IDENTIFIERS

  • Current Taxon Name (Soil Name): Ulysses
  • OSD
  • Series Extent
  • User Site ID: S1989KS081003
  • User Pedon ID: S1989KS081003
  • User Site Association ID: mlra72-benchmark lab pedonsmlra72-Ulysses labOLDmlra72-SDJR comp pedsmlra72-Ulysses lab pedons
  • Lab Information:
  • Certified Lab Pedon Description - no
  • Lab Source ID - SSL
  • Lab Pedon # - 89P0727
  • NCSS Pedon Lab Data NASIS Record ID - 61827
  • 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: 37.4101000
  • Std. Longitude: -101.0341250
  • Datum: WGS84
  • Township: 30S
  • Range: 34W
  • Section: 27
  • PLSS Details: 2500 feet south and 180 feet east of the northwest corner
  • Map Unit: 1856—Ulysses silt loam, 0 to 1 percent slopes
  • State: Kansas
  • County: KS081—Haskell
  • MLRA: 72—Central High Tableland
  • Non-MLRA Soil Survey Area: KS081—Haskell County, Kansas
  • 7.5 Minute USGS Quad: 37101-D1—Ryus, Kansas
  • PEDON

  • Describers Name: J. Fortner, M. Ransom, & R. Schlepp
  • Current Taxonomic Class: Fine-silty, mixed, superactive, mesic Torriorthentic Haplustolls
  • Current Taxon Kind: series
  • Pedon Type: classifies to current taxon name, full description
  • Pedon Purpose: laboratory sampling site
  • Pedon Record Orgin: Converted from SSL-CMS data
  • Pedon #: 3
  • Sampled As Information:
  • Soil Name - Ulysses
  • Taxonomic Class - Fine-silty, mixed, superactive, mesic Torriorthentic Haplustolls
  • Taxon Kind - series
  • PSC - 25 to 100 cm.
  • Classificaton Date - 7/10/2014
  • Classifier - Tom Cochran
  • Soil Taxonomic Edition - eleventh edition
  • Moisture Class - ustic
  • Moisture SUBClass - aridic (torric)
  • Dynamic Soil Properties:
  • Erosion Class - 1
  • Pedoderm Loose Cover Indicator - no
  • Hydric: no
  • QC Status: level 3
  • QA Status: level 3
  • Field Measured Properties: 23 centimeters of Depth to free carbonates and 26 percent of Estimated percent clay in PSCS


  • SITE

  • Landscape: upland
  • Geomorphic Component Hills: side slope
  • Hill Slope Profile: summit
  • Slope Shape Down: linear
  • Runoff: low
  • Drainage Class: well
  • Flooding: none flooding
  • Ponding: none ponding
  • Surface Fragments:
  • Benchmark Soil?: yes
  • VEGETATION

    SITE OBSERVATION

  • Observation Date: 7/1/1989 (actual site observation date)
  • Air Photo ID: 43
  • Surface Cover Properties:
  • Pedoderm Loose Cover Indicator - no
  • Drained? - no
  • Bedded Soil? - no
  • Forest Plantation? - no
  • Site Erosion Accelerated: water erosion
  • Pedon Diagnostic Features
    Feature Kind Feature Depth L-H Feature Thickness L-RV-H
    cm

