IDENTIFIERS

  • Current Taxon Name (Soil Name): Manter
  • OSD
  • Series Extent
  • User Site ID: S2006KS171104
  • User Pedon ID: S2006KS171104
  • Lab Information:
  • Certified Lab Pedon Description - yes
  • Lab Pedon # - 06N0852
  • NCSS Pedon Lab Data NASIS Record ID - 18416
  • Print Date: 11/21/2024
  • 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: 38.3838611
  • Std. Longitude: -100.7761678
  • Datum: WGS84
  • Township: 19s
  • Range: 31w
  • Section: 20
  • PLSS Details: 126 meters east and 292 meters north of the southwest corner
  • Map Unit: 1670—Manter fine sandy loam, 3 to 5 percent slopes
  • State: Kansas
  • County: KS171—Scott
  • MLRA: 72—Central High Tableland
  • Non-MLRA Soil Survey Area: KS171—Scott County, Kansas
  • 7.5 Minute USGS Quad: 38100-D7—Tractor, Kansas
  • PEDON

  • Describers Name: John Warner, Steve Graber, & Tom Cochran
  • Current Taxonomic Class: Fine-loamy, mixed, superactive, mesic Aridic Haplustalfs
  • Current Taxon Kind: taxadjunct
  • Pedon Type: taxadjunct to the series
  • Pedon Purpose: laboratory sampling site
  • Pedon Record Orgin: NASIS
  • Sampled As Information:
  • Soil Name - Manter
  • Taxonomic Class - Fine-loamy, mixed, superactive, mesic Aridic Haplustalfs
  • Taxon Kind - taxadjunct
  • PSC - 9 to 30 cm.
  • Classificaton Date - 11/14/2016
  • Classifier - Tom Cochran
  • Soil Taxonomic Edition - twelfth edition
  • Moisture Class - ustic
  • Moisture SUBClass - aridic (torric)
  • Dynamic Soil Properties:
  • Pedoderm Loose Cover Indicator - no
  • Hydric: no
  • QC Status: level 3
  • QA Status: level 3


  • SITE

  • Parent Material: eolian deposits
  • Landscape: tableland
  • Landform: sand sheet
  • Geomorphic Component Hills: side slope
  • Hill Slope Profile: backslope
  • Slope Position: middle third
  • Slope Complexity: simple
  • Slope Shape Across: linear
  • Slope Shape Down: linear
  • Drainage Class: well
  • Flooding: none flooding
  • Ponding: none ponding
  • Surface Fragments:
  • Benchmark Soil?: no
  • VEGETATION

    SITE OBSERVATION

  • Observation Date: 3/29/2006 (actual site observation date)
  • Air Photo ID: 47
  • Surface Cover Properties:
  • Site Obs. Cover Kind 1 - crop cover
  • Site Obs. Cover Kind 2 - close-grown crop
  • 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

