IDENTIFIERS

  • Current Taxon Name (Soil Name): Aslinger
  • OSD
  • Series Extent
  • User Site ID: 2008MO225052M
  • User Pedon ID: 2008MO225052
  • Lab Information:
  • Certified Lab Pedon Description - no
  • Lab Source ID - MCL
  • Lab Pedon # - M0822552
  • 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: 37.2266944
  • Std. Longitude: -93.0036944
  • Datum: WGS84
  • Country: US—United States
  • State: Missouri
  • County: MO225—Webster
  • MLRA: 116B—Springfield Plain
  • Non-MLRA Soil Survey Area: MO225—Webster County, Missouri
  • 7.5 Minute USGS Quad: 37093-B1—Oak Grove Heights, Missouri
  • PEDON

  • Describers Name: John Preston, Scott Paine, Katie Philbrick, Lee Perkins
  • Current Taxonomic Class: Fine-loamy, mixed, active, mesic Fragiaquic Paleudults
  • Current Taxon Kind: series
  • Pedon Type: classifies to current taxon name, full description
  • Pedon Purpose: laboratory sampling site
  • Pedon Record Orgin: Missouri Pedon
  • Pedon #: 52
  • Correlated Information:
  • Soil Name - Aslinger
  • PSC - 8 to 58 cm.
  • Classificaton Date - 1/31/2012
  • Soil Taxonomic Edition - tenth edition
  • Moisture Class - udic
  • Moisture Subclass - aquic
  • Sampled As Information:
  • Soil Name - Alsup
  • 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: fine-loamy loess derived from igneous, metamorphic and sedimentary rock over fine-loamy slope alluvium derived from sedimentary rock over clayey slope alluvium derived from sedimentary rock
  • Landscape: upland
  • Landform: hillslope
  • Hill Slope Profile: backslope
  • Slope Complexity: simple
  • Slope Shape Across: linear
  • Slope Shape Down: linear
  • Runoff: high
  • Drainage Class: somewhat poorly
  • Flooding: none flooding
  • Ponding: none ponding
  • Geology: Compton Limestone formation.
  • Surface Fragments:
  • Benchmark Soil?: no
  • VEGETATION

    SITE OBSERVATION

  • Observation Date: 12/3/2008 (actual site observation date)
  • Air Photo ID: 37093b1
  • 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
  • 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

    fragic soil properties

    lithologic discontinuity

    0—8

    8—152

    41—102

    41—152

    41—102

    102—152

    —8—

    —144—

    —61—

    —111—

    —61—

    —50—

    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

    5

    433.7

    292

    Ap—0 to 8 centimeters (0.0 to 3.1 inches); dark brown (10YR 3/3) exterior silt loam; 8 percent sand; 80 percent silt; 12 percent clay; moderate granular structure; friable; 5 percent by volume nonflat subangular indurated 2-?-75 millimeter chert fragments; clear smooth boundary.; observed in push tube
    Bt1—8 to 23 centimeters (3.1 to 9.1 inches); dark yellowish brown (10YR 4/4) broken face silt loam; 5 percent sand; 79 percent silt; 16 percent clay; moderate subangular blocky structure; firm; 1 percent medium faint irregular noncoherent cemented iron depletions with clear boundaries in matrix; 14 percent by volume nonflat subangular indurated 2-?-75 millimeter chert fragments; clear smooth boundary.; observed in push tube
    Bt2—23 to 41 centimeters (9.1 to 16.1 inches); strong brown (7.5YR 4/6) broken face silty clay loam; 6 percent sand; 66 percent silt; 28 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 2-?-75 millimeter chert fragments; clear wavy boundary.; observed in push tube
    2Btx1—41 to 74 centimeters (16.1 to 29.1 inches); strong brown (7.5YR 4/6) broken face gravelly silt loam; 9 percent sand; 64 percent silt; 27 percent clay; weak platy, and moderate subangular blocky structure; firm; 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 and 1 percent medium faint irregular noncoherent cemented pinkish gray (7.5YR 6/2), moist, iron depletions with clear boundaries in matrix; 20 percent by volume nonflat subangular indurated 2-?-75 millimeter chert fragments; clear wavy boundary.; observed in push tube
    2Btx2—74 to 102 centimeters (29.1 to 40.2 inches); red (2.5YR 4/6) broken face very gravelly silty clay loam; 15 percent sand; 55 percent silt; 30 percent clay; moderate subangular blocky, and weak prismatic structure; firm; 1 percent medium faint irregular noncoherent cemented gray (5YR 5/1), moist, iron depletions with clear boundaries in matrix and 1 percent medium faint irregular noncoherent cemented iron depletions with clear boundaries in matrix; 40 percent by volume nonflat subangular indurated 2-?-75 millimeter chert fragments; clear wavy boundary.; observed in push tube
    3Bt—102 to 152 centimeters (40.2 to 59.8 inches); dark red (2.5YR 3/6) broken face very gravelly clay loam; 24 percent sand; 39 percent silt; 37 percent clay; moderate subangular blocky structure; firm; 1 percent medium faint irregular noncoherent cemented iron depletions with clear boundaries in matrix and 1 percent medium faint irregular noncoherent cemented gray (5YR 5/1), moist, iron depletions with clear boundaries in matrix; 40 percent by volume nonflat subangular indurated 2-?-75 millimeter chert fragments.; observed in push tube