IDENTIFIERS

  • Current Taxon Name (Soil Name): Winnegan
  • OSD
  • Series Extent
  • User Site ID: 2009MO001051
  • User Pedon ID: 2009MO001051
  • Vegetation Plot ID: 2009MO00151
  • Lab Information:
  • Certified Lab Pedon Description - no
  • Lab Source ID - MCL
  • Lab Pedon # - M0900151
  • NCSS Pedon Lab Data NASIS Record ID - 30177
  • Print Date: 11/12/2024

    • 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: 40.1061111
  • Std. Longitude: -92.6431944
  • Datum: WGS84
  • Country: US—United States
  • State: Missouri
  • County: MO001—Adair
  • MLRA: 109—Iowa and Missouri Heavy Till Plain
  • Non-MLRA Soil Survey Area: MO001—Adair County, Missouri
  • 7.5 Minute USGS Quad: 40092-A6—Gifford, Missouri

    • PEDON

  • Describers Name: Amber Marshaus, Kim Worth
  • Current Taxonomic Class: Fine, mixed, mesic Aquic Hapludalfs
  • Current Taxon Kind: taxadjunct
  • Pedon Type: classifies to current taxon name, full description
  • Pedon Purpose: full pedon description
  • Pedon Record Orgin: Missouri Pedon
  • Pedon #: 151
  • Correlated Information:
  • Soil Name - Winnegan
  • PSC - 22 to 72 cm.
  • Classificaton Date - 1/31/2012
  • Soil Taxonomic Edition - tenth edition
  • Moisture Class - aquic
  • Moisture Subclass - aquic
  • Sampled As Information:
  • Soil Name - Winnegan
  • Classificaton Date - 2/23/2009
  • Dynamic Soil Properties:
  • Erosion Class - 0
  • Pedoderm Loose Cover Indicator - no
  • Hydric: no


    • SITE

  • Parent Material: clayey till derived from mixed
  • 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: somewhat poorly
  • Flooding: none flooding
  • Ponding: none ponding
  • Geology: Excello Sh. formation.
  • Surface Fragments:
  • Benchmark Soil?: no

    • VEGETATION

    SITE OBSERVATION

  • Observation Date: 2/23/2009 (actual site observation date)
  • Air Photo ID: 40092a6
  • 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

