LOCATION JUBIN              IN
Established Series
Rev. SWN-BGN
12/2009

JUBIN SERIES


The Jubin series consists of very deep, somewhat excessively drained soils on benches of hills. They formed in colluvium from sandstone and siltstone bedrock. Slopes range from 20 to 50 percent. Mean annual precipitation is about 1092 mm (43 inches), and mean annual temperature is about 12.8 degrees C (55 degrees F).

TAXONOMIC CLASS: Loamy-skeletal, mixed, active, mesic Typic Dystrudepts

TYPICAL PEDON: Jubin very stony loam on a 40 percent slope in a woodland at an elevation of 170.7 meters (560 feet) above mean sea level. (Colors are for moist soil unless otherwise stated.)

A--0 to 10 cm (0 to 4 inches); very dark grayish brown (10YR 3/2) very stony loam, light brownish gray (10YR 6/2) dry; weak very fine granular structure; friable; many fine to coarse roots; 10 percent boulders; 20 percent stones; 10 percent flagstones; 10 percent channers (sandstone); strongly acid; clear wavy boundary. [5 to 20 cm (2 to 8 inches) thick]

BA--10 to 61 cm (4 to 24 inches); dark yellowish brown (10YR 4/4) extremely bouldery loam; weak fine subangular blocky structure; friable; many fine to coarse roots; 15 percent boulders; 20 percent stones; 25 percent flagstones; 20 percent channers (sandstone); very strongly acid; gradual wavy boundary. [15 to 61 cm (6 to 24 inches) thick]

Bw1--61 to 96 cm (24 to 38 inches); yellowish brown (10YR 5/4) extremely bouldery fine sandy loam; weak fine subangular blocky structure; friable; many fine and medium roots; 60 percent boulders and stones; 10 percent stones; 10 percent channers (sandstone); very strongly acid; gradual wavy boundary.

Bw2--96 to 122 cm (38 to 48 inches); yellowish brown (10YR 5/4) extremely bouldery fine sandy loam; moderate fine and medium subangular blocky structure; friable; common fine roots; 60 percent boulders and stones; 10 percent flagstones (sandstone); very strongly acid; gradual wavy boundary.

Bw3--122 to 152 cm (48 to 60 inches); yellowish brown (10YR 5/4) extremely flaggy fine sandy loam; moderate fine and medium subangular blocky structure; friable; few fine roots; 60 percent flagstones; 10 percent channers (sandstone); very strongly acid; gradual wavy boundary.

Bw4--152 to 203 cm (60 to 80 inches); brown (10YR 5/3) extremely flaggy fine sandy loam; moderate fine and medium subangular blocky structure; friable; few fine roots; 60 percent flagstones; 10 percent channers (sandstone); very strongly acid. [Combined thickness of the Bw horizons is more than 152 cm (60 inches).]

TYPE LOCATION: Perry County, Indiana; 2 miles southeast of St. Croix; 1,000 feet east and 2,750 feet south of the northwest corner of sec. 6, T. 4 S., R. 1 W.; USGS Branchville, IN topographic quadrangle; lat. 38 degrees 11 minutes 59.6 seconds N. and long. 86 degrees 34 minutes 4.8 seconds W., UTM Zone 16, 537824 easting and 4228082 northing, NAD 83.

RANGE IN CHARACTERISTICS:
Depth to the base of the cambic horizon: more than 203 cm (80 inches)
Particle-size control section: averages 8 to 18 percent clay and 40 to 65 percent sand
Rock fragments: dominantly strongly cemented to indurated sandstone

A horizon:
Hue: 10YR
Value: 3 or 4
Chroma: 1 to 3
Texture: loam or fine sandy loam in the fine earth fraction
Rock fragment content: averages 35 to 60 percent, including stones, boulders, channers, and flagstones, with the stones and boulders the dominant sizes
Reaction: strongly acid to slightly acid

BA horizon:
Hue: 10YR
Value: 4 or 5
Chroma: 3 or 4
Texture: loam or fine sandy loam in the fine earth fraction
Rock fragment content: averages 35 to 90 percent, including stones, boulders, channers, and flagstones, with the flagstones, stones and boulders the dominant sizes
Reaction: very strongly acid to moderately acid

Bw, and BC horizon where present:
Hue: 10YR
Value: 4 or 5
Chroma: 3 or 4
Texture: loam or fine sandy loam in the fine earth fraction.
Rock fragment content: averages 35 to 90 percent, including stones, boulders, channers, and flagstones, with the stones and boulders the dominant sizes in the upper part and the flagstones and channers the dominant sizes in the lower part
Reaction: very strongly acid to moderately acid

COMPETING SERIES: These are the Berks, Blasdell, Brownstown, Brownsville, Cadosia, Calvin, Cloverlick, Deadline, Highsplint, Judyville, Keyesville, Lippitt, Manlius, Matewan, Nailkeg, Peaks, Solon (T), Sylco, Warwick, and Wyoming series. All these series except Cloverlick and Highsplint have a solum thickness less than 80 inches. Cloverlick soils average less than 40 percent sand in the particle-size control section. Highsplint soils average more than 35 percent silt in the lower part of the cambic horizon. Also, Cloverlick and Highsplint soils are not dominated by bouldery and stony fragments in the upper part of the solum.

GEOGRAPHIC SETTING: Jubin soils are on benches of hills, at the base of Pennsylvanian age sandstone and siltstone bedrock escarpments. They formed in colluvium from sandstone and siltstone bedrock. Slopes range from 20 to 50 percent. Mean annual temperature ranges from 11.1 to 13.9 degrees C (52 to 57 degrees F), and the mean annual precipitation ranges from 1016 to 1168 mm (40 to 46 inches). Frost-free days range from 170 to 200. Elevation ranges from 105.2 to 305 meters (345 to 1000 feet) above mean sea level.

GEOGRAPHICALLY ASSOCIATED SOILS: These are the Adyeville, Branchville, Deuchars, Ebal, Kitterman, and Tipsaw soils. The moderately deep, somewhat excessively drained Adyeville and Tipsaw soils are on backslopes of hills. The well drained Branchville soils are typically complexed with the Jubin soils and are on the lower part of the footslopes. The moderately well drained Deuchars, Ebal and Kitterman soils are on shoulders and backslopes of hills.

DRAINAGE AND SATURATED HYDRAULIC CONDUCTIVITY: Somewhat excessively drained. Saturated hydraulic conductivity is high (14.11 to 42.34 micrometers/s). Permeability is moderately rapid (2 to 6 inches per hour). The potential for surface water runoff is medium.

USE AND VEGETATION: Most areas are used for woodland and wildlife habitat. Native vegetation is mixed, deciduous hardwood forest.

DISTRIBUTION AND EXTENT: Southern Indiana. The acreage is of small extent in MLRA 120B.

MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Morgantown, West Virginia

SERIES ESTABLISHED: Perry County, Indiana, 1997. The source of the name is from a stream in Perry County.

REMARKS: Diagnostic surface and subsurface horizons recognized in this pedon are:
1) Ochric epipedon- the zone from 0 to 61 cm (24 inches) - (A and BA horizons);
2) Cambic horizon- the zone from 61 to 203 cm (24 to 80 inches) - (Bw1, Bw2, Bw3, Bw4 horizons).

The Jubin soils were included in mapping with the Muskingum soils in the 1969 Perry Co., IN Soil Survey.

ADDITIONAL DATA: Lab data on pedon number S92IN-123-002 is at the NSSC, Lincoln, NE.


National Cooperative Soil Survey
U.S.A.