LOCATION EXETTE             IA
Established Series
Rev. RJK-LDC-TWN
07/2004

EXETTE SERIES


The Exette series consists of very deep, well drained soils formed in loess. These soils are on short, convex to linear side slopes and head slopes on uplands. Slopes range from 5 to 25 percent. Mean annual air temperature is about 9 degrees C (47 degrees F). Mean annual precipitation is about 84 centimeters (33 inches).

TAXONOMIC CLASS: Fine-silty, mixed, superactive, mesic Dystric Eutrudepts

TYPICAL PEDON: Exette silt loam, on a north-facing, convex 11 percent slope, in a cultivated field. (Colors are for moist soil unless other wise stated.)

Ap--0 to 15 centimeters (0 to 6 inches); dark grayish brown (10YR 4/2) with some brown (10YR 4/3) mixings silt loam, light brownish gray (10YR 6/2) dry; weak fine granular structure; friable; neutral; abrupt smooth boundary. [13 to 20 centimeters (5 to 8 inches) thick]

BA--15 to 28 centimeters (6 to 11 inches); brown (10YR 4/3) silt loam; weak fine and very fine subangular blocky structure; friable; few dark grayish brown (10YR 4/2) coatings on faces of peds; slightly acid; clear smooth boundary. [13 to 25 centimeters (5 to 10 inches) thick]

Bw1--28 to 71 centimeters (11 to 24 inches); dark yellowish brown (10YR 4/4) silt loam; weak and moderate medium subangular and angular blocky structure; friable; brown (10YR 4/3) coatings on faces of peds; common prominent light gray (10YR 7/2) dry silt coatings on faces of peds; few fine distinct grayish brown (10YR 5/2) relict redoximorphic depletions; moderately acid; clear smooth boundary.

Bw2--71 to 84 centimeters (24 to 33 inches); dark yellowish brown (10YR 4/4) silt loam; weak medium subangular blocky structure; friable; common distinct light gray (10YR 7/2) dry silt coatings on faces of peds; common fine distinct strong brown (7.5YR 5/6) relict redoximorphic concentrations and common fine distinct grayish brown (10YR 5/2) redoximorphic depletions; slightly acid; clear smooth boundary. [Combined thickness of the Bw horizon is 30 to 64 centimeters (12 to 25 inches).]

BC--84 to 104 centimeters (33 to 41 inches); mottled grayish brown (2.5Y 5/2) and yellowish brown (10YR 5/6) silt loam; weak medium prismatic structure; friable; few fine prominent yellowish red (5YR 4/6) relict redoximorphic concentrations; neutral; clear smooth boundary. [20 to 30 centimeters (8 to 12 inches) thick]

C1--104 to 137 centimeters (41 to 54 inches); grayish brown (2.5Y 5/2) silt loam; massive; friable; few fine prominent yellowish brown (10YR 5/6) and yellowish red (5YR 5/6) relict redoximorphic concentrations; neutral; abrupt wavy boundary. [30 to 61 centimeters (12 to 24 inches) thick]

C2--137 to 152 centimeters (54 to 60 inches); light brownish gray (2.5Y 6/2) silt loam; massive; friable; coarse yellowish red (5YR 4/6) iron segregations; common fine distinct light olive brown (2.5Y 5/4) relict redoximorphic concentrations; slightly alkaline; slightly effervescent.

TYPE LOCATION: Major Land Resource Area (MLRA) 105; Fayette County, Iowa; about 3 miles north and 5 miles east of Fayette; about 262 meters (860 feet) south and 24 meters (79 feet) west of the northeast corner of section 7, T. 93 N., R. 7 W.; USGS Elgin quadrangle; lat. 42 degrees 53 minutes 15.7 seconds N. and long. 91 degrees 42 minutes 24.1 seconds W., NAD 83.

RANGE IN CHARACTERISTICS:
Depth to carbonates--greater than 102 centimeters (40 inches)
Content of clay in the particle-size control section (weighted average)--20 to 27 percent
Content of sand in the particle-size control section (weighted average)--less than 10 percent, typically less than 5 percent

A horizon:
Hue--10YR
Value--3
Chroma--1 or 2
Texture--silt loam
Clay content--18 to 26 percent
Reaction--moderately acid to neutral

Ap horizon (if it occurs):
Hue--10YR
Value--4
Chroma--2 or 3
Texture--silt loam
Clay content--18 to 26 percent
Reaction--moderately acid to neutral

E horizon (if it occurs):
Hue--10YR
Value--4 or 5
Chroma--2
Texture--silt loam
Clay content--18 to 25 percent
Reaction--moderately acid to neutral

