IDENTIFIERS

  • Current Taxon Name (Soil Name): HATTON
  • OSD
  • Series Extent
  • User Site ID: 2005MO139059
  • User Pedon ID: 2005MO139059
  • Lab Information:
  • Certified Lab Pedon Description - no
  • Lab Source ID - MCL
  • Lab Pedon # - M0513959
  • NCSS Pedon Lab Data NASIS Record ID - 30369
  • 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: 38.8522222
  • Std. Longitude: -91.4063889
  • Datum: WGS84
  • Township: T47N
  • Range: R4W
  • Section: 7
  • PLSS Details: 2,596 feet East and 2,638 feet North from the South West corner
  • Location Description: near center section 7
  • Country: US—United States
  • State: Missouri
  • County: MO139—Montgomery
  • MLRA: 115—Central Mississippi Valley Wooded Slopes
  • Non-MLRA Soil Survey Area: MO603—Montgomery and Warren Counties, Missouri
  • 7.5 Minute USGS Quad: 38091-G4—Pinnacle Lake, Missouri

    • PEDON

  • Describers Name: Mike Chalfant, David Dowdy, John Horton, Greg Caldwell
  • Current Taxonomic Class: Fine, smectitic, superactive, mesic Oxyaquic Vertic Hapludalfs
  • Current Taxon Kind: family
  • Pedon Type: within range of map unit
  • Pedon Purpose: full pedon description
  • Pedon Record Orgin: Missouri Pedon
  • Pedon #: 59
  • Sampled As Information:
  • Soil Name - HATTON
  • Taxonomic Class - Fine, smectitic, superactive, mesic Oxyaquic Vertic Hapludalfs
  • PSC - 18 to 69 cm.
  • Classificaton Date - 4/26/2005
  • Soil Taxonomic Edition - ninth edition
  • Moisture Class - udic
  • Moisture SUBClass - oxyaquic
  • Dynamic Soil Properties:
  • Erosion Class - 2
  • Pedoderm Loose Cover Indicator - no
  • Hydric: no


    • SITE

  • Parent Material: fine-silty loess derived from mixed
  • Landscape: hills
  • Landform: interfluve
  • Geomorphic Component Hills: interfluve
  • Hill Slope Profile: summit
  • Slope Position: upper third
  • Slope Complexity: simple
  • Slope Shape Across: concave
  • Slope Shape Down: concave
  • Runoff: low
  • Drainage Class: moderately well
  • Flooding: none flooding
  • Ponding: none ponding
  • Geology: Pre-illinoian Stage formation.
  • Surface Fragments:
  • Benchmark Soil?: no

    • VEGETATION

    SITE OBSERVATION

  • Observation Date: 4/26/2005 (actual site observation date)
  • Air Photo ID: 38091g4ne
  • Surface Water Kind: none observed
  • Surface Cover Properties:
  • Site Obs. Cover Kind 1 - other
  • Site Obs. Cover Kind 2 - rural transportation
  • 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

