LOCATION BECLABITO          NM+AZ CO
Established Series
Rev. JVC/RJA/LWH/CDH/DKR/WWJ
05/2006

BECLABITO SERIES


The Beclabito series consists of deep, well drained, sodic soils that formed in alluvium and residuum derived from sandstone and shale. Beclabito soils are on toeslopes between cuestas, and on footslopes and alluvial cones of escarpments. Permeability is moderately slow. Slopes are 1 to 45 percent. Mean annual precipitation is about 11 inches and mean annual temperature is about 51 degrees F.

TAXONOMIC CLASS: Fine-loamy, mixed, active, mesic Haplic Ustic Natrargids

TYPICAL PEDON: Beclabito fine sandy loam -- on a plane toeslope between cuestas sloping 4 percent to the east at 5,170 feet elevation -- rangeland. (Colors are for dry soil unless otherwise noted. When described, the pedon was dry throughout.)

A-- 0 to 4 inches; brown (7.5YR 5/4) fine sandy loam, brown (7.5YR 4/4) moist; moderate medium platy structure parting to weak fine granular; soft, very friable, slightly sticky and nonplastic; few fine and common very fine roots; slightly effervescent; moderately alkaline (pH 8.0); clear smooth boundary. (2 to 5 inches thick)

Btk-- 4 to 14 inches; strong brown (7.5YR 5/6) fine sandy loam, strong brown (7.5YR 4/6) moist; moderate medium prismatic structure parting to weak coarse subangular blocky; hard, firm, slightly sticky and slightly plastic; common fine and very fine roots; few very fine continuous tubular pores; common thin clay films on faces of peds, lining pores and bridging sand grains; strongly effervescent, secondary calcium carbonates segregated in few fine irregularly shaped accumulations on faces of peds; strongly alkaline (pH 8.6); clear smooth boundary. (3 to 10 inches thick)

Btkn1-- 14 to 23 inches; light brown (7.5YR 6/4) with pinkish white (7.5YR 8/2) sandy clay loam, strong brown (7.5YR 4/6) with light brown (7.5YR 6/4) moist; weak medium prismatic structure parting to moderate coarse subangular blocky; very hard, very firm, slightly sticky and slightly plastic; few fine and common very fine roots; few very fine continuous tubular pores; few thin clay films on faces of peds and bridging sand grains; violently effervescent; secondary calcium carbonates segregated in common medium and large irregularly shaped accumulations in soft masses and on faces of peds; strongly alkaline (pH 8.8); clear irregular boundary. (5 to 12 inches thick)

Btkn2-- 23 to 36 inches; strong brown (7.5YR 5/6) sandy clay loam, strong brown (7.5YR 4/6) moist; moderate medium prismatic structure parting to moderate coarse subangular blocky; very hard, very firm, slightly sticky and slightly plastic; few fine and common very fine roots; few very fine continuous tubular pores; few thin clay films on faces of peds, lining pores and bridging sand grains; strongly effervescent; secondary calcium carbonates segregated in few medium irregularly shaped accumulations on faces of peds; strongly alkaline (pH 9.0); abrupt wavy boundary. (0 to 13 inches thick)

2Bkn1-- 36 to 45 inches; very pale brown (10YR 7/4) parachannery sandy clay loam, yellowish brown (10YR 5/4) moist; moderate coarse subangular blocky structure; hard, firm, slightly sticky and slightly plastic; few fine and very fine roots; few very fine random tubular pores; 10 percent soft sandstone and 5 percent soft shale fragments; 5 percent channers; violently effervescent; secondary calcium carbonates segregated in few fine and medium irregularly shaped accumulations on faces of peds and on rock fragments; strongly alkaline (pH 9.0); clear wavy boundary. (6 to 16 inches thick)

2Bkn2-- 45 to 56 inches; light gray (10YR 7/1) parachannery clay loam, gray (10YR 5/1) moist; weak coarse subangular blocky structure; slightly hard, friable, sticky and plastic; few fine and very fine roots; common very fine random tubular pores; 10 percent soft sandstone and 10 percent soft shale fragments; violently effervescent; secondary calcium carbonates segregated in common, fine and medium, irregularly shaped accumulations on faces of peds and rock fragments; strongly alkaline (pH 9.0); abrupt wavy boundary. (11 to 24 inches thick)

2R-- 56 inches; hard sandstone bedrock

TYPE LOCATION: San Juan County, New Mexico; on the Navajo Indian Reservation about 18 miles west of Shiprock and 3 miles east of the village of Beclabito; 1,850 feet west and 750 feet south of the northeast corner of section 5, T.30N., R.20W; 36 degrees 50 minutes 53 seconds north latitude and 108 degrees 58 minutes 36 seconds west longitude.

RANGE IN CHARACTERISTICS:

Soil Moisture - Typically, the soil moisture control section (SMCS) is intermittently moist in some part from July to October and December to mid-April. The winter moisture peak is not as high as the summer peak. The SMCS 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. Ustic aridic moisture regime.

Soil temperature - 52 to 54 degrees F.

