IDENTIFIERS

  • Current Taxon Name (Soil Name): Neotoma
  • OSD
  • Series Extent
  • User Site ID: 1958OH073006
  • User Pedon ID: 1958-OH073-006
  • Lab Information:
  • Certified Lab Pedon Description - no
  • Lab Source ID - OHSTATE
  • Lab Pedon # - HO-006
  • NCSS Pedon Lab Data NASIS Record ID - 70323
  • Print Date: 5/20/2024
  • LOCATION

  • Location Description: Neotoma Valley; center of Sec. 16, Goodhope Twp. 120 ft. upslope from center of OSU botany weather station No. 1(mixed mesophytic quadrat).
  • State: Ohio
  • County: OH073—Hocking
  • PEDON

  • Describers Name: r. h. finney, Petro , Riemenschneider
  • Current Taxonomic Class: Loamy-skeletal, mixed, mesic Ultic Hapludalfs
  • Pedon Record Orgin: NASIS
  • Correlated Information:
  • Soil Name - Neotoma
  • Classificaton Date - 5/4/2012
  • Dynamic Soil Properties:
  • Pedoderm Loose Cover Indicator - no
  • Hydric: no


  • SITE

  • Parent Material: Colluvium; Wisconsinan lacustrine
  • Geomorphic Component Hills: nose slope
  • Drainage Class: moderately well
  • Geology: Wisconsinan formation.
  • Surface Fragments:
  • Benchmark Soil?: no
  • VEGETATION

    SITE OBSERVATION

  • Observation Date: 6/25/1958 (actual site observation 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
  • 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

    30

    280.4

    45

    Oe—0 to 4 centimeters (0.0 to 1.6 inches); fragments. Partially decomposed leaf litter, slightly matted in place. Not sampled.
    A—4 to 17 centimeters (1.6 to 6.7 inches); very dark grayish brown (10YR 3/2), very dark grayish brown (10YR 3/2), dry; Error; moderate medium granular structure; very friable; 10 percent by volume nonflat indurated unspecified fragments; slightly acid, pH 6.2; abrupt wavy boundary. Lab sample # OSU0007473
    BA—17 to 27 centimeters (6.7 to 10.6 inches); brown (7.5YR 4/4), brown (10YR 5/3), dry; Error; weak fine subangular blocky structure; very friable; 10 percent by volume nonflat indurated unspecified fragments; moderately acid, pH 5.9; gradual smooth boundary. Lab sample # OSU0007474
    B1—27 to 44 centimeters (10.6 to 17.3 inches); brown (7.5YR 4/4), 10YR 4 (10YR/4), dry; Error; weak fine and medium subangular blocky structure; very friable; 15 percent by volume nonflat indurated unspecified fragments; strongly acid, pH 5.4; diffuse boundary. Lab sample # OSU0007475
    B2—44 to 62 centimeters (17.3 to 24.4 inches); brown (7.5YR 4/4), light yellowish brown (10YR 6/4), dry; Error; weak medium subangular blocky structure; very friable; 20 percent by volume nonflat indurated unspecified fragments; very strongly acid, pH 5.0; gradual boundary. Lab sample # OSU0007476
    B3—62 to 75 centimeters (24.4 to 29.5 inches); yellowish brown (10YR 5/6) and brown (7.5YR 4/4), light yellowish brown (10YR 6/4), dry; Error; weak coarse subangular blocky structure; friable; 40 percent by volume nonflat indurated unspecified fragments; very strongly acid, pH 4.9; gradual boundary. Lab sample # OSU0007477
    2BC1—75 to 88 centimeters (29.5 to 34.6 inches); light yellowish brown (10YR 6/4), light yellowish brown (10YR 6/4), dry; Error; weak coarse subangular blocky structure; firm; 50 percent by volume nonflat indurated unspecified fragments; very strongly acid, pH 4.8; diffuse boundary. Lab sample # OSU0007478. Appears to be zone of mixing of sandstone and silts.
    2BC2—88 to 113 centimeters (34.6 to 44.5 inches); light yellowish brown (10YR 6/4) Error; massive; firm; light gray (10YR 7/2), moist, masses of reduced iron and reddish yellow (7.5YR 6/8), moist, masses of oxidized iron; 50 percent by volume nonflat indurated unspecified fragments; very strongly acid, pH 4.6; diffuse boundary. Lab sample # OSU0007479. This material appears to be of lacustrine or loessal origin.