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OSD Data Refresh - 2024-07-01
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4 changes: 2 additions & 2 deletions OSD/C/CHEKIKA.txt
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Expand Up @@ -2,13 +2,13 @@ LOCATION CHEKIKA FL

Established Series
Rev. CN/CAW; GRB
03/2005
06/2024

CHEKIKA SERIES

The Chekika series consists of very shallow, somewhat poorly drained, moderately permeable soils over limestone bedrock. They were formed by the scarification of oolitic limestone outcrops and the marly sediments that partially covers the limestone and fills the many cavities or solution holes. These soils are adjacent to the Miami Ridge. Near the type location, the mean annual temperature is about 74 degrees F., and the mean annual precipitation is about 63 inches. Slopes range from 0 to 2 percent.

TAXONOMIC CLASS: Loamy-skeletal, carbonatic, hyperthermic Lithic Udorthents
TAXONOMIC CLASS: Loamy-skeletal, carbonatic, isohyperthermic Lithic Udorthents

TYPICAL PEDON: Chekika very gravelly loam--cropland (Colors are for moist soil unless otherwise stated).

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27 changes: 15 additions & 12 deletions OSD/C/CLARESON.txt
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Expand Up @@ -2,11 +2,11 @@ LOCATION CLARESON KS+AR MO

Established Series
Rev. JMA-LEB-RGC
12/2020
06/2024

CLARESON SERIES

The Clareson series consists of moderately deep, well drained soils that formed in residuum weathered from limestone. These soils are on uplands. Slope ranges from 1 to 3 percent. Mean annual precipitation is about 1143 mm (45 inches), and mean annual temperature is about 14 degrees C (57 degrees F).
The Clareson series consists of moderately deep, well drained soils that formed in residuum weathered from limestone. These soils are on uplands. Slope ranges from 0 to 15 percent. Mean annual precipitation is about 1143 mm (45 inches), and mean annual temperature is about 14 degrees C (57 degrees F).

TAXONOMIC CLASS: Clayey-skeletal, mixed, superactive, thermic Typic Argiudolls

Expand All @@ -22,21 +22,25 @@ TYPICAL PEDON: Clareson stony silty clay loam, convex, 2 percent slope in nativ

R--76 cm (30 inches); hard limestone bedrock.

TYPE LOCATION: Crawford County, Kansas; about 4 miles west and l 3/4 miles south of Arcadia; 1,100 feet north and 150 feet east of the southwest corner of sec. 8, T. 28 S., R. 25 E; USGS Arma, Kansas topographic quadrangle; lat. 37 degrees 38 minutes 32.50 seconds N. and long. 94 degrees 48 minutes 15.36 seconds W.; UTM Zone 15, 340811 easting and 4167666 northing, NAD 83.
TYPE LOCATION: Crawford County, Kansas; about 4 miles west and 1 3/4 miles south of Arcadia; 1,100 feet north and 150 feet east of the southwest corner of sec. 8, T. 28 S., R. 25 E.

USGS topographic quadrangle--Arma, Kansas
Latitude 37.6183052
Longitude -94.7039413
Datum--WGS84
Coordinate Source--estimated from other source

RANGE IN CHARACTERISTICS:
Depth to bedrock: ranges from 51 to 102 centimeters (20 to 40 inches).
Depth to bedrock: ranges from 51 to 102 centimeters (20 to 40 inches)
Depth to argillic horizon: 36 to 64 cm (14 to 25 inches)
Mollic thickness: 20 to 51 centimeters (8 to 20 inches)
Particle-size control section (weighted average): 36 to 64 cm (14 to 25 inches)
Clay content: 38 to 70 percent
Rock fragments: 35 to 85 percent
Particle-size control section (weighted average): clay content averages 38 to 70 percent and rock fragment content averages 35 to 85 percent

A horizon:
Hue: 7.5YR or 10YR
Value: 2 or 3 and 3 to 5 dry
Chroma: 2 or 3
Texture: silt loam, silty clay loam, or their channery, flaggy, or stony analogues.
Texture: silt loam, silty clay loam, or their channery, flaggy, or stony analogues
Clay content: 20 to 39 percent
Sand content: 0 to 20 percent
Rock fragment content: 0 to 20 percent
Expand All @@ -59,7 +63,7 @@ Chroma: 2 to 6
Texture: very or extremely channery, flaggy, or stony silty clay, clay or silty clay loam
Clay content: 38 to 70 percent
Sand content: 0 to 25 percent
Rock fragment content: 35 to 85 percent limestone channers or flagstones.
Rock fragment content: 35 to 85 percent limestone channers or flagstones
Reaction: moderately acid to neutral

