LOCATION STROMAL            NM
Established Series
Rev. RCD-RJA-ACT
07/2007

STROMAL SERIES


The Stromal series consists of very deep, well drained, soils that formed in calcareous alluvium and eolian materials. Stromal soils are on high terraces and have slopes of 0 to 2 percent. The mean annual precipitation is about 13 inches. The mean annual temperature is about 60 degrees F.

TAXONOMIC CLASS: Coarse-loamy, mixed, active, thermic Ustic Calciargids

TYPICAL PEDON: Stromal fine sand--rangeland. (Colors are for dry soil unless otherwise noted.)

A1--0 to 8 inches; brown (10YR 5/3) fine sand, brown (10YR 4/3) moist; weakfine granular structure; soft, very friable, nonsticky and nonplastic; many very fine roots; common very fine pores; neutral; clear wavy boundary. (6 to 11 inches thick)

A2--8 to 17 inches; yellowish brown (10YR 5/4) fine sand, dark yellowish brown (10YR 4/4) moist; weak medium granular structure; soft, very friable, nonsticky and nonplastic; many very fine roots; common very fine pores; neutral; clear wavy boundary. (8 to 10 inches thick)

Bt--17 to 24 inches; light yellowish brown (10YR 6/4) loamy fine sand, yellowish brown (10YR 5/4) moist; weak coarse subangular blocky structure; slightly hard, friable, nonsticky and nonplastic; many very fine roots; common very fine pores; common thin clay bridges between sand grains; slightly alkaline; clear wavy boundary. (6 to 9 inches thick)

Btk--24 to 28 inches; very pale brown (10YR 7/3) loam, pale brown (10YR 6/3) moist; moderate coarse subangular blocky structure; hard, firm, slightly sticky and slightly plastic; common very fine roots; common very fine pores; few thin clay films on faces of peds and lining pores; many medium calcium carbonate concretions; strongly effervescent; moderately alkaline; clear wavy boundary. (4 to 10 inches thick)

Bk--28 to 50 inches; white (10YR 8/1) fine sandy loam, light gray (10YR 7/2) moist; massive; slightly hard, friable, slightly sticky and slightly plastic; common very fine roots; common very fine pores; calcium carbonate engulfed; strongly effervescent; moderately alkaline; clear wavy boundary. (4 to 25 inches thick)

C--50 to 60 inches; very pale brown (10YR 7/3) loamy fine sand, light gray (10YR 7/2) moist; single grain; loose, nonsticky and nonplastic; slightly effervescent; strongly alkaline.

TYPE LOCATION: Chaves County, New Mexico, 80 feet east and 0.4 of a mile south of windmill in Sec. 34, T. 9 S., R. 31 E.

RANGE IN CHARACTERISTICS:

Soil Moisture: Intermittently moist in some part of the soil moisture control section December through March and May through September.

Soil Temperature: 59 to 64 degrees F.

Depth to the calcic horizon: 20 to 40 inches

Depth to textures finer than loamy fine sand: 20 to 30 inches

A horizon:
Hue: 7.5YR or 10YR
Value: 5 or 6 dry, 3 or 4 moist
Chroma: 3 or 4
Texture: fine sand or loamy fine sand
Reaction: Neutral or slightly alkaline

Bt horizon:
Hue:7.5YR or 10YR
Value: 5 to 7 dry, 4 to 6 moist
Chroma: 3 or 4
Clay content: 8 to 18 percent on a weighted average

Bk horizon:
Hue: 7.5YR or 10YR
Value: 7 or 8 dry, 6 or 7 moist
Chroma: 1 to 3
Texture: loamy fine sand, fine sandy loam, or loam
Calcium carbonate equivalent: 15 to 40 percent

COMPETING SERIES: There are no competing series in the same family. Similar soils are the Jalmar and Pyote series. Jalmar soils have more than 18 percent clay in the particle-size control section, and do not have a calcic horizon. Pyote soils do not have a calcic horizon within 40 inches. In addition, Pyote soils have siliceous mineralogy.

GEOGRAPHIC SETTING: Stromal soils are on high terraces and formed in calcareous alluvium and eolian materials. Slope ranges from 0 to 2 percent. Annual precipitation ranges from 12 to 14 inches. Mean annual temperature ranges from 58 to 62 degrees F. The frost-free period is 195 to 205 days. Elevation ranges from 3,900 to 4,100 feet.

GEOGRAPHICALLY ASSOCIATED SOILS: These are the Faskin, Malstrom, Roswell, and the competing Jalmar and Pyote soils. Faskin soils have a sandy surface less than 20 inches thick and have a control section with more than 18 percent clay. Malstrom soils do not have a Bt horizon. Roswell soils are sandy throughout.

DRAINAGE AND PERMEABILITY: Well drained. Permeability is moderately rapid. Runoff is negligible to very slow.

USE AND VEGETATION: These soils are used for rangeland. The present vegetation is sand bluestem, little bluestem, sand dropseed, shinnery oak, small soapweed, and sagebrush.

DISTRIBUTION AND EXTENT: Southeastern New Mexico. The series is of small extent.

MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Phoenix, Arizona

SERIES ESTABLISHED: Chaves County (North Part), New Mexico, 1981.

REMARKS: Diagnostic horizons and features recognized in this pedon are:

Ochric epipedon: 0 to 17 inches. (A horizon)
Argillic horizon: 17 to 28 inches. (Bt and Btk horizons)
Calcic horizon: 28 to 50 inches. (Bk horizon)


National Cooperative Soil Survey
U.S.A.