IDENTIFIERS
Current Taxon Name (Soil Name):
Clarksville
OSD
Series Extent
User Site ID:
1994MO203926M
User Pedon ID:
1994MO203926M
Transect:
Transect Stop Number -
2
Lab Information:
Certified Lab Pedon Description -
yes
Lab Source ID -
MCL
Lab Pedon # -
M94E_W02
NCSS Pedon Lab Data NASIS Record ID -
31986
Print Date:
3/31/2025
LOCATION
Location In Web Soil Survey
AOI is roughly a square mile and pedon is marked in the center.
Location in SoilWeb
Location in Google Maps
Std. Latitude:
37.1336500
Std. Longitude:
-91.1004000
Datum:
WGS84
State:
Missouri
County:
MO203—Shannon
MLRA:
116A—Ozark Highland
Non-MLRA Soil Survey Area:
MO613—Shannon County, Missouri, North & West PartsMO203—Shannon County, Missouri
7.5 Minute USGS Quad:
37091-B1—Exchange, Missouri
PEDON
Describers Name:
DM
Current Taxonomic Class:
Loamy-skeletal, siliceous, active, mesic Typic Paleudults
Current Taxon Kind:
taxadjunct
Pedon Type:
within range of map unit
Pedon Purpose:
laboratory sampling site
Pedon Record Orgin:
Converted from PDP 3.x
Correlated Information:
Soil Name -
Clarksville
PSC -
46 to 86 cm.
Classificaton Date -
3/28/2011
Soil Taxonomic Edition -
eighth edition
Moisture Class -
udic
Sampled As Information:
Soil Name -
Clarksville
Taxonomic Class -
Loamy-skeletal, siliceous, semiactive, mesic Typic Paleudults
Taxon Kind -
series
PSC -
23 to 73 cm.
Classificaton Date -
7/13/1994
Dynamic Soil Properties:
Pedoderm Loose Cover Indicator -
no
Hydric:
no
Field Measured Properties:
46 Cation exchange capacity to clay ratio
SITE
Parent Material:
slope alluvium over residuum
Landscape:
hills
Landform:
hillslope
Geomorphic Component Hills:
side slope
Hill Slope Profile:
backslope
Slope Shape Across:
convex
Slope Shape Down:
linear
Drainage Class:
well
Surface Fragments:
Benchmark Soil?:
no
VEGETATION
SITE OBSERVATION
Observation Date:
7/13/1994 (actual site observation date)
Air Photo ID:
16
Surface Cover Properties:
Pedoderm Loose Cover Indicator -
no
Drained? -
no
Bedded Soil? -
no
Forest Plantation? -
no
Pedon Diagnostic Features
Feature Kind
Feature Depth L-H
Feature Thickness L-RV-H
cm
ochric epipedon
argillic horizon
3—56
56—166
—-
—-
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
44
—
—
268
—
230
—
—
—
—
—
—
—
—
—
—
—
—
—
—
Oi—0 to 3 centimeters (0.0 to 1.2 inches); slightly decomposed plant material; fragments.
