LOCATION KOOTENAI           ID
Established Series
Rev. PMH/SHB/RJE/JAL
10/2002

KOOTENAI SERIES


The Kootenai series consists of very deep, well drained soils on recessional moraines, outwash plains, terraces, and terrace escarpments. They formed in glacial outwash material derived dominantly from granite, gneiss, and schist with a mantle of loess and volcanic ash. Permeability is moderate in the upper part and very rapid below. Slopes range from 0 to 55 percent. Average annual precipitation is about 28 inches and average annual air temperature is about 45 degrees F.

TAXONOMIC CLASS: Ashy over loamy-skeletal, glassy over isotic, frigid Typic Vitrixerands

TYPICAL PEDON: Kootenai gravelly silt loam, forested; on a 10 percent slope at 2,557 feet elevation. When described on August 6, 1975, the soil was dry throughout. (Colors are for dry soil unless otherwise stated.)

Oi--0 to 1.5 inch; undecomposed and partially decomposed needles, leaves, and twigs.

Oe--1.5 to 2.0; decomposed needles, leaves, and twigs.

A--2 to 8 inches; brown (10YR 4/3) gravelly ashy silt loam, very dark grayish brown (10YR 3/2) moist; moderate medium and coarse subangular blocky structure parting to weak fine and medium granular; soft, very friable, nonsticky and nonplastic; many very fine and fine, common medium, and few coarse roots; common very fine and few fine, medium, and coarse tubular pores; 20 percent pebbles; slightly acid (pH 6.2); clear wavy boundary. (4 to 6 inches thick)

Bw1--8 to 24 inches; yellowish brown (10YR 5/4) gravelly ashy silt loam, brown (10YR 4/3) moist; weak medium and coarse subangular blocky structure; soft, friable, nonsticky and slightly plastic; common very fine and fine and few medium and coarse roots; common very fine, few fine, and medium tubular pores; 30 percent pebbles; slightly acid (pH 6.5); clear wavy boundary. (12 to 20 inches thick)

Bw2--24 to 28 inches; light yellowish brown (10YR 6/4) very gravelly ashy loam, dark yellowish brown (10YR 4/4) moist; weak medium and coarse subangular blocky structure; soft, friable, nonsticky and nonplastic; common very fine and fine, and few medium roots; common very fine, and few fine, and medium tubular pores; 30 percent pebbles, 15 percent cobbles; slightly acid (pH 6.5); abrupt smooth boundary. (4 to 10 inches thick)

2C--28 to 62 inches; variegated extremely gravelly coarse sand; single grain; loose, nonsticky and nonplastic; common very fine roots; very porous; 65 percent pebbles, 15 percent cobbles; neutral (pH 7.0).

TYPE LOCATION: Kootenai County, Idaho; about 4.5 miles west of Athol on State Highway 54; about 200 feet south and 200 feet east of the northwest corner, sec. 14, T. 53 N., R. 4 W. Latitude - 47 degrees, 56 minutes, 51 seconds North; Longitude - 116 degrees, 48 minutes, 20 seconds West; USGS - Spirit Lake East Quadrangle

RANGE IN CHARACTERISTICS:

Soil moisture - usually dry 45 to 60 consecutive days July to September, moist October to June
Average annual soil temperature - 45 to 47 degrees F.
Average summer soil temperature - 59 to 64 degrees F. without an O horizon
Reaction - moderately acid to neutral throughout
Solum thickness - 20 to 36 inches

A horizon
Value - 4 or 5 dry, 3 or 4 moist
Chroma - 2 to 4 dry, 2 or 3 moist
Texture - GR-ASHY-SIL, CB-ASHY-SIL, GR-ASHY-L, GR-ASHY-SL
Volcanic glass content in the 0.02 to 2.0 mm fraction - 30 to 80 percent
Acid-oxalate extractable Al plus 1/2 Fe - 0.4 to 1.4 percent
Phosphate retention - 25 to 60 percent
Bulk density - 0.70 to 1.00 g/cc
Rock fragments - 15 to 35 percent (up to 40% in lab database)

