LOCATION SOLVAY             KS 
Established Series
PRF, JCW LAG PRF
01/2000

SOLVAY SERIES

The Solvay series consists of very deep, somewhat poorly drained, moderate or moderately slowly permeable soils. They are formed in eolian over alluvium. These soils occur in interdunes on paleo-terraces in river valleys of the Great Bend Sand Plains (MLRA 79). Mean annual air temperature is 56 degrees F (13 degrees C), and mean annual precipitation is 29 inches (74 centimeters). Slope ranges from 0 to 2 percent.

TAXONOMIC CLASS: Fine-loamy, mixed, superactive, mesic Aquic Haplustalfs

TYPICAL PEDON: Solvay fine sandy loam in a pasture. (Colors are for moist soils unless otherwise stated.)

A--0 to 5 inches (0 to 13 centimeters); brown (10YR 5/3) fine sandy loam, brown (10YR 4/3) moist; weak fine and medium granular structure; soft, very friable, nonsticky and nonplastic; common very fine roots throughout; 9 percent clay; slightly acid; clear wavy boundary. ( thickness 5 to 18 inches; 13 to 46 centimeters thick)

2Bt1--5 to 14 inches (13 to 36 centimeters); brown (7.5YR 5/4) fine sandy loam, brown (7.5YR 4/4) moist; weak medium prismatic structure parting to weak medium subangular blocky; slightly hard, friable, slightly sticky and slightly plastic; common very fine roots throughout; 19 percent clay; few distinct discontinuous dark brown (7.5YR 3/4), moist, clay films on vertical faces of peds and very few faint patchy clay bridging between sand grains; few fine irregular masses of iron-manganese accumulation throughout; slightly acid; gradual wavy boundary.

2Bt2--14 to 23 inches (36 to 58 centimeters); brown (7.5YR 5/4) fine sandy loam, brown (7.5YR 4/4) moist; few medium distinct strong brown (7.5YR 5/6) moist irregular redoximorphic concentrations throughout; weak medium prismatic structure parting to weak medium subangular blocky; slightly hard, friable, slightly sticky and slightly plastic; common very fine and fine roots throughout; 17 percent clay; few distinct discontinuous dark brown (7.5YR 3/4), moist, clay films on vertical faces of peds and very few faint patchy clay bridging between sand grains and few distinct continuous pinkish gray (7.5YR 6/2), moist, skeletans on vertical faces of peds; common fine irregular masses of iron-manganese accumulation throughout; slightly acid; gradual wavy boundary.

2Bt3--23 to 37 inches (58 to 94 centimeters); brown (7.5YR 5/4) fine sandy loam, brown (7.5YR 4/4) moist; common medium faint strong brown (7.5YR 5/6) moist irregular redoximorphic concentrations throughout; weak medium prismatic structure parting to weak medium subangular blocky; slightly hard, very friable, slightly sticky and nonplastic; common very fine and fine roots throughout; 14 percent clay; very few distinct discontinuous dark brown (7.5YR 3/4), moist, clay films on vertical faces of peds and very few faint patchy clay bridging between sand grains and few distinct continuous pinkish gray (7.5YR 6/2), moist, redoximorphic depletions on faces of peds and in pores; common fine and medium irregular masses of iron-manganese accumulation throughout; slightly acid; gradual wavy boundary. (combined thickness 32 to 60 inches; 81 to 152 centimeters)

2BC1--37 to 58 inches (94 to 147 centimeters); brown (7.5YR 5/4) fine sandy loam, brown (7.5YR 4/4) moist; common medium distinct dark reddish brown (5YR 3/4) moist irregular redoximorphic concentrations throughout; weak medium prismatic structure parting to weak fine and medium subangular blocky; slightly hard, very friable, slightly sticky and nonplastic; common very fine roots throughout; 11 percent clay; few distinct continuous pinkish gray (7.5YR 6/2), moist, redoximorphic depletions on faces of peds and in pores; few fine and medium irregular masses of iron-manganese accumulation throughout; slightly acid; gradual wavy boundary.

2BC2--58 to 76 inches (147 to 193 centimeters); brown (7.5YR 5/4) loamy fine sand, brown (7.5YR 4/4) moist; few medium faint strong brown (7.5YR 5/6) moist irregular redoximorphic concentrations throughout; weak medium and coarse prismatic structure parting to weak medium subangular blocky; slightly hard, very friable, nonsticky and nonplastic; few very fine roots throughout; 11 percent clay; few distinct continuous light brownish gray (10YR 6/2), moist, redoximorphic depletions on faces of peds and in pores; slightly acid; gradual wavy boundary.

