LOCATION CEMENTLAKE         NM
Established Series
Rev. TRO/RLB
01/2004

CEMENTLAKE SERIES


The Cementlake series consists of deep, well drained, slowly permeable oils that formed in alluvial sediments derived from shale and sandstone onvalley sideslopes and terraces. Slopes range from 1 to 6 percent. Mean annual precipitation is about 14 inches, and the average annual temperature
is 50 degrees F.

TAXONOMIC CLASS: Fine, smectitic, mesic Aridic Natrustalfs

TYPICAL PEDON: Cementlake sandy loam--rangeland. (Colors are for dry soil unless otherwise noted.)

E--0 to 1 inch; very pale brown (10YR 7/3) sandy loam, yellowish brown (10YR 5/4) moist; weak very fine platy structure; hard, friable, nonsticky and nonplastic; many very fine vesicular pores; 5 percent pebbles; slightly alkaline; abrupt smooth boundary. (1 to 3 inches thick)

Btn--1 to 8 inches; yellowish brown (10YR 5/4) sandy clay, dark yellowish brown (10YR 4/4) moist; moderate coarse columnar structure parting to strong fine angular blocky; hard, firm, sticky and plastic; few very fine roots; few very fine tubular pores; many thin clay films on ped faces; 5 percent pebbles; very slightly effervescent; moderately alkaline; clear smooth boundary.

Btn2--8 to 17 inches; brown (10YR 5/3) sandy clay, brown (10YR 4/3) moist; moderate fine angular blocky structure; very hard, very firm, sticky nd plastic; few very fine roots; few very fine tubular pores; common thin lay films on ped faces; slightly effervescent; moderately alkaline; clear smooth boundary.

Btkz--17 to 32 inches; grayish brown (10YR 5/2) clay loam, dark grayish brown (10YR 4/2) moist; weak medium and fine angular blocky structure; very hard, friable sticky and plastic; few very fine roots; ommon very fine tubular pores; violently effervescent; calcium carbonate nd salts occur as common fine irregular soft seams and filaments; strongly alkaline; gradual smooth boundary.

Bkz--32 to 80 inches; grayish brown (10YR 5/2) stratified sandy clay loam and sandy clay, dark grayish brown (10YR 4/2) moist; weak fine angular blocky structure; hard, friable, sticky and plastic; very few very fine roots; common very fine tubular pores; slightly effervescent; calcium carbonate, gypsum, and salt occur as few fine irregular soft filaments; moderately alkaline.

TYPE LOCATION: Rio Arriba County, New Mexico; about 4 miles southeast of Cement Lake; 106 degrees 59 minutes 27 seconds west longitude and 36 degrees 35 minutes 45 seconds north latitude.

RANGE IN CHARACTERISTICS:

Soil Moisture: Intermittently moist in some part of the soil moisture control section December through May and July through September. The soil is driest during October. Aridic ustic moisture regime

Soil temperature: 47 to 50 degrees F.

E horizon - Value: 6 or 7 dry, 4 or 5 moist.

Chroma: 2 through 4.

Coarse fragments: 0 to 5 percent pebbles.

Btn horizon - Hue: 10YR or 7.5Y

Value: 4 or 5 dry, 3 through 5 moist.

Chroma: 2 through 4.

Texture: clay, clay loam, or sandy clay.

SAR: greater than 13.

Coarse fragments: 0 to 10 percent pebbles.

Btkz horizon - Hue: 10YR or 7.5Y.

Value: 5 or 6 dry, 4 through 6 moist.

Chroma: 2 through 4.

Texture: clay, sandy clay, silty clay loam, clay loam, or sandy clay loam.

Calcium carbonate equivalent: less than 15 percent.

Coarse fragments: 0 to 10 percent pebbles.

C horizon where present - Value 5 or 6 dry, 4 or 5 moist.

Chroma 2 or 3.

Texture clay, loam, silt loam.

Other features: Depth to the secondary calcium carbonate is 8 to 26 inches.

COMPETING SERIES: No competing series currently exist in this family.

GEOGRAPHIC SETTING: Cementlake soils are on valley sides and terraces.
They formed in alluvium derived from shale and sandstone. Slopes are 1 to 6 percent. Elevation is 7,000 to 7,400 feet. Mean annual temperature is 45 to 52 degrees F. Mean annual precipitation is 12 to 16 inches. The frost-free period is 100 to 130 days.

GEOGRAPHICALLY ASSOCIATED SOILS: These are the Orlie, Menefee, Vessilla and Sparham series. Orlie and Sparham lack natric horizons. Menefee and Vessilla soils are shallow to bedrock.

DRAINAGE AND PERMEABILITY: Well drained. Permeability is very slow, Runoff is medium.

USE AND VEGETATION: The Cementlake soils are used for livestock grazing. Present vegetation is big sagebrush, black sage, western wheat grass, galleta, and blue grama.

DISTRIBUTION AND EXTENT: North central New Mexico. This series is of small extent.

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

SERIES ESTABLISHED: Jicarilla Apache Area soil survey, New Mexico, 2003. The series was originally proposed in Rio Arriba County, New Mexico, 1998. The name Cementlake is from a stock pond near the type location, and a local USGS quad name.

REMARKS:

Diagnostic horizon and features recognized in this pedon are:

Ochric epipedon - The zone from the surface to a depth of 1/2 inches.

Natric horizon - The zone from 1/2 to 32 inches.


National Cooperative Soil Survey
U.S.A.