IDENTIFIERS

  • Current Taxon Name (Soil Name): Winnipeg
  • OSD
  • Series Extent
  • User Site ID: 1994MO225003M
  • User Pedon ID: 1994MO225003
  • Lab Information:
  • Certified Lab Pedon Description - no
  • Lab Source ID - MCL
  • Lab Pedon # - M9422503
  • Print Date: 5/20/2024
  • 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: 37.4738889
  • Std. Longitude: -92.9663889
  • Datum: WGS84
  • Country: US—United States
  • State: Missouri
  • County: MO225—Webster
  • MLRA: 116A—Ozark Highland
  • Non-MLRA Soil Survey Area: MO225—Webster County, Missouri
  • 7.5 Minute USGS Quad: 37092-D8—Beach, Missouri
  • PEDON

  • Describers Name: Lee Perkins
  • Current Taxonomic Class: Fine-silty, mixed, semiactive, mesic Typic Paleudalfs
  • Current Taxon Kind: series
  • Pedon Type: classifies to current taxon name, full description
  • Pedon Purpose: laboratory sampling site
  • Pedon Record Orgin: Missouri Pedon
  • Pedon #: 3
  • Correlated Information:
  • Soil Name - Winnipeg
  • PSC - 26 to 76 cm.
  • Classificaton Date - 2/1/2012
  • Soil Taxonomic Edition - tenth edition
  • Moisture Class - udic
  • Moisture Subclass - typic
  • Sampled As Information:
  • Soil Name - Peridge
  • Taxon Kind - series
  • PSC - 26 to 76 cm.
  • Classificaton Date - 8/30/1994
  • Dynamic Soil Properties:
  • Erosion Class - 1
  • Pedoderm Loose Cover Indicator - no
  • Hydric: no


  • SITE

  • Parent Material: fine-silty loess derived from igneous, metamorphic and sedimentary rock over fine-silty slope alluvium derived from sedimentary rock over clayey slope alluvium derived from sedimentary rock over clayey slope alluvium derived from sedimentary rock
  • Landscape: hills
  • Landform: structural bench
  • Geomorphic Component Terraces: tread
  • Slope Complexity: simple
  • Slope Shape Across: linear
  • Slope Shape Down: linear
  • Runoff: low
  • Drainage Class: well
  • Flooding: none flooding
  • Ponding: none ponding
  • Geology: Jefferson City Dolomite formation.
  • Surface Fragments:
  • Benchmark Soil?: no
  • VEGETATION

    SITE OBSERVATION

  • Observation Date: 8/30/1994 (actual site observation date)
  • Air Photo ID: 37092d8
  • Surface Water Kind: none observed
  • Surface Cover Properties:
  • Site Obs. Cover Kind 1 - grass/herbaceous cover
  • Site Obs. Cover Kind 2 - hayland
  • Pedoderm Loose Cover Indicator - no
  • Drained? - no
  • Bedded Soil? - no
  • Forest Plantation? - no
  • Site Erosion Accelerated: water erosion sheet
  • Pedon Diagnostic Features
    Feature Kind Feature Depth L-H Feature Thickness L-RV-H
    cm

