LOCATION PADDY              MT 
Established Series
Rev. JB-JAL
12/1999

PADDY SERIES


The Paddy series consists of shallow, well drained soils formed in residuum from hard shale and argillite. Paddy soils are on mountains. Slopes range from 15 to 45 percent. The mean annual precipitation is about 22 inches and the mean annual temperature is about 36 degrees F.

TAXONOMIC CLASS: Loamy, mixed, superactive Lithic Haplocryolls

TYPICAL PEDON: Paddy clay loam, forested (Colors are for dry soil unless otherwise noted).

Oi--0 to 1 inch; undecomposed grass, twigs, needles, bark, and roots. (1 to 2 inches thick)

A--1 to 4 inches; dark reddish gray (5YR 4/2) clay loam, dark reddish brown (5YR 3/2) moist; moderate fine granular structure; soft, very friable, slightly sticky and slightly plastic; many very fine and fine roots; common very fine pores; 5 percent pebbles; neutral (pH 6.6); abrupt smooth boundary. (3 to 5 inches thick)

Bw1--4 to 10 inches; weak red (2.5YR 4/2) clay loam, dusky red (2.5YR 3/2) moist; moderate fine granular structure; slightly hard, friable, slightly sticky and slightly plastic; many very fine and fine and few medium roots; common very fine and fine pores; 10 percent pebbles; slightly acid (pH 6.2); clear smooth boundary. (3 to 6 inches thick)

Bw2--10 to 16 inches; reddish brown (2.5YR 4/4) clay loam, dark reddish brown (2.5YR 3/4) moist; weak fine granular structure; slightly hard, friable, slightly sticky and slightly plastic; common fine and medium roots; common fine pores; 10 percent pebbles and 5 percent cobbles; moderately acid (pH 6.0); clear smooth boundary. (4 to 10 inches thick)

R--16 inches; thinly bedded hard red shale.

TYPE LOCATION: Gallatin County, Montana; 400 feet west and 2000 feet north of the SE corner of sec. 14, T.5N., R.4E.

RANGE IN CHARACTERISTICS:

Mean annual soil temperature - 36 to 40 degrees F.
Mean summer soil temperatured - 45 to 47 degrees F.
Mollic epipedon thickness - 6 to 10 inches.
Depth to R horizon - 10 to 20 inches.

A horizon - Hue: 5YR or 2.5YR
Chroma: 2 or 3
Clay content: 27 to 32 percent
Rock fragments: 5 to 10 percent pebbles.
Reaction: pH 6.6 to 7.3

Bw1 horizon - Hue: 2.5YR or 5YR
Value: 4 or 5 dry
Chroma: 2 or 3
Texture: clay loam or loam
Clay content: 25 to 35 percent
Rock fragments: 5 to 15 percent--0 to 5 percent cobbles, 5 to 10 percent pebbles
Reaction: pH 6.1 to 6.5

Bw2 horizon - Hue: 2.5YR or 5YR
Value: 4 or 5 dry
Chroma: 3 or 4
Texture: clay loam or loam
Clay content: 25 to 35 percent
Rock fragments: 10 to 20 percent--0 to 5 percent cobbles; 10 to 15 percent pebbles
Reaction: pH 5.6 to 6.0

COMPETING SERIES:

Dickle (OR) - has a xeric moisture regime.

Duncom (WY) - has horizon of secondary carbonate accumulation.

Hanagita (AK) - has mean annual soil temperature of less than 35 degrees F., has less than 18 percent clay in the particle-size control section.

Hazton (WY) - has less than 18 percent clay in the particle-size control section.

Heisspitz (CO) - has mean summer soil temperature of 48 to 55 degrees F., does not have an O horizon.

Jenkinson (WY) - is moderately or strongly alkaline throughout; is calcareous throughout.

Lotex (UT) - has less than 18 percent clay in the particle-size control section.

Skisams (CO) - has mean summer soil temperature of 52 to 58 degrees F., does not have an O horizon.

Spliten (ID) - has less than 18 percent clay in the particle-size control section, has mean summer soil temperature of 56 to 59 degrees F.

Splitro (WY) - has less than 18 percent clay in the particle-size control section.

Trump (CO) - has horizon of secondary carbonate accumulation.

Tuggle (MT) - has a paralithic contact above the lithic contact.

Udelope (NV) - has less than 18 percent clay in the particle-size control section.

GEOGRAPHIC SETTING:

Landform - mountains.
Elevation - 5,800 to 6,500 feet.
Slope - 15 to 45 percent.
Parent material - residuum from hard shale and argillite.
Climate - long, cold winters; cool, moist springs; short summers.
Mean annual precipitation - 20 to 24 inches.
Mean annual temperature - 34 to 38 degrees F.
Frost-free period - 50 to 70 days.

DRAINAGE AND PERMEABILITY: Well drained; moderately slow permeability.

USE AND VEGETATION: Mainly used for timber production and recreation. The potential native vegetation is Douglas fir, Idaho fescue, pinegrass, and lodgepole pine.

DISTRIBUTION AND EXTENT: This soil is of small extent in southwestern Montana.

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

SERIES ESTABLISHED: Gallatin County, Montana, 1997.

REMARKS: Soil interpretation record: MT1425. Diagnostic horizons and features recognized in this pedon include: a mollic epipedon from 1 to 10 inches (A, Bw1 horizons); a cambic horizon from from 10 to 16 inches (Bw2 horizon); a lithic contact at 16 inches (R horizon); a particle size control section from 10 to 16 inches (Bw2 horizon). Paddy soils have a cryic temperature regime and an ustic moisture regime.


National Cooperative Soil Survey
U.S.A.