IDENTIFIERS

  • Current Taxon Name (Soil Name): Bucyrus
  • OSD
  • Series Extent
  • User Site ID: 2006MO083005
  • User Pedon ID: 2006MO083005
  • Transect:
  • User Transect ID - 11206MO083-40078
  • Transect Stop Number - 5
  • Lab Information:
  • Certified Lab Pedon Description - no
  • Lab Source ID - MCL
  • Lab Pedon # - M0608305
  • NCSS Pedon Lab Data NASIS Record ID - 25903
  • 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: 38.5453333
  • Std. Longitude: -93.9922500
  • Datum: WGS84
  • Township: T43N
  • Range: R28W
  • Section: 3
  • PLSS Details: 406 feet W and 2168 feet S of the NE corner
  • Country: US—United States
  • State: Missouri
  • County: MO083—Henry
  • MLRA: 112—Cherokee Prairies
  • Non-MLRA Soil Survey Area: MO083—Henry County, Missouri
  • 7.5 Minute USGS Quad: 38093-E8—Blairstown, Missouri
  • PEDON

  • Describers Name: Sheila Staton-Clifton, Mark Abney, Craig Chatfield
  • Current Taxonomic Class: Fine, smectitic, thermic Vertic Paleudolls
  • Current Taxon Kind: series
  • Pedon Type: classifies to current taxon name, full description
  • Pedon Purpose: full pedon description
  • Pedon Record Orgin: Missouri Pedon
  • Pedon #: 5
  • Correlated Information:
  • Soil Name - Bucyrus
  • PSC - 30 to 81 cm.
  • Classificaton Date - 2/1/2012
  • Soil Taxonomic Edition - ninth edition
  • Moisture Class - udic
  • Moisture Subclass - typic
  • Sampled As Information:
  • Soil Name - Newtonia
  • Classificaton Date - 2/14/2006
  • Dynamic Soil Properties:
  • Erosion Class - 2
  • Pedoderm Loose Cover Indicator - no
  • Hydric: no


  • SITE

  • Parent Material: Quaternary System fine-silty loess derived from mixed over Pennsylvanian System clayey residuum weathered from limestone
  • Landscape: upland
  • Landform: ridge
  • Geomorphic Component Hills: crest
  • Hill Slope Profile: summit
  • Slope Position: upper third
  • Slope Complexity: simple
  • Slope Shape Across: linear
  • Slope Shape Down: convex
  • Runoff: low
  • Drainage Class: moderately well
  • Flooding: none flooding
  • Ponding: none ponding
  • Bedrock: indurated moderate weathered limestone, unspecified at 206cm with 10 to <45 and a strike of 0 degrees and a dip of 0 to 0 degrees
  • Geology: Weir Formation formation.
  • Surface Fragments:
  • Benchmark Soil?: no
  • VEGETATION

    SITE OBSERVATION

  • Observation Date: 2/14/2006 (actual site observation date)
  • Air Photo ID: 38093e8sw
  • Surface Water Kind: none observed
  • Surface Cover Properties:
  • Site Obs. Cover Kind 1 - crop cover
  • Site Obs. Cover Kind 2 - row crop
  • Pedoderm Loose Cover Indicator - no
  • Drained? - no
  • Bedded Soil? - no
  • Forest Plantation? - no
  • Site Erosion Accelerated: water erosion sheet
  • Pedon Restrictions
    Kind Hardness Restriction Depth L-H Restriction Thickness L-RV-H
    cm

    bedrock, lithic

    206 - 206

    - 1 -

    Pedon Diagnostic Features
    Feature Kind Feature Depth L-H Feature Thickness L-RV-H
    cm