A1—3 to 16 centimeters (1.2 to 6.3 inches); very dark grayish brown (10YR 3/2) extremely gravelly loam; moderate medium granular structure; very friable; 10.0 very fine roots and 1.0 fine roots; 10.0 very fine interstitial pores; 10 percent distinct very dark gray (10YR 3/1), moist, organic stains on upper surfaces of peds or rocks; 10 percent by volume nonflat angular indurated 75-162-250 millimeter chert fragments and 75 percent by volume nonflat angular indurated 2-40-75 millimeter chert fragments; extremely acid, pH 4.2, hellige-truog; clear wavy boundary. Lab sample # MU052175
A2—16 to 23 centimeters (6.3 to 9.1 inches); brown (10YR 4/3) extremely gravelly loam; moderate fine granular structure; very friable; 3.0 very fine and fine roots and 1.0 medium and coarse roots; 10.0 very fine interstitial pores; 25 percent distinct very dark grayish brown (10YR 3/2), moist, organic stains on faces of peds; 5 percent by volume nonflat angular indurated 75-162-250 millimeter chert fragments and 70 percent by volume nonflat angular indurated 2-40-75 millimeter chert fragments; extremely acid, pH 4.4, hellige-truog; clear smooth boundary. Lab sample # MU052176
BE1—23 to 36 centimeters (9.1 to 14.2 inches); brown (10YR 5/3) extremely gravelly loam; weak fine subangular blocky structure; very friable; 3.0 medium roots and 2.0 fine roots; 5.0 very fine interstitial and 3.0 fine tubular pores; 1 percent distinct very dark grayish brown (10YR 3/2), moist, organic stains on faces of peds; 1 percent fine spherical iron-manganese concretions; 60 percent by volume nonflat angular indurated 2-40-75 millimeter chert fragments; extremely acid, pH 4.4, hellige-truog; clear smooth boundary. Lab sample # MU052177
BE21—36 to 46 centimeters (14.2 to 18.1 inches); yellowish brown (10YR 5/4) very gravelly silt loam; weak fine subangular blocky structure; very friable; 2.0 very fine and fine roots and 3.0 medium roots and 1.0 coarse roots; 5.0 very fine interstitial and 1.0 fine tubular pores; 1 percent fine spherical iron-manganese concretions; 15 percent by volume nonflat subrounded indurated 2-40-75 millimeter chert fragments and 20 percent by volume nonflat angular indurated 2-40-75 millimeter chert fragments; very strongly acid, pH 4.5, hellige-truog; clear smooth boundary. Lab sample # MU052178
BE22—46 to 56 centimeters (18.1 to 22.0 inches); yellowish brown (10YR 5/4) very gravelly silt loam; weak fine subangular blocky structure; very friable; 2.0 very fine and fine roots and 3.0 medium roots and 1.0 coarse roots; 5.0 very fine interstitial and 1.0 fine tubular pores; 15 percent by volume nonflat subrounded indurated 2-40-75 millimeter chert fragments and 20 percent by volume nonflat angular indurated 2-40-75 millimeter chert fragments; very strongly acid, pH 4.7, hellige-truog. Lab sample # MU052179
Bt1—56 to 72 centimeters (22.0 to 28.3 inches); yellowish brown (10YR 5/4) very gravelly silt loam; weak fine subangular blocky structure; very friable; 3.0 medium roots and 2.0 fine roots and 1.0 coarse roots; 10.0 very fine interstitial pores; 1 percent distinct strong brown (7.5YR 5/6), moist, clay films on vertical faces of peds and 1 percent faint brown (10YR 5/3), moist, silt coats on vertical faces of peds; 3 percent fine spherical iron-manganese concretions; 25 percent by volume nonflat angular indurated 2-40-75 millimeter chert fragments and 25 percent by volume nonflat subrounded indurated 2-40-75 millimeter chert fragments; very strongly acid, pH 4.7, hellige-truog; clear smooth boundary. Lab sample # MU052180
