IDENTIFIERS

  • Current Taxon Name (Soil Name): WINNEGAN
  • OSD
  • Series Extent
  • User Site ID: 2007MO211060
  • User Pedon ID: 2007MO211060
  • Lab Information:
  • Certified Lab Pedon Description - no
  • Lab Source ID - MCL
  • Lab Pedon # - M0721160
  • NCSS Pedon Lab Data NASIS Record ID - 26301
  • Print Date: 11/23/2024

    • 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: 40.3219722
  • Std. Longitude: -92.8507778
  • Datum: WGS84
  • Township: T64N
  • Range: R17W
  • Section: 30
  • PLSS Details: 1,392 feet East and 2,263 feet South from the North West corner
  • Country: US—United States
  • State: Missouri
  • County: MO211—Sullivan
  • MLRA: 109—Iowa and Missouri Heavy Till Plain
  • Non-MLRA Soil Survey Area: MO211—Sullivan County, Missouri
  • 7.5 Minute USGS Quad: 40092-C7—Stahl, Missouri

    • PEDON

  • Describers Name: David Dowdy, Amber Marshaus
  • Current Taxonomic Class: Fine, smectitic, superactive, mesic Oxyaquic Vertic Hapludalfs
  • Current Taxon Kind: series
  • Pedon Type: classifies to current taxon name, full description
  • Pedon Purpose: full pedon description
  • Pedon Record Orgin: Missouri Pedon
  • Pedon #: 60
  • Correlated Information:
  • Soil Name - WINNEGAN
  • PSC - 13 to 64 cm.
  • Classificaton Date - 2/1/2012
  • Soil Taxonomic Edition - tenth edition
  • Moisture Class - udic
  • Moisture Subclass - oxyaquic
  • Sampled As Information:
  • Soil Name - WINNEGAN
  • Classificaton Date - 9/26/2007
  • Dynamic Soil Properties:
  • Erosion Class - 0
  • Pedoderm Loose Cover Indicator - no
  • Hydric: no


    • SITE

  • Parent Material: clayey till derived from mixed
  • Landscape: upland
  • Landform: till plain
  • Geomorphic Component Hills: side slope
  • Hill Slope Profile: backslope
  • Slope Position: upper third
  • Slope Complexity: simple
  • Slope Shape Across: concave
  • Slope Shape Down: concave
  • Runoff: negligible
  • Drainage Class: moderately well
  • Flooding: none flooding
  • Ponding: none ponding
  • Geology: Pre-illinoian Stage formation.
  • Surface Fragments:
  • Benchmark Soil?: no

    • VEGETATION

    SITE OBSERVATION

  • Observation Date: 9/26/2007 (actual site observation date)
  • Air Photo ID: 40092c7nw
  • Surface Water Kind: none observed
  • 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
  • Site Erosion Accelerated: water erosion gully
    • Pedon Diagnostic Features
    Feature Kind Feature Depth L-H Feature Thickness L-RV-H
    cm

