LOCATION HOSTA NMEstablished Series
TAXONOMIC CLASS: Fine, mixed, superactive, mesic Aridic Haplustalfs
TYPICAL PEDON: Hosta loam - rangeland. (Colors are for dry soil unless otherwise noted.)
A--0 to 2 inches; pale brown (10YR 6/3) loam, brown (10YR 4/3) moist; moderate medium platy structure; soft, very friable, nonsticky and slightly plastic; few very fine and fine roots; many fine vesicular pores; neutral (pH 7.2); abrupt smooth boundary.
Bt--2 to 4 inches; brown (10YR 4/3) clay loam, dark brown (10YR 3/3) moist; weak fine granular structure; soft friable, sticky and plastic; many very fine and common fine roots; common fine irregular pores; few faint bridges of clay films; slightly alkaline (pH 7.4); abrupt smooth boundary.
Btk1--4 to 11 inches; dark yellowish brown (10YR 4/4) clay loam, dark yellowish brown (10YR 3/4) moist; strong medium subangular blocky structure; very hard, very firm, sticky and plastic; common very fine and few fine and medium roots; common fine irregular pores; many prominent clay films on faces of peds; slightly effervescent; few fine filaments and masses of calcium carbonate; slightly alkaline (pH 7.6); clear smooth boundary.
Btk2--11 to 24 inches; yellowish brown (10YR 5/4) clay loam, dark yellowish brown (10YR 4/4) moist; strong medium subangular blocky structure; very hard, very firm, sticky and plastic; common very fine and few fine roots; common fine irregular pores; common prominent clay films on faces of peds; strongly effervescent; common fine filaments and masses of calcium of carbonate; slightly alkaline (pH 7.8); clear smooth boundary.
Btk3--24 to 37 inches; dark yellowish brown (10YR 4/4) clay, dark brown (10YR 3/3) moist; weak medium subangular blocky structure; very hard, very firm, very sticky and very plastic; few very fine roots; few fine irregular pores; common prominent clay films on faces of peds; slightly effervescent; few fine masses of calcium carbonate; slightly alkaline (pH 7.8); clear smooth boundary.
Btk4--37 to 51 inches; yellowish brown (10YR 5/4) clay, dark yellowish brown (10YR 4/4) moist; weak medium subangular blocky structure; very hard, very firm, very sticky and very plastic; few very fine roots; few very fine irregular pores; common distinct clay films on faces of peds; slightly effervescent; few fine masses of calcium carbonate; slightly alkaline (pH 7.8); clear smooth boundary.
Bk--51 to 65 inches; yellowish brown (10YR 5/4) sandy clay loam, dark yellowish brown (10YR 4/6) moist; massive; hard, firm, slightly sticky and slightly plastic; few very fine roots; few very fine irregular pores; strongly effervescent; common fine filaments of calcium carbonate; slightly alkaline (pH 7.8).
TYPE LOCATION: McKinley County, New Mexico; Horsehead Canyon Quadrangle; 400 feet north and 2,600 feet west of the southeast corner of sec. 5, T. 10 N., R. 17 W.; latitude 35 degrees, 7 minutes, 12 seconds and longitude 108 degrees, 39 minutes, 11 seconds.
RANGE IN CHARACTERISTICS:
Soil Moisture: The SMCS is usually moist, in all parts, for less than 90 cumulative days from April through October. It is usually dry, in some part, for more than 120 days cumulative days during the same period. It is continuously moist in some part November through April, but not moist all parts for 45 consecutive days from January through April. The period of maximum precipitation is July through October. The soil is driest during May and June. Aridic ustic moisture regime.
Soil temperature: averages 48 to 55 degrees F. at a depth of 20 inches
Rock fragments: less than 5 percent in any horizon
Carbonates: less than 5 percent calcium carbonate equivalent in any horizon
Particle-size control section: 35 to 55 percent clay
A horizon
Hue: 10YR or 2.5Y
Value: 4 to 6 dry, 4 or 5 moist
Chroma: 2, 3 or 4 dry and moist
Texture: Clay loam or loam
Reaction: Neutral or slightly alkaline
Bt & Btk horizon
Hue: to 7.5YR to 2.5Y
Value: 4, to 6 dry, 3 to 5 moist
Chroma: 3 or 4 dry, 2 to 4 moist
Texture: Clay loam, clay or sandy clay loam
Reaction: Slightly or moderately alkaline
Bk horizon
Hue: 7.5YR to 2.5Y
Value: 3, 4, 5, or 6 dry and moist
Chroma: 2 to 6 dry and moist
Texture: Silty clay loam, silty clay, clay, clay loam or sandy clay loam
COMPETING SERIES: These are the Durango (CO), Erramouspe (NM), Fikel (NM), Hualapai (AZ), Jacee (NM), Montecito (NM), Nogal (NM), Paguate (NM), Prater (CO), Teco (NM), Tinian (NM), and Wilmac (NM) series. Durango and Fikel soils have hues redder than 7.5YR. Hualapai, Jacee, Nogal, and Wilmac have a paralithic contact at 20 to 40 inches. Prater soils have 5 percent or more rock fragments in the profile. Erramouspe, Tinian and Paguate soils have a lithic contact at 20 to 40 inches. Montecito, Paguate, and Teco soils have calcic horizons.
GEOGRAPHIC SETTING: Hosta soils are on valley sides, drainageways, and plateaus at elevations of 6,600 to 7,600 feet. These soils formed in fan alluvium from shale and sandstone with some eolian deposits. Slopes are 1 to 8 percent. The average annual precipitation is 13 to 16 inches. Rain falls as intense summer thunderstorms and gentle winter rain or snow. The mean annual temperature is 46 to 53 degrees F. The frost-free period is 100 to 135 days.
GEOGRAPHICALLY ASSOCIATED SOILS: These are the Deschell, Orlie, Toldohn, and Nizhoni soils. Deschell and Orlie are fine-loamy and Toldohn and Nizhoni are clayey and loamy, respectively.
DRAINAGE AND PERMEABILITY: Well drained, medium runoff and slow permeability.
USE AND VEGETATION: These soils are used for livestock grazing. Native vegetation is big sagebrush, rabbitbrush, threeawns, western wheatgrass, bottlebrush squirreltail and blue grama.
DISTRIBUTION AND EXTENT: West central and Northwest, New Mexico. MLRA 35, LRR-D. This series is of moderate extent.
MLRA OFFICE RESPONSIBLE: Phoenix, Arizona
SERIES ESTABLISHED: McKinley County Area, New Mexico; McKinley County and Parts of Cibola and San Juan Counties, 2001.
REMARKS: Diagnostic horizons and features recognized in this pedon are:
Ochric epipedon - The zone from the surface to about 2 inches.
Argillic horizon - The zone from about 2 inches to 51 inches.
Classified according to Soil Taxonomy Second Edition, 1999.
The type location was moved in April 2002.