    ochric epipedon

    argillic horizon

    secondary carbonates

    free carbonates

    lithologic discontinuity

    lithologic discontinuity

    0—9

    9—30

    30—172

    30—203

    82—172

    172—203

    —9—

    —21—

    —142—

    —173—

    —90—

    —31—

    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

    2

    908.3

    300

    Ap—0 to 9 centimeters (0.0 to 3.5 inches);, dark brown (10YR 3/3) broken face, moist; sandy clay loam; 20 percent clay; moderate medium subangular blocky structure; soft, very friable, slightly sticky, slightly plastic; moderately slow permeability; 6.0 very fine roots throughout and 2.0 fine roots throughout; fragments; noneffervescent, by hcl, 1n; clear smooth boundary.; observed in pit, small. The color described in the field (10YR 3/3 moist) meets the mollic horizon criteria, but the measured total carbon is only 0.53 percent with a trace of calcium carbonate. This results in this pedon being classified in the Alfisols order.
    Bt1—9 to 20 centimeters (3.5 to 7.9 inches);, dark brown (10YR 3/3) broken face, moist; sandy clay loam; 26 percent clay; moderate medium subangular blocky structure; slightly hard, friable, slightly sticky, slightly plastic; moderately slow permeability; 3.0 very fine roots throughout and 1.0 fine roots throughout; 2.0 fine low-continuity tubular pores; 10 percent faint clay films on vertical faces of peds; fragments; noneffervescent, by hcl, 1n; clear smooth boundary.; observed in pit, small. The color described in the field (10YR 3/3 moist) meets the mollic horizon criteria, but the measured total carbon is only 0.41 percent with a trace of calcium carbonate. This results in this pedon being classified in the Alfisols order.; discontinuous - phpvsfiid 320494; discontinuous - phpvsfiid 320494
    Bt2—20 to 30 centimeters (7.9 to 11.8 inches);, dark grayish brown (10YR 4/2) broken face, moist; loam; 20 percent clay; moderate coarse subangular blocky structure; slightly hard, friable, slightly sticky, nonplastic; moderate permeability; 2.0 very fine roots throughout; 3.0 very fine low-continuity tubular pores; 5 percent faint clay films on vertical faces of peds; fragments; noneffervescent, by hcl, 1n; clear wavy boundary.; observed in pit, small. patchy - phpvsfiid 320495; patchy - phpvsfiid 320495
    Bk1—30 to 46 centimeters (11.8 to 18.1 inches);, brown (10YR 5/3) broken face, moist; loam; 22 percent clay; moderate coarse subangular blocky structure; soft, very friable, slightly sticky, slightly plastic; moderate permeability; 2.0 very fine roots throughout; 1.0 fine low-continuity tubular pores; 2 percent fine irregular carbonate masses in matrix and 3 percent fine irregular carbonate concretions in matrix; fragments; strong effervescence, by hcl, 1n; abrupt smooth boundary.; observed in pit, small
    Bk2—46 to 82 centimeters (18.1 to 32.3 inches);, brown (10YR 5/3) broken face, moist; sandy clay loam; 22 percent clay; weak fine prismatic parts to moderate medium subangular blocky structure; soft, very friable, slightly sticky, slightly plastic; moderately slow permeability; 1.0 very fine roots throughout; 5.0 fine low-continuity tubular pores; 1 percent fine irregular carbonate nodules in matrix and 1 percent fine irregular carbonate masses in matrix; fragments; strong effervescence, by hcl, 1n; gradual wavy boundary.; observed in pit, small
    2Bk3—82 to 137 centimeters (32.3 to 53.9 inches); light yellowish brown (10YR 6/4) broken face, yellowish brown (10YR 5/4) broken face, moist; silt loam; 15 percent clay; moderate medium prismatic parts to moderate medium subangular blocky structure; slightly hard, friable, slightly sticky, slightly plastic; moderate permeability; 1.0 very fine roots throughout; 5.0 very fine low-continuity tubular pores; 15 percent fine threadlike carbonate masses in matrix and 5 percent medium irregular carbonate masses in matrix; fragments; strong effervescence, by hcl, 1n; clear wavy boundary.; observed in pit, small
    2Bk4—137 to 172 centimeters (53.9 to 67.7 inches);, yellowish brown (10YR 5/4) broken face, moist; loam; 15 percent clay; moderate medium prismatic parts to moderate medium subangular blocky structure; slightly hard, friable, slightly sticky, slightly plastic; moderate permeability; 1.0 very fine roots throughout; 3.0 very fine low-continuity tubular pores; 10 percent fine irregular carbonate masses in matrix; fragments; strong effervescence, by hcl, 1n; clear wavy boundary.; observed in pit, small
    3C—172 to 203 centimeters (67.7 to 79.9 inches);, brown (7.5YR 5/3) broken face, moist; sandy loam; 8 percent clay; structureless massive; soft, very friable, nonsticky, nonplastic; moderate permeability; 1.0 very fine roots throughout; 3 percent fine irregular carbonate masses in matrix; fragments; strong effervescence, by hcl, 1n.; observed in pit, small