    Quercus alba

    white oak

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

    ochric epipedon

    argillic horizon

    redox depletions with chroma 2 or less

    secondary carbonates

    0—22

    22—116

    34—203

    51—203

    —22—

    —94—

    —169—

    —152—
    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

    23

    —

    —

    271.6

    —

    250

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    —

    —

    —

    —

    —

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    A—0 to 9 centimeters (0.0 to 3.5 inches); 60 percent very dark grayish brown (10YR 3/2) rubbed and 40 percent very dark grayish brown (10YR 3/2) broken face loam; weak very fine subangular blocky, and weak very fine granular structure; friable; 3.0 very fine roots throughout and 3.0 fine roots throughout; 2.0 very fine low-continuity dendritic tubular and 1.0 medium low-continuity dendritic tubular and 3.0 fine low-continuity dendritic tubular pores; 1 percent by volume nonflat subrounded very strongly coherent cemented 2-?-5 millimeter mixed fragments; noneffervescent, by hcl, 1n; abrupt wavy boundary.; observed in pit, small
    BA—9 to 22 centimeters (3.5 to 8.7 inches); 80 percent yellowish brown (10YR 5/4) broken face and 20 percent dark grayish brown (10YR 4/2) broken face loam; weak fine subangular blocky, and weak very fine subangular blocky structure; friable; 3.0 very fine roots throughout and 2.0 medium roots throughout and 3.0 fine roots throughout; 2.0 very fine moderate-continuity dendritic tubular pores; 3 percent faint dark yellowish brown (10YR 4/4), 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; 1 percent by volume nonflat subrounded very strongly coherent cemented 2-?-5 millimeter mixed fragments; noneffervescent, by hcl, 1n; clear smooth boundary.; observed in pit, small
    Bt1—22 to 34 centimeters (8.7 to 13.4 inches); yellowish brown (10YR 5/6) broken face clay loam; moderate fine subangular blocky, and moderate medium subangular blocky structure; firm; 1.0 very coarse roots throughout and 1.0 medium roots throughout and 2.0 fine roots throughout; 1.0 very fine moderate-continuity dendritic tubular pores; 35 percent prominent yellowish brown (10YR 5/4), moist, clay films on all faces of peds; 1 percent medium faint irregular noncoherent cemented brown (10YR 5/3), 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; 1 percent by volume nonflat subrounded very strongly coherent cemented 2-?-5 millimeter mixed fragments and 1 percent by volume nonflat subrounded very strongly coherent cemented 5-?-20 millimeter mixed fragments; noneffervescent, by hcl, 1n; clear smooth boundary.; observed in pit, small
    Bt2—34 to 51 centimeters (13.4 to 20.1 inches); yellowish brown (10YR 5/6) broken face clay; moderate medium subangular blocky, and moderate fine subangular blocky structure; very firm; 2.0 medium roots between peds and 10.0 fine roots between peds and 1.0 coarse roots throughout; 1.0 very fine moderate-continuity dendritic tubular pores; 70 percent prominent yellowish brown (10YR 5/4), moist, clay films on all faces of peds; 1 percent medium faint irregular noncoherent cemented yellowish brown (10YR 5/8), 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 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 (2.5Y 5/2), moist, iron depletions with clear boundaries in matrix; 2 percent by volume nonflat subrounded very strongly coherent cemented 2-?-5 millimeter mixed fragments; noneffervescent, by hcl, 1n; clear smooth boundary.; observed in pit, small
    Btk1—51 to 85 centimeters (20.1 to 33.5 inches); 70 percent yellowish brown (10YR 5/6) broken face and 30 percent light olive brown (2.5Y 5/4) broken face clay loam; moderate fine subangular blocky, and moderate medium subangular blocky, and weak medium prismatic structure; firm; 1.0 very coarse roots between peds and 2.0 medium roots between peds and 2.0 fine roots between peds and 1.0 coarse roots between peds; 1.0 very fine low-continuity dendritic tubular pores; 35 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 grayish brown (2.5Y 5/2), 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; 3 percent fine prominent spherical extremely weakly coherent cemented white (10YR 8/1), moist, carbonate masses with diffuse boundaries throughout; 1 percent by volume nonflat subrounded very strongly coherent cemented 5-?-20 millimeter mixed fragments and 2 percent by volume nonflat subrounded very strongly coherent cemented 2-?-5 millimeter mixed fragments; strong effervescence, by hcl, 1n; gradual smooth boundary.; observed in pit, small
    Btk2—85 to 116 centimeters (33.5 to 45.7 inches); 70 percent yellowish brown (10YR 5/6) broken face and 30 percent light olive brown (2.5Y 5/4) broken face clay loam; moderate fine subangular blocky, and moderate medium subangular blocky, and moderate fine prismatic structure; firm; 1.0 very coarse roots between peds and 2.0 medium roots between peds and 1.0 coarse roots between peds; 2.0 very fine low-continuity dendritic tubular pores; 35 percent distinct light olive brown (2.5Y 5/4), moist, clay films on all faces of peds; 1 percent medium faint irregular noncoherent cemented yellowish brown (10YR 5/8), moist, iron depletions with clear boundaries in matrix and 1 percent medium faint irregular noncoherent cemented gray (2.5Y 5/1), 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; 5 percent fine prominent spherical weakly coherent cemented white (10YR 8/1), moist, carbonate nodules with diffuse boundaries throughout; 2 percent by volume nonflat subrounded very strongly coherent cemented 2-?-5 millimeter mixed fragments; strong effervescence, by hcl, 1n; abrupt smooth boundary.; observed in pit, small
    2Btk3—116 to 147 centimeters (45.7 to 57.9 inches); light olive brown (2.5Y 5/4) broken face clay loam; moderate fine subangular blocky, and moderate medium subangular blocky, and moderate medium prismatic structure; very firm; 1.0 fine roots between peds; 1.0 very fine low-continuity dendritic tubular pores; 12 percent distinct light olive brown (2.5Y 5/3), 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 gray (2.5Y 5/1), 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; 6 percent fine prominent spherical weakly coherent cemented white (10YR 8/1), moist, carbonate nodules with diffuse boundaries throughout; 4 percent by volume nonflat subrounded very strongly coherent cemented 2-?-5 millimeter mixed fragments; strong effervescence, by hcl, 1n; clear smooth boundary.; observed in pit, small
    2Btk4—147 to 203 centimeters (57.9 to 79.9 inches); light olive brown (2.5Y 5/4) broken face clay loam; moderate fine subangular blocky, and moderate fine angular blocky, and moderate medium angular blocky, and moderate medium subangular blocky, and moderate medium prismatic structure; very firm; 1.0 fine roots between peds; 1.0 very fine low-continuity dendritic tubular pores; 35 percent distinct grayish brown (2.5Y 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 gray (2.5Y 5/1), 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; 8 percent fine prominent spherical weakly coherent cemented white (10YR 8/1), moist, carbonate nodules with diffuse boundaries throughout; 1 percent by volume nonflat subrounded very strongly coherent cemented 5-?-20 millimeter mixed fragments and 3 percent by volume nonflat subrounded very strongly coherent cemented 2-?-5 millimeter mixed fragments; strong effervescence, by hcl, 1n.; observed in pit, small