BC horizon: (when present)
Expand All @@ -69,7 +73,7 @@ Chroma: 2 to 6
Texture: very or extremely channery, flaggy, or stony silty clay or clay
Clay content: 40 to 70 percent
Sand content: 0 to 20 percent
Rock fragment content: 35 to 85 percent limestone channers or flagstones.
Rock fragment content: 35 to 85 percent limestone channers or flagstones
Reaction: moderately acid to neutral

COMPETING SERIES: There are no competing series.
Expand All @@ -84,14 +88,13 @@ USE AND VEGETATION: Soils are mostly in native grass pasture. Most common gras

DISTRIBUTION AND EXTENT: MLRA 76, MLRA 84A, MLRA 112, and MLRA 116A in southeastern Kansas, southwestern Missouri and northwestern Arkansas. The series is of large extent.

SOIL SURVEY REGIONAL OFFICE (SSRO) RESPONSIBLE: Indianapolis, Indiana
SOIL SURVEY REGIONAL OFFICE (SSRO) RESPONSIBLE: Salina, Kansas

SERIES ESTABLISHED: Crawford County, Kansas, 1969.

REMARKS: Diagnostic horizons and features recognized in this pedon are:
Mollic epipedon: from the surface to a depth of 36 cm (14 inches) (A and BA horizons).
Argillic horizon: from a depth of 36 to 64 cm (14 to 25 inches) (Bt horizon).
05/2003 Cation-exchange activity class added, horizon nomenclature updated.

NASIS data mapunit ID 745328 represents the typical pedon. Other NASIS DMU ID's are 745325, 745326, 745327 and 745330.

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4 changes: 2 additions & 2 deletions OSD/C/COLLEEN.txt
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Expand Up @@ -2,7 +2,7 @@ LOCATION COLLEEN VA

Established Series
Rev. SKT-WJE-MHC
1/93
06/2024

COLLEEN SERIES

Expand Down Expand Up @@ -46,7 +46,7 @@ USE AND VEGETATION: These soils are used for hay, pasture, and woodland.

DISTRIBUTION AND EXTENT: Virginia. Northern Piedmont uplands. The series is of small extent.

MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Morgantown, West Virginia
SOIL SURVEY REGIONAL OFFICE (SSRO) RESPONSIBLE: AUBURN, ALABAMA

SERIES ESTABLISHED: Nelson County, Virginia, 1992.

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16 changes: 8 additions & 8 deletions OSD/H/HILLSDALE.txt
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Expand Up @@ -2,7 +2,7 @@ LOCATION HILLSDALE MI+IN

Established Series
Rev. RLM-WEF-RAB
08/2012
06/2024

HILLSDALE SERIES

Expand All @@ -28,7 +28,7 @@ TYPE LOCATION: St. Joseph County, Michigan; about 2 miles south and 1.5 miles we

RANGE IN CHARACTERISTICS:
Thickness of the solum: 102 to more than 203 cm (40 to more than 80 inches)
Depth to carbonates: 102 to more than 203 cm (40 to more than 80 inches)
Depth to carbonates: commonly 102 to more than 203 cm (40 to more than 80 inches), but ranges to 85 cm (33 inches)
Rock fragment content: averages 1 to 14 percent throughout the series control section, although some individual subhorizons have none
Particle-size control section: averages less than 50 percent fine sand and very fine sand less than 18 percent clay, although some subhorizons can contain more than 18 percent clay
Series control section: averages 50 to 85 percent sand
Expand All @@ -46,7 +46,7 @@ Value: 5 to 7
Chroma: 2 to 4
Texture: sandy loam, fine sandy loam, loam, or loamy sand

EB horizon:
EB or BE horizon, where present:
Hue: 10YR
Value: 4 to 7
Chroma: 3 to 6
Expand All @@ -64,7 +64,7 @@ Hue: 7.5YR or 10YR
Value: 4 or 5
Chroma: 3 to 8
Texture: sandy loam or loamy sand; some pedons have pockets of sand or loamy sand
Reaction: strongly acid to neutral
Reaction: strongly acid to moderately alkaline

C horizon:
Hue: 7.5YR or 10YR
Expand All @@ -78,15 +78,15 @@ COMPETING SERIES: These are the Brownsburg, Crumstown, Eleva, Mecan, and Oshtemo

GEOGRAPHIC SETTING: Hillsdale soils are on ground moraines and end moraines. Slope gradients are mostly 2 to 18 percent but range from 0 to 40 percent. Hillsdale soils formed in loamy till. Mean annual precipitation ranges from 737 to 940 mm (29 to 37 inches). Mean annual temperature ranges from 7.8 to 11.7 degrees C (46 to 53 degrees F). Frost-free period is 130 to 180 days. Elevation is 177 to 466 meters (580 to 1,530 feet) above mean sea level.

