IDENTIFIERS

  • Current Taxon Name (Soil Name): Winnegan
  • OSD
  • Series Extent
  • User Site ID: 2009MO171056
  • User Pedon ID: 2009MO171056
  • Vegetation Plot ID: 2009MO17156
  • Lab Information:
  • Certified Lab Pedon Description - no
  • Lab Source ID - MCL
  • Lab Pedon # - M0917156
  • NCSS Pedon Lab Data NASIS Record ID - 30066
  • 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: 40.5561111
  • Std. Longitude: -92.7256111
  • Datum: WGS84
  • Country: US—United States
  • State: Missouri
  • County: MO171—Putnam
  • MLRA: 109—Iowa and Missouri Heavy Till Plain
  • Non-MLRA Soil Survey Area: MO171—Putnam County, Missouri
  • 7.5 Minute USGS Quad: 40092-E6—Coatsville, Missouri

    • PEDON

  • Describers Name: Amber Marshaus
  • Current Taxonomic Class: Fine, mixed, mesic Oxyaquic 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 #: 156
  • Correlated Information:
  • Soil Name - Winnegan
  • PSC - 24 to 74 cm.
  • Classificaton Date - 1/31/2012
  • Soil Taxonomic Edition - tenth edition
  • Moisture Class - aquic
  • Moisture Subclass - oxyaquic
  • Sampled As Information:
  • Soil Name - Winnegan
  • Classificaton Date - 1/22/2009
  • Dynamic Soil Properties:
  • Erosion Class - 0
  • Pedoderm Loose Cover Indicator - no
  • Hydric: no


    • SITE

  • Parent Material: fine-silty loess derived from mixed over clayey till derived from igneous, metamorphic and sedimentary rock
  • Landscape: till plain
  • Landform: hillslope
  • Geomorphic Component Hills: side slope
  • Hill Slope Profile: backslope
  • Slope Complexity: simple
  • Slope Shape Across: linear
  • Slope Shape Down: linear
  • Runoff: negligible
  • Drainage Class: moderately well
  • Flooding: none flooding
  • Ponding: none ponding
  • Geology: Holocene Stage formation.
  • Surface Fragments:
  • Benchmark Soil?: no

    • VEGETATION

    SITE OBSERVATION

  • Observation Date: 1/22/2009 (actual site observation date)
  • Air Photo ID: 40092e6
  • Surface Water Kind: none observed
  • 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
  • Site Erosion Accelerated: water erosion sheet
    • Vegetation Plot Plants
    Plant Symbol Scientific Name National Vernacular Name Plant Type Group Canopy Cover % Vegetation Stata Level

    QUAL

    QUVE

    Quercus alba

    Quercus velutina

    white oak

    black oak

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    —

    —

    —

    —

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    Pedon Diagnostic Features
    Feature Kind Feature Depth L-H Feature Thickness L-RV-H
    cm

