LOCATION TINNEY             NM
Established Series
Rev. DGS/RLB
07/2008

TINNEY SERIES


The Tinney series consists of very deep, well drained, moderately slow permeable soils that formed in alluvium. These nearly level to gently sloping soils are on inset fans on fan piedmonts. Slope ranges from 1 to 3 percent. Mean annual precipitation is about 11 inches and the mean annual air temperature is about 62 degrees F.

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

TYPICAL PEDON: Tinney loam - rangeland (Colors are for dry soil unless otherwise stated).

A--0 to 3 inches; light brown (7.5YR 6/4), crushed, loam, brown (7.5YR 4/4), crushed, moist; moderately thin platy structure parting to moderate very fine granular; slightly sticky and slightly plastic; common very fine roots throughout; 20 percent clay; violently effervescent throughout (HCl, 1 normal); abrupt smooth boundary (2 to 6 inches thick).

Bw--3 to 17 inches; brown (7.5YR 5/4), crushed, loam, brown (7.5YR 4/4), crushed, moist; moderate coarse prismatic structure parting to moderate fine subangular blocky; slightly hard, very friable, slightly sticky and slightly plastic; common very fine roots throughout; 20 percent clay; violently effervescent throughout (HCl, 1 normal); gradual smooth boundary (8 to 18 inches thick).

2Bt--17 to 36 inches; brown (7.5YR 5/4), crushed, sandy clay loam, brown (7.5YR 4/4), crushed, moist; weak coarse prismatic structure parting to moderate medium subangular blocky; slightly hard, very friable, slightly sticky and nonplastic; common very fine roots throughout; few distinct clay films on faces of peds; 25 percent clay; violently effervescent throughout (HCl, 1 normal); abrupt smooth boundary (6 to 25 inches thick).

3Bk1--36 to 45 inches; pink (7.5YR 8/3), exterior, and pink (7.5YR 7/3), interior, and pink (7.5YR 7/3), crushed, loam, light brown (7.5YR 6/4), crushed, moist; weak fine subangular blocky structure; very hard, friable, weakly cemented by carbonates, slightly sticky and nonplastic; common very fine roots throughout; 19 percent clay; many prominent continuous carbonate coats; violently effervescent throughout (HCl, 1 normal); clear smooth boundary.

3Bk2--45 to 57 inches; pink (7.5YR 8/3), exterior, and pink (7.5YR 7/4), interior, and pink (7.5YR 7/3), crushed, loam, light brown (7.5YR 6/4), crushed, moist; moderate fine subangular blocky structure; very hard, friable, very weakly cemented by carbonates, slightly sticky and nonplastic; common very fine roots throughout; 19 percent clay; many prominent discontinuous carbonate coats; violently effervescent throughout (HCl, 1 normal); clear smooth boundary (15 to 35 inches combined thickness of Bk1 and Bk2 horizons).

3Bk3--57 to 80 inches; light brown (7.5YR 6/4), crushed, loam, strong brown (7.5YR 5/6), crushed, moist; weak fine subangular blocky structure; hard, very friable, slightly sticky and slightly plastic; 19 percent clay; few prominent discontinuous carbonate coats; violently effervescent throughout (HCl, 1 normal).

TYPE LOCATION: Otero County, New Mexico; approximately 5 miles south and 2.7 miles east of Oro Grande;1,000 feet north and 400 feet west of the southeast corner, sec. 17, T. 23 S., R. 9 E. USGS Oro Grande South topographic quadrangle; latitude 32 degrees 18 minutes 3.5 seconds north and longitude 106 degrees 2 minutes 12 seconds west. UTM zone 13, 402402E, 3574084N; NAD 27.

RANGE IN CHARACTERISTICS:

Soil moisture: The soil moisture control section is usually dry in all parts less than three-fourths of the time that the soil temperature exceeds 41 degrees F. Ustic aridic moisture regime.

Mean annual soil temperature: 61 to 65 degrees F.

