IDENTIFIERS

  • Current Taxon Name (Soil Name): Taterhill
  • OSD
  • Series Extent
  • User Site ID: 1994MO153065M
  • User Pedon ID: 1994MO153065
  • Lab Information:
  • Certified Lab Pedon Description - no
  • Lab Source ID - MCL
  • Lab Pedon # - M9415343
  • Print Date: 11/11/2024

    • 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: 36.6182778
  • Std. Longitude: -92.5144722
  • Datum: WGS84
  • Country: US—United States
  • State: Missouri
  • County: MO153—Ozark
  • MLRA: 116A—Ozark Highland
  • Non-MLRA Soil Survey Area: MO153—Ozark County, Missouri
  • 7.5 Minute USGS Quad: 36092-E5—Isabella, Missouri

    • PEDON

  • Describers Name: D F Festervand, G Campbell, T Dohman, K Schrable
  • Current Taxonomic Class: Fine-loamy, mixed, semiactive, mesic Oxyaquic Paleudults
  • Current Taxon Kind: taxon above family
  • Pedon Type: taxadjunct to the series
  • Pedon Purpose: laboratory sampling site
  • Pedon Record Orgin: Missouri Pedon
  • Pedon #: 65
  • Correlated Information:
  • Soil Name - Taterhill
  • PSC - 10 to 60 cm.
  • Classificaton Date - 2/1/2012
  • Soil Taxonomic Edition - tenth edition
  • Moisture Class - udic
  • Moisture Subclass - oxyaquic
  • Sampled As Information:
  • Soil Name - Britwater
  • Taxon Kind - series
  • Classificaton Date - 7/15/1994
  • Dynamic Soil Properties:
  • Erosion Class - 1
  • Pedoderm Loose Cover Indicator - no
  • Hydric: no


    • SITE

  • Parent Material: loamy slope alluvium derived from igneous, metamorphic and sedimentary rock over loamy slope alluvium derived from sedimentary rock
  • Landscape: river valley
  • Landform: strath terrace
  • Geomorphic Component Terraces: tread
  • Slope Complexity: simple
  • Slope Shape Across: linear
  • Slope Shape Down: linear
  • Runoff: medium
  • Drainage Class: moderately well
  • Flooding: none flooding
  • Ponding: none ponding
  • Geology: Jefferson City Dolomite formation.
  • Surface Fragments:
  • Benchmark Soil?: no

    • VEGETATION

    SITE OBSERVATION

  • Observation Date: 7/15/1994 (actual site observation date)
  • Air Photo ID: 36092e5
  • 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—10

    10—203

    46—203

    —10—

    —193—

    —157—
    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

    —

    —

    269.4

    —

    120

    —

    —

    —

    —

    —

    —

    —

    —

    —

    —

    —

    —

    —

    —
    Ap—0 to 10 centimeters (0.0 to 3.9 inches); brown (10YR 4/3) silt loam; 52 percent silt; 12 percent clay; moderate medium granular structure; friable; 10.0 fine roots; 5 percent by volume nonflat indurated 2-?-75 millimeter limestone, cherty fragments; clear smooth boundary. Lab sample # MU050995; observed in pit, small
    Bt1—10 to 23 centimeters (3.9 to 9.1 inches); 75 percent strong brown (7.5YR 4/6) and 25 percent brown (10YR 4/3) silt loam; 53 percent silt; 14 percent clay; weak fine subangular blocky structure; friable; 3.0 fine roots; 5 percent by volume nonflat indurated 2-?-75 millimeter limestone, cherty fragments; clear smooth boundary.; observed in pit, small
    Bt2—23 to 46 centimeters (9.1 to 18.1 inches); strong brown (7.5YR 4/6) gravelly loam; 50 percent silt; 22 percent clay; moderate medium subangular blocky structure; friable; 3.0 fine roots; 30 percent distinct clay films on all faces of peds; 1 percent medium faint irregular noncoherent cemented iron depletions with clear boundaries in matrix; 20 percent by volume nonflat indurated 2-?-75 millimeter limestone, cherty fragments; clear smooth boundary.; observed in pit, small
    2Bt3—46 to 79 centimeters (18.1 to 31.1 inches); yellowish red (5YR 5/6) gravelly loam; 44 percent silt; 26 percent clay; moderate medium subangular blocky structure; firm; 3.0 fine roots; 30 percent prominent clay films on all faces of peds; 1 percent medium faint irregular noncoherent cemented iron depletions with clear boundaries in matrix; 15 percent by volume nonflat indurated 2-?-75 millimeter limestone, cherty fragments; clear smooth boundary.; observed in pit, small
    2Bt4—79 to 104 centimeters (31.1 to 40.9 inches); red (2.5YR 4/6) gravelly loam; 43 percent silt; 27 percent clay; moderate medium subangular blocky structure; firm; 3.0 fine roots; 30 percent prominent clay films on all faces of peds and 30 percent light brownish gray (10YR 6/2), moist, silt coats; 1 percent medium faint irregular noncoherent cemented iron depletions with clear boundaries in matrix; 15 percent by volume nonflat indurated 2-?-75 millimeter limestone, cherty fragments; gradual smooth boundary.; observed in pit, small
    2Bt5—104 to 168 centimeters (40.9 to 66.1 inches); red (2.5YR 4/6) gravelly clay loam; 44 percent silt; 30 percent clay; moderate medium subangular blocky structure; firm; 0.5 fine roots; 30 percent light brownish gray (10YR 6/2), moist, silt coats and 65 percent prominent clay films on all faces of peds; 15 percent by volume nonflat indurated 2-?-75 millimeter limestone, cherty fragments; gradual wavy boundary.; observed in pit, small
    2Bt6—168 to 203 centimeters (66.1 to 79.9 inches); red (2.5YR 4/6) gravelly loam; 44 percent silt; 26 percent clay; moderate medium subangular blocky structure; firm; 30 percent light brownish gray (10YR 6/2), moist, silt coats and 65 percent prominent clay films on all faces of peds; 1 percent medium faint irregular noncoherent cemented iron depletions with clear boundaries in matrix; 20 percent by volume nonflat angular indurated 2-?-75 millimeter limestone, cherty fragments.; observed in pit, small