GEOGRAPHICALLY ASSOCIATED SOILS: The somewhat poorly drained Teasdale soils and the poorly drained and very poorly drained Barry soils form a drainage sequence with the Hillsdale soils and are closely associated. Oshtemo and Spinks soils are associated on low moraines. Oshtemo soils are at slightly lower elevations and Spinks soils are commonly at slightly higher elevations.
GEOGRAPHICALLY ASSOCIATED SOILS: The somewhat poorly drained Teasdale soils and the poorly drained and very poorly drained Barry soils form a drainage sequence with the Hillsdale soils and are closely associated. The moderately well drained Elmdale, Marlette, and Miami soils are on lower positions on moraines. Oshtemo and Spinks soils are associated on low moraines. Oshtemo soils are at slightly lower elevations and the sandier Spinks soils are commonly at slightly higher elevations.

DRAINAGE AND SATURATED HYDRAULIC CONDUCTIVITY: Well drained. The potential for surface runoff is negligible to high depending upon the slope. Saturated hydraulic conductivity is moderately high. Permeability is moderate.
DRAINAGE AND SATURATED HYDRAULIC CONDUCTIVITY: Well drained. The potential for surface runoff is negligible to high depending upon the slope. Saturated hydraulic conductivity is moderately high or high. Permeability is moderate.

USE AND VEGETATION: Most areas are cultivated. Corn, small grains, soybeans, and legume-grass hay are the principal crops. Steep areas are in permanent pasture or forest. Wooded areas are in oaks, hickory and maple. Native vegetation is hardwood forest.

DISTRIBUTION AND EXTENT: MLRAs 97, 98, 111B, and 111C in Michigan and Indiana. The series is of large extent.
DISTRIBUTION AND EXTENT: MLRAs 97, 98, and 111 in Michigan and Indiana. The series is of large extent.

MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: AMHERST, MASSACHUSETTS
SOIL SURVEY REGIONAL OFFICE (SSRO) RESPONSIBLE: Morgantown, West Virginia

SERIES ESTABLISHED: Hillsdale County, Michigan, 1924.

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4 changes: 2 additions & 2 deletions OSD/K/KROME.txt
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Expand Up @@ -2,13 +2,13 @@ LOCATION KROME FL

Established Series
Rev. CN/WGH
9/91
06/2024

KROME SERIES

The Krome series consists of very shallow, moderately well drained, moderately permeable soils over limestone. They formed by scarification of outcrops of oolitic limestone, and the loamy residuum that partially covers the limestone and fills the many cavities or solution holes. These soils are on broad areas of the Miami Ridge. Slopes are predominantly 0 to 2 percent, but range to 5 percent.

TAXONOMIC CLASS: Loamy-skeletal, carbonatic, hyperthermic Lithic Udorthents
TAXONOMIC CLASS: Loamy-skeletal, carbonatic, isohyperthermic Lithic Udorthents

TYPICAL PEDON: Krome very gravelly loam in cropland (tomatoes). (Colors are for moist soil unless otherwise stated.)

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2 changes: 1 addition & 1 deletion OSD/N/NAFF.txt
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Expand Up @@ -2,7 +2,7 @@ LOCATION NAFF WA+ID

Established Series
Rev. TLA/CLM/TJR
04/2024
06/2024

NAFF SERIES

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8 changes: 4 additions & 4 deletions OSD/O/OAKVILLE.txt
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Expand Up @@ -2,7 +2,7 @@ LOCATION OAKVILLE IN+IL MI NY OH WI

Established Series
Rev. WEF-RAR-RAB
09/2012
06/2024

OAKVILLE SERIES

Expand Down Expand Up @@ -76,7 +76,7 @@ Chroma: 1 to 6
Texture: fine sand, loamy fine sand, sand, or loamy sand
Reaction: very strongly acid to neutral