    ochric epipedon

    argillic horizon

    0—18

    18—76

    —18—

    —58—
    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

    —

    270

    —

    —

    —

    —

    —

    —

    —

    —

    —

    —

    —

    —

    —

    —
    Ap—0 to 18 centimeters (0.0 to 7.1 inches); dark grayish brown (10YR 4/2) broken face silty clay loam; weak fine subangular blocky structure; friable; 10.0 very fine tubular and 10.0 fine tubular pores; fragments; clear smooth boundary. Lab sample # MU026807; observed in push tube
    Bt1—18 to 36 centimeters (7.1 to 14.2 inches); dark yellowish brown (10YR 4/6) broken face silty clay; moderate fine subangular blocky structure; very firm; 3.0 very fine tubular and 3.0 fine tubular pores; 15 percent ; fragments; clear smooth boundary. Lab sample # MU026808; observed in push tube
    Bt2—36 to 76 centimeters (14.2 to 29.9 inches); brown (10YR 4/3) broken face silty clay; moderate very fine subangular blocky structure; firm; 10.0 very fine vesicular and 10.0 fine vesicular pores; 20 percent ; 1 percent medium faint irregular noncoherent cemented dark yellowish brown (10YR 4/6), moist, iron depletions with clear boundaries in matrix and 1 percent medium faint irregular noncoherent cemented grayish brown (10YR 5/2), moist, iron depletions with clear boundaries in matrix; fragments; clear smooth boundary. Lab sample # MU026809; observed in push tube
    2Bw1—76 to 122 centimeters (29.9 to 48.0 inches); 60 percent brown (10YR 5/3) broken face and 40 percent light brownish gray (10YR 6/2) broken face silt loam; moderate thin platy structure; friable; 10 percent and 15 percent prominent light gray (10YR 7/1), moist, skeletans; 1 percent medium faint irregular noncoherent cemented strong brown (7.5YR 5/8), moist, iron depletions with clear boundaries in matrix; fragments; clear smooth boundary. Lab sample # MU026810; observed in push tube
    2Bw2—122 to 145 centimeters (48.0 to 57.1 inches); 70 percent yellowish brown (10YR 5/4) broken face and 30 percent light brownish gray (10YR 6/2) broken face silt loam; moderate subangular blocky structure; friable; 1 percent medium faint irregular noncoherent cemented yellowish brown (10YR 5/8), moist, iron depletions with clear boundaries in matrix; fragments; clear smooth boundary. Lab sample # MU026811; observed in push tube
    3Btb1—145 to 213 centimeters (57.1 to 83.9 inches); yellowish brown (10YR 5/4) broken face clay; moderate very fine subangular blocky structure; very firm; 60 percent ; 1 percent medium faint irregular noncoherent cemented 7.5YR 3/6 (7.5YR 3/6), moist, iron depletions with clear boundaries in matrix and 1 percent medium faint irregular noncoherent cemented gray (10YR 6/1), moist, iron depletions with clear boundaries in matrix and 1 percent medium faint irregular noncoherent cemented black (10YR 2/1), moist, iron depletions with clear boundaries in matrix; fragments; gradual smooth boundary. Lab sample # MU026812; observed in push tube
    3Btb2—213 to 239 centimeters (83.9 to 94.1 inches); yellowish brown (10YR 5/6) broken face gravelly clay loam; weak fine subangular blocky, and weak coarse prismatic structure; firm; 30 percent distinct clay films; 1 percent medium faint irregular noncoherent cemented dark yellowish brown (10YR 4/6), moist, iron depletions with clear boundaries in matrix and 1 percent medium faint irregular noncoherent cemented gray (10YR 6/1), moist, iron depletions with clear boundaries in matrix and 1 percent medium faint irregular noncoherent cemented black (10YR 2/1), moist, iron depletions with clear boundaries in matrix; 30 percent by volume nonflat subangular indurated 2-?-5 millimeter chert fragments; clear smooth boundary.; observed in push tube
    3Btk—239 to 457 centimeters (94.1 to 179.9 inches); yellowish brown (10YR 5/6) broken face clay loam; weak fine subangular blocky structure; firm; 40 percent prominent carbonate coats; 1 percent medium faint irregular noncoherent cemented yellowish brown (10YR 5/8), moist, iron depletions with clear boundaries in matrix and 1 percent medium faint irregular noncoherent cemented yellowish brown (10YR 5/6), moist, iron depletions with clear boundaries in matrix and 1 percent medium faint irregular noncoherent cemented black (10YR 2/1), moist, iron depletions with clear boundaries in matrix; nonflat subangular indurated 2-?-5 millimeter limestone, unspecified fragments and nonflat subrounded indurated 2-?-5 millimeter mixed fragments and 10 percent by volume nonflat subangular indurated 2-?-5 millimeter chert fragments; clear smooth boundary.; observed in push tube
    3C—457 to 533 centimeters (179.9 to 209.8 inches); 50 percent yellowish brown (10YR 5/6) broken face and 50 percent gray (10YR 6/1) broken face clay loam; massive; firm; 1 percent medium faint irregular noncoherent cemented yellowish brown (10YR 5/8), moist, iron depletions with clear boundaries in matrix and 1 percent medium faint irregular noncoherent cemented black (10YR 2/1), moist, iron depletions with clear boundaries in matrix; nonflat subrounded indurated 2-?-5 millimeter mixed fragments and 4 percent by volume nonflat subangular indurated 2-?-5 millimeter chert fragments; clear smooth boundary.; observed in push tube
    4C—533 to 569 centimeters (209.8 to 224.0 inches); 20 percent light yellowish brown (10YR 6/4) broken face and 20 percent very pale brown (10YR 8/2) broken face and 60 percent light greenish gray (10Y 8/1) broken face clay; firm; 1 percent medium faint irregular noncoherent cemented yellowish red (5YR 5/8), moist, iron depletions with clear boundaries in matrix; fragments; abrupt smooth boundary.; observed in push tube
    4C—569 to 569 centimeters (224.0 to 224.0 inches); fragments.; observed in push tube