LOCATION VOSBURG            CO+NM
Established Series
JPP/DKR/TWH
03/2005

VOSBURG SERIES


The Vosburg series consists of very deep, well drained soils that formed in alluvium weathered from sandstone and shale. Vosburg soils are on valleys, upland swales, toe slopes, foot slopes, and alluvial fans and have slopes of 0 to 12 percent. Mean annual precipitation is about 17 inches and the mean annual temperature is about 47 degrees F.

TAXONOMIC CLASS: Fine-loamy, mixed, superactive, mesic Pachic Argiustolls

TYPICAL PEDON: Vosburg fine sandy loam-cultivated. (Colors are for dry soil unless otherwise noted)

A--0 to 15 inches; dark grayish brown (10YR 4/2) fine sandy loam, very dark brown (10YR 2/2) moist; weak fine granular structure; loose, very friable, slightly sticky and nonplastic; neutral (pH 7.2); clear smooth boundary. (2 to 19 inches thick)

BA--15 to 18 inches; dark grayish brown (10YR 4/2) clay loam, very dark grayish brown (10YR 3/2) moist; weak medium subangular blocky structure parting to weak medium granular; slightly hard, friable, moderately sticky and moderately plastic; slightly alkaline (pH 7.4); clear smooth boundary. (2 to 6 inches thick)

Bt--18 to 31 inches; dark grayish brown (10YR 4/2) sandy clay loam, very dark grayish brown (10YR 3/2) moist; moderate medium subangular blocky structure parting to moderate medium granular; hard, friable, moderately sticky and moderately plastic; many prominent clay films on faces of peds; slightly alkaline (pH 7.6); gradual smooth boundary. (10 to 25 inches thick)

Bk1--31 to 50 inches; brown (10YR 5/3) sandy clay loam, brown (10YR 4/3) moist; moderate medium subangular blocky structure parting to moderate fine subangular blocky; hard, friable, moderately sticky and moderately plastic; strongly effervescent; few irregular masses of calcium carbonate; slightly alkaline (pH 7.8); gradual smooth boundary. (10 to 15 inches thick)

Bk2--50 to 60 inches; brown (10YR 5/3) sandy clay loam, brown (10YR 4/3) moist; massive; hard, friable, moderately sticky and moderately plastic; violently effervescent; common irregular masses of calcium carbonate; slightly alkaline (pH 7.8).

TYPE LOCATION: La Plata County, Colorado; in Hay Gulch, about 1,700 feet east and 600 feet north of the southwest corner of Sec. 15, T. 34 N., R. 12 W. U.S.G.S. Mormon Reservoir quad.; Lat. 37 degrees, 11 minutes, 02 seconds N., and Long. 108 degrees, 08 minutes, 20 seconds W.

RANGE IN CHARACTERISTICS:
Soil moisture: The moisture control section is dry for 15 consecutive days from May 15 to July 15 when the soil temperature at 20 inches is greater than 41 degrees F. (5 degrees C.) It is not dry in all parts of the moisture control section for 90 cumulative days following the summer solstice to October 20. The PE Index is 42 at the type location. Ustic moisture regime bordering on aridic.

Mean annual soil temperature: 47 to 52 degrees F.
Thickness of the mollic epipedon: 20 to 60 inches
Depth to uniformly calcareous material: 15 to 50 inches
Rock fragment content: 0 to 15 percent, mainly gravel size.
Lithology of rock fragments: sandstone and shale

A horizon:
Hue:10YR or 7.5YR
Value: 3 through 5, 2 or 3 moist
Chroma: 1 through 3
Reaction: slightly acid to slightly alkaline.

An AB or BA horizon may be present above the argillic horizon.

Bt horizon:
Hue:10YR or 7.5YR; Subhorizons redder than 7.5YR occur in some pedons.
Value: 3 through 6, 2 through 5 moist
Chroma: 1 through 4
Texture: sandy clay loam, loam, or clay loam
Clay content: 18 to 35 percent
Silt content: 5 to 45 percent
Sand content: 25 to 65 percent
Reaction: neutral to moderately alkaline.

