LOCATION KATPA              WY
Established Series
Rev. JFD-RJE-JAL
09/2002

KATPA SERIES


The Katpa series consists of very deep, well drained soils on mountain sideslopes. These soils formed in local alluvium or colluvium derived from limestone and loess. Slopes are 40 to 70 percent. Katpa soils have moderate permeability. Mean annual precipitation is about 28 inches, and mean annual temperature isabout 37 degrees F.

TAXONOMIC CLASS: Loamy-skeletal, carbonatic Calcic Pachic Haplocryolls

TYPICAL PEDON: Katpa gravelly silt loam, on a 46 percent slope with south aspect at 8480 feet elevation, in an area of subalpine fir/western meadowrue h.t., open canopy woodland. (Colors are for dry soil unless otherwise noted.)

Oi--0 to 0.5 inch; discontinuous forest litter of nondecomposed and decomposed needles and leaves; abrupt broken boundary. (0 to 5 inches thick)

A1--0.5 to 2 inches; brown (10YR 5/3) gravelly silt loam, very dark grayish brown (10YR 3/2) moist; weak coarse granular structure parting to weak fine granular; soft, very friable, nonsticky and slightly plastic; many very fine roots; many very fine irregular pores; 20 percent pebbles, trace cobbles and stones; neutral (pH 6.6); abrupt smooth boundary. (1 to 5 inches thick)

A2--2 to 7 inches; brown (10YR 4/3) gravelly silt loam, very dark grayish brown (10YR 3/2) moist; moderate medium subangular blocky structure parting to weak fine granular; slightly hard, very friable, slightly sticky and slightly plastic; many very fine and few medium roots; many very fine irregular pores; 25 percent pebbles, trace cobbles and stones; slightly alkaline (pH 7.5); abrupt wavy boundary. (0 to 10 inches thick)

A3--7 to 16 inches; brown (10YR 5/3) very gravelly silt loam, dark brown (10YR 3/3) moist; moderate medium subangular blocky structure; slightly hard, friable, slightly sticky and slightly plastic; many very fine and few medium roots; many very fine tubular pores; 40 percent pebbles, trace cobbles and stones; slightly alkaline (pH 7.6); clear wavy boundary. (5 to 10 inches thick)

Bk1--16 to 32 inches; brown (10YR 5/3) extremely gravelly silt loam, dark brown (10YR 3/3) moist; weak very fine granular structure; soft, very friable, nonsticky and slightly plastic; many very fine, few fine and common medium roots; many very fine irregular pores; common hard pendants of carbonates and many coats of soft powdery lime on underside of cobbles and coarse pebbles; slightly effervescent; 45 percent pebbles, 20 percent cobbles and trace stones; slightly alkaline (pH 7.8), gradual wavy boundary. (10 to 20 inches thick)

Bk2--32 to 60 inches; brown (10YR 5/3) extremely cobbly loam, brown (10YR 4/3) moist; weak very fine granular structure; soft, very friable, nonsticky and slightly plastic; common very fine and few medium roots; many very fine irregular pores; many hard pendants of carbonates and many coats of soft powdery lime on underside of rock fragments; strongly effervescent; 30 percent pebbles, 50 percent cobbles and trace stones; moderately alkaline (pH 8.0).

TYPE LOCATION: Teton County, Wyoming: 750 feet west and 100 feet north of the southeast corner of section 12, T. 43 N., R. 118 W.; Latitude - 43 degrees North, 41 minutes, 48 seconds; Longitude - 111 degrees West, 56 minutes, 31 seconds.

RANGE IN CHARACTERISTICS:
Mean annual soil temperature - 36 to 42 degrees F.
Mean summer soil temperature - 41 to 46 degrees F. with an O horizon; 49 to 53 degrees F. without an O horizon.
Moisture control section - between 8 and 24 inches; dry throughout the moisture control section for 30 to 45 consecutive days during the four months following the summer solstice.
Mollic epipedon thickness - 16 to 40 inches.
Depth to carbonates - 10 to 25 inches.
Depth to calcic horizon - 16 to 40 inches.
Control section - Calcium carbonate equivalent of the less than 20mm size fraction: greater than 40 percent.

A horizons - Hue: 7.5YR or 10YR
Value: 4 or 5 dry, 3 or 4 moist
Chroma: 2 or 3 dry or moist
Texture: silt loam or loam
Clay content: 10 to 18 percent
Rock fragments: 15 to 60 percent--0 to 10 percent stones; 0 to
20 percent cobbles; 10 to 40 percent pebbles
Calcium carbonate equivalent in the less than 2mm size fraction: 0 to 5 percent
Reaction: 6.6 to 7.8

Bk1 horizon - Hue: 7.5YR or 10YR
Value: 4 or 5 dry, 3 moist
Chroma: 3 dry or moist
Texture: loam or silt loam
Clay content: 12 to 18 percent
Rock fragments: 40 to 70 percent--0 to 10 percent stones; 0 to 30
percent cobbles; 30 to 60 percent pebbles
Effervescence: slightly or strongly effervescent
Calcium carbonate equivalent of the less than 2mm size fraction: 2 to 15 percent
Reaction: 7.4 to 7.8

Bk2 horizon - Hue: 7.5YR or 10YR
Value: 5, 6 or 7 dry; 4 or 5 moist
Chroma: 3 or 4 dry or moist
Texture: loam or sandy loam
Clay content: 4 to 16 percent
Rock fragments: 60 to 90 percent--0 to 10 percent stones; 5 to
50 percent cobbles; 30 to 70 percent pebbles
Effervescence: strongly or violently effervescent
Calcium carbonate equivalent in the less than 2 mm size fraction: 15 to 40 percent
Reaction: 7.9 to 8.4

COMPETING SERIES:

Kitchell (UT) - have 18 to 35 percent clay in the particle size control section; have a mean annual soil temperature of 42 to 47 degrees F.

GEOGRAPHIC SETTING:
Landform - south facing mountain sideslopes.
Elevation - 6,700 to 9,800 feet.
Slope - 40 to 70 percent.
Parent material - local alluvium and colluvium derived from
limestone and loess.
Climate - 4 to 10 foot winter snowpack, moist summers.
Mean annual air temperature - 34 to 40 degrees F.
Mean annual precipitation - 24 to 34 inches.
Frost free period - 15 to 45 days.

DRAINAGE AND PERMEABILITY: Well drained, moderate permeability, moderate runoff.

USE AND VEGETATION: Katpa soils are used for recreation and wildlife habitat. These soils commonly support open canopy forested communities. These communities are commonly associated with the subalpine fir/western meadowrue plant association.

DISTRIBUTION AND EXTENT: Western Wyoming and southeastern Idaho. These soils are of small extent.

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

SERIES ESTABLISHED: Targhee National Forest, Teton County, Wyoming, 1997.

REMARKS:
Diagnostic horizons and features recognized in this pedon are:
Mollic epipedon - The zone from the mineral soil surface to 32 inches (the A1, A2, A3 and Bk1 horizons).
Calcic horizon - The zone from 16 to 60 inches (the Bk1 and Bk2 horizons).
Particle size control section - The zone from 10 to 40 inches (part of the A3, the Bk1 and part of the Bk2 horizons).
Carbonatic mineralogy - greater than 40 percent CaCO3 in the less than 20mm size fraction.
Moisture regime - udic.


National Cooperative Soil Survey
U.S.A.