IDENTIFIERS
Current Taxon Name (Soil Name):
Lenzburg
OSD
Series Extent
User Site ID:
S2010IL157003
User Pedon ID:
S2010IL157003
Lab Information:
Certified Lab Pedon Description -
no
Lab Source ID -
SSL
Lab Pedon # -
11N0118
NCSS Pedon Lab Data NASIS Record ID -
40119
Print Date:
12/4/2024
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:
38.1731333
Std. Longitude:
-89.7191194
Datum:
WGS84
Township:
4S
Range:
6W
Section:
24
Map Unit:
871B—Lenzburg gravelly silty clay loam, 1 to 7 percent slopes, stony
State:
Illinois
County:
IL157—Randolph
MLRA:
114—Southern Illinois and Indiana Thin Loess and Till Plain
Non-MLRA Soil Survey Area:
IL157—Randolph County, Illinois
7.5 Minute USGS Quad:
38089-B6—Tilden, Illinois
PEDON
Describers Name:
Erik Gerhard, Dwayne Williams
Pedon Purpose:
research site
Pedon Record Orgin:
NASIS
Pedon #:
3
Sampled As Information:
Soil Name -
Lenzburg
PSC -
25 to 100 cm.
Classificaton Date -
9/22/2010
Soil Taxonomic Edition -
tenth edition
Dynamic Soil Properties:
Pedoderm Loose Cover Indicator -
no
Hydric:
no
SITE
Anthropogenic Feature:
reclaimed land on surface mine
Geomorphic Component Hills:
interfluve
Slope Position:
upper third
Slope Complexity:
simple
Slope Shape Across:
linear
Slope Shape Down:
linear
Surface Fragments:
Benchmark Soil?:
no
VEGETATION
SITE OBSERVATION
Observation Date:
9/22/2010 (actual site observation date)
Surface Cover Properties:
Site Obs. Cover Kind 1 -
grass/herbaceous cover
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
—
—
—-
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
—
—
139
—
323
—
—
—
—
—
—
—
—
—
—
—
—
—
—
Ap1—0 to 26 centimeters (0.0 to 10.2 inches); brown (10YR 4/3) crushed silt loam; 3 percent sand; 79 percent silt; 18 percent clay; weak fine granular structure; friable; 6.0 very fine roots throughout and 6.0 medium roots throughout and 6.0 fine roots throughout; 5 percent fine prominent spherical strong brown (7.5YR 5/6), moist, masses of oxidized iron with clear boundaries throughout; 3 percent by volume 2-3-5 millimeter mixed fragments; neutral, pH 6.7, hellige-truog; gradual smooth boundary. Lab sample # 11N00564; observed in pit, small
Ap2—26 to 51 centimeters (10.2 to 20.1 inches); brown (10YR 5/3) crushed silt loam; 3 percent sand; 76 percent silt; 21 percent clay; moderate medium platy structure; friable; 6.0 very fine roots throughout and 6.0 fine roots throughout; 10 percent medium prominent spherical yellowish brown (10YR 5/8), moist, masses of oxidized iron with clear boundaries throughout and 10 percent fine distinct spherical grayish brown (10YR 5/2), moist, masses of reduced iron with clear boundaries throughout; 3 percent by volume 2-3-5 millimeter mixed fragments; neutral, pH 7.1, hellige-truog; gradual smooth boundary. Lab sample # 11N00565; observed in pit, small
Bw—51 to 203 centimeters (20.1 to 79.9 inches); dark grayish brown (10YR 4/2) broken face gravelly loam; 35 percent sand; 33 percent silt; 32 percent clay; massive; very firm; 0.9 fine roots between peds; 10 percent fine prominent spherical yellowish brown (10YR 5/8), moist, masses of oxidized iron with clear boundaries throughout and 10 percent coarse distinct spherical grayish brown (10YR 5/2), moist, masses of reduced iron with clear boundaries throughout and 10 percent fine distinct clay depletions on faces of peds and 10 percent coarse distinct clay depletions on faces of peds; 5 percent by volume nonflat subrounded 2-2-5 millimeter shale, calcareous fragments and 15 percent by volume nonflat subrounded 2-5-15 millimeter limestone, unspecified fragments; slightly alkaline, pH 7.8, hellige-truog. Lab sample # 11N00566; observed in pit, small. Due to the nature of the reclaimed material this horizon also contained strong coarse angular blocky structure. When this structure was added to the horizon, Nasis 6 recognized this horizon as two separate horizons. So it was removed and added to the text notes. Occasional cobbles and stones are found in this horizon