IDENTIFIERS

  • Current Taxon Name (Soil Name): Satanta
  • OSD
  • Series Extent
  • User Site ID: 08KS187321
  • User Pedon ID: 08KS187321
  • User Site Association ID: mlra72-DalhartKansas State University Laboratory Pedons
  • Transect:
  • User Transect ID - 7208KS187-5217-3
  • Transect Stop Number - 1
  • Transect Interval - 208.0
  • Lab Information:
  • Certified Lab Pedon Description - no
  • Lab Source ID - KSU
  • Lab Pedon # - 08KS187321
  • NCSS Pedon Lab Data NASIS Record ID - 40892
  • Print Date: 2/16/2025
  • 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: 37.7008743
  • Std. Longitude: -101.9844208
  • Datum: WGS84
  • Township: 27s
  • Range: 43w
  • Section: 14
  • Location Description: 681 meters north and 417 meters west of the southeast corner
  • Map Unit: 5217—Dalhart fine sandy loam, 0 to 1 percent slopes
  • State: Kansas
  • County: KS187—Stanton
  • MLRA: 72—Central High Tableland
  • Non-MLRA Soil Survey Area: KS187—Stanton County, Kansas
  • 7.5 Minute USGS Quad: 37101-F8—Johnson NW, Kansas
  • PEDON

  • Describers Name: Tom Cochran
  • Current Taxonomic Class: Fine-loamy, mixed, superactive, mesic Aridic Argiustolls
  • Current Taxon Kind: family
  • Pedon Type: within range of map unit
  • Pedon Purpose: full pedon description
  • Pedon Record Orgin: NASIS
  • Sampled As Information:
  • Soil Name - Satanta
  • Taxonomic Class - Fine-loamy, mixed, superactive, mesic Aridic Argiustolls
  • PSC - 11 to 26 cm.
  • Classificaton Date - 4/23/2008
  • Soil Taxonomic Edition - tenth edition
  • Moisture Class - ustic
  • Dynamic Soil Properties:
  • Pedoderm Loose Cover Indicator - no
  • Hydric: no


  • SITE

  • Parent Material: eolian deposits over loess over eolian deposits
  • Landscape: plains
  • Landform: interfluve
  • Hill Slope Profile: summit
  • Drainage Class: well
  • Flooding: none flooding
  • Ponding: none ponding
  • Surface Fragments:
  • Benchmark Soil?: no
  • VEGETATION

    SITE OBSERVATION

  • Observation Date: 4/23/2008 (actual site observation date)
  • Air Photo ID: 1
  • Surface Cover Properties:
  • Site Obs. Cover Kind 1 - grass/herbaceous cover
  • Pedoderm Loose Cover Indicator - no
  • Drained? - no
  • Bedded Soil? - no
  • Forest Plantation? - no
  • Pedon Diagnostic Features
    Feature Kind Feature Depth L-H Feature Thickness L-RV-H
    cm

    mollic epipedon

    argillic horizon

    secondary carbonates

    lithologic discontinuity

    lithologic discontinuity

    0—26

    11—26

    26—198

    26—

    104—

    —26—

    —15—

    —172—

    —-

    —-

    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

    0

    1077.2

    0

    A—0 to 11 centimeters (0.0 to 4.3 inches);, dark brown (10YR 3/3) broken face, moist; fine sandy loam; 15 percent clay; weak fine subangular blocky structure; soft, very friable, slightly sticky, nonplastic; moderate permeability; 4.0 very fine roots throughout and 1.0 fine roots throughout; fragments; noneffervescent, by hcl, 1n; clear smooth boundary. Lab sample # KSUSS4237; observed in push tube. This pedon had unmistakeable mollic color to 13 cm. With mixing to 18 cm, I decided this pedon would make mollic criteria.
    Bt—11 to 26 centimeters (4.3 to 10.2 inches);, dark brown (10YR 3/3) broken face, moist; loam; 24 percent clay; weak medium subangular blocky structure; slightly hard, friable, moderately sticky, moderately plastic; moderate permeability; 2.0 very fine roots throughout; 20 percent distinct clay bridges between sand grains; fragments; noneffervescent, by hcl, 1n; clear smooth boundary. Lab sample # KSUSS4238; observed in push tube. discontinuous - phpvsfiid 402317; discontinuous - phpvsfiid 402317
    2Bk1—26 to 104 centimeters (10.2 to 40.9 inches);, brown (10YR 5/3) broken face, moist; silt loam; 20 percent clay; moderate medium prismatic structure; slightly hard, friable, moderately sticky, very plastic; moderate permeability; 1.0 very fine roots throughout and 1.0 fine roots in cracks; 1.0 very fine low-continuity tubular and 1.0 fine low-continuity tubular pores; 3 percent fine irregular carbonate masses in matrix; fragments; strong effervescence, by hcl, 1n; abrupt smooth boundary.; observed in push tube
    3Bk2—104 to 145 centimeters (40.9 to 57.1 inches);, strong brown (7.5YR 5/6) broken face, moist; sandy clay loam; 22 percent clay; weak medium prismatic structure; slightly hard, friable, moderately sticky, very plastic; moderate permeability; 1.0 very fine roots throughout; 1.0 very fine low-continuity tubular and 1.0 fine low-continuity tubular pores; 1 percent fine irregular carbonate masses in matrix; fragments; slight effervescence, by hcl, 1n; gradual smooth boundary.; observed in push tube
    3Bk3—145 to 198 centimeters (57.1 to 78.0 inches);, strong brown (7.5YR 5/6) broken face, moist; sandy loam; 18 percent clay; weak coarse subangular blocky structure; soft, very friable, slightly sticky, slightly plastic; moderate permeability; 1.0 very fine low-continuity tubular pores; 2 percent fine irregular carbonate masses in matrix; fragments; strong effervescence, by hcl, 1n; abrupt smooth boundary.; observed in push tube
    3C—198 to 230 centimeters (78.0 to 90.6 inches);, strong brown (7.5YR 5/6) broken face, moist; loamy sand; 7 percent clay; weak fine subangular blocky structure; loose, loose, nonsticky, nonplastic; moderately rapid permeability; fragments; very slight effervescence, by hcl, 1n.; observed in push tube