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  1. Examples include artifacts, buried soil, artificial drainage, component, correlation, horizon, and normal year. This glossary also contains a selection of taxonomic class terms from great groups, subgroups, or families. Examples include Arenic, Leptic, Ombroaquic, Pachic, and Rhodic.

  2. Jan 1, 2014 · Ortstein (German: ort-place, stein-stone) is defined by Soil Survey Staff as all or part of the spodic horizon, when moist, it is at least weakly cemented into a massive horizon that is present in more than half of each pedon.

    • Jacek Chodorowski
    • jchodor@poczta.umcs.lublin.pl
  3. May 1, 2011 · According to Soil Taxonomy (ST), ortstein consists of spodic materials and occurs in a layer that is ≥25 mm thick and ≥50% cemented (Fig. 1A-1C; 34). In ST, ortstein is both a diagnostic subsurface horizon and the only rupture-resistance class recognized in the system.

  4. Jan 1, 2014 · According to Soil Taxonomy (ST), ortstein consists of spodic materials and occurs in a layer that is ≥25 mm thick and ≥50 % cemented (Soil Survey Staff 2010) (Fig. 18.1). In ST, ortstein is both a diagnostic subsurface horizon and the only rupture-resistance class recognized in the system.

    • James G. Bockheim
    • 2014
  5. A classification system is needed to organize knowledge on the thousands of natural bodies known as soils. Pedon is the smallest unit of soil that embodies the essential characteristics of a soil. Polypedon is a laterally contiguous group of similar pedons. It is a soil individual.

    • 547KB
    • 8
  6. Rationale of Soil Taxonomy in Canada. The nature of soil; Nature and purpose of soil classification; Misconceptions about soil taxonomy; Attributes of the Canadian system; Bases of criteria for defining taxa at various categorical levels; Relationship of taxonomic classes to environments; Relationship of the Canadian system to other systems of ...

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  8. May 1, 2011 · According to Soil Taxonomy (ST), ortstein consists of spodic materials and occurs in a layer that is ≥25 mm thick and ≥50 % cemented (Soil Survey Staff 2010) (Fig. 18.1).

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