LOCATION OCTAGON IN+ILEstablished Series
TAXONOMIC CLASS: Fine-loamy, mixed, active, mesic Mollic Oxyaquic Hapludalfs
TYPICAL PEDON: Octagon silt loam, on a 5 percent slope in a cultivated field at an elevation of 710 feet. (Colors are for moist soil unless otherwise stated.)
Ap--0 to 9 inches; very dark grayish brown (10YR 3/2) silt loam, grayish brown (10YR 5/2) dry; moderate medium granular structure; friable; common fine roots; common small yellowish brown (10YR 5/6) fragments of subsoil; neutral; abrupt smooth boundary. (6 to 9 inches thick)
Bt1--9 to 15 inches; yellowish brown (10YR 5/6) loam; moderate fine subangular blocky structure; friable; common very fine roots; thin discontinuous dark yellowish brown (10YR 4/4) clay films on faces of peds; 2 percent fine gravel; moderately acid; clear wavy boundary.
Bt2--15 to 29 inches; yellowish brown (10YR 5/6) clay loam; moderate medium subangular blocky structure; firm; common very fine roots; thin continuous brown (7.5YR 4/2) clay films on faces of peds; thin continuous yellowish brown (10YR 5/4) silt coatings on faces of peds; 5 percent fine gravel; moderately acid; clear wavy boundary.
Bt3--29 to 38 inches; yellowish brown (10YR 5/4) clay loam; moderate coarse subangular blocky structure; firm; few very fine roots; medium continuous very dark grayish brown (10YR 3/2) organo-clay films on faces of peds and as linings in channels; 5 percent fine gravel; neutral; clear wavy boundary. (Combined thickness of the Bt horizons is 18 to 30 inches.)
Cd--38 to 68 inches; yellowish brown (10YR 5/4) loam; massive; firm; thin continuous very dark grayish brown (10YR 3/2) and dark brown (7.5YR 3/2) organo-clay films lining channels and vertical cracks; 8 percent fine gravel; strongly effervescent; moderately alkaline.
TYPE LOCATION: White County, Indiana; about 1 mile south of Chalmers; 1280 feet east and 390 feet south of the northwest corner of sec. 3, T. 25 N., R. 4 W.; U.S.G.S. Monticello South topographic quadrangle; lat. 40 degrees 38 minutes 51.27 seconds N. and long. 86 degrees 51 minutes 55.50 seconds W., NAD 27; UTM Zone 16, 511378 easting and 4499648 northing, NAD 83.
RANGE IN CHARACTERISTICS:
Depth to carbonates: 24 to 40 inches
Thickness of the silty material: 0 to 18 inches
A or Ap horizon:
Hue: 10YR
Value: 2 or 3 (4 or 5 dry)
Chroma: 1 to 3
Texture: silt loam, loam, or fine sandy loam
Reaction: moderately acid to neutral
Rock fragment content: 0 to 4 percent
Bt or 2Bt horizon:
Hue: 7.5YR or 10YR
Value: 4 or 5
Chroma: 3 to 6
Texture: dominantly clay loam or loam, but ranges to silty clay loam where the silt cap is near the maximum thickness, and ranges to sandy clay loam or fine sandy loam where the sandy overwash cap is near the maximum thickness
Clay content: 18 to 34 percent
Reaction: moderately acid or slightly acid in the upper part and moderately acid to neutral in the lower part
Rock fragment content: 0 to 10 percent
Cd or 2Cd horizon:
Hue: 7.5YR to 2.5Y
Value: 5 or 6
Chroma: 3 or 4
Texture: loam or fine sandy loam with less than 60 percent sand
Reaction: slightly alkaline or moderately alkaline and carbonates are present
Rock fragment content: 2 to 10 percent
COMPETING SERIES: This is the Glenhall series. Glenhall soils do not have carbonates within a depth of 40 inches.
GEOGRAPHIC SETTING: Octagon soils formed in Wisconsinan age till on till plains and moraines. Octagon soils may have as much as 18 inches of silty material at the surface or a cap of fine sandy loam sediments is possible in some areas. Slope gradients range from 2 to 20 percent. Mean annual temperature ranges from 48 to 53 degrees F., mean annual precipitation ranges from 30 to 42 inches, frost-free period ranges from 130 to 180 days, and elevation ranges from 580 feet to 1530 feet above sea level.
GEOGRAPHICALLY ASSOCIATED SOILS: These are the Chalmers, Conover, Corwin, Miami, Montmorenci, Odell, Parr, and Wolcott soils. The poorly drained Chalmers and very poorly drained Wolcott soils are in depressions. Conover and Odell soils are somewhat poorly drained and are on lower lying rises. Corwin and Montmorenci soils are moderately well drained and are on slightly lower lying rises. Miami soils have lighter colored epipedons and are on similar landscape positions. Parr soils have mollic epipedons and are on similar landscape positions.
DRAINAGE AND PERMEABILITY: Moderately well drained. The potential for surface runoff is low to high. Saturated hydraulic conductivity is moderately high or high in the subsoil (4.23 to 14.11 micrometers/s); and low to high in the dense till (0.07 to 14.11 micrometers/s).Permeability is moderate in the subsoil and moderate to very slow in the dense till.
USE AND VEGETATION: Mostly cropped to corn and soybeans. Small grain and mixed hay are also grown. Native vegetation is mixed hardwood trees, shrubs and prairie grass.
DISTRIBUTION AND EXTENT: MLRAs 95B, 108, 110, and 111 in west-central Indiana and northeastern Illinois. The series is of moderate extent.
MLRA OFFICE RESPONSIBLE: Indianapolis, Indiana.
SERIES ESTABLISHED: Tippecanoe County, Indiana, 1955.
REMARKS: Diagnostic horizons and features recognized in this pedon are: ochric epipedon (mollic intergrade) - 0 to 9 inches (Ap horizon); argillic horizon - 9 to 38 inches (Bt1, Bt2, Bt3 horizons). Oxyaquic conditions - the zone from 15 to 38 inches (Bt2, Bt3).
Seven pedons were evaluated from Indiana, all support the appearance of dense glacial till.
ADDITIONAL DATA: Data for this pedon, WH7628, is available in the April 1979 Purdue Agricultural Station Bulletin No.222, Soil Characterization in Indiana IV. 1976-1977 data, page 145. No Transect data is available at this time. Field work is required.