Soil depth - 40 to 60 inches to bedrock

Silicate clay content, control section weighted average - 18 to 35 percent

Depth to base of Natric horizon - 20 to 40 inches

Depth to calcic horizon - 14 to 35 inches

Reaction - moderately to strongly alkaline

A horizon - Hue: 5YR or 7.5YR
Value: 5 or 6 dry, 3 or 4 moist
Texture: fine sandy loam or very cobbly very fine sandy loam
Salinity, mmhos/cm: 0 to 2
Sodicity, SAR: 0 to 5
Rock fragments: Total range is 0 to 60 percent
0 to 25 percent cobbles
0 to 10 percent channers
0 to 30 percent gravel
0 to 10 percent stones
0 to 5 percent boulders

Bt, Btk or Btn horizon - Hue: 5YR or 7.5YR
Value: 5 or 6 dry, 4 or 5 moist
Chroma: 4 through 6
Texture: fine sandy loam, sandy clay loam or gravelly clay loam
Clay content: 18 to 35 percent
Salinity, mmhos/cm: 0 to 4
Sodicity, SAR: 5 to 30
Rock fragments: Total range is 0 to 25 percent
0 to 10 percent channers
0 to 10 percent gravel
0 to 5 percent cobbles
Calcium carbonate equivalence: 5 to 10 percent

Btkn horizons - Hue: 5YR or 7.5YR
Value: 5 through 8 dry, 4 through 6 moist
Chroma: 2 through 6
Texture: fine sandy loam, sandy clay loam, gravelly clay loam or gravelly sandy clay loam
Clay content: 18 to 35 percent
Salinity, mmhos/cm: 0 to 8
Sodicity, SAR: 5 to 30
Rock fragments: Total is 0 to 35 percent
0 to 10 percent channers
0 to 25 percent gravel
0 to 10 percent cobbles
Calcium carbonate equivalence: 10 to 30 percent
Other features: 0 to 20 percent soft, slakable shale or sandstone fragments

2Bkn, 2BCkn and Bkyn horizons - Hue: 2.5YR through 5GY
Value: 5 through 8 dry, 4 through 6 moist
Chroma: 1 through 6
Texture: sandy loam, fine sandy loam, sandy clay loam, clay loam, silty clay loam or clay
Clay content: 10 to 50 percent
Salinity, mmhos/cm: 2 to 16
Sodicity, SAR: 13 to 30
Rock fragments: Total is 0 to 15 percent
0 to 10 percent channers
0 to 5 percent gravel
Calcium carbonate equivalence: 5 to 40 percent depending on texture
Other features: 5 to 60 percent soft, slakable shale or sandstone fragments; some pedons have up to 5 percent secondary gypsum.

COMPETING SERIES: There are no competing series.

GEOGRAPHIC SETTING: Beclabito soils are on toeslopes between cuestas and on footslopes and alluvial cones of escarpments. They formed in alluvium and residuum derived from Jurassic and Cretaceous sandstone and shale. Slopes range from 1 to 45 percent. Elevation ranges from 4,900 to 6,500 feet. The mean annual precipitation is 8 to 13 inches about half of which falls as rain from high-intensity thunderstorms between July and September. The remainder falls as gentle rain or snow between December and mid-April. The mean annual temperature is 50 to 52 degrees F. The average frost-free period is 130 to 150 days.

GEOGRAPHICALLY ASSOCIATED SOILS: These are the Bodot, Farview, McElmo, and Snapill soils. Bodot soils are moderately deep and lack natric horizons. Farview soils are very shallow to sandstone on adjacent dipslopes of cuestas and summits of structural benches. McElmo soils are fine textured, have gypsic horizons and are on adjacent dipslopes of cuestas. Snapill soils are fine-silty and have argillic horizons.

DRAINAGE AND PERMEABILITY: Well drained; medium to rapid runoff; moderately slow permeability

USE AND VEGETATION: Beclabito soils are used for livestock grazing. Present vegetation is galleta, alkali sacaton, Indian ricegrass, sand dropseed, bottlebrush squirreltail, shadscale and scattered, small Utah juniper.

DISTRIBUTION AND EXTENT: Beclabito soils are of small extent on the Four Corners Platform and Blanding Basin portions of the Colorado Plateau province in northwest New Mexico, northeast Arizona, and southwest Colorado. LRR-D, MLRA 35.

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

SERIES ESTABLISHED: Shiprock Area, Parts of San Juan County, New Mexico and Apache County, Arizona; 1993.

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

Ochric epipedon - The zone from the soil surface to a depth of about 4 inches. (A horizon)

Natric horizon - The zone from 4 to about 36 inches. (Btk, Btkn1, and Btkn2 horizons)

Haplic subgroup - SAR of less than 13 in most of the natric horizon, but greater than 13 within 16 inches of the upper boundary (lower Btkn1 horizon).

Calcic horizon - The zone from 14 to about 56 inches. (Btkn1, Btkn2, 2Bkn and 2BCkn horizons)

Lithic contact - The presence of hard sandstone bedrock at about 56 inches.

At the type location in the Shiprock Area the mean annual precipitation ranges from 8 to 12 inches, but in the Ute Mountain Area the precipitation ranges from 10 to 13 inches.

ADDITIONAL DATA: Salinity values were determined with a Wheatstone bridge and Instant EC Salinity kit. Calcium carbonate equivalence determined with a field volume calcimeter. One pedon sampled for BIA soils lab in Gallup, New Mexico as sample S88NM-045-1. Lab results confirm the Haplic subgroup placement.

Classified according to Keys to Soil Taxonomy Ninth Edition, 2003


National Cooperative Soil Survey
U.S.A.