LOCATION JONESBORO OH
Established Series
Rev. TEL-SJH-DBD
11/2021
JONESBORO SERIES
The Jonesboro series consists of very deep, moderately well drained soils formed in loess and the underlying till on till plains. Slope ranges from 0 to 12 percent. Mean annual precipitation is about 889 mm (35 inches), and mean annual temperature is about 11 degrees C (52 degrees F).
TAXONOMIC CLASS: Fine-silty, mixed, superactive, mesic Glossaquic Hapludalfs
TYPICAL PEDON: Jonesboro silt loam, on a 1 percent slope in a cultivated field. (Colors are for moist soil unless otherwise stated.)
Ap--0 to 18 cm (0 to 7 inches); brown (10YR 4/3) silt loam, pale brown (10YR 6/3) dry; weak medium and fine subangular blocky structure; friable; many fine and common medium roots; few fine black (10YR 2/1) manganese concretions throughout; moderately acid; abrupt wavy boundary. [10 to 23 cm (4 to 9 inches) thick]
Bt1--18 to 36 cm (7 to 14 inches); yellowish brown (10YR 5/4) silty clay loam; moderate medium and fine subangular blocky structure; friable; common fine and common medium roots; common faint brown (10YR 4/3) clay films in pores and root channels; few very fine faint brown (7.5YR 4/4) masses of oxidized iron throughout; few fine black (10YR 2/1) manganese concretions throughout; strongly acid; clear wavy boundary.
Bt2--36 to 46 cm (14 to 18 inches); yellowish brown (10YR 5/6) silty clay loam; moderate medium and fine subangular blocky structure; friable; common fine and few medium roots; few faint brown (10YR 4/3) clay films in pores and root channels; common fine prominent light brownish gray (10YR 6/2) iron depletions throughout; common fine distinct brown (7.5YR 4/4) masses of oxidized iron throughout; very strongly acid; gradual irregular boundary. [Combined thickness of the Bt horizon is 25 to 51 cm (10 to 20 inches).]
Bt/E--46 to 71 cm (18 to 28 inches); 70 percent yellowish brown (10YR 5/6) silty clay loam (Bt); moderate medium and coarse prismatic structure parting to moderate medium subangular blocky; firm; few fine roots; common distinct dark grayish brown (10YR 4/2) clay films on faces of peds; 30 percent light brownish gray (2.5Y 6/2) silt loam material (E) in upper part, tonguing to 10 percent in the lower part; many faint light gray (10YR 7/1) clay depletions on faces of prisms; common medium faint light brownish gray (10YR 6/2) iron depletions throughout; few medium prominent brown (7.5YR 4/4) masses of oxidized iron on faces of peds; common fine black (10YR 2/1) manganese concretions throughout; very strongly acid; abrupt smooth boundary. [20 to 36 cm (8 to 14 inches) thick]
2B't1--71 to 107 cm (28 to 42 inches); brown (7.5YR 4/4) silty clay loam; moderate medium and coarse prismatic structure parting to moderate medium and coarse subangular blocky; very firm; few fine roots; many prominent grayish brown (10YR 5/2) clay films on faces of prisms; few fine distinct grayish brown (10YR 5/2) iron depletions throughout; few distinct light brownish gray (10YR 6/2) clay depletions on faces of prisms; many fine black (10YR 2/1) manganese concretions throughout; moderately acid; clear wavy boundary.
2B't2--107 to 152 cm (42 to 60 inches); brown (10YR 4/3) silty clay; moderate medium subangular blocky structure; firm; many distinct dark grayish brown (10YR 4/2) clay films on faces of peds; common medium distinct gray (10YR 5/1) iron depletions throughout; common fine and medium black (10YR 2/1) manganese concretions throughout; about 2 percent rock fragments; neutral; clear wavy boundary.
2B't3--152 to 183 cm (60 to 72 inches); yellowish brown (10YR 5/6) clay; weak medium subangular blocky structure; firm; common distinct grayish brown (10YR 5/2) clay films on faces of peds; many medium prominent grayish brown (10YR 5/2) iron depletions throughout; common fine strong brown (7.5YR 5/6) iron concretions throughout; about 2 percent rock fragments; slightly alkaline; clear wavy boundary.
2B't4--183 to 203 cm (72 to 80 inches); yellowish brown (10YR 5/6) silty clay; weak medium subangular blocky structure; firm; common distinct dark grayish brown (10YR 4/2) clay films on faces of peds; common medium prominent grayish brown (10YR 5/2) iron depletions throughout; many medium and coarse black (10YR 2/1) manganese concretions throughout; about 2 percent rock fragments; slightly alkaline. [Combined thickness of the 2Bt horizon is 71 to 102 cm (28 to 40 inches).]