    ochric epipedon

    argillic horizon

    lithologic discontinuity

    lithologic discontinuity

    lithologic discontinuity

    0—26

    26—195

    40—87

    87—133

    133—195

    —26—

    —169—

    —47—

    —46—

    —62—

    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

    4

    358.7

    45

    Ap—0 to 12 centimeters (0.0 to 4.7 inches); brown (10YR 4/3) silt loam; 14 percent sand; 72 percent silt; 14 percent clay; moderate medium platy structure; friable; 10.0 fine roots throughout; 1 percent medium faint irregular noncoherent cemented iron depletions with clear boundaries in matrix; fragments; abrupt smooth boundary. Lab sample # MU006131; observed in pit, small
    A2—12 to 26 centimeters (4.7 to 10.2 inches); brown (10YR 4/3) silt loam; 13 percent sand; 74 percent silt; 13 percent clay; weak fine granular, and weak medium platy structure; friable; 3.0 fine roots between peds; 1 percent medium faint irregular noncoherent cemented iron depletions with clear boundaries in matrix; fragments; clear smooth boundary. Lab sample # MU006132; observed in pit, small
    Bt1—26 to 40 centimeters (10.2 to 15.7 inches); 50 percent yellowish brown (10YR 5/4) and 50 percent brown (10YR 4/3) silt loam; 10 percent sand; 69 percent silt; 21 percent clay; weak fine subangular blocky structure; friable; 3.0 fine roots between peds; 10 percent faint clay films on all faces of peds and 10 percent faint clay films on surfaces along pores; 1 percent medium faint irregular noncoherent cemented iron depletions with clear boundaries in matrix; 2 percent by volume nonflat subrounded indurated 2-?-75 millimeter unspecified fragments; clear smooth boundary. Lab sample # MU006133; observed in pit, small
    2Bt2—40 to 66 centimeters (15.7 to 26.0 inches); 50 percent brown (7.5YR 5/4) and 50 percent brown (7.5YR 4/4) silty clay loam; 10 percent sand; 63 percent silt; 27 percent clay; weak medium subangular blocky structure; firm; 3.0 fine roots between peds; 25 percent distinct clay films on all faces of peds and 25 percent distinct clay films on surfaces along pores; 1 percent medium faint irregular noncoherent cemented iron depletions with clear boundaries in matrix; 4 percent by volume nonflat subrounded indurated 2-?-75 millimeter unspecified fragments; clear smooth boundary. Lab sample # MU006134; observed in pit, small
    2Bt3—66 to 87 centimeters (26.0 to 34.3 inches); brown (7.5YR 4/4) silty clay loam; 13 percent sand; 55 percent silt; 32 percent clay; weak fine subangular blocky structure; firm; 0.5 fine roots between peds; 40 percent distinct clay films on all faces of peds and 40 percent distinct clay films on surfaces along pores; 1 percent medium faint irregular noncoherent cemented iron depletions with clear boundaries in matrix and 1 percent medium faint irregular noncoherent cemented iron depletions with clear boundaries in matrix; 2 percent by volume nonflat subangular indurated 2-?-75 millimeter unspecified fragments; clear wavy boundary. Lab sample # MU006135; observed in pit, small
    3Bt4—87 to 105 centimeters (34.3 to 41.3 inches); dark red (2.5YR 3/6) silty clay loam; 14 percent sand; 51 percent silt; 35 percent clay; moderate fine subangular blocky structure; firm; 0.5 fine roots between peds; 55 percent prominent clay films on all faces of peds and 55 percent prominent clay films on surfaces along pores; 1 percent medium faint irregular noncoherent cemented iron depletions with clear boundaries in matrix and 1 percent medium faint irregular noncoherent cemented iron depletions with clear boundaries in matrix; 2 percent by volume nonflat subangular indurated 2-?-75 millimeter unspecified fragments; gradual smooth boundary. Lab sample # MU006136; observed in pit, small
    3Bt5—105 to 133 centimeters (41.3 to 52.4 inches); dark reddish brown (2.5YR 3/4) silty clay loam; 14 percent sand; 51 percent silt; 35 percent clay; weak fine subangular blocky, and weak coarse subangular blocky structure; firm; 0.5 fine roots between peds; 20 percent prominent light yellowish brown (10YR 6/4), moist, skeletans on vertical faces of peds and 40 percent prominent clay films on all faces of peds and 40 percent prominent clay films on surfaces along pores; 2 percent by volume nonflat subangular indurated 2-?-75 millimeter unspecified fragments; abrupt smooth boundary. Lab sample # MU006137; observed in pit, small
    4Bt6—133 to 178 centimeters (52.4 to 70.1 inches); dark red (2.5YR 3/6) extremely gravelly clay loam; 22 percent sand; 40 percent silt; 38 percent clay; moderate fine subangular blocky structure; firm; 10 percent prominent light yellowish brown (10YR 6/4), moist, skeletans on rock fragments and 55 percent prominent clay films on all faces of peds; 20 percent by volume nonflat subangular indurated 75-?-250 millimeter unspecified fragments and 30 percent by volume nonflat subangular indurated 2-?-75 millimeter unspecified fragments and 40 percent by volume nonflat angular indurated 2-?-75 millimeter unspecified fragments; gradual smooth boundary. Lab sample # MU006138; observed in pit, small
    4Bt7—178 to 195 centimeters (70.1 to 76.8 inches); dark red (2.5YR 3/6) very gravelly clay; moderate fine subangular blocky structure; firm; 55 percent prominent clay films on all faces of peds; 25 percent by volume nonflat subangular indurated 75-?-250 millimeter unspecified fragments and 30 percent by volume nonflat angular indurated 2-?-75 millimeter unspecified fragments.; observed in pit, small