IDENTIFIERS

  • Current Taxon Name (Soil Name): WABASH
  • OSD
  • Series Extent
  • User Site ID: 2003MO117041
  • User Pedon ID: 2003MO117041
  • Lab Information:
  • Certified Lab Pedon Description - no
  • Lab Source ID - MCL
  • Lab Pedon # - M0311741
  • NCSS Pedon Lab Data NASIS Record ID - 26069
  • Print Date: 5/31/2024
  • 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: 39.6865417
  • Std. Longitude: -93.2991167
  • Datum: WGS84
  • Township: T56N
  • Range: R21W
  • Section: 7
  • PLSS Details: 2350 feet east and 830 feet south of the northwest corner
  • Country: US—United States
  • State: Missouri
  • County: MO117—Livingston
  • MLRA: 107—Iowa and Missouri Deep Loess Hills
  • Non-MLRA Soil Survey Area: MO117—Livingston County, Missouri
  • 7.5 Minute USGS Quad: 39093-F3—Fountain Grove, Missouri
  • PEDON

  • Describers Name: Larry Gray, Kim Worth, LeAnn Bullard, Greg Caldwell
  • Current Taxonomic Class: Fine, mixed, mesic Cumulic Vertic Epiaquolls
  • Current Taxon Kind: series
  • Pedon Type: map unit inclusion
  • Pedon Purpose: full pedon description
  • Pedon Record Orgin: Windows Pedon
  • Pedon #: 41
  • Correlated Information:
  • Soil Name - WABASH
  • PSC - 25 to 102 cm.
  • Classificaton Date - 4/11/2012
  • Soil Taxonomic Edition - ninth edition
  • Moisture Class - aquic
  • Moisture Subclass - typic
  • Sampled As Information:
  • Soil Name - SND
  • Classificaton Date - 8/31/2003
  • Dynamic Soil Properties:
  • Erosion Class - 0
  • Pedoderm Loose Cover Indicator - no
  • Hydric: no


  • SITE

  • Parent Material: clayey alluvium derived from mixed
  • Landscape: river valley
  • Landform: flood plain
  • Geomorphic Component Hills: interfluve
  • Slope Complexity: simple
  • Slope Shape Across: concave
  • Slope Shape Down: concave
  • Runoff: negligible
  • Drainage Class: poorly
  • Flooding: frequent flooding for brief periods
  • Ponding: frequent ponding for brief periods
  • Geology: Holocene Stage formation.
  • Surface Fragments:
  • Benchmark Soil?: no
  • VEGETATION

    SITE OBSERVATION

  • Observation Date: 8/31/2003 (actual site observation date)
  • Air Photo ID: 39093f3se
  • Surface Water Kind: flooded
  • Surface Water Depth: 15
  • Surface Cover Properties:
  • Site Obs. Cover Kind 1 - wetlands
  • Site Obs. Cover Kind 2 - crop shrubs
  • Pedoderm Loose Cover Indicator - no
  • Drained? - no
  • Bedded Soil? - no
  • Forest Plantation? - no
  • Site Erosion Accelerated: water erosion gully
  • Pedon Diagnostic Features
    Feature Kind Feature Depth L-H Feature Thickness L-RV-H
    cm

    mollic epipedon

    cambic horizon

    0—64

    23—193

    —64—

    —170—

    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

    2

    201.2

    315

    Ap—0 to 23 centimeters (0.0 to 9.1 inches); very dark grayish brown (10YR 3/2) interior silty clay; moderate very fine and fine granular, and moderate fine and medium subangular blocky structure; firm; 6.0 very fine and fine roots; 6.0 very fine and fine vesicular pores; 5 percent light brownish gray (10YR 6/2), moist, coats; 1 percent medium faint irregular noncoherent cemented dark yellowish brown (10YR 4/6), moist, iron depletions with clear boundaries in matrix; 1 percent fine black (10YR 2/1), moist, manganese concretions; fragments; clear smooth boundary. Lab sample # MU006973; observed in push tube
    Bg1—23 to 43 centimeters (9.1 to 16.9 inches); very dark grayish brown (10YR 3/2) interior silty clay; moderate fine subangular blocky structure; firm; 3.0 very fine and fine roots; 6.0 very fine and fine vesicular pores; 5 percent light brownish gray (10YR 6/2), moist, coats; 1 percent medium faint irregular noncoherent cemented dark yellowish brown (10YR 4/6), moist, iron depletions with clear boundaries in matrix; 1 percent fine black (10YR 2/1), moist, manganese concretions; fragments; clear smooth boundary. Lab sample # MU006974; observed in push tube
    Bg2—43 to 66 centimeters (16.9 to 26.0 inches); very dark gray (2.5Y 3/1) interior silty clay; moderate very fine and fine subangular blocky structure; firm; 0.5 very fine roots; 3.0 very fine vesicular pores; 1 percent medium faint irregular noncoherent cemented yellowish red (5YR 4/6), moist, iron depletions with clear boundaries in matrix; 10 percent fine black (10YR 2/1), moist, manganese concretions; fragments; clear smooth boundary. Lab sample # MU006975; observed in push tube
    Bg3—66 to 109 centimeters (26.0 to 42.9 inches); 60 percent very dark gray (10YR 3/1) interior and 40 percent dark gray (10YR 4/1) interior silty clay; moderate fine subangular blocky, and weak thin platy structure; firm; 0.5 very fine roots; 3.0 very fine vesicular pores; 1 percent medium faint irregular noncoherent cemented yellowish red (5YR 4/6), moist, iron depletions with clear boundaries in matrix; 1 percent fine black (10YR 2/1), moist, manganese concretions; fragments; clear smooth boundary. Lab sample # MU006976; observed in push tube
    Bg4—109 to 157 centimeters (42.9 to 61.8 inches); 40 percent dark gray (10YR 4/1) interior and 60 percent very dark gray (10YR 3/1) interior silty clay loam; moderate very fine and fine subangular blocky structure; firm; 3.0 very fine vesicular pores; 1 percent dark yellowish brown (10YR 4/4), moist, and light brownish gray (10YR 6/2), moist, coats; 1 percent medium faint irregular noncoherent cemented yellowish red (5YR 4/6), moist, iron depletions with clear boundaries in matrix; 10 percent fine black (10YR 2/1), moist, manganese concretions; fragments; clear smooth boundary. Lab sample # MU006978; observed in push tube
    Bg5—157 to 193 centimeters (61.8 to 76.0 inches); black (10YR 2/1) interior silty clay; moderate fine and medium subangular blocky structure; firm; 0.5 very fine vesicular pores; fragments. Lab sample # MU006979; observed in push tube