    ochric epipedon

    argillic horizon

    0—13

    13—178

    —13—

    —165—
    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

    13

    —

    —

    281

    —

    210

    —

    —

    —

    —

    —

    —

    —

    —

    —

    —

    —

    —

    —

    —
    Ap—0 to 13 centimeters (0.0 to 5.1 inches); brown (10YR 4/3) broken face silt loam; 19 percent sand; 54 percent silt; 27 percent clay; weak fine subangular blocky, and weak thick platy structure; friable; 10.0 very fine roots throughout and 0.5 medium roots throughout and 10.0 fine roots throughout; 3.0 fine dendritic tubular pores; fragments; clear smooth boundary. Lab sample # MU008577; observed in push tube
    Bt1—13 to 25 centimeters (5.1 to 9.8 inches); yellowish brown (10YR 5/6) broken face clay loam; 21 percent sand; 40 percent silt; 39 percent clay; moderate fine subangular blocky structure; firm; 3.0 fine roots throughout; 3.0 fine dendritic tubular pores; 35 percent distinct brown (10YR 4/3), moist, clay films on all faces of peds; 1 percent medium faint irregular noncoherent cemented black (10YR 2/1), moist, iron depletions with clear boundaries in matrix; 1 percent by volume nonflat subangular very strongly coherent cemented 2-?-5 millimeter unspecified fragments; clear smooth boundary. Lab sample # MU008578; observed in push tube
    Bt2—25 to 43 centimeters (9.8 to 16.9 inches); yellowish brown (10YR 5/4) broken face silty clay; 1 percent sand; 57 percent silt; 42 percent clay; moderate medium subangular blocky structure; firm; 3.0 very fine roots throughout and 3.0 fine roots throughout; 3.0 very fine dendritic tubular and 3.0 fine dendritic tubular pores; 35 percent faint brown (10YR 4/3), moist, clay films on all faces of peds; 1 percent medium faint irregular noncoherent cemented yellowish brown (10YR 5/6), moist, iron depletions with clear boundaries in matrix and 1 percent medium faint irregular noncoherent cemented black (10YR 2/1), moist, iron depletions with clear boundaries in matrix; fragments; clear smooth boundary. Lab sample # MU008579; observed in push tube
    Bt3—43 to 56 centimeters (16.9 to 22.0 inches); yellowish brown (10YR 5/6) broken face silty clay; 4 percent sand; 55 percent silt; 41 percent clay; weak fine subangular blocky structure; firm; 3.0 fine roots throughout; 0.5 fine dendritic tubular pores; 12 percent distinct dark yellowish brown (10YR 4/4), moist, clay films on all faces of peds; 1 percent medium faint irregular noncoherent cemented black (10YR 2/1), moist, iron depletions with clear boundaries in matrix and 1 percent medium faint irregular noncoherent cemented dark grayish brown (10YR 4/2), moist, iron depletions with clear boundaries in matrix; fragments; clear smooth boundary. Lab sample # MU008580; observed in push tube
    Bt4—56 to 81 centimeters (22.0 to 31.9 inches); yellowish brown (10YR 5/6) broken face clay loam; 35 percent sand; 36 percent silt; 29 percent clay; moderate fine subangular blocky, and moderate coarse prismatic structure; very firm; 3.0 very fine roots throughout; 3.0 very fine dendritic tubular and 3.0 fine dendritic tubular pores; 35 percent prominent reddish gray (2.5YR 5/1), moist, clay films on all faces of peds; 1 percent medium faint irregular noncoherent cemented black (10YR 2/1), moist, iron depletions with clear boundaries in matrix and 1 percent medium faint irregular noncoherent cemented yellowish brown (10YR 5/8), moist, iron depletions with clear boundaries in matrix; 4 percent by volume nonflat subangular very strongly coherent cemented 2-?-5 millimeter unspecified fragments; slight effervescence, by hcl, 1n; clear smooth boundary.; observed in push tube
    Bt5—81 to 140 centimeters (31.9 to 55.1 inches); yellowish brown (10YR 5/4) broken face clay loam; 35 percent sand; 36 percent silt; 29 percent clay; moderate coarse prismatic structure; very firm; 3.0 fine roots between peds; 0.5 fine dendritic tubular pores; 12 percent distinct gray (10YR 6/1), moist, clay films on all faces of peds; 1 percent medium faint irregular noncoherent cemented black (10YR 2/1), moist, iron depletions with clear boundaries in matrix and 1 percent medium faint irregular noncoherent cemented reddish gray (2.5YR 5/1), moist, iron depletions with clear boundaries in matrix; 8 percent by volume nonflat subangular very strongly coherent cemented 2-?-5 millimeter unspecified fragments; strong effervescence, by hcl, 1n; gradual smooth boundary.; observed in push tube
    Bt6—140 to 178 centimeters (55.1 to 70.1 inches); yellowish brown (10YR 5/6) broken face clay loam; 34 percent sand; 36 percent silt; 30 percent clay; moderate coarse prismatic structure; very firm; 3.0 fine roots between peds; 0.5 fine dendritic tubular pores; 35 percent distinct gray (10YR 6/1), moist, clay films on all faces of peds; 1 percent medium faint irregular noncoherent cemented black (10YR 2/1), moist, iron depletions with clear boundaries in matrix and 1 percent medium faint irregular noncoherent cemented gray (10YR 6/1), moist, iron depletions with clear boundaries in matrix; 5 percent by volume nonflat subangular very strongly coherent cemented 2-?-5 millimeter unspecified fragments; strong effervescence, by hcl, 1n.; observed in push tube