Depth to cambic horizon: 2 to 6 inches

Depth to the argillic horizon: 10 to 20 inches

Depth to calcic horizon: 20 to 40 inches

Particle-size control section (weighted average)
Clay content: 18 to 27 percent
Coarse fragment content: 0 to 1 percent

A horizon
Hue: 5YR or 7.5YR
Value: 4 to 6, dry or moist
Chroma: 3 or 4, dry or moist

Bw horizon
Hue: 5YR or 7.5YR
Value: 5 to 7 dry, 4 to 6 moist
Chroma: 3 to 6, dry or moist

2Bt horizon
Hue: 5YR or 7.5YR
Value: 5 to 7 dry, 4 to 6 moist
Chroma: 3 to 6, dry or moist
Texture: loam or sandy clay loam

3Bk horizon
Hue: 5YR or 7.5YR
Value: 6 to 8 dry, 4 to 6 moist
Chroma: 2 to 6, dry or moist
Texture: loam, fine sandy loam, or sandy clay loam

COMPETING SERIES: These are the Amarose (NM), Berino (NM), Grizzle (AZ), Gulch (AZ), Headquarters (NM), McAllister (AZ), McNeal (AZ), and Redona (NM) series. Amarose soils have series control sections that range to neutral and have hue of 2.5YR. It also has Btk horizon with 25 to 40 percent clay. The base of the argillic horizon is greater than 60 inches. Berino soils do not have cambic horizons. Grizzle soils are moderately deep to sandstone. Gulch soils have accumulations of gypsum in the profile. Headquarters soils have calcic horizons within 20 inches of the surface. McNeal soils have calcic horizons within 20 inches of the surface. Redona soils have up to 15 percent rock fragments in the series control section. Amarose and Redona soils are moist in the soil moisture control section during May and June and occur in the Great Plains. McAllister soils do not have a cambic horizon above the argillic horizon.

GEOGRAPHIC SETTING:
Parent material: alluvium
Landform: inset fans on fan piedmonts
Slope: 1 to 3 percent
Mean annual temperature: 60 to 64 degrees F.
Mean annual precipitation: 10 to 12 inches
Precipitation pattern: precipitation falls mostly during the months of July through September. The driest months are March and April. Precipitation during the months of January, February, and March is less than 13 percent of the total.
Frost-free period: 170 to 210 days
Elevation: 4,200 to 5,300 feet

GEOGRAPHICALLY ASSOCIATED SOILS: These are the Bankston, Bissett, Crossen, and Reyab series. Bankston soils are moderately deep to bedrock and are on hills. Bissett soils are shallow to bedrock and are on hills. Crossen soils are shallow and very shallow to a petrocalcic horizon are on erosional fan remnants on the fan piedmont. Reyab soils are fine-silty and do not have calcic horizons and are on similar positions.

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

USE AND VEGETATION: Used for grazing livestock. Vegetation is of the desert grassland type consisting of tobosa, burrograss, threeawn, creosotebush, mesquite, tarbush, desert holly, and globemallow.

DISTRIBUTION AND EXTENT: Southern New Mexico; LRR D, MLRA 42. The series is of small extent.

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

SERIES ESTABLISHED: Otero County, New Mexico; 2001.

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

Particle-size control section: The zone from 17 to 36 inches. (2Bt horizon)

Ochric epipedon: The zone from 0 to 3 inches. (A horizon)

Cambic horizon: The zone from 3 to 17 inches. (Bw horizon)

Argillic horizon: The zone from 17 to 36 inches. (2Bt horizon)

Calcic horizon: The zone from 36 to 57 inches. (3Bk1, 3Bk2 and 3Bk3 horizons)

Ustic feature: The soil has an aridic moisture regime that borders on the ustic regime.

The assignment of the cation-exchange activity class is inferred from lab data from similar soils in the surrounding area.

Classified according to Soil Taxonomy, Second Edition, 1999; Keys to Soil Taxonomy, Tenth Edition, 2006.

Updated competing series section 3/17/08, CEM


National Cooperative Soil Survey
U.S.A.