Bw horizon:
Hue--10YR or 2.5Y
Value--4 to 6
Chroma--1 to 4
Texture--silt loam
Clay content--18 to 27 percent
Special features--redoximorphic features, present above a depth of 76 centimeters (30 inches), are considered relict
Reaction--moderately acid to neutral

BC horizon:
Hue--10YR or 2.5Y
Value--4 to 6
Chroma--1 to 8
Texture--silt loam
Clay content--15 to 20 percent
Reaction--moderately acid to neutral
Special features--matrix colors and redoximorphic features are considered relict

C horizon:
Hue--10YR or 2.5Y
Value--4 to 6
Chroma--1 to 8
Texture--silt loam
Clay content--15 to 20 percent
Reaction--moderately acid to slightly alkaline
Special features--matrix colors and redoximorphic features are considered relict

COMPETING SERIES: These are the Contrary, Drury, and Killduff series.
Contrary--are in areas that have a mean annual air temperature range of 10 to 12 degrees C (50 to 54 degrees F)
Drury--have matrix hues of 7.5YR or 10YR in the cambic horizon and do not have redoximorphic features within a depth of 76 centimeters (30 inches)
Killduff--have a clay content of 27 and 33 percent in the particle-size control section

GEOGRAPHIC SETTING:
Parent material--loess
Landform--short, convex to linear side slopes and head slopes on uplands
Slopes--5 to 25 percent
Elevation--305 to 427 meters (1000 to 1400 feet) above sea level
Mean annual air temperature--7 to 10 degrees C (45 to 50 degrees F)
Mean annual precipitation--81 to 86 centimeters (32 to 34 inches)
Frost-free period--145 to 180 days

GEOGRAPHICALLY ASSOCIATED SOILS: These are the Chaseburg, Downs, Dubuque, and Fayette soils.
Chaseburg--are at lower elevations on base slopes, have a clay content of 10 to 18 percent in the particle-size control section, and have stratified layers in the lower two thirds of the series control section
Downs--are at higher elevations on side slopes and interfluves, have a clay content of 25 to 35 percent in the particle-size control section, and have surface layers 15 to 23 centimeters (6 to 9 inches) thick
Dubuque--are at higher elevations on side slopes and interfluves and have a lithic contact of dolomitic limestone within depths of 51 to 102 centimeters (20 to 40 inches)
Fayette--are at higher elevations on side slopes and interfluves, have a clay content of 27 to 35 percent in the particle-size control section, and have surface layers 2 to 10 centimeters (1 to 4 inches) thick

DRAINAGE AND PERMEABILITY:
Drainage class--well drained--saturation does not occur within a depth of 1.8 meters (6 feet) during the wettest periods of normal years
Saturated hydraulic conductivity--moderately high
Surface runoff potential--medium or high

USE AND VEGETATION:
The more gently sloping areas are cultivated. The principal crops are corn in a rotation with oats and legume hay. The more steeply sloping areas are pastured. The native vegetation is deciduous trees.

DISTRIBUTION AND EXTENT:
Physiographic Division--Interior Plains
Physiographic Province--Central Lowland
Physiographic section(s)--Dissected till plains, Wisconsin driftless section
MLRA(s)--Eastern Iowa and Minnesota Till Prairies (104), Northern Mississippi Valley Loess Hills (105), and Illinois and Iowa Deep Loess and Drift (108)
LRR M; eastern Iowa
Extent--small

MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: St. Paul, Minnesota

SERIES ESTABLISHED: Fayette County, Iowa, 1975.

REMARKS:
Particle-size control section--the zone from a depth of 25 to 100 centimeters (10 to 40 inches) (BA, Bw1, Bw2, and BC horizons);
series control section--the zone from the surface to a depth of 150 centimeters (60 inches) (Ap, BA, Bw1, Bw2, BC, C1 and C2 horizons).

Diagnostic horizons and features recognized in this pedon:
ochric epipedon--the zone from the surface to a depth of 15 centimeters (0 to 6 inches) (Ap horizon);
cambic horizon--the zone from a depth of 15 to 104 centimeters (6 to 41 inches) (BA, Bw1, Bw2, and BC horizons);
udic moisture regime.

Cation-exchange activity class is inferred from lab data from similar soils in the surrounding area.

Taxonomy version--second edition, 1999.

The gray colors described in this pedon were not used in the classification of this soil as they are considered to be inherited from a relict deoxidized and leached weathering zone

ADDITIONAL DATA:
Complete physical and chemical data are available in R. J. Kuehls M. S. thesis, Iowa State University, Ames, Iowa.


National Cooperative Soil Survey
U.S.A.