LOCATION WALES              UT+NV
Established Series
Rev. VLP/RSJ/MJD/JBF
03/2010

WALES SERIES


The Wales series consists of very deep, well drained soils formed in alluvium derived from sandstone, shale, limestone, and igneous rocks. Wales soils are on alluvial fans, alluvial flats, valley floors, drainageways, and floodplains. Slopes are 0 to 8 percent. The mean annual precipitation is about 250 mm and the mean annual air temperature is about 9 degrees C.

TAXONOMIC CLASS: Fine-loamy, mixed, superactive, calcareous, mesic Xeric Torrifluvents

TYPICAL PEDON: Wales loam - rangeland (Colors are for air dry soil unless otherwise noted.)

Ap1--0 to 8 cm; brown (10YR 5/3) loam, dark brown (10YR 3/3) moist; moderate very thin platy structure parting to moderate very fine granular; slightly hard, friable, moderately sticky and moderately plastic; few fine and very fine roots; few fine and common very fine vesicular pores; strongly effervescent; moderately alkaline (pH 8.3); clear smooth boundary.

Ap2--8 to 23 cm; brown (10YR 5/3) silt loam, dark brown (7.5YR 3/4) moist; weak coarse subangular blocky structure parting to moderate fine and very fine subangular blocky; slightly hard, firm, moderately sticky and moderately plastic; few fine and very fine roots; few medium, fine and common very fine random tubular pores; strongly effervescent; moderately alkaline (pH 8.4); abrupt wavy boundary.

C1--23 to 43 cm; brown (10YR 5/3) silt loam, dark brown (7.5YR 3/4) moist; weak medium and fine subangular blocky structure; slightly hard, friable, slightly sticky and slightly plastic; few fine and very fine roots; few medium, fine and common very fine random tubular pores; strongly effervescent; moderately alkaline (pH 8.3); clear wavy boundary.

C2--43 to 53 cm; brown (10YR 5/3) silt loam, dark brown (10YR 3/3) moist; weak thin platy structure parting to weak fine subangular blocky; hard, friable, moderately sticky and moderately plastic; few fine and very fine roots; few medium and common very fine random tubular pores; strongly effervescent; moderately alkaline (pH 8.2); abrupt smooth boundary.

Ab--53 to 66 cm; brown (10YR 5/3) loam; dark brown (7.5YR 3/2) moist; moderate thin platy structure parting to weak fine subangular blocky; hard, firm, moderately sticky and moderately plastic; few very fine roots; few medium, common fine and very fine random tubular pores; slightly effervescent; moderately alkaline (pH 8.1); clear smooth boundary.

C3--66 to 81 cm; brown (10YR 5/3) loam, dark brown (7.5YR 3/4) moist; weak coarse subangular blocky structure parting to weak medium subangular blocky; slightly hard, firm, moderately sticky and moderately plastic; few very fine roots; few medium, common fine and very fine random tubular pores; strongly effervescent; moderately alkaline (pH 8.4); clear smooth boundary.

C4--81 to 104 cm; pale brown (10YR 6/3) sandy loam, brown (7.5YR 4/4) moist; weak coarse and medium subangular blocky structure; slightly hard, friable, slightly sticky and slightly plastic; few very fine roots; few fine and common very fine random tubular pores; strongly effervescent; moderately alkaline (pH 8.2); gradual wavy boundary.

C5--104 to 135 cm; brown (7.5YR 5/4) silt loam, brown (7.5YR 4/4) moist; weak coarse and medium subangular blocky structure; very hard, friable, slightly sticky and slightly plastic; few very fine roots; few fine and common very fine random tubular pores; strongly effervescent; moderately alkaline (pH 8.2); clear wavy boundary.

C6--135 to 145 cm; pale brown (10YR 6/3) sand, brown (10YR 4/3) moist; single grain; loose, nonsticky and nonplastic; few fine and common very fine interstitial pores; slightly effervescent; strongly alkaline (pH 8.8); clear smooth boundary.

