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Freeman soil series

Landscape--Columbia basalt plateau

Landform--loess hills

Slope--0 to 25 percent

Parent material--Holocence and late Pleistocence loess with a minor amount of volcanic ash in upper part

Mean annual precipitation--about 580 mm

Mean annual air temperature--about 8 degrees C

Depth class--very deep

Drainage class--moderately well drained

Soil moisture regime--xeric

Soil temperature regime--mesic

Soil moisture subclass--aquic

 

TAXONOMIC CLASS: Fine-silty, mixed, superactive, mesic Aquandic Palexeralfs

 

Mean annual soil temperature--8 to 9 degrees C

Moisture control section--usually moist, but dry 60 to 75 consecutive days following summer solstice in most years

Depth to argillic horizon--40 to 75 cm

Average content of clay in particle-size control section--20 to 35 percent in upper part, 27 to 40 percent in lower part

Thickness of volcanic ash influence--18 to 25 cm

 

 

USE AND VEGETATION:

Use--dominantly crop production

Common crops--small grain, peas, alfalfa, grass

Potential natural vegetation--ponderosa pine, scattered Douglas-fir, Idaho fescue, bluebunch wheatgrass, pinegrass, sedges, rose, common snowberry, serviceberry

 

DISTRIBUTION AND EXTENT: Eastern Washington and possibly northern Idaho; MLRA 9; moderate extent

 

For a detailed description, visit:

soilseries.sc.egov.usda.gov/OSD_Docs/F/FREEMAN.html

 

For acreage and geographic distribution, visit:

casoilresource.lawr.ucdavis.edu/see/#freeman

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Uploaded on January 25, 2011
Taken in January 2000