IDENTIFIERS

  • Current Taxon Name (Soil Name): Webster
  • OSD
  • Series Extent
  • User Site ID: S1954MN161113B
  • User Pedon ID: S1954MN161113B
  • Lab Information:
  • Certified Lab Pedon Description - no
  • Lab Source ID - SSL
  • Lab Pedon # - 40A1695
  • NCSS Pedon Lab Data NASIS Record ID - 35853
  • Print Date: 5/20/2024

    • 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: 43.8899956
  • Std. Longitude: -93.6455002
  • Datum: WGS84
  • Township: 105N
  • Range: 24W
  • Section: 25
  • PLSS Details: Cornfield in SE SE1/4
  • State: Minnesota
  • County: MN161—Waseca
  • MLRA: 103—Central Iowa and Minnesota Till Prairies
  • Non-MLRA Soil Survey Area: MN161—Waseca County, Minnesota

    • PEDON

  • Describers Name: A. H. Paschall
  • Current Taxonomic Class: Fine-loamy, mixed, superactive, mesic Typic Endoaquolls
  • Current Taxon Kind: series
  • Pedon Purpose: full pedon description
  • Pedon Record Orgin: Converted from PDP 3.x
  • Pedon #: 113
  • Correlated Information:
  • Soil Name - Webster
  • PSC - 25 to 100 cm.
  • Classificaton Date - 7/23/2007
  • Moisture Class - aquic
  • Sampled As Information:
  • Soil Name - Webster
  • Classificaton Date - 7/11/1954
  • Dynamic Soil Properties:
  • Erosion Class - 0
  • Pedoderm Loose Cover Indicator - no
  • Hydric: no


    • SITE

  • Landform: depression
  • Drainage Class: poorly
  • Surface Fragments: 0.00 percent
  • Benchmark Soil?: no

    • VEGETATION

    SITE OBSERVATION

  • Observation Date: 7/11/1954 (actual site observation date)
  • Surface Cover Properties:
  • Site Obs. Cover Kind 1 - crop cover
  • Pedoderm Loose Cover Indicator - no
  • Drained? - no
  • Bedded Soil? - no
  • Forest Plantation? - no
    • 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

    0

    —

    —

    —

    —

    —

    —

    —

    —

    —

    —

    —

    —

    —

    —

    —

    —

    —

    —
    Ap—0 to 18 centimeters (0.0 to 7.1 inches); black (10YR 2/1) silty clay loam; subangular blocky parts to weak very fine angular blocky structure; moderately plastic; fragments. Lab sample # 40A13408
    A12—18 to 33 centimeters (7.1 to 13.0 inches); black (10YR 2/1) silty clay loam; massive; moderately sticky; fragments; clear smooth boundary. Lab sample # 40A13409. This layer has been compacted by cultivation.
    B21—33 to 43 centimeters (13.0 to 16.9 inches); very dark gray (10YR 3/1) silty clay loam; weak very fine angular blocky parts to weak very fine angular blocky structure; friable, slightly sticky; fragments smooth boundary. Lab sample # 40A13410
    B22—43 to 58 centimeters (16.9 to 22.8 inches); dark gray (5Y 4/1) and olive gray (5Y 5/2) silty clay loam; massive parts to weak very fine angular blocky; friable; fragments. Lab sample # 40A13411. Material tongues down into the next horizon.
    C1—58 to 66 centimeters (22.8 to 26.0 inches); olive gray (5Y 5/2) and olive (5Y 5/3) clay loam; massive parts to weak very fine angular blocky; friable, moderately sticky; 21.0 tubular pores; fragments. Lab sample # 40A13412. Pores are worm holes filled with very dark gray material (10YR 3/1).
    C2—66 to 84 centimeters (26.0 to 33.1 inches); olive (5Y 5/3) and pale yellow (5Y 7/3) clay loam; massive parts to weak very fine angular blocky; friable, moderately sticky; fragments; strong effervescence, by hcl, unspecified. Lab sample # 40A13413
    C3—84 to 117 centimeters (33.1 to 46.1 inches); olive (5Y 5/3) clay loam; massive; friable, slightly sticky; 2-39-75 millimeter shale, unspecified fragments. Lab sample # 40A13414
    C4—117 centimeters (46.1 inches); gray (5Y 5/1) and olive (5Y 5/3) clay loam; 21 percent yellowish brown (10YR 5/8) medium distinct mottles; friable; fragments. Lab sample # 40A13415. Sample was obtained with an auger, hence no structure determinations.