    mollic epipedon

    secondary carbonates

    free carbonates

    cambic horizon

    lithologic discontinuity

    lithologic discontinuity

    0—23

    23—274

    23—274

    23—69

    150—262

    262—274

    —23—

    —251—

    —251—

    —46—

    —112—

    —12—

    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

    1

    899

    135

    46

    14

    15

    Ap—0 to 10 centimeters (0.0 to 3.9 inches);, dark brown (10YR 3/3) exterior, moist; loam; moderate fine granular structure; slightly hard, very friable, slightly sticky, slightly plastic; common fine and medium roots throughout; fragments; noneffervescent, by hcl, unspecified; clear smooth boundary. Lab sample # 89P04071; observed in pit, small
    Bw—10 to 23 centimeters (3.9 to 9.1 inches); brown (10YR 4/3) exterior, dark brown (10YR 3/3) exterior, moist; loam; weak medium prismatic parts to weak medium subangular blocky structure; hard, friable, slightly sticky, slightly plastic; few fine and medium roots throughout; few fine tubular pores; fragments; noneffervescent, by hcl, unspecified; clear smooth boundary. Lab sample # 89P04072; observed in pit, small
    Bk1—23 to 38 centimeters (9.1 to 15.0 inches); pale brown (10YR 6/3) exterior, yellowish brown (10YR 5/4) exterior, moist; silty clay loam; weak medium prismatic parts to weak fine and medium subangular blocky structure; slightly hard, very friable, slightly sticky, slightly plastic; few medium roots throughout; common fine tubular pores; 11 percent fine cylindrical carbonate threads; fragments; strong effervescence, by hcl, unspecified; clear smooth boundary. Lab sample # 89P04073; observed in pit, small
    Bk2—38 to 71 centimeters (15.0 to 28.0 inches); light yellowish brown (10YR 6/4) exterior, yellowish brown (10YR 5/4) exterior, moist; silty clay loam; weak medium prismatic parts to weak medium subangular blocky structure; slightly hard, very friable, slightly sticky, slightly plastic; common fine roots throughout; common fine tubular pores; 11 percent fine and medium spherical carbonate masses; fragments; strong effervescence, by hcl, unspecified; gradual wavy boundary. Lab sample # 89P04074; observed in pit, small
    Bk3—71 to 117 centimeters (28.0 to 46.1 inches); light yellowish brown (10YR 6/4) exterior, yellowish brown (10YR 5/4) exterior, moist; silty clay loam; weak medium prismatic structure; slightly hard, very friable, slightly sticky, slightly plastic; few fine roots throughout; common fine tubular pores; 11 percent fine cylindrical carbonate threads and 1 percent fine spherical carbonate masses; fragments; strong effervescence, by hcl, unspecified; gradual wavy boundary. Lab sample # 89P04075; observed in pit, small
    Bk4—117 to 150 centimeters (46.1 to 59.1 inches); yellowish brown (10YR 5/4) exterior, dark yellowish brown (10YR 4/4) exterior, moist; silty clay loam; weak medium prismatic structure; slightly hard, very friable, slightly sticky, slightly plastic; few fine roots throughout; common fine tubular pores; 11 percent fine spherical carbonate threads and 1 percent fine and medium spherical carbonate concretions; fragments; strong effervescence, by hcl, unspecified; gradual wavy boundary. Lab sample # 89P04076; observed in pit, small
    2Bk5—150 to 206 centimeters (59.1 to 81.1 inches); brown (7.5YR 4/4) exterior, dark brown (7.5YR 3/4) exterior, moist; silt loam; weak medium prismatic structure; slightly hard, very friable, slightly sticky, slightly plastic; few fine roots throughout; common fine tubular pores; 11 percent fine cylindrical carbonate threads and 1 percent fine and medium spherical carbonate nodules; fragments; strong effervescence, by hcl, unspecified; diffuse smooth boundary. Lab sample # 89P04077; observed in pit, small. This horizon is probably material from the Laverne member of the Ogallala Formation and is likely eolian in nature.
    2Bk6—206 to 262 centimeters (81.1 to 103.1 inches); brown (7.5YR 4/4) exterior, dark brown (7.5YR 3/4) exterior, moist; clay loam; weak medium prismatic structure; slightly hard, very friable, slightly sticky, slightly plastic; few very fine roots throughout; 11 percent fine spherical carbonate nodules and 11 percent fine cylindrical carbonate threads; fragments; strong effervescence, by hcl, unspecified; diffuse smooth boundary. Lab sample # 89P04078; observed in pit, small. This horizon is probably material from the Laverne member of the Ogallala Formation and is likely eolian in nature.
    3Bk7—262 to 274 centimeters (103.1 to 107.9 inches); light brown (7.5YR 6/4) exterior, brown (7.5YR 5/4) exterior, moist; very fine sandy loam; structureless massive; slightly hard, very friable, nonsticky, nonplastic; common fine tubular pores; 1 percent coarse spherical carbonate masses and 11 percent fine cylindrical carbonate threads; fragments; strong effervescence, by hcl, unspecified. Lab sample # 89P04079; observed in pit, small. effervescence is continuous; This horizon is probably material from the Laverne member of the Ogallala Formation and is likely eolian in nature.; The structure of this horizon was described as massive, but experience tells me if a large enough piece was observed it would prove to be very coarse prismatic structure.