds; continuous faint clay films of faces of peds; slightly alkaline (pH 7.8); clear wavy boundary.

Btn2--7 to 14 inches; brown (10YR 5/3) clay, dark brown (10YR 4/3) moist; strong fine and medium prismatic structure parting to strong medium and fine angular blocky; extremely hard, firm, sticky and plastic; few fine and very fine roots compressed along faces of peds and few very fine roots in matrix; few very fine tubular pores; dark grayish brown (10YR 4/2) coats on vertical faces of peds; continuous faint clay films on faces of peds; moderately alkaline (pH 7.9); clear wavy boundary. (The combined thickness of the Btn horizons is 8 to 20 inches)

Btkn--14 to 22 inches; grayish brown (2.5Y 5/2) clay, dark grayish brown (2.5Y 4/2) moist; strong fine and medium prismatic structure parting to moderate fine and medium angular and subangular blocky; very hard, friable, sticky and plastic; few very fine roots; few very fine tubular pores; common faint clay films on vertical faces of peds; common fine masses of lime; strongly effervescent; moderately alkaline (pH 8.4); clear wavy boundary. (0 to 13 inches thick)

Bknyz1--22 to 36 inches; light brownish gray (2.5Y 6/2) clay loam, grayish brown (2.5Y 5/2) moist; moderate medium prismatic structure parting to moderate medium subangular blocky; very hard, friable, sticky and plastic; few very fine roots; few very fine pores; common fine masses of lime; common fine masses and seams of gypsum and other salts; strongly effervescent; moderately alkaline (pH 8.4); clear wavy boundary. (8 to 30 inches thick)

Bknyz2--36 to 46 inches; grayish brown (2.5Y 5/2) sandy clay loam, dark grayish brown (2.5Y 4/2) moist; weak medium prismatic structure parting to weak medium subangular blocky; very hard, friable, slightly sticky and slightly plastic; few very fine roots; few very fine pores; few to common fine masses of lime; common fine masses and seams of gypsum and other salts; strongly effervescent; moderately alkaline (pH 8.4); clear irregular boundary. (0 to 15 inches thick)

2Bknyz--46 to 60 inches; brown (10YR 5/3) gravelly sandy loam, dark brown (10YR 4/3) moist; weak coarse prismatic structure; hard, very friable, slightly sticky and nonplastic; 25 percent pebbles; lime disseminated throughout and as crusts on underside of rock fragments and as seams; common fine masses and seams of gypsum and other salts; strongly effervescent; moderately alkaline (pH 8.4).

TYPE LOCATION: Blaine County, Montana; about 1,740 feet north and 50 feet east of SW corner of sec. 8, T. 25 N., R. 18 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 above.

Depth to k horizon - 10 to 24 inches, in some pedons it is as deep as 40 inches.

Depth to gypsum - 10 to 28 inches.

Soil phases - shaly substratum; gullied.

Some pedons have a BC or Bz horizon below 40 inches and do not have a lithologic discontinuity.

A horizon - Hue: 10YR or 2.5Y

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

Chroma: 2 or 3

Texture: loam, clay loam, silty clay loam, silt loam, clay, silty clay

Clay content: 10 to 50 percent

Rock fragments: 0 to 15 percent pebbles

Reaction: pH 6.6 to 7.8

E horizon - Hue: 10YR or 2.5Y

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

Chroma: 2 or 3

Textures: loam, silt loam, silty clay loam, clay loam, silty clay, or clay

Clay content: 10 to 50 percent

Rock fragments: 0 to 15 percent pebbles

Reaction: pH 6.6 to 7.8

Btn1 horizon - Hue: 10YR or 2.5Y

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

Chroma: 2, 3, or 4

Textures: clay, silty clay, silty clay loam

Clay content: 35 to 55 percent

Rock fragments: 0 to 10 percent pebbles

Structure: fine to coarse columnar or medium or coarse blocky

Hardness: extremely or very hard when dry

EC: 1 to 8 mmhos/cm

SAR: 10 to 20; pedons with sodium adsorption ratio of less than 13 have more exchangeable magnesium plus sodium than calcium plus exchange acidity at pH 8.2.

