LOCATION WILLIS             WA+OR
Established Series
Rev. ETH/RJE/TLA
11/2008

WILLIS SERIES


This Willis series consists of moderately deep to a duripan, well drained soils formed in loess containing minor amounts of volcanic ash. Willis soils are on uplands, alluvial fan terraces, and terraces. Slopes range from 0 to 65 percent. The mean annual precipitation is about 10 inches. The mean annual temperature is about 49 degrees F.

TAXONOMIC CLASS: Coarse-silty, mixed, superactive, mesic Haploduridic Durixerolls

TYPICAL PEDON: Willis silt loam - cultivated. (Colors are for dry soil unless otherwise stated).

Ap--0 to 8 inches; grayish brown (10YR 5/2) silt loam, very dark grayish brown (10YR 3/2) moist; weak fine granular structure; soft, very friable, slightly sticky and slightly plastic; many roots; slightly alkaline (pH 7.4); abrupt smooth boundary. (6 to 18 inches thick)

Bw--8 to 24 inches; brown (10YR 5/3) silt loam, dark brown (10YR 3/3) moist; weak medium subangular blocky structure; slightly hard, friable, slightly sticky and slightly plastic; common roots; few very fine tubular pores; slightly alkaline (pH 7.6); abrupt wavy boundary. (8 to 17 inches thick)

Bk--24 to 29 inches; pale brown (10YR 6/3) silt loam, dark yellowish brown (10YR 4/4) moist; massive; hard, friable, slightly sticky and slightly plastic; common roots; few very fine tubular pores; strongly effervescent; strongly alkaline (pH 8.6); abrupt smooth boundary. (4 to 18 inches thick)

2Bkqm--29 inches; lime-silica indurated duripan, lenses 1 to 12 inches thick that do not break down on acid treatment alone.

TYPE LOCATION: Adams County, Washington; about 500 feet south and 100 feet west of the NE corner of section 18, T. 20 N., R. 36 E.

RANGE IN CHARACTERISTICS: The mean annual soil temperature is 49 to 54 degrees F. The soil is usually dry in all parts between depths of 4 and 12 inches for one-half to three-fourths of the time when the soil temperature is above 41 degrees F. The depth to the duripan is 20 to 40 inches. In some pedons the pan grades into alternate layers of duripan and loess or is abruptly over basalt or Ringold sediments. The depth to calcium carbonate is 15 to 27 inches. The mollic epipedon is 7 to 18 inches thick. The particle-size control section has 10 to 15 percent clay.
The A horizon has value of 4 or 5 dry, 2 or 3 moist and chroma of 2 or 3 dry. Texture is silt loam, fine sandy loam or very fine sandy loam. It has 0 to 5 percent fine gravel. Reaction is neutral or slightly alkaline.
The Bw horizon has value of 5 or 6 dry and 3 or 4 moist, and chroma of 3 or 4 moist or dry. It has 0 to 5 percent fine gravel. It has subangular blocky or coarse prismatic structure. Reaction is neutral to moderately alkaline.
The Bk horizon has value of 5 to 8 dry and 3 to 6 moist and chroma of 1 to 4 moist or dry. It has 0 to 5 percent gravel and 0 to 3 percent cobbles. Reaction is moderately or strongly alkaline. It is slightly to strongly effervescent and contains 1 to 10 percent calcium carbonate.

COMPETING SERIES: There are no competing series. The Baker, Burke, and Endicott series are similar. Baker soils are coarse-loamy. Endicott soils are usually moist. Burke soils do not have a mollic epipedon.

GEOGRAPHIC SETTING: The Willis soils are on uplands, alluvial fan terraces, and terraces at elevations of 500 to 3,000 feet. Slopes are 0 to 65 percent. The soils formed in loess containing minor amounts of volcanic ash. The climate is semiarid with warm, dry summers and cool, moist winters. The mean annual precipitation is 9 to 12 inches. The average January temperature is 29 degrees F, average July temperature is 71 degrees F, and mean annual temperature is 48 to 52 degrees F. The frost-free season is 125 to 190 days.

GEOGRAPHICALLY ASSOCIATED SOILS: These are the Esquatzel, Farrell, Mikkalo, and Ritzville soils. Esquatzel soils are deep, are on bottomlands and lack a duripan. Farrell and Ritzville soils are deep upland soils. Mikkalo soils have a lithic contact at 20 to 40 inches.

DRAINAGE AND PERMEABILITY: Well-drained; slow or medium runoff; moderate permeability above the lime-silica cemented layer.

USE AND VEGETATION: Used for production of small grains in a dryland winter wheat-summer fallow rotation and for grazing. The native vegetation is mainly bluebunch wheatgrass, Sandberg bluegrass, arrowleaf, balsamroot, yarrow, and big sagebrush.

DISTRIBUTION AND EXTENT: Eastern Washington and eastern Oregon; MLRA 8. The series is of moderate extent.

MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Portland, Oregon

SERIES ESTABLISHED: Adams County, Washington, 1973.

REMARKS: Diagnostic horizons and features recognized in this pedon are:
Mollic epipedon from the surface to 8 inches
Cambic horizon from 8 to 24 inches
Zone of carbonate accumulation from 24 to 29 inches
Duripan 29 inches
The zone from 8 to 24 inches has mollic colors but has less than 1 percent organic matter.


National Cooperative Soil Survey
U.S.A.