IDENTIFIERS

  • Current Taxon Name (Soil Name): Canina
  • OSD
  • Series Extent
  • Local Phase: silt loam
  • User Site ID: S2004OK007003
  • User Pedon ID: S2004OK007003
  • Lab Information:
  • Certified Lab Pedon Description - yes
  • Lab Source ID - KSSL
  • Lab Pedon # - 04N1155
  • NCSS Pedon Lab Data NASIS Record ID - 16912
  • Print Date: 2/17/2025

    • 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: 36.5265007
  • Std. Longitude: -100.4944687
  • Datum: WGS84
  • Township: 1N
  • Range: 24E
  • Section: 29
  • PLSS Details: NE1/4
  • Country: US—United States
  • State: Oklahoma
  • County: OK007—Beaver
  • MLRA: 77A—Southern High Plains, Northern Part
  • Regional Office: SC—South Central
  • Non-MLRA Soil Survey Area: OK007—Beaver County, Oklahoma

    • PEDON

  • Describers Name: Steven McGowen, Jim Ford, Troy Collier, Charles Cail, Richard Gelnar, Tyson Morley, T. Craig Byrd
  • Current Taxonomic Class: Fine-silty, mixed, superactive, mesic Calcidic Haplustalfs
  • Current Taxon Kind: series
  • Pedon Type: OSD pedon
  • Pedon Purpose: laboratory sampling site
  • Pedon Record Orgin: NASIS
  • Correlated Information:
  • Soil Name - Canina
  • PSC - 33 to 83 cm.
  • Classificaton Date - 2/21/2008
  • Classifier - Steven McGowen
  • Soil Taxonomic Edition - tenth edition
  • Moisture Class - ustic
  • Moisture Subclass - aridic (torric)
  • Sampled As Information:
  • Soil Name - Canina
  • Classificaton Date - 9/14/2004
  • Dynamic Soil Properties:
  • Erosion Class - 0
  • Pedoderm Loose Cover Indicator - no
  • Hydric: no
  • Certification Status: certified
  • QC Status: level 1
  • QA Status: not reviewed


    • SITE

  • Landscape: upland
  • Landform: parna dune
  • Geomorphic Component Flats: rise
  • Hill Slope Profile: summit
  • Slope Position: upper third
  • Slope Complexity: simple
  • Slope Shape Across: convex
  • Slope Shape Down: convex
  • Geology: Undifferentiated member of the Loess formation.
  • Surface Fragments:
  • Benchmark Soil?: no

    • VEGETATION

    SITE OBSERVATION

  • Observation Date: 9/14/2004 (actual site observation date)
  • Air Photo ID: 134
  • Surface Cover Properties:
  • Site Obs. Cover Kind 1 - grass/herbaceous cover
  • Site Obs. Cover Kind 2 - rangeland, grassland
  • Pedoderm Loose Cover Indicator - no
  • Drained? - no
  • Bedded Soil? - no
  • Forest Plantation? - no
  • Current Weather - sunny
    • Pedon Diagnostic Features
    Feature Kind Feature Depth L-H Feature Thickness L-RV-H
    cm

