IDENTIFIERS

  • Current Taxon Name (Soil Name): Gobbler
  • OSD
  • Series Extent
  • User Site ID: 1996MO119091M
  • User Pedon ID: 1996MO119091
  • User Site Association ID: 8445
  • Transect:
  • User Transect ID - 96-10
  • Transect Stop Number - 5
  • Transect Interval - 70.0
  • Lab Information:
  • Certified Lab Pedon Description - no
  • Lab Source ID - MCL
  • Lab Pedon # - M9611953
  • Print Date: 11/23/2024
  • 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: 36.7427222
  • Std. Longitude: -94.5624889
  • Datum: WGS84
  • Map Unit: 73352—Jollymill-Bendavis complex, 3 to 15 percent slopes
  • State: Missouri
  • County: MO119—McDonald
  • MLRA: 116B—Springfield Plain
  • Non-MLRA Soil Survey Area: MO119—McDonald County, Missouri
  • PEDON

  • Describers Name: Scott Eversoll, Ken Gregg and Jeff Woodward
  • Current Taxonomic Class: Clayey-skeletal, mixed, semiactive, mesic Typic Hapludalfs
  • Current Taxon Kind: series
  • Pedon Type: within range of map unit
  • Pedon Purpose: laboratory sampling site
  • Pedon Record Orgin: Converted from PDP 3.x
  • Correlated Information:
  • Soil Name - Gobbler
  • PSC - 38 to 88 cm.
  • Classificaton Date - 4/18/2012
  • Moisture Class - udic
  • Sampled As Information:
  • Soil Name - Jollymill
  • Taxon Kind - series
  • Classificaton Date - 11/21/1996
  • Dynamic Soil Properties:
  • Pedoderm Loose Cover Indicator - no
  • Hydric: no


  • SITE

  • Parent Material: slope alluvium and/or residuum weathered from cherty limestone
  • Landscape: plateau
  • Landform: ridge
  • Geomorphic Component Hills: interfluve
  • Hill Slope Profile: shoulder
  • Slope Shape Across: convex
  • Slope Shape Down: convex
  • Drainage Class: well
  • Surface Fragments: 0.00 percent
  • Benchmark Soil?: no
  • VEGETATION

    SITE OBSERVATION

  • Observation Date: 11/21/1996 (actual site observation date)
  • Air Photo ID: 5A
  • Surface Cover Properties:
  • 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

    lithic contact

    0—38

    38—147

    147—0

    —-

    —-

    —-

    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

    15

    332

    55

    A—0 to 10 centimeters (0.0 to 3.9 inches); dark grayish brown (10YR 4/2) extremely gravelly silt loam; weak very fine granular structure; very friable; 25.0 very fine to coarse roots throughout; 25.0 fine interstitial and tubular pores; 70 percent by volume subrounded 2-39-75 millimeter limestone, cherty fragments; strongly acid, pH 5.2, hellige-truog; clear smooth boundary. Lab sample # MU017967
    E—10 to 38 centimeters (3.9 to 15.0 inches); 60 percent pale brown (10YR 6/3) and 40 percent very pale brown (10YR 7/3) extremely gravelly silt; moderate very fine granular structure; very friable; 20.0 very fine to coarse roots throughout; 20.0 fine interstitial and tubular pores; 5 percent by volume subrounded 75-162-250 millimeter limestone, cherty fragments and 60 percent by volume subrounded 2-39-75 millimeter limestone, cherty fragments; very strongly acid, pH 4.9, hellige-truog; clear wavy boundary. Lab sample # MU017968
    Bt1—38 to 53 centimeters (15.0 to 20.9 inches); strong brown (7.5YR 5/6) extremely gravelly silt loam; moderate very fine subangular blocky structure; friable; 8.0 very fine to medium roots throughout; 10.0 fine interstitial and tubular pores; 5 percent faint yellowish red (5YR 4/6) clay films on faces of peds and 15 percent distinct brown (7.5YR 5/4) skeletans on faces of peds; 65 percent by volume subangular 2-39-75 millimeter limestone, cherty fragments; very strongly acid, pH 5.0, hellige-truog; clear wavy boundary. Lab sample # MU017969. patchy - phpvsfiid 154775; patchy - phpvsfiid 154776; patchy - phpvsfiid 154775; patchy - phpvsfiid 154776
    Bt2—53 to 71 centimeters (20.9 to 28.0 inches); red (2.5YR 5/8) extremely gravelly silty clay loam; moderate very fine and fine subangular blocky structure; firm; 6.0 very fine to medium roots throughout; 10.0 fine interstitial and tubular pores; 10 percent distinct dark red (2.5YR 3/6) clay films on faces of peds and 10 percent distinct brown (7.5YR 5/4) skeletans on faces of peds; 5 percent by volume subangular 75-162-250 millimeter limestone, cherty fragments and 60 percent by volume subangular 2-39-75 millimeter limestone, cherty fragments; very strongly acid, pH 5.0, hellige-truog; clear wavy boundary. Lab sample # MU017970. patchy - phpvsfiid 154778; discontinuous - phpvsfiid 154777; patchy - phpvsfiid 154778; discontinuous - phpvsfiid 154777
    2Bt3—71 to 114 centimeters (28.0 to 44.9 inches); dark red (2.5YR 3/6) clay; moderate very fine and fine subangular blocky structure; very firm; 1.0 very fine and fine roots throughout; 2.0 fine interstitial and tubular pores; 25 percent distinct yellowish red (5YR 5/6) silt coats on faces of peds and 25 percent faint dark red (2.5YR 3/6) clay films on faces of peds; 5 percent by volume subangular 2-39-75 millimeter limestone, cherty fragments; very strongly acid, pH 5.0, hellige-truog; abrupt wavy boundary. Lab sample # MU017971. discontinuous - phpvsfiid 154027; discontinuous - phpvsfiid 154779; discontinuous - phpvsfiid 154027; discontinuous - phpvsfiid 154779
    2BC—114 to 147 centimeters (44.9 to 57.9 inches); 60 percent dark red (2.5YR 3/6) and 40 percent red (2.5YR 4/8) very gravelly clay; massive; very firm; 1.0 very fine and fine roots throughout; 1.0 fine interstitial pores; 50 percent by volume subrounded 2-39-75 millimeter limestone, unspecified fragments; very strongly acid, pH 4.8, hellige-truog; abrupt irregular boundary. Lab sample # MU017972
    R—147 centimeters (57.9 inches); bedrock; fragments.