COMPETING SERIES: These are the Acquango, Aldo, Bigapple, Biltmore, Boplain, Breeze (T), Caesar, Chute, Dabney, Hodge, Osolo, Pahuk, Penwood, Perks, Pinegrove, Plainfield, Poquonock, Ronda, Samoa, Sardak, Sarpy, Scotah, Spessard, Suncook, Tyner, Wapanucket, and Windsor series. Acquango soils are very slightly saline to moderately saline in the series control section. Aldo, Caesar, Dabney, Osolo, Perks, Pinegrove, Plainfield, and Spessard soils average less than 50 percent fine sand in the particle-size control section. Bigapple and Breeze soils have anthrotransported material within the series control section. Biltmore soils have few to many mica flakes in the series control section. Boplain soils have a paralithic contact in the lower part of the series control section. Chute and Suncook soils are less than 46 cm (18 inches) to the base of soil development. Hodge, Sardak, and Sarpy soils have carbonates within the series control section. Pahuk, Ronda, and Samoa soils do not have a Bw horizon. Penwood soils have hue redder than 7.5YR in the Bw horizon. Poquonock soils have a densic contact within the series control section. Scotah soils have an irregular decrease in organic matter within the series control section. Tyner soils average more than 10 percent silt plus clay in the particle-size control section. Wapanucket soils have less than 70 percent sand in the lower part of the series control section. Windsor soils are from outside LRR L and M and typically average less than 50 percent fine sand in the particle-size control section.
COMPETING SERIES: These are the Acquango, Aldo, Biltmore, Boplain, Caesar, Chute, Dabney, Gardiner, Hodge, Osolo, Pahuk, Penwood, Perks, Pinegrove, Plainfield, Poquonock, Rikers, Ronda, Samoa, Sardak, Sarpy, Scotah, Spessard, Suncook, Tyner, Wapanucket, and Windsor series. Acquango soils are very slightly saline to moderately saline in the series control section. Aldo, Caesar, Dabney, Osolo, Perks, Pinegrove, Plainfield, and Spessard soils average less than 50 percent fine sand in the particle-size control section. Biltmore soils have few to many mica flakes in the series control section. Boplain soils have a paralithic contact in the lower part of the series control section. Chute and Suncook soils are less than 46 cm (18 inches) to the base of soil development. Gardiner and Scotah soils have an irregular decrease in organic matter within the series control section. Hodge, Sardak, and Sarpy soils have carbonates within the series control section. Pahuk, Ronda, and Samoa soils do not have a Bw horizon. Penwood soils have hue redder than 7.5YR in the Bw horizon. Poquonock soils have a densic contact within the series control section. Rikers soils have anthrotransported material within the series control section. Tyner soils average more than 10 percent silt plus clay in the particle-size control section. Wapanucket soils have less than 70 percent sand in the lower part of the series control section. Windsor soils are from outside LRR L and M and typically average less than 50 percent fine sand in the particle-size control section.

GEOGRAPHIC SETTING: Oakville soils are on dunes and beach ridges on outwash plains, lake plains, and moraines. Slope ranges from 0 to 60 percent. Oakville soils formed in sandy eolian deposits. Mean annual precipitation ranges from 737 to 1067 mm (29 to 42 inches). Mean annual temperature ranges from 7.8 to 11.7 degrees C (47 to 53 degrees F). Frost-free period is 130 to 180 days. Elevation is 177 to 466 meters (580 to 1,530 feet) above mean sea level.

Expand All @@ -86,9 +86,9 @@ DRAINAGE AND SATURATED HYDRAULIC CONDUCTIVITY: Excessively drained. Potential fo

USE AND VEGETATION:. Soils are mostly in idle cropland or in woodland. Some areas are in pasture. Vegetables, small grain, and legume-grass hay are the principal crops when cultivated. Native vegetation is mixed hardwoods with oak and white pine the principal species.

DISTRIBUTION AND EXTENT: MLRA's 95A, 95B, 97, 98, 99, 101, 108B, 110, 111C, 115B, 115C, 139, 142, 143, and 144A in southern Michigan, northern Illinois, northern Indiana, northwestern Ohio, New York, and eastern Wisconsin. The series is of large extent.
DISTRIBUTION AND EXTENT: MLRA's 95A, 95B, 97, 98, 99, 101, 108B, 110, 111, 115B, 115C, 139, 142, 143, and 144A in southern Michigan, northern Illinois, northern Indiana, northwestern Ohio, New York, and eastern Wisconsin. The series is of large extent.

MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: AMHERST, MASSACHUSETTS
SOIL SURVEY REGIONAL OFFICE (SSRO) RESPONSIBLE: MORGANTOWN, WEST VIRGINIA

SERIES ESTABLISHED: Macomb County, Michigan, 1970.

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4 changes: 2 additions & 2 deletions OSD/P/PINEYWOODS.txt
Original file line number Diff line number Diff line change
Expand Up @@ -2,7 +2,7 @@ LOCATION PINEYWOODS VA

Established Series
Rev. SKT-WJE-MHC
01/2006
06/2024

PINEYWOODS SERIES

Expand Down Expand Up @@ -50,7 +50,7 @@ USE AND VEGETATION: These soils are used mainly for woodland.

DISTRIBUTION AND EXTENT: Northern Piedmont upland in Virginia. The series is of small extent.

MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Morgantown, West Virginia
SOIL SURVEY REGIONAL OFFICE (SSRO) RESPONSIBLE: AUBURN, ALABAMA

SERIES PROPOSED: Nelson County, Virginia, 1987.

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