LOCATION CABREROS           NM
Established Series
Rev. AJM/CDH/TWH
01/2008

CABREROS SERIES


The Cabreros series consists of well drained soils that are moderately deep to monzonite bedrock. Cabreros soils formed in slope alluvium and eolian material derived from monzonite on toeslopes of structural benches on sills. Slope ranges from 2 to 6 percent. Mean annual precipitation is about 11 inches and the mean annual air temperature is about 51 degrees F.

TAXONOMIC CLASS: Fine-loamy, mixed, superactive, mesic Ustic Calciargids

TYPICAL PEDON: Cabreros fine sandy loam, on a 2 percent slope, east southeast aspect, at 6,215 feet elevation - rangeland. (Colors are for dry soil unless otherwise noted. When described on June 16, 2004, the profile was dry throughout.)

A--0 to 2 inches; yellowish brown (10YR 5/4) fine sandy loam, dark yellowish brown (10YR 4/4) moist; weak fine subangular blocky structure parting to weak fine granular; soft, very friable, nonsticky and nonplastic; many very fine and fine roots; many very fine and fine interstitial pores; 5 percent gravel; neutral (pH 7.1); clear wavy boundary. (1 to 3 inches thick)

Bt1--2 to 9 inches; brown (7.5YR 5/4) loam, brown (7.5YR 4/4) moist; moderate medium subangular blocky structure; hard, friable, slightly sticky and slightly plastic; common very fine and fine roots; common medium vesicular pores; common distinct clay coatings on ped faces; 5 percent gravel; slightly alkaline (pH 7.4); gradual wavy boundary.

Bt2--9 to 18 inches; strong brown (7.5YR 5/6) clay loam, strong brown (7.5YR 4/6) moist; strong medium prismatic structure parting to strong medium subangular blocky; very hard, friable, moderately sticky and moderately plastic; common prominent and many distinct clay films on ped faces; 3 percent gravel; moderately alkaline (pH 8.3); clear wavy boundary. (combined thickness of the Bt horizons is 7 to 17 inches)

Btk--18 to 25 inches; brown (7.5YR 5/4) loam, strong brown (7.5YR 4/6) moist; moderate medium subangular blocky structure; hard, friable, moderately sticky and slightly plastic; few prominent and common distinct clay films on ped faces; common medium irregularly shaped calcium carbonate seams; 6 percent calcium carbonate equivalent; strongly alkaline (pH 8.6); clear wavy boundary. (7 to 20 inches thick)

BCk--25 to 34 inches; pale red (2.5YR 7/2) gravelly sandy loam, light reddish brown (2.5YR 6/4) moist; weak medium and weak coarse subangular blocky structure; slightly hard, friable, slightly sticky and nonplastic; 5 percent paragravel; 15 percent gravel and 5 percent cobbles; carbonates disseminated throughout matrix; 36 percent calcium carbonate equivalent; moderately alkaline (pH 8.4); abrupt wavy boundary. (4 to 12 inches thick)

Cr--34 to 47 inches; moderately cemented monzonite bedrock. (6 to 16 inches thick)

R--47 to 57 inches; indurated monzonite bedrock.

TYPE LOCATION: Santa Fe County, New Mexico; about 8.5 miles southeast of Cerrillos; northwest quarter of northeast quarter, Sec. 19, T.13N., R.9E; USGS Captain Davis Mountain 7.5 minute topographic quad; Longitude 106 degrees, 01 minute, 36.22 seconds west; Latitude 35 degrees, 20 minutes, 47.14 seconds north, NAD 83; UTM 13S 0406702 3911747.

RANGE IN CHARACTERISTICS:
Soil moisture - The soil moisture control section is intermittently moist in some part from July to October and December to March. It is assumed to be dry in all parts 50 to 75 percent of the time (cumulative), when the soil temperature at 20 inches is 41 degrees F. or higher. The soils are driest in May and June. The soil moisture regime is aridic bordering on ustic.