TYPE LOCATION: Clinton County, Ohio; 5.25 miles north of Blanchester, in Vernon Township; about 4000 feet northwest of the intersection of Nauvoo Road and State Route 133, along State Route 133, then about 1000 feet west; USGS Blanchester, Ohio topographic quadrangle; lat. 39 degrees 44 minutes 04 seconds N. and long. 83 degrees 59 minutes 40 seconds W., NAD 27.
RANGE IN CHARACTERISTICS:
Depth to the base of the argillic horizon: 152 to 254 cm (60 to 100 inches)
Thickness of the loess: 46 to 102 cm (18 to 40 inches)
Ap or A horizon:
Hue: 10YR
Value: 4 or 5
Chroma: 2 or 3, except for eroded pedons that include chroma of 4
Texture: silt loam
Rock fragment content: 0 to 2 percent
Reaction: slightly acid or neutral
Some pedons have an E or BE horizon.
Bt horizon:
Hue: 7.5YR or 10YR
Value: 4 or 5
Chroma: 4 to 8
Texture: silt loam or silty clay loam
Redox features: iron depletions of low chroma within the upper 25 cm (10 inches)
Rock fragment content: 0 to 2 percent
Reaction: very strongly acid to slightly acid
Bt/E horizon:
Hue: 7.5YR or 10YR
Value: 4 to 6
Chroma: 2 to 6
Texture: silt loam or silty clay loam
Rock fragment content: 0 to 2 percent
Reaction: very strongly acid or strongly acid
2B't horizon:
Hue: 7.5YR or 10YR
Value: 4 or 5
Chroma: 2 to 8
Texture: silty clay loam, silty clay, clay loam, or clay
Redox features: common or many iron depletions of low chroma
Rock fragment content: 2 to 10 percent
Reaction: strongly acid to slightly alkaline
COMPETING SERIES: There are no other series in this family.
GEOGRAPHIC SETTING: Jonesboro soils are on ridgetops and shoulders of the loess-capped till plains of Illinoian age. Slope ranges from 0 to 12 percent. The soils formed in 46 to 102 cm (18 to 40 inches) of loess and the underlying till. Mean annual precipitation ranges from 940 to 1170 mm (37 to 46 inches). Mean annual temperature ranges from 9 to 14 degrees C (48 to 57 degrees F). Frost-free period is 155 to 225 days. Elevation is 271 to 311 meters (890 to 1020 feet) above mean sea level.
GEOGRAPHICALLY ASSOCIATED SOILS: These are the
Loudon,
Nicely,
Rossmoyne,
Schaffer,
Secondcreek, and
Westboro soils. Loudon soils are fine textured and are on adjacent side slopes. Nicely soils have more sand in the upper part of the solum and are on shoulders and backslopes. Rossmoyne soils have a fragipan and are on similar positions. The somewhat poorly drained Schaffer and Westboro soils are in drainageways and swales. The very poorly drained Secondcreek soils are in depressions.
DRAINAGE AND SATURATED HYDRAULIC CONDUCTIVITY: Moderately well drained. The depth to the top of an intermittent perched high water table ranges from 46 to 91 cm (1.5 to 3.0 feet) between January and May in normal years. The potential for surface runoff is negligible to high depending on slope gradient. Saturated hydraulic conductivity is moderately high in the upper solum and moderately low in the lower solum. Permeability is moderate in the upper solum and slow in the lower solum.
USE AND VEGETATION: Most areas are used for cropland. Principal crops are corn, wheat, soybeans, grass and legumes, and tobacco.
DISTRIBUTION AND EXTENT: Southwestern Ohio; MLRA 114A. The series is of small extent.
SOIL SURVEY REGIONAL OFFICE (SSRO) RESPONSIBLE: AMHERST, MASSACHUSETTS
SERIES ESTABLISHED: Clinton County, Ohio, 1999.
REMARKS: This soil was previously included with Rossmoyne soils.
Diagnostic horizons and features recognized in this pedon are:
Ochric epipedon: from the surface to a depth of 18 cm (Ap horizon).
Argillic horizon: from a depth of 18 to 203 cm (Bt, Bt/E, 2Bt horizons).
Glossic horizon: from a depth of 46 to 71 cm (Bt/E). E material in the Bt/E horizon is a clay depletion resulting from aquic conditions.
ADDITIONAL DATA: Characterization data is available through The Ohio State University Soil Characterization Laboratory, for pedon CT-82
National Cooperative Soil Survey
U.S.A.