    ochric epipedon

    argillic horizon

    lithologic discontinuity

    redox depletions with chroma 2 or less

    secondary carbonates

    0—24

    24—203

    43—43

    63—

    119—

    —24—

    —179—

    —1—

    —1—

    —1—
    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

    17

    —

    —

    264.6

    —

    93

    —

    —

    —

    —

    —

    —

    —

    —

    —

    —

    —

    —

    —

    —
    A—0 to 9 centimeters (0.0 to 3.5 inches); very dark grayish brown (10YR 3/2) rubbed silt loam; moderate fine granular structure; friable; 3.0 very fine roots throughout and 3.0 fine roots throughout; 3.0 medium low-continuity dendritic tubular and 10.0 fine low-continuity dendritic tubular and 10.0 fine low-continuity dendritic tubular pores; fragments; noneffervescent, by hcl, 1n; abrupt smooth boundary.; observed in pit, small
    AB—9 to 24 centimeters (3.5 to 9.4 inches); 70 percent brown (10YR 4/3) broken face and 30 percent very dark grayish brown (10YR 3/2) broken face silt loam; moderate fine subangular blocky, and moderate medium subangular blocky structure; friable; 3.0 very fine roots throughout and 10.0 medium roots throughout and 3.0 fine roots throughout; 3.0 very fine low-continuity dendritic tubular and 0.5 medium low-continuity dendritic tubular pores; 1 percent medium faint irregular noncoherent cemented yellowish brown (10YR 5/4), moist, iron depletions with clear boundaries in matrix and 1 percent medium faint irregular noncoherent cemented yellowish brown (10YR 5/6), moist, iron depletions with clear boundaries in matrix; fragments; noneffervescent, by hcl, 1n; clear smooth boundary.; observed in pit, small
    Bt1—24 to 43 centimeters (9.4 to 16.9 inches); yellowish brown (10YR 5/4) broken face silt loam; moderate fine subangular blocky, and weak medium subangular blocky structure; firm; 10.0 very fine roots throughout and 3.0 medium roots throughout and 10.0 fine roots throughout; 3.0 very fine low-continuity dendritic tubular and 0.5 medium low-continuity dendritic tubular pores; 3 percent faint grayish brown (10YR 5/2), 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 brown (10YR 5/3), moist, iron depletions with clear boundaries in matrix; fragments; noneffervescent, by hcl, 1n; clear wavy boundary.; observed in pit, small
    2Bt2—43 to 63 centimeters (16.9 to 24.8 inches); yellowish brown (10YR 5/4) broken face silty clay; moderate fine subangular blocky, and weak coarse prismatic structure; firm; 3.0 medium roots throughout and 3.0 fine roots throughout and 0.5 coarse roots throughout; 0.5 medium low-continuity dendritic tubular and 3.0 fine low-continuity dendritic tubular pores; 8 percent distinct brown (10YR 5/3), moist, clay films on all faces of peds; 1 percent medium faint irregular noncoherent cemented grayish brown (10YR 5/2), moist, iron depletions with clear boundaries in matrix and 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 strong brown (7.5YR 5/6), moist, iron depletions with clear boundaries in matrix; 1 percent by volume nonflat subangular very strongly coherent cemented 2-?-5 millimeter mixed fragments; noneffervescent, by hcl, 1n; abrupt wavy boundary.; observed in pit, small
    2Bt3—63 to 89 centimeters (24.8 to 35.0 inches); yellowish brown (10YR 5/6) broken face clay; moderate fine subangular blocky, and moderate medium subangular blocky, and weak coarse prismatic structure; firm; 3.0 very fine roots throughout and 0.5 very coarse roots throughout and 10.0 medium roots throughout and 0.5 fine roots throughout; 3.0 fine low-continuity dendritic tubular pores; 10 percent distinct brown (10YR 5/3), moist, clay films on all faces of peds; 1 percent medium faint irregular noncoherent cemented strong brown (7.5YR 5/6), moist, iron depletions with clear boundaries in matrix and 1 percent medium faint irregular noncoherent cemented grayish brown (10YR 5/2), 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; 1 percent by volume nonflat subangular very strongly coherent cemented 2-?-5 millimeter mixed fragments; noneffervescent, by hcl, 1n; clear smooth boundary.; observed in pit, small
    2Bt4—89 to 119 centimeters (35.0 to 46.9 inches); yellowish brown (10YR 5/6) broken face clay loam; moderate medium subangular blocky, and moderate fine prismatic structure; very firm; 0.5 medium roots throughout and 0.5 fine roots throughout and 0.5 coarse roots throughout; 0.5 very fine low-continuity dendritic tubular and 0.5 fine low-continuity dendritic tubular pores; 10 percent distinct dark yellowish brown (10YR 4/6), moist, clay films on all faces of peds; 1 percent medium faint irregular noncoherent cemented strong brown (7.5YR 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 and 1 percent medium faint irregular noncoherent cemented grayish brown (10YR 5/2), moist, iron depletions with clear boundaries in matrix and 1 percent medium faint irregular noncoherent cemented strong brown (7.5YR 4/6), moist, iron depletions with clear boundaries in matrix; 2 percent by volume nonflat subangular very strongly coherent cemented 2-?-5 millimeter mixed fragments; noneffervescent, by hcl, 1n; abrupt smooth boundary.; observed in pit, small
    2Btk1—119 to 153 centimeters (46.9 to 60.2 inches); dark yellowish brown (10YR 4/6) broken face clay loam; moderate medium subangular blocky, and moderate medium angular blocky, and strong fine prismatic structure; very firm; 3.0 very fine roots throughout and 3.0 fine roots throughout; 3.0 very fine low-continuity dendritic tubular and 0.5 medium low-continuity dendritic tubular pores; 30 percent prominent 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 and 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 5/6), moist, iron depletions with clear boundaries in matrix and 1 percent medium faint irregular noncoherent cemented grayish brown (2.5Y 5/2), moist, iron depletions with clear boundaries in matrix; 2 percent fine prominent threadlike noncoherent cemented light gray (10YR 7/1), moist, carbonate, finely disseminated with diffuse boundaries throughout; 3 percent by volume nonflat subangular very strongly coherent cemented 2-?-75 millimeter mixed fragments; noneffervescent, by hcl, 1n; gradual smooth boundary.; observed in pit, small
    2Btk2—153 to 203 centimeters (60.2 to 79.9 inches); dark yellowish brown (10YR 4/6) broken face clay loam; moderate medium angular blocky, and strong medium prismatic structure; very firm; 3.0 very fine low-continuity dendritic tubular and 0.5 medium low-continuity dendritic tubular pores; 20 percent prominent brown (10YR 4/3), moist, clay films on all faces of peds; 1 percent medium faint irregular noncoherent cemented grayish brown (2.5Y 5/2), 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 and 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 strong brown (7.5YR 5/6), moist, iron depletions with clear boundaries in matrix; 8 percent medium prominent cylindrical extremely weakly coherent cemented white (10YR 8/1), moist, carbonate nodules with diffuse boundaries throughout; 3 percent by volume nonflat subangular very strongly coherent cemented 2-?-75 millimeter mixed fragments; strong effervescence, by hcl, 1n.; observed in pit, small