IDENTIFIERS

  • Current Taxon Name (Soil Name): Beetree
  • OSD
  • Series Extent
  • User Site ID: S2006TN133046
  • User Pedon ID: 2006TN133046
  • Lab Information:
  • Certified Lab Pedon Description - yes
  • Lab Source ID - SSL
  • Lab Pedon # - 07N0185
  • NCSS Pedon Lab Data NASIS Record ID - 19213
  • Print Date: 5/19/2024
  • 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: 36.2044220
  • Std. Longitude: -85.2301102
  • Datum: WGS84
  • Location Description: SAMPLE SITE ON CEDAR CHAPEL RD
  • Map Unit: SpF—Shelocta-Pineville complex, 20 to 70 percent slopes, very stony
  • Country: US—United States
  • State: Tennessee
  • County: TN133—Overton
  • MLRA: 122—Highland Rim and Pennyroyal
  • Non-MLRA Soil Survey Area: TN133—Overton County, Tennessee
  • 7.5 Minute USGS Quad: 36085-B2—Obey City, Tennessee
  • PEDON

  • Describers Name: Gabe Krantz
  • Current Taxonomic Class: Fine-loamy, siliceous, semiactive, thermic Typic Dystrudepts
  • Current Taxon Kind: series
  • Pedon Type: not classified to current taxon name
  • Pedon Purpose: research site
  • Pedon Record Orgin: PedonPC
  • Correlated Information:
  • Soil Name - Beetree (flagged as OSD)
  • PSC - 25 to 100 cm.
  • Classificaton Date - 7/2/2013
  • Soil Taxonomic Edition - eleventh edition
  • Moisture Class - udic
  • Moisture Subclass - typic
  • Sampled As Information:
  • Soil Name - PINEVILLE
  • Taxon Kind - series
  • Classificaton Date - 11/14/2006
  • Dynamic Soil Properties:
  • Erosion Class - 1
  • Pedoderm Loose Cover Indicator - no
  • Hydric: no


  • SITE

  • Parent Material: gravelly colluvium derived from sandstone and shale
  • Geomorphic Component Mountains: mountainflank, upper third
  • Hill Slope Profile: backslope
  • Slope Position: upper third
  • Slope Complexity: complex
  • Slope Shape Across: convex
  • Slope Shape Down: linear
  • Drainage Class: well
  • Flooding: none flooding
  • Ponding: none ponding
  • Geology: Pennington Formation formation.
  • Surface Fragments:
  • Benchmark Soil?: no
  • VEGETATION

    SITE OBSERVATION

  • Observation Date: 11/14/2006 (entry creation date)
  • Surface Cover Properties:
  • Site Obs. Cover Kind 1 - tree cover
  • Site Obs. Cover Kind 2 - hardwoods
  • Pedoderm Loose Cover Indicator - no
  • Drained? - no
  • Bedded Soil? - no
  • Forest Plantation? - no
  • Pedon Diagnostic Features
    Feature Kind Feature Depth L-H Feature Thickness L-RV-H
    cm

    ochric epipedon

    cambic horizon

    0—10

    18—187

    —-

    —-

    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

    495

    310

    A—0 to 10 centimeters (0.0 to 3.9 inches); very dark grayish brown (10YR 3/2) channery loam; 42 percent sand; 41 percent silt; 17 percent clay; weak medium granular structure; very friable; 6.0 medium roots throughout; 20 percent by volume flat subangular indurated 2-?-150 millimeter sandstone, unspecified fragments; neutral, pH 7.0, pH meter; clear smooth boundary. Lab sample # 07N01142; observed in cut
    BA—10 to 18 centimeters (3.9 to 7.1 inches); dark yellowish brown (10YR 4/4) channery loam; 43 percent sand; 40 percent silt; 17 percent clay; weak medium subangular blocky structure; very friable; 4.0 medium roots throughout; 20 percent by volume flat subangular indurated 2-?-150 millimeter sandstone, unspecified fragments; 51 Percent of Base Saturation; slightly acid, pH 6.5, pH meter; clear smooth boundary. Lab sample # 07N01143; observed in cut
    Bw1—18 to 55 centimeters (7.1 to 21.7 inches); dark yellowish brown (10YR 4/6) channery loam; 44 percent sand; 38 percent silt; 18 percent clay; moderate medium subangular blocky structure; friable; 4.0 medium roots throughout; 20 percent by volume flat subangular indurated 2-?-150 millimeter sandstone, unspecified fragments; 10 Percent of Base Saturation; 71 Percent of Aluminum Saturation; very strongly acid, pH 5.0, pH meter; gradual smooth boundary. Lab sample # 07N01144; observed in cut. Originally sampled as a Bt, however, lab data indicates clay percentages are the same throughout the upper 187 cm.
    Bw2—55 to 130 centimeters (21.7 to 51.2 inches); dark yellowish brown (10YR 4/6) channery loam; 42 percent sand; 39 percent silt; 19 percent clay; moderate medium subangular blocky structure; friable; 25 percent by volume flat subangular indurated 2-?-250 millimeter sandstone, unspecified fragments; 15 Percent of Base Saturation; 66 Percent of Aluminum Saturation; strongly acid, pH 5.1, pH meter; gradual smooth boundary. Lab sample # 07N01145; observed in cut. Originally sampled as a Bt, however, lab data indicates clay percentages are the same throughout the upper 187 cm.
    Bw3—130 to 187 centimeters (51.2 to 73.6 inches); reddish brown (5YR 4/4) fine sandy loam; 61 percent sand; 21 percent silt; 18 percent clay; moderate coarse subangular blocky structure; friable; 5 percent by volume flat subangular indurated 2-?-100 millimeter sandstone, unspecified fragments; 26 Percent of Base Saturation; 45 Percent of Aluminum Saturation; strongly acid, pH 5.2, pH meter; gradual smooth boundary. Lab sample # 07N01146; observed in cut. Originally sampled as a Bt, however, lab data indicates clay percentages are the same throughout the upper 187 cm.
    2BC—187 to 200 centimeters (73.6 to 78.7 inches); 75 percent yellowish brown (10YR 5/4) and 20 percent light olive brown (2.5Y 5/3) and 5 percent dark yellowish brown (10YR 4/6) cobbly loam; 27 percent sand; 50 percent silt; 23 percent clay; weak coarse subangular blocky structure; friable; 1 percent by volume rounded noncoherent cemented 2-?-10 millimeter iron-manganese concretions fragments and 30 percent by volume flat subangular indurated 2-?-250 millimeter sandstone, unspecified fragments; 20 Percent of Base Saturation; 59 Percent of Aluminum Saturation; strongly acid, pH 5.3, pH meter. Lab sample # 07N01147; observed in cut. Lincoln lab: "material change is suggested between the Bt1 and Bt2 horizons, another between the Bt3 and BC horizons"