IDENTIFIERS

  • Current Taxon Name (Soil Name): Collinsville
  • OSD
  • Series Extent
  • User Site ID: 1996MO097009
  • User Pedon ID: 1996MO097009
  • User Site Association ID: 8417
  • Transect:
  • User Transect ID - 95-10
  • Transect Stop Number - 2
  • Transect Interval - 100.0
  • Lab Information:
  • Certified Lab Pedon Description - no
  • Lab Source ID - MCL
  • Lab Pedon # - M9609709
  • NCSS Pedon Lab Data NASIS Record ID - 32469
  • 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: 37.3050417
  • Std. Longitude: -94.4168528
  • Datum: WGS84
  • Township: T30N
  • Range: R32W
  • Section: 35
  • PLSS Details: 1950 feet N and 1100 feet W of the SE corner
  • Location Description: SW 1/4 SE 1/4 SEC 35 T30N R32W; 1950 feet north and 1100 feet west of the southeast corner of section 35
  • Map Unit: 40029—Sylvania loam, 8 to 15 percent slopes
  • State: Missouri
  • County: MO097—Jasper
  • MLRA: 112—Cherokee Prairies
  • Non-MLRA Soil Survey Area: MO097—Jasper County, Missouri

    • PEDON

  • Describers Name: ACP
  • Current Taxonomic Class: Fine-loamy, mixed, thermic Lithic Hapludolls
  • Current Taxon Kind: taxadjunct
  • Pedon Type: map unit inclusion
  • Pedon Purpose: soil survey inventory
  • Pedon Record Orgin: Converted from PDP 3.x
  • Correlated Information:
  • Soil Name - Collinsville
  • PSC - 0 to 25 cm.
  • Classificaton Date - 4/18/2012
  • Moisture Class - udic
  • Sampled As Information:
  • Soil Name - Collinsville
  • Classificaton Date - 4/8/1996
  • Dynamic Soil Properties:
  • Erosion Class - 1
  • Pedoderm Loose Cover Indicator - no
  • Hydric: no


    • SITE

  • Parent Material: residuum weathered from sandstone
  • Landscape: plains
  • Geomorphic Component Hills: side slope
  • Slope Shape Across: convex
  • Slope Shape Down: convex
  • Runoff: medium
  • Drainage Class: well
  • Flooding: none flooding
  • Ponding: none ponding
  • Bedrock: sandstone, noncalcareous
  • Surface Fragments:
  • Benchmark Soil?: no

    • VEGETATION

    SITE OBSERVATION

  • Observation Date: 4/8/1996 (actual site observation date)
  • Air Photo ID: 7
  • Surface Cover Properties:
  • Site Obs. Cover Kind 1 - grass/herbaceous cover
  • 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

    lithic contact

    0—25

    25—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

    8

    —

    —

    296

    —

    100

    991

    —

    —

    13.9

    25

    2.8

    —

    —

    —

    —

    —

    —

    —

    —
    Ap—0 to 10 centimeters (0.0 to 3.9 inches); very dark grayish brown (10YR 3/2) crushed, brown (10YR 4/3) crushed, dry; fine sandy loam; strong fine granular structure; very friable; 10.0 very fine and fine roots throughout; 10.0 very fine and fine high-continuity interstitial and tubular pores; 1 percent by volume subangular 2-39-75 millimeter sandstone, noncalcareous fragments; moderately acid, pH 5.6, hellige-truog; clear smooth boundary. Lab sample # MU055395
    A—10 to 25 centimeters (3.9 to 9.8 inches); dark brown (10YR 3/3) crushed, brown (10YR 4/3) crushed, dry; fine sandy loam; strong medium subangular blocky parts to moderate fine granular structure; very friable; 7.0 very fine and fine roots throughout; 10.0 very fine and fine high-continuity interstitial and tubular pores; 1 percent by volume subangular 2-39-75 millimeter sandstone, noncalcareous fragments; moderately acid, pH 5.9, hellige-truog; abrupt smooth boundary. Lab sample # MU055396
    R—25 centimeters (9.8 inches); bedrock; fragments.