IDENTIFIERS
Current Taxon Name (Soil Name):
Wea
OSD
Series Extent
User Site ID:
1970OH057020
User Pedon ID:
1970-OH057-020
Lab Information:
Certified Lab Pedon Description -
no
Lab Source ID -
OHSTATE
Lab Pedon # -
GN-020
NCSS Pedon Lab Data NASIS Record ID -
72634
Print Date:
11/21/2024
LOCATION
Location Description:
2 1/2 mi. NNW of Xenia, 1.2 mi. NE of Fairground Rd., 1400 ft. NNW of farm roadway and 200 ft. from the farm boundary on Harner farm.
State:
Ohio
County:
OH057—Greene
PEDON
Describers Name:
garner
Current Taxonomic Class:
Fine-loamy, mixed, mesic Typic Argiudolls
Pedon Record Orgin:
NASIS
Correlated Information:
Soil Name -
Wea
Classificaton Date -
5/4/2012
Dynamic Soil Properties:
Pedoderm Loose Cover Indicator -
no
Hydric:
no
SITE
Parent Material:
Wisconsinan outwash
Landform:
outwash plain
Drainage Class:
well
Geology:
Wisconsinan formation.
Surface Fragments:
Benchmark Soil?:
no
VEGETATION
SITE OBSERVATION
Observation Date:
8/18/1970 (actual site observation date)
Surface Cover Properties:
Site Obs. Cover Kind 1 -
grass/herbaceous cover
Site Obs. Cover Kind 2 -
other grass/herbaceous cover
Pedoderm Loose Cover Indicator -
no
Drained? -
no
Bedded Soil? -
no
Forest Plantation? -
no
Setting and Climate
Slope
Slope Length USLE
Upslope Length
Elev.
Corr. Elev
Aspect
MAP
REAP
FFD
MAAT
MSAT
MWAT
MAST
MSST
MWST
MFFP
PE Index
Climate Station ID
Climate Station Name
Climate Station Type
%
m
degrees
mm
mm
C
mm
1
—
—
251.5
—
—
—
—
—
—
—
—
—
—
—
—
—
—
—
Ap1—0 to 20 centimeters (0.0 to 7.9 inches); very dark gray (10YR 3/1) Error; weak fine granular structure; friable; fragments; slightly acid, pH 6.5; clear smooth boundary. Lab sample # OSU0020289
A2—20 to 46 centimeters (7.9 to 18.1 inches); black (10YR 2/1) Error; strong medium subangular blocky, and strong subangular blocky structure; friable; fragments; slightly acid, pH 6.5; gradual smooth boundary. Lab sample # OSU0020290
BA—46 to 66 centimeters (18.1 to 26.0 inches); brown (10YR 4/3) Error; moderate fine and medium subangular blocky structure; firm; very dark grayish brown (10YR 3/2), moist, organic stains on faces of peds and 15 percent faint clay films; fragments; moderately acid, pH 6.0; clear smooth boundary. Lab sample # OSU0020291. patchy - phpvsfiid 979897; patchy - phpvsfiid 979897
2B—66 to 86 centimeters (26.0 to 33.9 inches); brown (7.5YR 4/4) Error; weak coarse subangular blocky structure; firm; brown (7.5YR 4/2), moist, clay films; 5 percent by volume nonflat indurated unspecified fragments; slightly acid, pH 6.5; gradual smooth boundary. Lab sample # OSU0020292
2BC1—86 to 107 centimeters (33.9 to 42.1 inches); brown (10YR 4/3) Error; subangular blocky structure; friable; dark brown (7.5YR 3/2), moist, clay films on sand and gravel; 5 percent by volume nonflat indurated unspecified fragments; neutral, pH 7.0; abrupt irregular boundary. Lab sample # OSU0020293. Evidence of stratification still evident.; patchy - phpvsfiid 979899; patchy - phpvsfiid 979899
2BC2—107 to 114 centimeters (42.1 to 44.9 inches); dark brown (7.5YR 3/2) Error; massive; friable; 33 percent fine distinct yellowish brown (10YR 5/4), moist, masses of oxidized iron and 33 percent fine distinct yellowish brown (10YR 5/6), moist, masses of oxidized iron; 5 percent by volume nonflat indurated unspecified fragments; moderately alkaline, pH 8.0; abrupt irregular boundary. Lab sample # OSU0020294. Sticky. Mottles are around sand grains. Non-calcareous.
2C1—114 to 152 centimeters (44.9 to 59.8 inches); dark yellowish brown (10YR 4/4) Error; single grain; loose; 38 percent by volume nonflat indurated 2-35-75 millimeter unspecified fragments; strong effervescence. Lab sample # OSU0020295. Matrix color tends slightly towards 7/5YR hue. Stratified. Upper 1 to 2 inches has ghosts of partially weathered limestone pebbles.
2C2—152 to 165 centimeters (59.8 to 65.0 inches); fragments. Excavations made in the area have exposed the stratified outwash to a depth of 10 ft. and greater. The outwash is variable both vertically and horizontally, but tends to contains a greater proportion of gravel at greater depths. The strata are generally e