IDENTIFIERS

  • Current Taxon Name (Soil Name): Eldridge
  • OSD
  • Series Extent
  • User Site ID: S1955NH017003
  • User Pedon ID: 55NH017003
  • Lab Information:
  • Certified Lab Pedon Description - yes
  • Lab Source ID - SSL
  • Lab Pedon # - 40A0476
  • NCSS Pedon Lab Data NASIS Record ID - 33004
  • Print Date: 11/23/2024

    • 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: 43.1699982
  • Std. Longitude: -70.9263916
  • Datum: WGS84
  • Location Description: Strafford County, New Hampshire. From a pit on the Adams feet field on the grass plots of the Agronomy Department, University of New Hampshire. This field is located approximately half-way between Dover and Durham, New Hampshire.
  • State: New Hampshire
  • County: NH017—Strafford
  • MLRA: 144A—New England and Eastern New York Upland, Southern Part
  • Non-MLRA Soil Survey Area: NH017—Strafford County, New Hampshire

    • PEDON

  • Describers Name: A.B. Prince, H.R. Adams, D. van der Voet, W. H. Lyford.
  • Current Taxonomic Class: Sandy over loamy, mixed, active, nonacid, mesic Oxyaquic Udorthents
  • Current Taxon Kind: taxadjunct
  • Pedon Type: taxadjunct to the series
  • Pedon Record Orgin: Converted from PDP 3.x
  • Pedon #: 3
  • Correlated Information:
  • Soil Name - Eldridge
  • PSC - 25 to 100 cm.
  • Classificaton Date - 7/10/2013
  • Classifier - Marissa Theve
  • Soil Taxonomic Edition - eleventh edition
  • Moisture Class - udic
  • Moisture Subclass - oxyaquic
  • Sampled As Information:
  • Soil Name - Heinsburg
  • Classificaton Date - 7/7/1956
  • Dynamic Soil Properties:
  • Pedoderm Loose Cover Indicator - no
  • Hydric: no
  • Certification Status: certified
  • QC Status: not reviewed


    • SITE

  • Surface Fragments:
  • Benchmark Soil?: no

    • VEGETATION

    SITE OBSERVATION

  • Observation Date: 7/7/1956 (actual site observation date)
  • Surface Cover Properties:
  • 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

    lithologic discontinuity

    0—25

    61—102

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    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

    3

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    Ap—0 to 25 centimeters (0.0 to 9.8 inches); brown (10YR 4/3) loamy sand; weak fine granular structure; friable; 21.0 roots; fragments. Lab sample # 40A03555. There is little tendency for the soil to clod when plowed or even when dug from the profile.
    Bw1—25 to 51 centimeters (9.8 to 20.1 inches); yellowish brown (10YR 5/6) sand; single grain; very friable; 3.0 roots; fragments; very strongly acid, pH 5.0, unspecified. Lab sample # 40A03556. This perhaps is an eroded soil and this particular horizon may be the original B22. As much as 8 or 10 inches may have been lost judging solely on the basis of an expected stronger B21 color for the noneroded soil.
    Bw2—51 to 61 centimeters (20.1 to 24.0 inches); light olive brown (2.5Y 5/4) very fine sandy loam; massive parts to weak platy; friable; brittle; 3.0 roots; fragments; slightly acid, pH 6.4, unspecified. Lab sample # 40A03557. At the time of sampling, this horizon was definitely more moist than the horizon above. This horizon contains more roots than the horizon below.
    2C—61 to 102 centimeters (24.0 to 40.2 inches); olive gray (5Y 4/2) clay loam; platy structure; firm, nonsticky, slightly plastic; 3.0 medium pores; reddish brown (5YR 4/4) coats on faces of peds; fragments. Lab sample # 40A03558. Coats are 1/8-1/4 inch, in size and are apparently around most of the weak 1/8-1/4 angular blocks of which this horizon is composed. Pores are glazed and irregular in shape. The red coats, themselves, are not especially glazed and perhaps are iron oxide rather than silicate clays. Roots are throughout, not in any particular location. No tendency for prismatic structure was noted. No gray mottles.; discontinuous - phpvsfiid 1091793; discontinuous - phpvsfiid 1091793