IDENTIFIERS

  • Current Taxon Name (Soil Name): Newtonia
  • OSD
  • Series Extent
  • User Site ID: 1999MO097002
  • User Pedon ID: 1999MO097002
  • Transect:
  • User Transect ID - 99-4
  • Transect Stop Number - 4
  • Transect Interval - 80.0
  • Lab Information:
  • Certified Lab Pedon Description - no
  • Lab Source ID - MCL
  • Lab Pedon # - M9909702
  • NCSS Pedon Lab Data NASIS Record ID - 27889
  • 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: 37.2794556
  • Std. Longitude: -94.1491917
  • Datum: WGS84
  • Township: T29N
  • Range: R30W
  • Section: 1
  • PLSS Details: 4750 feet S and 2000 feet W of the NE corner
  • Location Description: SW 1/4 NE 1/4 Sec 1 T29N R30W; 4750 feet south and 2000 feet west of the northeast corner of section 1
  • Map Unit: 40020—Newtonia-Eldorado silt loams, 1 to 3 percent slopes, moderately eroded
  • 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-silty, mixed, thermic Typic Paleudolls
  • Current Taxon Kind: taxadjunct
  • Pedon Type: within range of map unit
  • Pedon Purpose: soil survey inventory
  • Pedon Record Orgin: Converted from PDP 3.x
  • Correlated Information:
  • Soil Name - Newtonia
  • PSC - 23 to 74 cm.
  • Classificaton Date - 4/18/2012
  • Moisture Class - udic
  • Sampled As Information:
  • Soil Name - Newtonia
  • Classificaton Date - 2/17/1999
  • Dynamic Soil Properties:
  • Erosion Class - 2
  • Pedoderm Loose Cover Indicator - no
  • Hydric: no


  • SITE

  • Parent Material: loess and/or residuum and/or residuum weathered from cherty limestone
  • Landscape: plateau
  • Slope Shape Across: linear
  • Slope Shape Down: convex
  • Runoff: medium
  • Drainage Class: well
  • Flooding: none flooding
  • Ponding: none ponding
  • Surface Fragments:
  • Benchmark Soil?: no
  • VEGETATION

    SITE OBSERVATION

  • Observation Date: 2/17/1999 (actual site observation date)
  • Air Photo ID: 14E
  • Surface Cover Properties:
  • Site Obs. Cover Kind 1 - crop 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

    argillic horizon

    0—23

    23—102

    —-

    —-

    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

    314

    Ap—0 to 23 centimeters (0.0 to 9.1 inches); dark brown (10YR 3/3) crushed, yellowish brown (10YR 5/4) crushed, dry; silt loam; moderate medium subangular blocky parts to moderate very fine and fine granular structure; very friable; 3.0 very fine and fine roots throughout; 8.0 very fine and fine moderate-continuity interstitial and tubular pores; 1 percent by volume subangular 2-39-75 millimeter limestone, cherty fragments; clear smooth boundary. Lab sample # MU019453
    2Bt1—23 to 33 centimeters (9.1 to 13.0 inches); yellowish red (5YR 4/6) interior silt loam; moderate fine subangular blocky parts to moderate very fine and fine granular structure; friable; 1.0 very fine and fine roots throughout; 8.0 very fine and fine moderate-continuity interstitial and tubular pores; 20 percent distinct dark brown (10YR 3/3), moist, organic stains on faces of peds and 20 percent prominent dark reddish brown (5YR 3/4), moist, clay films on faces of peds; 1 percent by volume subangular 2-39-75 millimeter limestone, cherty fragments; clear smooth boundary. Lab sample # MU019454. discontinuous - phpvsfiid 155814; continuous - phpvsfiid 155815; discontinuous - phpvsfiid 155814; continuous - phpvsfiid 155815
    2Bt2—33 to 61 centimeters (13.0 to 24.0 inches); yellowish red (5YR 4/6) interior silty clay loam; moderate fine subangular blocky parts to weak very fine and fine granular structure; friable; 1.0 very fine and fine roots throughout; 8.0 very fine and fine moderate-continuity interstitial and tubular pores; 5 percent distinct dark brown (10YR 3/3), moist, organic stains on faces of peds and 20 percent prominent dark reddish brown (5YR 3/4), moist, clay films on faces of peds and 30 percent prominent yellowish red (5YR 4/6), moist, clay films on faces of peds; 1 percent fine irregular black (N 2/0) iron-manganese concretions throughout; 1 percent by volume subangular 2-39-75 millimeter limestone, cherty fragments; gradual smooth boundary. Lab sample # MU019455. discontinuous - phpvsfiid 155817; patchy - phpvsfiid 155816; discontinuous - phpvsfiid 155818; discontinuous - phpvsfiid 155817; patchy - phpvsfiid 155816; discontinuous - phpvsfiid 155818
    2Bt3—61 to 91 centimeters (24.0 to 35.8 inches); red (2.5YR 4/8) interior silty clay; moderate medium subangular blocky parts to weak very fine and fine granular structure; friable; 0.5 very fine and fine roots throughout; 5.0 very fine and fine moderate-continuity interstitial and tubular pores; 40 percent prominent red (2.5YR 4/8), moist, clay films on faces of peds; 1 percent by volume subangular 2-39-75 millimeter limestone, cherty fragments; clear smooth boundary. Lab sample # MU019456. discontinuous - phpvsfiid 155819; discontinuous - phpvsfiid 155819
    2Bt4—91 to 102 centimeters (35.8 to 40.2 inches); red (2.5YR 4/8) interior extremely gravelly clay loam; moderate medium subangular blocky structure; firm; 0.1 very fine and fine roots throughout; 4.0 very fine and fine moderate-continuity interstitial and tubular pores; 30 percent distinct red (2.5YR 4/8), moist, clay films on faces of peds; 5 percent by volume subangular 75-162-250 millimeter limestone, cherty fragments and 50 percent by volume subangular 2-39-75 millimeter limestone, cherty fragments. Lab sample # MU019457. 30 percent of rock fragments is tripolitic; discontinuous - phpvsfiid 155820; discontinuous - phpvsfiid 155820