IDENTIFIERS

  • Current Taxon Name (Soil Name): Rueter
  • OSD
  • Series Extent
  • User Site ID: 2008MO209057M
  • User Pedon ID: 2008MO209057
  • Lab Information:
  • Certified Lab Pedon Description - no
  • Lab Source ID - MCL
  • Lab Pedon # - M0820957
  • Print Date: 11/21/2024
  • 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: 36.8830000
  • Std. Longitude: -93.4141111
  • Datum: WGS84
  • Country: US—United States
  • State: Missouri
  • County: MO209—Stone
  • MLRA: 116A—Ozark Highland
  • Non-MLRA Soil Survey Area: MO209—Stone County, Missouri
  • 7.5 Minute USGS Quad: 36093-H4—Hurley, Missouri
  • PEDON

  • Describers Name: John Preston, Scott Paine, Katie Philbrick, Lee Perkins
  • Current Taxonomic Class: Loamy-skeletal, siliceous, active, mesic Mollic Paleudalfs
  • Current Taxon Kind: taxon above family
  • Pedon Type: taxadjunct to the series
  • Pedon Purpose: laboratory sampling site
  • Pedon Record Orgin: Missouri Pedon
  • Pedon #: 57
  • Correlated Information:
  • Soil Name - Rueter
  • PSC - 8 to 58 cm.
  • Classificaton Date - 2/1/2012
  • Soil Taxonomic Edition - tenth edition
  • Moisture Class - udic
  • Moisture Subclass - typic
  • Sampled As Information:
  • Soil Name - Clarksville
  • Taxonomic Class - Loamy-skeletal, siliceous, semiactive, mesic Typic Paleudults
  • Taxon Kind - series
  • PSC - 8 to 58 cm.
  • Classificaton Date - 12/3/2008
  • Dynamic Soil Properties:
  • Erosion Class - 1
  • Pedoderm Loose Cover Indicator - no
  • Hydric: no


  • SITE

  • Parent Material: gravelly slope alluvium derived from sedimentary rock over Burlington Limestone clayey residuum weathered from cherty limestone
  • Landscape: upland
  • Landform: knob
  • Geomorphic Component Hills: crest
  • Hill Slope Profile: summit
  • Slope Position: upper third
  • Slope Complexity: simple
  • Slope Shape Across: linear
  • Slope Shape Down: linear
  • Runoff: medium
  • Drainage Class: well
  • Flooding: none flooding
  • Ponding: none ponding
  • Geology: Burlington Limestone formation.
  • Surface Fragments:
  • Benchmark Soil?: no
  • VEGETATION

    SITE OBSERVATION

  • Observation Date: 12/3/2008 (actual site observation date)
  • Air Photo ID: 36093h4
  • Surface Water Kind: none observed
  • Surface Cover Properties:
  • Site Obs. Cover Kind 1 - grass/herbaceous cover
  • Site Obs. Cover Kind 2 - pastureland, tame
  • 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

    0—8

    8—152

    69—152

    —8—

    —144—

    —83—

    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

    3

    371.6

    220

    Ap—0 to 8 centimeters (0.0 to 3.1 inches); dark brown (10YR 3/3) exterior gravelly silt loam; 11 percent sand; 77 percent silt; 12 percent clay; moderate granular structure; very friable; 25 percent by volume nonflat subangular indurated 2-?-75 millimeter chert fragments; abrupt smooth boundary. Lab sample # MU001544; observed in push tube
    Bt1—8 to 19 centimeters (3.1 to 7.5 inches); dark brown (10YR 3/3) broken face very gravelly silt loam; 9 percent sand; 75 percent silt; 16 percent clay; moderate subangular blocky structure; friable; 45 percent by volume nonflat subangular indurated 2-?-75 millimeter chert fragments; clear wavy boundary.; observed in push tube
    Bt2—19 to 44 centimeters (7.5 to 17.3 inches); brown (7.5YR 4/4) broken face very gravelly silt loam; 8 percent sand; 70 percent silt; 22 percent clay; moderate subangular blocky structure; friable; 1 percent medium faint irregular noncoherent cemented iron depletions with clear boundaries in matrix; 50 percent by volume nonflat subangular indurated 2-?-75 millimeter chert fragments; clear wavy boundary.; observed in push tube
    Bt3—44 to 69 centimeters (17.3 to 27.2 inches); brown (7.5YR 4/4) broken face extremely gravelly silty clay loam; 6 percent sand; 67 percent silt; 27 percent clay; moderate subangular blocky structure; firm; 1 percent medium faint irregular noncoherent cemented iron depletions with clear boundaries in matrix; 10 percent by volume nonflat subangular indurated 75-?-250 millimeter chert fragments and 50 percent by volume nonflat subangular indurated 2-?-75 millimeter chert fragments; clear wavy boundary.; observed in push tube
    2Bt4—69 to 93 centimeters (27.2 to 36.6 inches); red (2.5YR 4/6) broken face extremely gravelly clay; 6 percent sand; 52 percent silt; 42 percent clay; moderate subangular blocky structure; firm; 1 percent medium faint irregular noncoherent cemented iron depletions with clear boundaries in matrix; 20 percent by volume nonflat subangular indurated 75-?-250 millimeter chert fragments and 50 percent by volume nonflat subangular indurated 2-?-75 millimeter chert fragments; clear wavy boundary.; observed in push tube
    2Bt5—93 to 152 centimeters (36.6 to 59.8 inches); red (10R 4/6) broken face extremely gravelly clay; 12 percent sand; 40 percent silt; 48 percent clay; moderate subangular blocky structure; firm; 1 percent medium faint irregular noncoherent cemented iron depletions with clear boundaries in matrix; 20 percent by volume nonflat subangular indurated 75-?-250 millimeter chert fragments and 50 percent by volume nonflat subangular indurated 2-?-75 millimeter chert fragments.; observed in push tube