IDENTIFIERS

  • Current Taxon Name (Soil Name): Perry
  • OSD
  • Series Extent
  • User Site ID: S1985LA021003
  • User Pedon ID: 85LA021003
  • Lab Information:
  • Certified Lab Pedon Description - no
  • Lab Source ID - SSL
  • Lab Pedon # - 85P0751
  • NCSS Pedon Lab Data NASIS Record ID - 57017
  • 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: 32.2402763
  • Std. Longitude: -92.0527802
  • Datum: WGS84
  • Township: 14N
  • Range: 4E
  • Section: 34
  • PLSS Details: SW 1/4 NW 1/4
  • Location Description: 160 steps E of field road intersection, and 110 steps N of field road.
  • State: Louisiana
  • County: LA021—Caldwell
  • MLRA: 131—Southern Mississippi Valley Alluvium
  • PEDON

  • Describers Name: William H. Boyd, Gail Bowden, Emile Williams
  • Current Taxonomic Class: Very-fine, smectitic, nonacid, thermic Vertic Haplaquepts
  • Current Taxon Kind: series
  • Pedon Purpose: full pedon description
  • Pedon Record Orgin: Converted from SSL-CMS data
  • Pedon #: 3
  • Correlated Information:
  • Soil Name - Perry
  • PSC - 25 to 100 cm.
  • Classificaton Date - 7/11/2007
  • Moisture Class - aquic
  • Sampled As Information:
  • Soil Name - Perry
  • Taxonomic Class - Very-fine, montmorillonitic, nonacid, thermic Vert
  • Taxon Kind - series
  • Classificaton Date - 10/1/1985
  • Moisture Class - aquic
  • Dynamic Soil Properties:
  • Erosion Class - 1
  • Pedoderm Loose Cover Indicator - no
  • Hydric: no


  • SITE

  • Landscape: river valley
  • Landform: abandoned channel
  • Anthropogenic Feature: leveled land
  • Slope Shape Down: linear
  • Drainage Class: somewhat poorly
  • Surface Fragments: 0.00 percent
  • Benchmark Soil?: no
  • VEGETATION

    SITE OBSERVATION

  • Observation Date: 10/1/1985 (actual site observation date)
  • Microrelief Elevation: 1
  • Surface Cover Properties:
  • Site Obs. Cover Kind 1 - crop cover
  • Pedoderm Loose Cover Indicator - no
  • Drained? - no
  • Bedded Soil? - no
  • Forest Plantation? - no
  • Site Erosion Accelerated: water erosion
  • Pedon Diagnostic Features
    Feature Kind Feature Depth L-H Feature Thickness L-RV-H
    cm

    ochric epipedon

    cambic horizon

    0—13

    13—119

    —-

    —-

    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

    16

    132

    17

    16

    1Ap—0 to 13 centimeters (0.0 to 5.1 inches); dark grayish brown (10YR 4/2) interior clay; moderate fine subangular blocky structure; firm; 5.5 fine roots throughout; fragments; very strongly acid, pH 5.0, hellige-truog; clear wavy boundary. Lab sample # 85P03967; very moist when described;. Clay eontenct exceeds 60% in all horizons.; many fine roots throughout
    1Bw1g—13 to 33 centimeters (5.1 to 13.0 inches); gray (10YR 5/1) interior clay; 30 percent strong brown (7.5YR 5/6) medium prominent mottles; weak coarse subangular blocky structure; very sticky, very plastic; 0.5 very fine roots throughout; fragments; very strongly acid, pH 5.0, hellige-truog; clear wavy boundary. Lab sample # 85P03968; very moist when described;. On previous examinations of this pedon many intersecting slickensides were observed in horizons 2 and 3, recent heavy rains have saturated these upper horizons.; few very fine roots throughout; many medium prominent 7.5YR56 mottles
    1Bw2g—33 to 64 centimeters (13.0 to 25.2 inches); gray (10YR 5/1) interior clay; 30 percent strong brown (7.5YR 5/6) fine prominent and 30 percent strong brown (7.5YR 5/6) medium prominent mottles; weak coarse subangular blocky structure; very sticky, very plastic; 0.5 very fine roots throughout; fragments; strongly acid, pH 5.5, hellige-truog; clear wavy boundary. Lab sample # 85P03969; very moist when described;. few very fine roots throughout; many fine prominent 7.5YR56 mottles; many medium prominent 7.5YR56 mottles
    2BC—64 to 119 centimeters (25.2 to 46.9 inches); reddish brown (5YR 4/3) interior clay; 1 percent gray (10YR 5/1) fine prominent mottles; moderate medium subangular blocky structure; firm; 1 percent medium spherical carbonate concretions; fragments; violent effervescence, by hcl, unspecified; moderately alkaline, pH 8.0, hellige-truog; gradual wavy boundary. Lab sample # 85P03970; moist when described;. Intersecting slickensides and wedge shaped structural aggregates that have their long axis tilted are common and comprise about 50 to 80 percent of these two horizons. (4 and 5); few medium carbonate concretions concentrations; few fine prominent 10YR51 mottles; effervescence is discontinuous
    2C1—119 to 157 centimeters (46.9 to 61.8 inches); reddish brown (5YR 4/3) interior clay; 1 percent gray (10YR 5/1) fine prominent mottles; weak medium subangular blocky structure; firm; 11 percent coarse spherical carbonate concretions and 1 percent medium irregular carbonate masses; fragments; violent effervescence, by hcl, unspecified; moderately alkaline, pH 8.0, hellige-truog; gradual wavy boundary. Lab sample # 85P03971; moist when described;. few medium soft masses of carbonate concentrations; common coarse carbonate concretions concentrations; few fine prominent 10YR51 mottles; effervescence is discontinuous
    2C2—157 to 213 centimeters (61.8 to 83.9 inches); reddish brown (5YR 4/3) interior clay; 1 percent gray (10YR 5/1) fine prominent mottles; weak medium subangular blocky structure; firm; 11 percent coarse spherical carbonate concretions and 1 percent medium irregular carbonate masses; fragments; violent effervescence, by hcl, unspecified; moderately alkaline, pH 8.0, hellige-truog. Lab sample # 85P03972; moist when described;. Intersecting slickensides comprise aobut 30 to 50 percent of this horizon, which also contained a few tilted wedge shaped structural aggregates.; few medium soft masses of carbonate concentrations; common coarse carbonate concretions concentrations; few fine prominent 10YR51 mottles; effervescence is discontinuous