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  1. May 1, 2011 · Soils with some form of ortstein were classified primarily into four soil temperature classes, including frigid (38 soil series), mesic (20), hyperthermic (16), and isomesic (7). The dominant mineralogy class was mixed (50 soil series), followed by siliceous (21), isotic (15), and amorphic (3).

    • James Bockheim
    • 19
    • 2011
    • 01 May 2011
  2. Jan 1, 2014 · Origin: Ortstein is usually a hard, partly or entirely cemented illuvial horizon B of podzol or gley-podzol soils, formed as a result of illuviation of aluminum, iron, manganese, and humus compounds from the overlying horizons.

    • Jacek Chodorowski
    • jchodor@poczta.umcs.lublin.pl
  3. Soils of the Podzolic order are defined based on a combination of morphological and chemical criteria of the B horizons. Soils of the order must meet all the following morphological limits and those specified under either 1 or 2 of the chemical limits.

  4. May 1, 2011 · Soils with ortstein occur on lesser slopes (p = 0.001) and at lower elevations (p = 0.015) than soils without ortstein. The lower depth boundary and thickness of the spodic horizon were significantly greater (p = 0.001) in soils with ortstein than in those without ortstein.

    • James Bockheim
    • 2011
    • ACKNOWLEDGMENTS
    • Soil series
    • Placudands
    • Typic Placudands

    Th is project was supported by grants from the National Science Foundation and the Huron Mountain Wildlife Foundation. Th e author acknowledges the helpful comments of three anonymous reviewers and the associate editor.

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    Typic Haplorthods Lamellic Haplorthods Alfi c Haplorthods Entic Haplorthods Aquic Haplorthods Aquentic Haplorthods Typic Placorthods

    Success, Constable, Duane, Bandon, Battydoe, Furlong, Guard Lake, Kaleva, Kalkaska, Colton, Redstone Blue Lake, Island Lake Cheboygan, Keweenaw Duel, East Lake, Hartwick, Ishpeming, Ocqueoc Flackville, Waumbek Occur Kahanui Salmonriver

  5. May 1, 2011 · Soils with ortstein occur on lesser slopes (p = 0.001) and at lower elevations (p = 0.015) than soils without ortstein. The lower depth boundary and thickness of the spodic horizon were...

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  7. Jan 1, 2014 · Soils bearing ortstein and placic horizons are used for cranberry and blueberry culture, truck crops, and forestry operations but have many limitations for other kinds of land use. The factors influencing the distribution and formation of these cemented horizons are poorly understood.

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