2BC3--76 to 80 inches (193 to 203 centimeters); light brown (7.5YR 6/3) loamy fine sand, brown (7.5YR 5/3) moist; few medium faint strong brown (7.5YR 5/6) moist irregular redoximorphic concentrations throughout; weak medium and coarse prismatic structure parting to weak medium subangular blocky; soft, very friable, nonsticky and nonplastic; few very fine roots throughout; 9 percent clay; few distinct continuous light gray (10YR 7/2), moist, redoximorphic depletions on vertical faces of peds; slightly acid.(combined thickness 0 to 35 inches; 0 to 89 centimeters)

TYPE LOCATION: Reno County, Kansas; 6 miles (9.6 kilometers) east of Hutchinson, 2325 feet (709 meters) south and 1170 feet (357 meters) west of the northeast corner of sec. 8 T. 23 S. R 4 S.; (USGS Hutchinson SE topographic quadrangle; lat. 38 degrees 3 minutes 56.5 seconds N. and long. 97 degrees 46 minutes 44.2 seconds W)

RANGE IN CHARACTERISTICS:

Soil moisture regime: ustic moisture regime bordering on udic
Soil temperature regime: mesic
Mean annual soil temperature: 56 to 58 degrees F (13 to 14 degrees C).
Particle-size control section: 18 to 34 percent clay
Depth to bedrock: greater than 80 inches (203 centimeters)
Depth to secondary calcium carbonate: greater than 30 inches (76 centimeters)
Thickness of the ochric epipedon: 5 to 18 inches (13 to 45 centimeters)
Water table: depth is 2.0 to 4.0 feet (0.6 to 1.2 meters), kind is apparent, months are Feb. - May.
Some pedons have Ap, BA, 2A, 2AB, 2BA, 2BC, 2Cg, horizons.

A horizon:

Hue: 10YR
Value: 4 to 6 (dry) 3 or 4 (moist)
Chroma: 2 or 3
Texture: loamy fine sand, loamy sand, fine sandy loam or sandy loam
Reaction: slightly acid

2Bt horizon:

Hue: 10YR or 7.5YR
Some pedons have a hue of 2.5Y in the lower part.
Value: 4 to 7 (dry) 3 to 6 (moist)
Chroma: 2 to 4
Texture: sandy clay loam, fine sandy loam, or loam, but it includes clay loam in some pedons
Redoximorphic features: 5 to 50 percent
Reaction: slightly acid or neutral

2BC horizon:

Hue: 10YR or 7.5YR
Value: 5 to 7 (dry) 4 to 6 (moist)
Chroma: 2 to 4
Texture: fine sandy loam, sandy loam, loamy fine sand and sandy clay loam
Redoximorphic features: 5 to 20 percent
Reaction: slightly acid to neutral

COMPETING SERIES: The Solvay series is the only series in its family.

GEOGRAPHIC SETTING: Solvay soils

Parent material: eolian over alluvium
Landform: interdunes on paleo-terraces and on some terraces
Slopes: 0 to 2 percent
Elevation: 1515 to 1805 feet (461.8 to 550.2 meters)
Mean annual air temperature: 56 to 58 degrees F (13 to 14 degrees C).
Mean annual precipitation: 24 to 35 inches (61 to 89 centimeters)
Wettest months: Feb. - Oct.
Driest months: Nov. - Jan.
Frost-free period: 187 to 225 days

GEOGRAPHICALLY ASSOCIATED SOILS: These include the Carway (Tentative), Dillhut (Tentative), Hayes (Tentative), Langdon (Tentative), Plev (Tentative), Pratt, Tivin (Tentative), Turon (Tentative) and Warnut (Tentative) series. The poorly drained Carway soils have fine textured buried soil material between 20 and 40 inches (50 to 102 centimeters). They are in depressions. The moderately well drained, sandy Dillhut soils do not have an argillic horizon and are on low dunes. The well drained, coarse-loamy Hayes soils are on dunes. The well drained, sandy Pratt and Turon soils are on dunes. Langdon and Tivin soils are excessively drained and on high dunes. The poorly drained, sandy Plev soils are in depressions. The poorly drained, fine-loamy Warnut soils are in depressions.

DRAINAGE AND PERMEABILITY: Solvay soils are somewhat poorly drained. Runoff is very low and permeability is moderate. An apparent water table is present with an upper limit of 24 inches (61 centimeters) and a lower limit of 48 inches (122 centimeters) during February through May in most years.

USE AND VEGETATION: Mostly cultivated; winter wheat and grain sorghum are the principal crops. Some areas are used for pasture.

DISTRIBUTION AND EXTENT: South Central Kansas. LRR H (Great Plains Winter Wheat and Range), MLRA 79 (Great Bend Sand Plains). The series is of small extent.

MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Denver, Colorado

SERIES ESTABLISHED: Reno County, Kansas

REMARKS: Diagnostic horizons and features recognized in this pedon are:
ochric epipedon: The zone from 0 to 5 inches (0 to 13 centimeters) (A)
argillic horizon: The zone from 5 to 37 inches (13 to 94 centimeters) (2Bt1, 2Bt2, 2Bt3)
Water table: The presence of an apparent water table from 2.0 to 4.0 feet (0.6 to 1.2 meters) during the months of Feb. - May.
Keys to Soil Taxonomy: Eighth edition, 1998

ADDITIONAL DATA: Solvay soils were formerly mapped as Plevna or Carwile.

SOLVAY SERIES
LRR=H
DATE: 03/22/95: Series Proposed: Initial draft for Solvay.
12/23/99 PRF: series established per Reno County final correlation.


National Cooperative Soil Survey
U.S.A.