LOCATION MCCUTCHEN NV
Established Series
Rev. LNL/LR/LCL/JBF
06/2016
MCCUTCHEN SERIES
The McCutchen series consists of very deep, well drained soils that formed in alluvium derived mainly from ignimbrite with an influence of carbonates from ground water. McCutchen soils are on toe slopes of fan remnants and alluvial fans. Slopes are 0 to 2 percent. The mean annual precipitation is about 175 mm and the mean annual air temperature is about 11 degrees C.
TAXONOMIC CLASS: Coarse-loamy, mixed, superactive, mesic Typic Haplocalcids
TYPICAL PEDON: McCutchen loam - rangeland (Colors for dry conditions unless otherwise noted).
A1--0 to 3 cm; gray (10YR 6/1) loam, grayish brown (10YR 5/2) moist; massive; soft, very friable, nonsticky and nonplastic; devoid of plant roots; many very fine interstitial pores; slightly effervescent; strongly alkaline (pH 8.7); abrupt smooth boundary. (1 to 4 cm thick)
A2--3 to 8 cm; light gray (10YR 7/2) loam, brown (10YR 5/3) moist; moderate thick platy structure; soft, very friable, slightly sticky and slightly plastic; few fine and medium roots; many fine and medium vesicular pores; slightly effervescent; strongly alkaline (pH 8.7); abrupt smooth boundary. (5 to 10 cm thick)
Bw1--8 to 25 cm; light brownish gray (10YR 6/2) fine gravelly loam (15 percent fine gravel), brown (10YR 4/3) moist; weak thick platy structure; slightly hard, friable, slightly sticky and slightly plastic; many fine and medium roots; common very fine and fine tubular, and many very fine interstitial pores; slightly effervescent; strongly alkaline (pH 8.7); clear smooth boundary. (10 to 20 cm thick)
Bw2--25 to 41 cm; very pale brown (10YR 7/3) loam, brown (10YR 5/3) moist; strong medium platy structure; slightly hard, friable, slightly sticky and slightly plastic; common very fine and fine roots; many very fine interstitial pores; strongly effervescent; strongly alkaline (pH 8.7); clear smooth boundary. (13 to 23 cm thick).
Bk--41 to 91 cm; light gray (10YR 7/2) sandy loam, pale brown (10YR 6/3) moist; massive; very hard, firm, slightly sticky and slightly plastic; few very fine and fine roots; few very fine tubular and many micro and very fine interstitial pore; carbonate is disseminated; crumbles in dilute hydrochloric acid; violently effervescent; strongly alkaline (pH 8.7); clear wavy boundary. (30 to 60 cm thick)
2C--91 to 152 cm; very pale brown (10YR 8/2) loamy sand, light brownish gray (10YR 6/2) moist; massive; slightly hard, friable, nonsticky and nonplastic; few very fine roots; many very fine interstitial pores; violently effervescent; strongly alkaline (pH 8.7).
TYPE LOCATION: Lincoln County, Nevada. 2640 feet east and 1320 feet north of the southeast corner of section 23, T. 2 S., R. 55 E., MDBM; USGS Honest John Well 7.5 minute topographic quadrangle; latitude 37 degrees 45 minutes 18 seconds N and longitude 115 degrees 45 minutes 37 seconds W; WGS84 Decimal Degrees 37.7550000 latitude, -115.7602778 longitude.
RANGE IN CHARACTERISTICS:
Soil moisture: Usually dry; moist in winter and spring and for brief periods in late summer due to convection storms; typic aridic soil moisture regime.
Mean annual soil temperature: 12 to 15 degrees C.
Reaction: Moderately alkaline or strongly alkaline.
Depth to calcic horizon: 30 to 50 cm.
Thickness of calcic horizon: 30 to 60 cm.
Other features: Mineralogy is mixed but has a strong influence from pyroclastic materials.
Particle-size control section - Clay content: Average 5 to 18 percent.
Rock fragments: Average 0 to 15 percent.
A horizon
Value: 7 or 6 dry and 5 or 4 moist.
Chroma: 1 through 3.
Bw horizons
Value: 7 or 6 dry and 5 or 4 moist.
Chroma: 2 or 3.
Texture: Stratified and is predominantly sandy loam, fine sandy loam or loam.
Effervescence: Slightly effervescent or strongly effervescent.
Bk horizon
Value: 7 or 8 dry and 6 or 7 moist.
Chroma: 1 or 2.
Rock fragments: Average 0 to 25 percent.
Texture: Stratified and is predominantly sandy loam, fine sandy loam or loam.
Consistence: Very hard or hard dry and firm or very firm moist.
Calcium carbonate equivalent: 10 to 20 percent.
2C horizon
Value: 7 or 8 dry and 6 or 7 moist.
Chroma: 1 or 2.
Texture: Loamy sand or gravelly loamy sand.
Rock fragments: Average 0 to 25 percent.
Calcium carbonate equivalent: 5 to 15 percent.
COMPETING SERIES: These are the
Bluechief,
Boreham,
Hiko Springs,
Kaito,
Kinan,
Moffat,
Nakai,
Nakoy,
Nolava,
Nuahs,
Pagina,
Riemod and
Trook series
Bluechief and
Pagina soils are moderately deep to bedrock.
Boreham,
Nakoy,
Nolava,
Riemod and
Trook soils have mean annual soil temperatures less than 12 degrees C.
Hiko Springs soils have an A horizon that is strongly effervescent.
Kaito soils have bedrock at 100 to 150 cm.
Kinan,
Moffat and
Nakai soils have hues redder than 10YR and lack pyroclastic materials.
Nuahs soils have a depth of 5 to 30 cm to the top of the calcic horizon.
GEOGRAPHIC SETTING: McCutchen soils are on toe slopes of alluvial fans near or adjacent to playas. They have developed in alluvium derived mainly from ignimbrite, and have been influenced by precipitation of carbonate in the lower horizons when the playas contained water. These soils are at elevations of 1,370 to 1,585 meters. The mean annual precipitation is 150 to 200 mm. The mean annual air temperature is10 to 13 degrees C and the frost-free period 130 to 150 days.
GEOGRAPHICALLY ASSOCIATED SOILS: These are the
Fang,
Jarboe and
Kawich soils. Fang and Kawich soils lack calcic horizons. Jarboe soils have fine-loamy particle-size control sections.
DRAINAGE AND SATURATED HYDRAULIC CONDUCTIVITY: Well drained. These soils apparently developed under more poorly drained conditions when the playas contained water, slow runoff; moderately low saturated hydraulic conductivity.
USE AND VEGETATION: Used for livestock grazing. The dominant vegetation consists of shadscale, gray molly, bud sagebrush, littleleaf horsebrush, and greasewood.
DISTRIBUTION AND EXTENT: South central Nevada, MLRA 29, not extensive.
MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Davis, California
SERIES ESTABLISHED: Lincoln County, Nevada, Penoyer Valley, 1965. McCutchen is the name of a pass at the northern end of Penoyer Valley.
REMARKS: These soils were formerly classified as Calcium Carbonate Solonchaks.
Diagnostic horizons and features recognized in this pedon are:
Ochric epipedon - The zone from the soil surface to 18 cm (A1, A2 and part of the Bw1 horizons).
Cambic horizon - The zone from 8 to 41 cm (Bw1 and Bw2 horizons).
Calcic horizon - The zone from 41 to 91 cm (Bk horizon).
Particle-size control section - The zone from 25 to 100 cm (Bw2, Bk and part of 2C horizons).
National Cooperative Soil Survey
U.S.A.