LOCATION DECHAMPS           WI
Established Series
Rev. TLK-JAL-JJJ
04/2009

DECHAMPS SERIES


The Dechamps series consists of very deep, somewhat poorly drained soils that formed in predominantly sandy alluvium. These soils are on flood plains. Permeability is moderate to rapid. Slope ranges from 0 to 2 percent. Mean annual precipitation is about 31 inches. Mean annual air temperature is about 42 degrees F.

TAXONOMIC CLASS: Sandy, mixed, frigid Aquic Udifluvents

TYPICAL PEDON: Dechamps fine sandy loam, on a 1 percent, slightly concave slope, in an area of mixed conifer and northern hardwood forest, at an elevation of about 790 feet above mean sea level. (Colors are for moist soil unless otherwise stated.)

A--0 to 3 inches; dark reddish brown (5YR 2/2) fine sandy loam, dark reddish gray (5YR 4/2) dry; weak fine granular structure; very friable; many fine and medium, and common coarse roots; moderately acid; abrupt wavy boundary. (3 to 7 inches thick)

C1--3 to 8 inches; dark reddish brown (5YR 3/3) fine sandy loam; massive; friable; many fine and medium, and common coarse roots; moderately acid; clear wavy boundary.

C2--8 to 35 inches; stratified dark reddish brown (5YR 3/4) and reddish brown (5YR 4/4) loamy fine sand, fine sand and thin strata of fine sandy loam; massive with some depositional platyness; friable; common fine and medium, and few coarse roots; few fine distinct dark reddish gray (5YR 4/2) redox depletions; common medium and coarse distinct yellowish red (5YR 4/6) iron accumulations in the matrix; few fine dark reddish brown (2.5YR 2/4) iron-manganese accumulations; moderately acid; gradual wavy boundary.

C3--35 to 49 inches; stratified dark reddish brown (2.5YR 3/4) and reddish brown (5YR 4/4) fine sandy loam and fine sand; massive; very friable; common fine and medium roots; thin lenses (< 1 inch) of loam; few fine distinct dark reddish gray (5YR 4/2) redox depletions; many coarse distinct yellowish red (5YR 4/6) and few fine distinct red (2.5YR 4/6) iron accumulations in the matrix; moderately acid; clear wavy boundary.

C4--49 to 80 inches; stratified reddish brown (5YR 4/4) and reddish brown (2.5YR 4/4) loamy fine sand, sand, and fine sandy loam; massive; friable; few fine and medium roots; several thin lenses (< 1 inch) of silt loam and loam containing organic materials; 3 inch band of very gravely coarse sand from 66 to 69 inches; many medium and coarse distinct yellowish red (5YR 4/6) and few fine distinct dark red (2.5YR 3/6) iron accumulations in the matrix and along pores; common coarse distinct dark reddish gray (5YR 4/2) iron depletions in the matrix: strongly acid.

TYPE LOCATION: Bayfield County, Wisconsin; about 2.5 miles west and 7.5 miles north of Iron River; 20 feet north and 400 feet east of the southwest corner of section 35, T. 49 N., R. 9 W.; Iron River Watershed; USGS Blaine Creek WI topographic quadrangle; lat. 46 degrees 40 minutes 33 seconds N. and long. 91 degrees 28 minutes 03 seconds W., NAD 27.

RANGE IN CHARACTERISTICS:
Organic Matter: irregular decrease with depth
Depth to stratification: 0 to 12 inches
Depth to redoximorphic features: 6 to 18 inches
Cobble content: 0 to 15 percent by volume, throughout
Gravel content: 0 to 15 percent by volume, throughout
Saturation: 6 to 30 inches for 1 month or more in most years

A horizon:
Hue: 5YR or 7.5YR
Value: 2 or 3
Chroma: 1 to 3
Texture: fine sandy loam
Reaction: strongly acid to slightly acid
Thickness Range: 3 to 7 inches

C horizon:
Hue: 2.5YR or 5YR
Value: 3 or 4
Chroma: 2 to 4
Texture: stratified textures of sand; loamy sand; fine sand; loamy fine sand; fine sandy loam; very fine sandy loam; loam and silt loam; very thin strata of silty clay loam, clay loam, or sandy clay loam occur in some pedons. The finer textured stratifications are the thinnest strata. The sand content of any of the stratified layers is always greater than 40 percent, and the weighted average sand content is always above 70 percent. Very fine sand is abundant, but is never greater than 40 percent of the sand fraction. Clay content is usually about 5 to 10 percent, except it may be higher in thin or very thin layers.
Redoximorphic features: Redox depletions above 20 inches
Reaction: moderately acid to slightly alkaline

COMPETING SERIES:
There are no other series in this family.

GEOGRAPHIC SETTING:
Parent material: alluvium
Landscape: flood plains
Landform: slightly depressional swales on flood plains
Slope: 0 to 2 percent
Elevation: 600 to 1600 feet above mean sea level
Mean annual air temperature: 39 to 45 degrees F
Mean annual precipitation: 28 to 33 inches
Frost-free period: 125 to 140 days

GEOGRAPHICALLY ASSOCIATED SOILS:
Arnheim--are on slightly lower landscapes and are poorly drained
Pelkie--are on slightly higher landscapes and are moderately well drained
Moquah--are on slightly higher landscapes and are moderately well drained

DRAINAGE AND PERMEABILITY:
Drainage: Somewhat poorly drained
Permeability: Moderate to rapid
Seasonal High Water Table: apparent at 0.5 to 2.5 feet for more than 20 consecutive days and more than 30 cumulative days, from September to June in most years
Runoff: low or medium
Flooding: Frequent or occasional flooding for brief durations in March, April, May, June, September, and October. None or rare flooding for brief or very brief durations in January, February, July, August, November, and December

USE AND VEGETATION: Most of this soil is forested with the primary species being red maple, silver maple, balsam fir, quaking aspen, black ash, willow, speckled alder, and red-osier dogwood.

DISTRIBUTION AND EXTENT: MLRAs 90A, 91, 92, 93B, 94D; Northern Wisconsin and possibly the Upper Peninsula of Michigan. This series is of small extent.

MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: St. Paul, Minnesota; MLRA SSO 10-4 (Duluth, Minnesota).

SERIES ESTABLISHED: Douglas County, Wisconsin, 2005. Name comes from nearby river.

REMARKS: Diagnostic horizons and features recognized in this pedon are: ochric epipedon - the zone from the surface to 3 inches (A horizon); particle-size control section 10 to 40 inches; irregular decrease in organic carbon with increasing depth; redox depletions above 20 inches; redox concentrations 8 to 80 inches.

Only series status, responsibility, and scrivener's errors changed - 3/09.

ADDITIONAL DATA: For laboratory data on this pedon see pedon no. S93WI-007-001 from the NSSL.


National Cooperative Soil Survey
U.S.A.