IDENTIFIERS
Current Taxon Name (Soil Name):
Cardington
OSD
Series Extent
User Site ID:
YYYYOH117013
User Pedon ID:
YYYY-OH117-013
Lab Information:
Certified Lab Pedon Description -
no
Lab Source ID -
OHSTATE
Lab Pedon # -
MW-013
NCSS Pedon Lab Data NASIS Record ID -
70836
Print Date:
11/12/2024
LOCATION
Location Description:
3000 ft. S of center of Fulton and 500 ft. E of the range line on Lutheran camp property; 0 cm from beech tree stem. Low-flow side of beech tree.
State:
Ohio
County:
OH117—Morrow
PEDON
Describers Name:
Gersper
Current Taxonomic Class:
Fine, illitic, mesic Aquic Hapludalfs
Pedon Record Orgin:
NASIS
Correlated Information:
Soil Name -
Cardington
Classificaton Date -
5/4/2012
Dynamic Soil Properties:
Pedoderm Loose Cover Indicator -
no
Hydric:
no
SITE
Parent Material:
Wisconsinan till
Landform:
ground moraine
Drainage Class:
moderately well
Geology:
Wisconsinan formation.
Surface Fragments:
Benchmark Soil?:
no
VEGETATION
SITE OBSERVATION
Observation Date:
1/25/2000 (entry creation date)
Surface Cover Properties:
Site Obs. Cover Kind 1 -
tree cover
Site Obs. Cover Kind 2 -
hardwoods
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
—
—
—
335.3
—
—
—
—
—
—
—
—
—
—
—
—
—
—
—
A—0 to 6 centimeters (0.0 to 2.4 inches); very dark grayish brown (10YR 3/2) Error; moderate fine granular structure; very friable; fragments; abrupt smooth boundary. Lab sample # OSU0018250. Occcasional pebble-sized shale and sandstone fragments.
E1—6 to 14 centimeters (2.4 to 5.5 inches); 5 percent gray (10YR 5/1) and yellowish brown (10YR 5/4) Error; weak subangular blocky structure; friable; fragments; clear wavy boundary. Lab sample # OSU0018251. Occcasional pebble-sized fragments.
E2—14 to 25 centimeters (5.5 to 9.8 inches); light yellowish brown (10YR 6/4) Error; weak subangular blocky structure; friable; fragments; clear wavy boundary. Lab sample # OSU0018252. Roots comprise about 30% of volume.
BE—25 to 35 centimeters (9.8 to 13.8 inches); yellowish brown (10YR 5/6) and yellowish brown (10YR 5/4) Error; subangular blocky structure; firm; pale brown (10YR 6/3), moist, skeletans; , moist, iron-manganese concretions; fragments; clear smooth boundary. Lab sample # OSU0018253. Few fine and medium pores.
Bt1—35 to 49 centimeters (13.8 to 19.3 inches); strong brown (7.5YR 5/6) and yellowish brown (10YR 5/4) Error; moderate medium subangular blocky structure; firm; light yellowish brown (10YR 6/4), moist, skeletans; , moist, iron-manganese concretions and 11 percent fine faint gray (10YR 6/1), moist, masses of reduced iron; fragments; clear wavy boundary. Lab sample # OSU0018254. Very slightly sticky and slightly plastic. Occasional thin clay film in voids. Few to common, fine and medium pores.
Bt2—49 to 61 centimeters (19.3 to 24.0 inches); brown (7.5YR 4/4) and brown (10YR 5/3) Error; moderate subangular blocky structure; firm; light brownish gray (2.5Y 6/2), moist, masses of reduced iron and 11 percent fine distinct gray (10YR 6/1), moist, masses of reduced iron; 1 percent by volume nonflat indurated unspecified fragments; clear wavy boundary. Lab sample # OSU0018255. Slightly sticky and slightly plastic. Coarse skeleton is pebble-sized. Less than 5% thin clay films in voids, channels, and along partings. Few exped pores; common inped pores.
Bt3—61 to 83 centimeters (24.0 to 32.7 inches); dark yellowish brown (10YR 4/4) and brown (7.5YR 4/4) Error; moderate coarse subangular blocky structure; firm; grayish brown (10YR 5/2), moist, masses of reduced iron and gray (10YR 5/1), moist, masses of reduced iron and 11 percent fine distinct gray (10YR 5/1), moist, masses of reduced iron and 11 percent fine distinct strong brown (7.5YR 5/6), moist, masses of oxidized iron; 2 percent by volume nonflat indurated unspecified fragments; clear wavy boundary. Lab sample # OSU0018256. Very slightly sticky and moderately plastic. Coarse skeleton is mainly pebble-sized. About 25% thin, strong brown (7.5YR 5/6) clay films on primary and secondary surfaces (films tend to be thicker in voids and channels). Few exped pores; common inped por
BCt—83 to 105 centimeters (32.7 to 41.3 inches); dark yellowish brown (10YR 4/4) and brown (10YR 4/3) Error; weak subangular blocky structure; firm; gray (10YR 5/1), moist, masses of reduced iron and 11 percent fine faint gray (10YR 5/1), moist, masses of reduced iron; 5 percent by volume nonflat indurated unspecified fragments; diffuse wavy boundary. Lab sample # OSU0018257. Very slightly sticky and moderately plastic. Coarse skeleton mainly of pebble-sized shale and limestone fragments (very little grit size black shale fragments compared to other BC horizons described nearby). About 20% thin, dark brown (7.5YR 4/4) clay fil
C1—105 to 123 centimeters (41.3 to 48.4 inches); dark yellowish brown (10YR 4/6) and brown (10YR 4/3) Error; weak subangular blocky structure; firm; 11 percent fine faint gray (10YR 5/1), moist, masses of reduced iron; 12 percent by volume nonflat indurated 2-35-75 millimeter unspecified fragments; slight effervescence; diffuse boundary. Lab sample # OSU0018258. The subangular blocky units break into very thick platy units. Coarse skeleton mainly of grit- and pebble-sized black shale and pebble-sized limestone fragments. Occasional thin clay films in voids. Few fine and medium exped pores; common fine and medium
C2—123 to 130 centimeters (48.4 to 51.2 inches); dark yellowish brown (10YR 4/4) and brown (10YR 4/3) Error; weak subangular blocky structure; firm; 11 percent fine faint gray (10YR 5/1), moist, masses of reduced iron; 12 percent by volume nonflat indurated 2-35-75 millimeter unspecified fragments; slight effervescence; diffuse boundary. Lab sample # OSU0018259. The subangular blocky units break into very thick platy units. The tendency to break into platy units is not as great as in C1. Coarse skeleton mainly of grit- and pebble-sized black shale and pebble-sized limestone fragments. Occasional thin clay films i