C7--145 to 152 cm; brown (10YR 5/3) silt loam, brown (7.5YR 4/4) moist; moderate thin platy structure parting to moderate medium and fine subangular blocky; hard, friable, slightly sticky and slightly plastic; few medium, fine and common very fine random tubular pores; strongly effervescent; moderately alkaline (pH 8.3).

TYPE LOCATION: Iron County, Utah; about 0.75 miles north-northeast of Newcastle, about 2,170 feet south and 1,480 feet east of the northwest corner of section 9, T. 36 S., R. 15 W; USGS Newcastle 7.5 minute quadrangle; latitude 37 degrees 41 minutes 8 seconds N and longitude 113 degrees 32 minutes 38 seconds W; NAD 83.

RANGE IN CHARACTERISTICS:
Soil moisture: Usually dry; moist in winter and spring and for brief periods in late summer due to convection storms; aridic bordering on xeric soil moisture regime.
Mean annual soil temperature: 8.0 to 12 degrees C.
Mean summer soil temperature: 17 to 19 degrees C.
Organic matter content: Decreases irregularly with depth or remains above .35 percent to a depth of 125 cm.

Particle-size control section - Clay content: 18 to 27 percent.
Sand content: More than 15 percent.
Rock fragments: 0 to 15 percent gravel.

A horizon
Hue: 10YR or 7.5YR.
Value: 5 or 6 dry, 3 through 6 moist.
Chroma: 2 through 6.
Reaction: Slightly alkaline to strongly alkaline.

C horizon
Hue: 10YR or 7.5YR.
Value: 5 through 8 dry, 3 through 6 moist.
Chroma: 2 through 6.
Texture: Loam or silt loam; thin layers of sand to silty clay loam are present in some pedons.
Clay content: 18 to 27 percent.
Sand content: More than 15 percent fine sand or coarser.
Rock fragments: 0 to 20 percent gravel.
Reaction: Moderately alkaline to strongly alkaline.

COMPETING SERIES: There are no competing series.

GEOGRAPHIC SETTING: Wales soils are on gently to strongly sloping alluvial fans, alluvial flats, valley floors, drainageways,and flood plains at elevations of 1,430 to 2,110 meters. Slopes are 0 to 8 percent. They formed in mixed alluvium from sandstone, shale, limestone, and igneous rocks. The climate is dry subhumid. Mean annual air temperature ranges from 7 to 11 degrees C. Average annual precipitation ranges from 200 to 300 mm. Frost free period is 100 to 140 days.

GEOGRAPHICALLY ASSOCIATED SOILS: These are the Amtoft, Atepic, Borvant, Fontreen, and Lodar soils. Amtoft, Atepic and Lodar soils are less than 50 cm deep over a lithic or paralithic contact. Borvant soils are less than 50 cm deep over a petrocalcic horizon. Fontreen soils have mollic epipedons and have more than 35 percent coarse fragments in their control section.

DRAINAGE AND PERMEABILITY: Well drained; medium runoff; moderate permeability; moderately high saturated hydraulic conductivity.

USE AND VEGETATION: These soils are used as livestock grazing. The principal plants are big sagebrush, western wheatgrass, bluebunch wheatgrass, Indian ricegrass, squirreltail grass, yellowbrush and rabbitbrush.

DISTRIBUTION AND EXTENT: Central Utah, and west central Nevada; MLRA 47, 28A; these soils are of moderate extent.

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

SERIES ESTABLISHED: Sanpete Soil Survey Area, Utah, 1971.

REMARKS: In April 1995 the type location was moved from Sanpete County to Iron County to better represent the series concept.

Diagnostic horizons and features recognized in this pedon are:
Ochric epipedon - The zone from 0 to 18 cm (Ap1 and part of the Ap2 horizons).
Xeric feature - Soil moisture regime is aridic bordering on xeric.
Particle-size control section - The zone from 25 to 100 cm (C2, Ab, C3 and part of the C1 and C4 horizons).


National Cooperative Soil Survey
U.S.A.