Mean annual soil temperature: 52 to 54 degrees F (11.1 to 12.2 C).
Depth to argillic horizon: 1 to 3 inches (3 to 8 cm).
Depth to calcic horizon: 15 to 30 inches (40 to 75 cm).
Depth to paralithic contact: 20 to 40 inches (50 to 100 cm).
Depth to lithic contact: 30 to 60 inches (50 to 150 cm).
Lithology of rock fragments: monzonite

Particle-size control section (weighted averages)
Silicate clay content: 20 to 35 percent
Rock fragment content: 0 to 15 percent

A horizon
Hue: 7.5YR to 10YR
Value: 3 to 5 dry, 3 or 4 moist
Chroma: 3 to 5 dry or moist
Texture: sandy loam or fine sandy loam
Rock fragments: 0 to 10 percent gravel
Reaction: neutral or slightly alkaline

Bt horizons
Hue: 7.5YR to 10YR
Value: 3 to 5 dry or moist
Chroma: 3 to 6 dry or moist
Texture: loam, sandy clay loam, gravelly sandy clay loam, or clay loam
Rock fragments: 0 to 15 percent gravel and 5 percent cobbles
Reaction: neutral or slightly alkaline

Btk horizons
Hue: 7.5YR to 10YR
Value: 5 to 6 dry, 4 to 5 moist
Chroma: 3 to 6 dry or moist
Calcium carbonate equivalent: 3 to 10 percent
Texture: loam, silt loam, sandy clay loam, or clay loam
Rock fragments: 0 to 10 percent gravel and 0 to 10 percent cobbles
Reaction: moderately alkaline or strongly alkaline

BCk horizons
Hue: 2.5YR to 7.5YR
Value: 5 to 8 dry, 4 to 6 moist
Chroma: 1 to 4 dry or moist
Calcium carbonate equivalent: 15 to 50 percent
Texture: silt loam, sandy clay loam, gravelly sandy loam, gravelly sandy clay loam, or cobbly sandy clay loam
Pararock fragment content: 0 to 15 percent paragravel
Rock fragments: 0 to 15 percent gravel, and 0 to 10 percent cobbles
Reaction: moderately alkaline or strongly alkaline

COMPETING SERIES: These are the Alvey, Barx, Cerrillos, Clovis, Fernando, Flaco, Horchata, Maysdorf, Millett, Palabria, Progresso, Sanostee, Scholle, Selpats, Solirec, Spenlo, Threetop, Tuweep, and Wineg. The Alvey, Barx, Cerrillos, Clovis, Maysdorf, Millett, Scholle, Selpats and Solirec soils are very deep to bedrock. The Fernando, Palaria, and Wineg soils are deep to bedrock. The Flaco and Tuweep soils are formed in volcanic parent material. The Horchata, Progresso, Sanostee, Spenlo, and Threetop soils are moderately deep to sedimentary rock.

GEOGRAPHIC SETTING: Cabreros soils are located on toeslopes of structural benches on sills at elevations from 6,000 to 7,000 feet and slopes of 2 to 6 percent. They formed in slope alluvium and eolian material derived from monzonite. Mean annual precipitation ranges from 10 to 13 inches with about 45 percent falling as rain from high-intensity convective thunderstorms between July and September. Mean annual air temperature ranges from 50 to 52 degrees F with a frost-free period of about 150 to 170 days.

GEOGRAPHICALLY ASSOCIATED SOILS: These are the Hagerman and Kech series found on adjacent upland areas, neither of which have calcic horizons. In addition, Kech soils are shallow to sedimentary bedrock.

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

USE AND VEGETATION: Dominant use is for rangeland. The historic climax vegetation is blue grama, galleta, oak, black grama, and oneseed juniper. The ecological site is Hills(R036XB124NM).

DISTRIBUTION AND EXTENT: Cabreros soils are of small extent on the Galisteo Basin part of the Mexican Highland section of the Basin and Range province in northcentral New Mexico. The MLRA is 36.

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

SERIES ESTABLISHED: Santa Fe County (Santa Fe Area), New Mexico, 2008. The name Cabreros is taken from a mesa near the type location.

REMARKS: Diagnostic horizons and features recognized in this pedon are:
Ochric epipedon- 0 to 2 inches (A horizon)
Argillic horizon- 2 to 25 inches (Bt and Btk horizons)
Secondary carbonates- 18 to 34 inches. (Btk and BCk horizon)
Calcic horizon- 25 to 34 inches (BCk horizon)
Particle-size control section 2 to 22 inches (upper 20 inches of the argillic horizon)
Paralithic Material- 34 to 47 inches (Cr horizon)
Lithic contact- at 47 inches (R horizon)

Classified according to Keys to Soil Taxonomy Tenth Edition, 2006.

ADDITIONAL DATA: Calcium carbonate equivalent was measured with a clacimeter.


National Cooperative Soil Survey
U.S.A.