LOCATION KECKO              ID
Established Series
Rev. DMD/MEJ/CLM
02/1999

KECKO SERIES


The Kecko series consists of very deep or deep to a duripan, well drained soils that formed in alluvium and eolian material. Kecko soils are on terraces and basalt plains, and have slopes of 0 to 20 percent. Permeability is moderately rapid. The average annual precipitation is about 9 inches and the average annual air temperature is about 50 degrees F.

TAXONOMIC CLASS: Coarse-loamy, mixed, superactive, mesic Xeric Haplocalcids

TYPICAL PEDON: Kecko loamy fine sand - cultivated. (Colors are for dry soil unless otherwise noted.)

Ap--0 to 4 inches; brown (10YR 5/3) loamy fine sand, very dark grayish brown (10YR 3/2 moist; single grain; loose, nonsticky and nonplastic; many very fine and medium roots; many very fine irregular and common fine irregular pores; neutral; clear smooth boundary (4 to 10 inches thick)

Bw1--4 to 9 inches; brown (10YR 5/3) fine sandy loam, very dark grayish brown (10YR 3/2) moist; moderate medium subangular blocky structure; slightly hard, friable, nonsticky and nonplastic; many very fine roots; common fine tubular pores; neutral; gradual wavy boundary.

Bw2--9 to 21 inches; brown (10YR 5/3) loam, dark grayish brown (10YR 4/2) moist; moderate medium subangular blocky structure; slightly hard, friable, slightly sticky and slightly plastic; common very fine and fine roots; common fine tubular pores; neutral; gradual wavy boundry. (Combined thickness of Bw is 15 to 30 inches thick.)

Bk1--21 to 26 inches; pale brown (10YR 6/3) very fine sandy loam, brown (10YR 4/3) moist; moderate medium subangular blocky structure; hard, friable, slightly sticky and slightly plastic; common very fine and fine roots; common fine tubular pores; strongly effervescent; moderately alkaline; clear wavy boundary.

Bk2--26 to 42 inches; very pale brown (10YR 7/3) very fine sandy loam, brown (10YR 5/3) moist; wweak fine platy structure; hard, friable, slightly sticky and slightly plastic; common very fine roots; few fine tubular pores; strongly effervescent; moderately alkaline; clear wavy boundary. (Combined thickness of Bk is 10 to 25 inches thick.)

2C--42 to 62 inches; very pale brown (10YR 7/3) coarse silt loam, brown (10YR 5/3) moist; massive; soft, very friable, nonsticky and nonplastic; few very fine roots; few fine tubular pores; strongly effervescent; moderately alkaline.

TYPE LOCATION: Minidoka County, Idaho; 1 mile west and 4 miles north of Rupert; 570 feet south and 72 feet east of the northwest corner of the SE 1/4 of section 6, T. 9 S., R. 24 E.

RANGE IN CHARACTERISTICS:

Depth to the 2C horizon - greater than 40 inches
Depth to bedrock - more than 60 inches
Average annual soil temperature - 47 to 54 degrees F.
Depth to carbonates and calcic horizon - 20 to 40 inches
Present in some pedons - Bkqm horizons (below 40 inches)
Particle-size control section
clay content - 10 to 18 percent
gravel - 0 to 10 percent

Ap horizon
Value - 5 or 6 dry, 2 through 4 moist
Chroma - 2 or 3 dry or moist
Reaction - neutral or slightly alkaline

Bw horizon
Value - 5 or 6 dry, 3 to 5 moist
Chroma - 2 through 4 dry or moist
Texture - FSL, SL, VFSL, LVFS, or L

Bk horizon
Value - 6 through 8 dry, 4 through 6 moist
Chroma - 2 through 4 dry or moist
Texture - FSL, VFSL, LFS, LVFS, FS, S, L, LS, or SL
Calcium carbonate equivalent - 15 to 25 percent

2C and 3C horizons
Value - 6 through 8 dry, 4 through 6 moist
Chroma - 2 or 3 dry, 3 or 4 moist
Texture - L, SIL, SL, LS, S, LVFS, STX-LS, STX-SL, FS
Calcium carbonate equivalent - 15 to 25 percent

COMPETING SERIES: These are the Bertelson, Briabbit, Crestline, Delco, Escalante, Palisade, Sagehill, Somsen and Strevell series. Crestline soils have carbonates at 10 to 20 inches and have a gravelly control section. Briabbit soils have paralithic contact above a depth of 40 inches. Sagehill soils have 2 to 8 percent clay in the particle-size control section. Bertelson, Escalante and Palisade soils are calcareous to the surface. Delco soils have a calcic horizon at 3 to 18 inches. Somsen soils are 20 to 40 inches to bedrock. Strevell soils have a calcic horizon at 10 to 20 inches.

GEOGRAPHIC SETTING: Kecko soils are on basalt plains and terraces at elevations of 2,800 to 4,600 feet. Slopes are 0 to 20 percent. The soils formed in alluvium and eolian material from mixed sources. The semiarid climate has relatively dry summers. The average annual precipitation is 8 to 11 inches, including 1 to 3 feet of snow. The average annual temperature is 46 to 52 degrees F. The frost-free period is 100 to 140 days.

GEOGRAPHICALLY ASSOCIATED SOILS: These are the Declo, Escalante, Paulville, Quincy, and Taunton soils. Declo soils are calcareous to the surface. Escalante soils have hues of 7.5YR and are calcareous to the surface. Paulville soils have argillic horizons. Quincy soils have a sandy control section. Taunton soils have duripans above 40 inches.

DRAINAGE AND PERMEABILITY: Well drained; slow or medium runoff; moderately rapid permeability.

USE AND VEGETATION: Kecko soils are used mostly for irrigated cropland and to a minor extent, rangeland. The natural vegetation is mainly basin big sagebrush, rabbitbrush, bluebunch wheatgrass, and Indian ricegrass. Crops are alfalfa, sugar beets, potatoes, beans, wheat, oats, barley, and pasture.

DISTRIBUTION AND EXTENT: Kecko soils are moderately extensive in south central Idaho.

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

SERIES ESTABLISHED: Minidoka County, Idaho, 1973.

REMARKS: Diagnostic horizons and features recognized in this pedon are:

Ochric epipedon - the zone from the soil surface to 4 inches (Ap horizon)

Cambic horizon - the zone from 4 to 21 inches (Bw1 and Bw2 horizons)

Calcic horizon - the zone from 21 to 42 inches (Bk1 and Bk2 horizons)


National Cooperative Soil Survey
U.S.A.