IDENTIFIERS

  • Current Taxon Name (Soil Name): Gressy
  • OSD
  • Series Extent
  • User Site ID: 1983MO059001M
  • User Pedon ID: 1983MO059001
  • Lab Information:
  • Certified Lab Pedon Description - no
  • Lab Source ID - MCL
  • Lab Pedon # - M9305906
  • Print Date: 11/24/2024

    • 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: 37.8759444
  • Std. Longitude: -93.0519444
  • Datum: WGS84
  • Township: T36N
  • Range: R19W
  • Section: 8
  • PLSS Details: 1136 feet E and 1195 feet N of the SW corner
  • Country: US—United States
  • State: Missouri
  • County: MO059—Dallas
  • MLRA: 116A—Ozark Highland
  • Non-MLRA Soil Survey Area: MO059—Dallas County, Missouri
  • 7.5 Minute USGS Quad: 37093-H1—Branch, Missouri

    • PEDON

  • Describers Name: Lee Perkins
  • Current Taxonomic Class: Fine-loamy, mixed, semiactive, mesic Typic Paleudalfs
  • Current Taxon Kind: series
  • Pedon Type: not classified to current taxon name
  • Pedon Purpose: laboratory sampling site
  • Pedon Record Orgin: Missouri Pedon
  • Pedon #: 1
  • Correlated Information:
  • Soil Name - Gressy
  • PSC - 33 to 83 cm.
  • Classificaton Date - 2/1/2012
  • Soil Taxonomic Edition - tenth edition
  • Moisture Class - udic
  • Moisture Subclass - typic
  • Sampled As Information:
  • Soil Name - Claiborne
  • Taxon Kind - series
  • PSC - 33 to 83 cm.
  • Classificaton Date - 8/12/1983
  • Dynamic Soil Properties:
  • Erosion Class - 1
  • Pedoderm Loose Cover Indicator - no
  • Hydric: no


    • SITE

  • Parent Material: silty slope alluvium derived from igneous, metamorphic and sedimentary rock
  • Landscape: hills
  • Landform: hillslope
  • Geomorphic Component Hills: side slope
  • Hill Slope Profile: backslope
  • 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: Jefferson City Dolomite formation.
  • Surface Fragments:
  • Benchmark Soil?: no

    • VEGETATION

    SITE OBSERVATION

  • Observation Date: 8/12/1983 (actual site observation date)
  • Air Photo ID: 37093h1
  • 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

    0—33

    33—163

    —33—

    —130—
    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

    6

    —

    —

    285.9

    —

    349

    —

    —

    —

    —

    —

    —

    —

    —

    —

    —

    —

    —

    —

    —
    Ap—0 to 15 centimeters (0.0 to 5.9 inches); brown (10YR 4/3), pale brown (10YR 6/3), dry; silt loam; 60 percent silt; 16 percent clay; weak very fine granular structure; friable; 3.0 fine roots; 5 percent by volume nonflat indurated 2-?-75 millimeter unspecified fragments; abrupt smooth boundary. Lab sample # MU001461; observed in pit, small
    BA—15 to 33 centimeters (5.9 to 13.0 inches); yellowish red (5YR 5/6) silt loam; 56 percent silt; 24 percent clay; weak very fine subangular blocky structure; friable; 3.0 fine roots; 6 percent by volume nonflat indurated 2-?-75 millimeter unspecified fragments; clear smooth boundary. Lab sample # MU001462; observed in pit, small
    Bt1—33 to 46 centimeters (13.0 to 18.1 inches); red (2.5YR 4/6) clay loam; 49 percent silt; 31 percent clay; moderate fine subangular blocky structure; firm; 0.5 fine roots; 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; 10 percent by volume nonflat indurated 2-?-75 millimeter unspecified fragments; clear smooth boundary. Lab sample # MU001463; observed in pit, small
    Bt2—46 to 130 centimeters (18.1 to 51.2 inches); red (2.5YR 4/6) silty clay loam; 49 percent silt; 33 percent clay; moderate fine subangular blocky structure; firm; 0.5 fine roots; 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; 12 percent by volume nonflat indurated 2-?-75 millimeter unspecified fragments; gradual smooth boundary. Lab sample # MU001464; observed in pit, small
    Bt3—130 to 163 centimeters (51.2 to 64.2 inches); red (2.5YR 4/6) clay loam; 42 percent silt; 35 percent clay; weak fine 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; 10 percent by volume nonflat indurated 2-?-75 millimeter unspecified fragments. Lab sample # MU001465; observed in pit, small