Bk or Btk horizons:
Hue: 10YR or 7.5YR
Texture: sandy loam, loam, clay loam
Reaction: slightly alkaline to strongly alkaline.

COMPETING SERIES: These are the Albinas (WY), Bluewater (NM), Farnum (KS), Funmar (KS), Garrett (WY), Haxtun (CO), Jarita (NM), Keya (SD), Ownyate (NM), Prosper (SD), Renner (SD), Sampson (CO), Tracylee (WY), and Wetterdon (WY) soils. Albinas, Keya, Prosper, Renner, Sampson, and Woodly soils are moist in some part of the moisture control section from May 15 to July 15 and are in a climatic setting that receives three-fourths of the precipitation between April and September. Bluewater soils are somewhat poorly drained and have redox features at depths of 23 to 45 inches. Garrett soils have Bt horizons of 5YR or redder. Farnum and Funmar soils have mean annual soil temperatures higher than 52 degrees F. Haxtun soils have buried B horizons. Jarita soils are 20 to 40 inches thick over a lithic contact. Keya and Tracylee soils are noncalcareous throughout. Ownyate soils have rock fragments of igneous and metamorphic lithology. Prosper soils have thinner solum and are usually moist. The Wetterdon soils are moist in most parts of their moisture control section during April, May and June.

GEOGRAPHIC SETTING: Vosburg soils are on upland swales, in valleys, on foot slopes, toe slopes and alluvial fans. Slopes range from 0 to 12 percent. The soils formed in alluvium weathered from sandstone and shale. Elevation ranges from 6,000 to 7,800 feet. Mean annual temperature ranges from 45 to 50 degrees F., and mean summer temperature ranges from 60 to 68 degrees F. Mean annual precipitation is 14 to 18 inches and is distributed fairly evenly throughout the year with about half the precipitation falling between April and September. May and June are the driest months. PE Index is about 50 at the type location and ranges from 25 to 60 for the series.

GEOGRAPHICALLY ASSOCIATED SOILS: These are the Lazear, Pulpit, Witt, and Zyme soils. Lazear and Zyme soils are shallow and are on steep side slopes. Pulpit is moderately deep over sandstone and is formed in loess. Witt is on mesa tops and is formed in loess.

DRAINAGE AND PERMEABILITY: Well drained; low to medium runoff. Moderate permeability.

USE AND VEGETATION: These soils are used for irrigated and dry cropland and for rangeland. Crops are alfalfa, pasture, and small grains. Native vegetation is big sagebrush, Indian ricegrass, junegrass, western wheatgrass, blue grama, needleandthread, oakbrush, and rabbitbrush.

DISTRIBUTION AND EXTENT: Vosburg soils occur in western Colorado and northwest New Mexico. The series is of small extent. MLRA 36.

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

SERIES ESTABLISHED: La Plata County Area, Colorado, 1982.

REMARKS: Diagnostic horizons and features recognized in this pedon:
Mollic epipedon (Pachic feature): from 0 to 31 inches (A, BA, and Bt horizons)
Argillic horizon: from 18 to 31 inches (Bt horizon)
Particle-size control section: The zone from 18 to 31 inches (the Bt horizon)

This revision (2/01) clarifies the moisture regime as aridic ustic. The precipitation range was redefined from 12 to 20 inches to 14 to 18 inches. This new range reflects the original concept of the series.

Keys to Soil Taxonomy: Series classified according to Eighth Edition, 1998.

The superactive cation exchange activity class was added in 03/2003 to the taxonomic classification by the National Soil Survey Center on request of the Lakewood MLRA office, without review of the soil series property data. The remainder of this document has not been updated.


National Cooperative Soil Survey
U.S.A.