2Bt2—72 to 87 centimeters (28.3 to 34.3 inches); yellowish brown (10YR 5/4) very gravelly loam; weak fine subangular blocky structure; friable; 0.1 very fine roots and 1.0 medium roots and 0.1 fine roots; 7.0 very fine interstitial and 2.0 fine tubular pores; 1 percent faint strong brown (7.5YR 5/6), moist, clay films on vertical faces of peds and 4 percent distinct pale brown (10YR 6/3), moist, silt coats on vertical faces of peds; 3 percent fine spherical iron-manganese concretions; 25 percent by volume nonflat subrounded indurated 2-40-75 millimeter chert fragments and 25 percent by volume nonflat angular indurated 2-40-75 millimeter chert fragments; very strongly acid, pH 4.8, hellige-truog; clear smooth boundary. Lab sample # MU052181. stone line occurs at 43 inches
2Bt3—87 to 97 centimeters (34.3 to 38.2 inches); strong brown (7.5YR 5/6) gravelly loam; moderate fine and medium subangular blocky structure; friable; 0.1 very fine and fine roots and 1.0 medium roots; 15.0 very fine vesicular pores; 1 percent distinct strong brown (7.5YR 4/6), moist, clay films on all faces of peds and 25 percent distinct light yellowish brown (10YR 6/4), moist, silt coats on all faces of peds; 3 percent fine spherical iron-manganese concretions; 25 percent by volume nonflat subrounded indurated 2-40-75 millimeter chert fragments; very strongly acid, pH 4.8, hellige-truog; clear smooth boundary. Lab sample # MU052182
2Bt4—97 to 102 centimeters (38.2 to 40.2 inches); 70 percent strong brown (7.5YR 5/6) very gravelly loam; strong medium and coarse subangular blocky structure; friable; 0.1 very fine and fine roots; 2.0 fine interstitial and 9.0 fine tubular pores; 1 percent distinct yellowish red (5YR 5/6), moist, clay films on all faces of peds and 1 percent distinct yellowish brown (10YR 5/4), moist, silt coats in root channels and/or pores; 1 percent fine spherical iron-manganese concretions; 10 percent by volume nonflat subrounded indurated 75-162-250 millimeter chert fragments and 10 percent by volume nonflat angular indurated 2-40-75 millimeter chert fragments and 15 percent by volume nonflat subrounded indurated 2-40-75 millimeter chert fragments; very strongly acid, pH 4.9, hellige-truog; gradual wavy boundary. Lab sample # MU052183
2Bt5—102 to 130 centimeters (40.2 to 51.2 inches); 90 percent yellowish red (5YR 5/8) gravelly clay loam; moderate medium subangular blocky structure; firm; 0.1 very fine and fine roots; 5.0 fine tubular pores; 35 percent distinct red (2.5YR 4/8), moist, clay films on faces of peds and in pores; 3 percent fine spherical iron-manganese concretions; 15 percent by volume nonflat subrounded indurated 2-40-75 millimeter chert fragments; very strongly acid, pH 4.8, hellige-truog; clear smooth boundary. Lab sample # MU052184
3Bt61—130 to 143 centimeters (51.2 to 56.3 inches); 65 percent yellowish red (5YR 5/8) gravelly clay; moderate coarse subangular blocky parts to weak fine subangular blocky structure; firm; 1.0 medium roots and 0.1 fine roots; 12.0 fine tubular pores; 40 percent prominent red (2.5YR 5/6), moist, clay films on all faces of peds; 10 percent fine spherical iron-manganese concretions; 20 percent by volume nonflat subrounded indurated 2-40-75 millimeter chert fragments; very strongly acid, pH 4.8, hellige-truog; clear wavy boundary. Lab sample # MU052185
3Bt62—143 to 153 centimeters (56.3 to 60.2 inches); 65 percent yellowish red (5YR 5/8) gravelly clay; fragments; very strongly acid, pH 4.8, hellige-truog. Lab sample # MU052186
3Bt7—153 to 166 centimeters (60.2 to 65.4 inches); 70 percent yellowish red (5YR 5/8) and 10 percent brownish yellow (10YR 6/8) very gravelly clay; moderate medium subangular blocky parts to moderate very fine and fine angular blocky structure; firm; 0.1 fine roots; 4.0 fine tubular pores; 35 percent prominent red (2.5YR 5/8), moist, clay films on all faces of peds; 20 percent by volume nonflat subrounded indurated 2-40-75 millimeter chert fragments and 25 percent by volume nonflat angular indurated 2-40-75 millimeter chert fragments; very strongly acid, pH 4.8, hellige-truog. Lab sample # MU052187. possible coarse prismatic structure parting to others fine gravel concentrations occur in pockets