Reaction: pH 7.4 to 9.0

Btn2 horizon - Hue: 10YR or 2.5Y

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

Chroma: 2, 3, or 4

Textures: clay, silty clay, or silty clay loam

Clay content: 35 to 55 percent

Rock fragments: 0 to 10 percent pebbles

Structure: fine to coarse prismatic or medium or coarse blocky

Hardness: extremely or very hard when dry

EC: 1 to 8 mmhos/cm

SAR: 10 to 20; pedons with sodium adsorption ratio of less than 13 have more exchangeable magnesium plus sodium than calcium plus exchange acidity at pH 8.2.

Reaction: pH 7.4 to 9.0

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

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

Chroma: 2 or 3

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

Clay content: 35 to 55 percent

Rock fragments: 0 to 10 percent pebbles

Calcium carbonate equivalent: 5 to 15 percent

EC: 2 to 8 mmhos/cm

SAR: 13 to 20

Reaction: pH 7.4 to 9.0

Bknyz & Bkyz horizons - Hue: 10YR, 2.5Y, or 5Y

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

Chroma: 2, 3, or 4

Textures: clay loam, sandy clay loam, clay, or silty clay

Clay content: 30 to 50 percent

Rock fragments: 0 to 10 percent pebbles

Calcium carbonate equivalent: 5 to 15 percent

EC: 8 to 16 mmhos/cm

SAR: 13 to 30

Gypsum: 1 to 5 percent

Reaction: pH 7.9 to 9.0

2Bknyz horizon - Hue: 10YR, 2.5Y, or 5Y

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

Chroma: 1, 2, 3, or 4 (1 chroma is lithochromatic)

Textures: sandy loam, loam, sandy clay loam, or silty clay loam

Clay content: 10 to 35 percent

Rock fragments: 15 to 25 percent pebbles

Calcium carbonate equivalent: 5 to 15 percent

EC: 8 to 16 mmhos/cm

SAR: 13 to 30

Gypsum: 1 to 5 percent

Reaction: pH 7.9 to 9.0

COMPETING SERIES:

Creed (MT) - has A and E horizons that have a combined thickness of 4 to 10 inches; very slowly permeable in the Bt horizons.

Elloam (MT) - formed in till that has a bulk density of 1.55 or greater above a depth of 40 inches.

Loburn (SD) - has a combined A and E horizon thickness of more than 4 inches.

Oburn (MT) - is skeletal above a depth of 40 inches.

Thoeny (MT) - formed in till that has a bulk density of 1.55 or greater above a depth of 40 inches.

Waltham (MT) - does not have Btn horizons; formed in till.

Weingart (MT) - has a paralithic contact of semiconsolidated shale at depths of 20 to 40 inches.

GEOGRAPHIC SETTING:

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

Elevation - 1,900 to 5,200 feet. (In Wyoming the elevation is to 7,800 feet)

Slope- 0 to 25 percent.

Parent material - alluvium or glacialfluvial deposits derived mainly from till and sedimentary rock.

Climate - long, cold winters; moist springs; hot, dry summers.

Mean annual precipitation - 10 to 14 inches, most of which falls in the spring and early summer.

Mean annual air temperature - 39 to 45 degrees F.

Frost-free period - 95 to 135 days. (In Wyoming the range is 85 to 135 days)

DRAINAGE AND PERMEABILITY: Well drained; very slow permeability.

USE AND VEGETATION: Gerdrum soils are used mainly for range. A few small areas are used for dryland and irrigated crops. The potential native plant community is mainly western wheatgrass, bluebunch wheatgrass, green needlegrass, needleandthread, forbs, and shrubs.

DISTRIBUTION AND EXTENT: Central and eastern Montana and possibly in adjacent states. Gerdrum soils are extensive.

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

SERIES ESTABLISHED: Blaine County, Montana, 1976.

REMARKS: Soil interpretation records: MT0286, MT0766.

Diagnostic horizons and features recognized in this pedon are: ochric epipedon - from the soil surface to 4 inches (A, E horizons); natric horizon - from 10 to 22 inches (Btn1, Btn2, Btkn horizons); horizons of accumulations of lime and/or gypsum and other salts (Btkn, Bknyz1, Bknyz2, 2Bknyz horizons); particle-size control section - from the top of the argillic horizon to 22 inches (Btn1, Btn2, Btkn horizons). Gerdrum soils have a frigid temperature regime and an ustic moisture regime bordering on aridic.

LABORATORY DATA: S71MT-69-1, S69MT-5-2, S80MT-11-1


National Cooperative Soil Survey
U.S.A.