Bw horizon
Hue - 10YR or 7.5YR
Value - 4 through 7 dry, 3 to 5 moist
Chroma - 3 or 4 dry or moist
Texture - GR-ASHY-SIL, GR-ASHY-L, GR-ASHY-SL upper part, GRV-ASHY-L, GRV-ASHY-SL, GRV-ASHY-SIL, CBV-ASHY-L, CBV-ASHY-SL in lower part
Volcanic glass content in the 0.02 to 2.0 mm fraction - 5 to 50 percent
Acid-oxalate extractable Al + 1/2 Fe - 0.4 to 0.9 percent
Phosphate retention - 25 to 35 percent
Bulk density - 0.70 to 1.25 g/cc upper part, 0.75 to 1.30 g/cc lower part
Rock fragments - 5 to 50 percent in the upper part, averages less than 35 percent
10 to 70 percent in the lower part

2C horizon
Texture - GRX-COS, GRX-LCOS, CBV-COS, CBV-LCOS
Rock fragments - 50 to 85 percent

COMPETING SERIES: These are the Brannan, Capoose, Crackler, Elbowlake, Farway, Kellerbutte, Natapoc, Nevine, Olot, Rouen, Saska, and Vingulch series. The Brannan and Crackler soils are deep to a lithic contact. The Capoose, Olot, Rouen, and Vingulch soils are moderately deep to a lithic contact. The Elbowlake, Natapoc, and Nevine soils have densic horizons. The Farway, Kellerbutte, and Saska soils do not have sandy-skeletal material above 40 inches.

GEOGRAPHIC SETTING: Kootenai soils are on recessional moraines, outwash plains, terraces, and terrace escarpments. Slopes range from 0 to 55 percent. These soils formed in glacial outwash derived dominantly from granite, gneiss, and schist with a mantle of loess and volcanic ash. Elevations range from 2,100 to 2,700 feet. The average annual precipitation ranges from 25 to 30 inches and the average annual air temperature ranges from 43 to 46 degrees F. The frost-free period ranges from 90 to 120 days.

GEOGRAPHICALLY ASSOCIATED SOILS: These are the Avonville, Bonner, Garrison, and McGuire soils. Avonville soils are on outwash plains and terraces and have umbric epipedons. Garrison soils are on outwash plains and terraces and have mollic epipedons. Bonner soils are on outwash plains and terraces and have volcanic ash mantles greater than 14 inches thick. McGuire soils are on outwash terraces and terrace escarpments and are loamy-skeletal and mesic.

DRAINAGE AND PERMEABILITY: Well drained. Runoff is slow on gentle slopes and medium to rapid on steeper slopes. Permeability is moderate in the upper part and very rapid below.

USE AND VEGETATION: These soils are used for timber production, grazing, wildlife habitat, recreation, and some small grains, hay and pasture. Some of these soils are irrigated. Natural vegetation is mainly Douglas-fir, ponderosa pine, lodgepole pine, and western larch, with an understory of bluebunch wheatgrass, elk sedge, pine reedgrass, western fescue, strawberry, common snowberry, white spirea, and rose.

DISTRIBUTION AND EXTENT: Northern Idaho, and possibly northeastern Washington, and northwestern Montana. The series is moderately extensive.

MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Bozeman, Montana

SERIES ESTABLISHED: Kootenai County, Idaho, 1919.

REMARKS: This revision hanges the classification from Coarse-loamy over sandy or sandy-skeletal, mixed, frigid Andic Xerochrepts to Ashy over loamy-skeletal, glassy over isotic, frigid Typic Vitrixerands.

Diagnostic horizons and features recognized in the pedon are:

Ochric epipedon - From 0 to 8 inches (Oi, Oe and A horizon)

Cambic horizon - From 8 to 27 inches (Bw1 and Bw2 horizons)

Particle-size control section - From 2 to 42 inches (A, Bw, and part of the 2C horizons)

ADDITIONAL DATA: National Soil Survey Laboratory Pedon Numbers - S78ID-017-001, S78ID-017-004, S78ID-017-005, S78ID-017-007, and S78ID-017-009


National Cooperative Soil Survey
U.S.A.