    ochric epipedon

    argillic horizon

    0—33

    33—103

    —33—

    —-
    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

    1.5

    —

    —

    855

    —

    90

    508

    —

    185

    14

    —

    —

    15

    —

    —

    —

    —

    —

    —

    —
    A1—0 to 15 centimeters (0.0 to 5.9 inches); grayish brown (10YR 5/2) rubbed, very dark grayish brown (10YR 3/2) rubbed, moist; silt loam; moderate coarse prismatic parts to moderate medium granular, and moderate coarse prismatic parts to moderate fine granular structure; soft, very friable; 3.0 very fine roots and 7.0 fine roots; 0.5 medium and 0.5 fine pores; 10 percent worm casts and 1 percent fine threadlike carbonate masses on surfaces along pores; fragments; strong effervescence, by hcl, 1n; clear smooth boundary.; observed in trench
    A2—15 to 33 centimeters (5.9 to 13.0 inches); brown (10YR 5/3) broken face, brown (10YR 4/3) broken face, moist; silt loam; moderate coarse prismatic parts to moderate medium subangular blocky structure; soft, very friable; 0.5 very fine roots and 3.0 fine roots; 0.5 fine pores; 10 percent worm casts and 1 percent fine threadlike carbonate masses on surfaces along root channels and 1 percent fine carbonate nodules in matrix; fragments; violent effervescence, by hcl, 1n; clear smooth boundary.; observed in trench
    Btk1—33 to 47 centimeters (13.0 to 18.5 inches); brown (7.5YR 5/4) broken face, brown (7.5YR 4/4) broken face, moist; silty clay loam; moderate coarse prismatic parts to moderate medium subangular blocky structure; slightly hard, friable; 3.0 very fine roots and 0.5 medium roots; 0.5 fine pores; 15 percent distinct clay films on all faces of peds; 10 percent worm casts and 1 percent fine carbonate masses on surfaces along root channels and 10 percent medium carbonate masses on surfaces along root channels; fragments; violent effervescence, by hcl, 1n; clear smooth boundary.; observed in trench. discontinuous - phpvsfiid 269263; discontinuous - phpvsfiid 269263
    Btk2—47 to 68 centimeters (18.5 to 26.8 inches); light brown (7.5YR 6/4) broken face, brown (7.5YR 5/4) broken face, moist; silty clay loam; strong medium prismatic parts to moderate medium subangular blocky, and strong coarse prismatic parts to moderate medium subangular blocky structure; slightly hard, friable; 0.5 fine roots; 0.5 fine pores; 35 percent prominent organic stains on all faces of peds and 35 percent prominent clay films on all faces of peds; 1 percent worm casts and 1 percent fine carbonate masses on surfaces along root channels and 10 percent medium carbonate masses in matrix; fragments; violent effervescence, by hcl, 1n; gradual smooth boundary.; observed in trench. continuous - phpvsfiid 269043; continuous - phpvsfiid 269044; continuous - phpvsfiid 269043; continuous - phpvsfiid 269044
    Btk3—68 to 103 centimeters (26.8 to 40.6 inches); brown (7.5YR 5/4) broken face, pink (7.5YR 7/4) broken face, moist; silt loam; strong medium prismatic parts to moderate medium subangular blocky, and strong coarse prismatic parts to moderate medium subangular blocky structure; slightly hard, friable; 0.1 medium roots and 0.1 fine roots; 0.5 medium and 3.0 fine pores; distinct silt coats on top faces of peds and 35 percent distinct clay films on all faces of peds and 35 percent faint organic stains on all faces of peds; 1 percent worm casts and 1 percent fine threadlike carbonate masses on surfaces along root channels and 1 percent fine carbonate masses in matrix; fragments; violent effervescence, by hcl, 1n; gradual smooth boundary.; observed in trench. silt caps occur on horzintal faces of peds <1mm thick.; continuous - phpvsfiid 269046; discontinuous - phpvsfiid 269047; discontinuous - phpvsfiid 269078; continuous - phpvsfiid 269046; discontinuous - phpvsfiid 269047; discontinuous - phpvsfiid 269078
    Btk4—103 to 138 centimeters (40.6 to 54.3 inches); brown (7.5YR 5/4) broken face, pink (7.5YR 7/4) broken face, moist; silty clay loam; weak coarse prismatic parts to weak medium subangular blocky, and weak medium prismatic parts to weak medium subangular blocky structure; slightly hard, friable; 0.1 very fine roots; 0.5 medium and 3.0 fine pores; 15 percent faint clay films on all faces of peds; 10 percent fine carbonate nodules in matrix and 1 percent fine threadlike carbonate masses on surfaces along root channels; fragments; violent effervescence, by hcl, 1n; diffuse smooth boundary.; observed in trench. Horizon is composed of medium and fine sand sized carbonates from an eolian source. Clay films occur on prism faces.; discontinuous - phpvsfiid 269048; discontinuous - phpvsfiid 269048
    BCk—138 to 203 centimeters (54.3 to 79.9 inches); light brown (7.5YR 6/4) broken face, pink (7.5YR 7/4) broken face, moist; stratified stratified silty clay loam; weak medium prismatic structure; slightly hard, friable; 0.1 very fine roots; 0.5 medium and 3.0 fine pores; 1 percent fine threadlike carbonate masses on surfaces along root channels; fragments; violent effervescence, by hcl, 1n.; observed in trench. Structure parts to horizontally stratified bedded parna dune material of medium and fine sand sized carbonate particles. No evidence of cross bedding in the stratification. Thin silt beds interbedded with very fine granular fine and medium sand sized carbonates and coarse siltsized aggregates. Coarse sands comprise 1-2% by volume.