    mollic epipedon

    argillic horizon

    lithic contact

    0—30

    30—160

    206—206

    —30—

    —130—

    —1—

    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

    256.6

    45

    Ap—0 to 10 centimeters (0.0 to 3.9 inches); dark brown (10YR 3/3) interior silt loam; 22 percent clay; moderate fine granular structure; very friable; 0.5 very fine roots throughout and 0.5 fine roots throughout; fragments; abrupt smooth boundary. Lab sample # MU005786; observed in push tube
    A—10 to 30 centimeters (3.9 to 11.8 inches); dark brown (7.5YR 3/3) interior silty clay loam; 29 percent clay; moderate fine granular, and weak fine subangular blocky structure; very friable; 0.5 very fine roots throughout and 0.5 fine roots throughout; fragments; clear smooth boundary. Lab sample # MU005787; observed in push tube
    Bt1—30 to 56 centimeters (11.8 to 22.0 inches); 40 percent dark brown (7.5YR 3/3) interior and 60 percent brown (7.5YR 4/4) interior silty clay loam; 34 percent clay; moderate medium subangular blocky, and weak fine prismatic structure; friable; 0.5 very fine roots throughout and 0.5 fine roots throughout; 45 percent brown (7.5YR 4/3), moist, clay films on vertical faces of peds; fragments; clear smooth boundary. Lab sample # MU005788; observed in push tube
    2Bt2—56 to 97 centimeters (22.0 to 38.2 inches); 40 percent dark reddish brown (5YR 3/3) interior and 60 percent reddish brown (5YR 4/4) interior silty clay; 40 percent clay; moderate medium subangular blocky, and moderate fine prismatic structure; firm; 0.5 very fine roots throughout and 0.5 fine roots throughout; 50 percent dark reddish brown (2.5YR 3/4), moist, clay films on vertical faces of peds; 1 percent medium faint irregular noncoherent cemented iron depletions with clear boundaries in matrix; 2 percent by volume very strongly coherent cemented limestone, cherty fragments; clear smooth boundary. Lab sample # MU005789; observed in push tube
    2Bt3—97 to 132 centimeters (38.2 to 52.0 inches); yellowish red (5YR 4/6) interior silty clay; 43 percent clay; moderate medium subangular blocky, and moderate fine prismatic structure; firm; 0.5 very fine roots throughout and 0.5 fine roots throughout; 65 percent dark reddish brown (5YR 3/4), moist, clay films on vertical faces of peds; 1 percent medium faint irregular noncoherent cemented iron depletions with clear boundaries in matrix; 4 percent by volume flat very strongly coherent cemented limestone, cherty fragments; clear smooth boundary. Lab sample # MU005790; observed in push tube
    2Bt4—132 to 160 centimeters (52.0 to 63.0 inches); red (2.5YR 4/6) interior silty clay; 48 percent clay; strong medium subangular blocky, and moderate fine prismatic structure; very firm; 0.5 very fine roots throughout and 0.5 fine roots throughout; 75 percent dark reddish brown (5YR 3/4), moist, clay films on vertical faces of peds; 1 percent medium faint irregular noncoherent cemented iron depletions with clear boundaries in matrix; 8 percent by volume flat very strongly coherent cemented limestone, cherty fragments; abrupt smooth boundary. Lab sample # MU005791; observed in push tube
    2BC—160 to 206 centimeters (63.0 to 81.1 inches); 80 percent yellowish red (5YR 4/6) interior and 20 percent yellowish red (5YR 5/8) interior clay; 54 percent clay; massive, and weak fine subangular blocky; very firm; 0.5 very fine roots throughout and 0.5 fine roots throughout; 60 percent dark reddish brown (2.5YR 3/4), moist, clay films on vertical faces of peds; 1 percent medium faint irregular noncoherent cemented iron depletions with clear boundaries in matrix and 1 percent medium faint irregular noncoherent cemented reddish yellow (7.5YR 6/8), moist, iron depletions with clear boundaries in matrix; 40 percent by volume flat subrounded very strongly coherent cemented limestone, cherty fragments. Lab sample # MU005792; observed in push tube
    2R—206 to 206 centimeters (81.1 to 81.1 inches); fragments.; observed in push tube