IDENTIFIERS

  • Current Taxon Name (Soil Name): MARSHALL
  • OSD
  • Series Extent
  • User Site ID: S1957NE177005
  • User Pedon ID: S1957NE177005
  • Lab Information:
  • Certified Lab Pedon Description - no
  • Lab Source ID - SSL
  • Lab Pedon # - 40A2283
  • NCSS Pedon Lab Data NASIS Record ID - 36980
  • Print Date: 9/24/2024

    • 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: 41.5088882
  • Std. Longitude: -96.2216644
  • Datum: WGS84
  • Township: 18N
  • Range: 11E
  • Section: 30
  • PLSS Details: .3 mile west and 180 feet south of northeast corner
  • State: Nebraska
  • County: NE177—Washington
  • MLRA: 106—Nebraska and Kansas Loess-Drift Hills
  • Non-MLRA Soil Survey Area: NE177—Washington County, Nebraska

    • PEDON

  • Describers Name: J.A. Elder and H.L. Kollmorgen
  • Pedon Record Orgin: Converted from PDP 3.x
  • Pedon #: 5
  • Correlated Information:
  • Soil Name - MARSHALL
  • Classificaton Date - 9/6/2001
  • Moisture Class - udic
  • Sampled As Information:
  • Soil Name - Marshall
  • Classificaton Date - 7/7/1957
  • Dynamic Soil Properties:
  • Pedoderm Loose Cover Indicator - no
  • Hydric: no


    • SITE

  • Drainage Class: excessively
  • Surface Fragments:
  • Benchmark Soil?: no

    • VEGETATION

    SITE OBSERVATION

  • Observation Date: 7/7/1957 (actual site observation date)
  • Surface Cover Properties:
  • 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

    6

    —

    —

    —

    —

    90

    —

    —

    —

    —

    —

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    A1p—0 to 15 centimeters (0.0 to 5.9 inches); very dark grayish brown (10YR 3/2) silty clay loam; weak very fine and fine granular structure; friable; fragments; abrupt smooth boundary. Lab sample # 40A17916
    B1—15 to 23 centimeters (5.9 to 9.1 inches); very dark grayish brown (10YR 3/2) silty clay loam; moderate very fine and fine subangular blocky parts to moderate fine granular structure; friable; 3 percent worm casts; fragments; clear wavy boundary. Lab sample # 40A17917
    B21—23 to 43 centimeters (9.1 to 16.9 inches); brown (10YR 4/3) silty clay loam; weak coarse prismatic parts to strong very fine and fine subangular blocky structure; 21 percent worm casts; fragments; clear wavy boundary. Lab sample # 40A17918
    B22—43 to 69 centimeters (16.9 to 27.2 inches); brown (10YR 4/3) silty clay loam; moderate medium and coarse prismatic parts to weak very fine and fine subangular blocky structure; friable; 3 percent worm casts; fragments; gradual wavy boundary. Lab sample # 40A17919
    B23—69 to 107 centimeters (27.2 to 42.1 inches); light olive brown (2.5Y 5/4) silty clay loam; yellowish brown (10YR 5/6) and 21 percent gray (10YR 5/1) medium distinct mottles; weak coarse prismatic parts to weak very fine and fine subangular blocky structure; very friable; 21.0 fine pores; 30 percent black stains in root channels and/or pores; fragments; gradual wavy boundary. Lab sample # 40A17920
    B3—107 to 137 centimeters (42.1 to 53.9 inches); light olive brown (2.5Y 5/4) silt loam; yellowish brown (10YR 5/6) and 21 percent gray (10YR 5/1) medium mottles; weak coarse prismatic parts to weak very fine subangular blocky structure; very friable; 21.0 very fine pores; 75 percent black stains; 3 percent worm casts throughout; fragments. Lab sample # 40A17921
    C—137 to 165 centimeters (53.9 to 65.0 inches); light olive brown (2.5Y 5/4) silt loam; gray (10YR 5/1) and yellowish brown (10YR 5/6) mottles; massive; very friable; 3.0 pores; fragments. Lab sample # 40A17922. The B3 and C horizons appeared very similar except for slightly developed structure aggregates in the B3; they appeared to have a faint coating in places but were difficult to recognize as blocks even in the B3 horizon. The mottling is similar in the B3 and C except the C has somewhat more gray mottlings and the manganese specks and streaks were more numerous and somewhat larger