IDENTIFIERS

  • Current Taxon Name (Soil Name): Satanta
  • OSD
  • Series Extent
  • User Site ID: 08KS175308
  • User Pedon ID: 08KS175308
  • User Site Association ID: mlra72-DalhartKansas State University Laboratory Pedons
  • Transect:
  • User Transect ID - 7208KS175-5217-1
  • Transect Stop Number - 8
  • Transect Interval - 338.0
  • Lab Information:
  • Certified Lab Pedon Description - no
  • Lab Source ID - KSU
  • Lab Pedon # - 08KS175308
  • NCSS Pedon Lab Data NASIS Record ID - 40887
  • 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: 37.3503304
  • Std. Longitude: -100.9650040
  • Datum: WGS84
  • Township: 31s
  • Range: 34w
  • Section: 13
  • Location Description: 684 meters north and 497 meters west of the southeast corner
  • Map Unit: 5217—Dalhart fine sandy loam, 0 to 1 percent slopes
  • State: Kansas
  • County: KS175—Seward
  • MLRA: 72—Central High Tableland
  • Non-MLRA Soil Survey Area: KS175—Seward County, Kansas
  • 7.5 Minute USGS Quad: 37100-C8—Sublette SW, 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 - 13 to 34 cm.
  • Classificaton Date - 3/19/2008
  • Soil Taxonomic Edition - tenth edition
  • Moisture Class - ustic
  • Dynamic Soil Properties:
  • Pedoderm Loose Cover Indicator - no
  • Hydric: no


  • SITE

  • Parent Material: 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: 3/19/2008 (actual site observation date)
  • Air Photo ID: 2
  • Surface Cover Properties:
  • Site Obs. Cover Kind 1 - crop 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

    0—34

    13—34

    34—230

    —34—

    —21—

    —196—

    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

    892.2

    0

    Ap—0 to 13 centimeters (0.0 to 5.1 inches);, dark brown (10YR 3/3) broken face, moist; fine sandy loam; 14 percent clay; weak coarse granular structure; soft, very friable, nonsticky, nonplastic; moderate permeability; 1.0 very fine roots throughout; fragments; noneffervescent, by hcl, 1n; abrupt smooth boundary. Lab sample # KSUSS4231; 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—13 to 34 centimeters (5.1 to 13.4 inches);, dark brown (10YR 3/3) broken face, moist; sandy clay loam; 26 percent clay; weak fine subangular blocky structure; slightly hard, friable, slightly sticky, moderately plastic; moderate permeability; 1.0 very fine low-continuity dendritic tubular pores; 15 percent distinct clay bridges between sand grains; fragments; noneffervescent, by hcl, 1n; clear smooth boundary. Lab sample # KSUSS4232; 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.; discontinuous - phpvsfiid 401827; discontinuous - phpvsfiid 401827
    Bk1—34 to 57 centimeters (13.4 to 22.4 inches);, brown (7.5YR 4/4) broken face, moist; loam; 22 percent clay; weak medium prismatic structure; soft, very friable, moderately sticky, moderately plastic; moderate permeability; 1.0 very fine low-continuity dendritic tubular pores; 2 percent fine threadlike carbonate masses in matrix and 2 percent medium irregular carbonate masses in matrix; fragments; strong effervescence, by hcl, 1n; abrupt smooth boundary.; observed in push tube
    Bk2—57 to 82 centimeters (22.4 to 32.3 inches);, light brown (7.5YR 6/4) broken face, moist; fine sandy loam; 14 percent clay; weak medium subangular blocky structure; soft, very friable, slightly sticky, slightly plastic; moderate permeability; 3.0 very fine low-continuity tubular pores; 10 percent coarse irregular carbonate masses in matrix and 5 percent fine threadlike carbonate masses in matrix; fragments; violent effervescence, by hcl, 1n; clear smooth boundary.; observed in push tube
    Bk3—82 to 189 centimeters (32.3 to 74.4 inches);, brown (7.5YR 5/4) broken face, moist; fine sandy loam; 12 percent clay; weak medium prismatic structure; soft, very friable, slightly sticky, nonplastic; moderate permeability; 1 percent coarse spherical carbonate nodules in matrix and 1 percent fine irregular carbonate masses in matrix and 2 percent fine threadlike carbonate masses in matrix; fragments; very slight effervescence, by hcl, 1n; diffuse smooth boundary.; observed in push tube
    Bk4—189 to 230 centimeters (74.4 to 90.6 inches);, strong brown (7.5YR 5/6) broken face, moist; sandy clay loam; 22 percent clay; weak coarse prismatic structure; slightly hard, friable, slightly sticky, slightly plastic; moderate permeability; 5 percent fine threadlike carbonate masses in matrix; fragments; slight effervescence, by hcl, 1n.; observed in push tube