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  2. Podzol - Wikipedia

    en.wikipedia.org/wiki/Podzol

    The colour is strongest in the upper part, and change at a depth of 50 to 100 centimetres (20 to 40 in) progressively to the part of the soil that is mainly not affected by processes; that is the parent material. The soil profiles are designated by the letters A , E (eluviated soil), B and C (parent material).

  3. File:Podzol A soils.svg - Wikipedia

    en.wikipedia.org/wiki/File:Podzol_A_soils.svg

    You are free: to share – to copy, distribute and transmit the work; to remix – to adapt the work; Under the following conditions: attribution – You must give appropriate credit, provide a link to the license, and indicate if changes were made.

  4. Brown podzolic - Wikipedia

    en.wikipedia.org/wiki/Brown_podzolic

    The result is that leaching of the soil profile occurs; in which mobile chemicals are washed out of the topsoil, or A horizon, and accumulate lower down, in the B horizon. These soils have large amounts (more than 5%) of organic carbon in the surface horizon, which is therefore dark in colour.

  5. Canadian system of soil classification - Wikipedia

    en.wikipedia.org/wiki/Canadian_system_of_soil...

    Podzol soil monolith with inconspicuous eluviation; coarse granular structure of top mineral horizon (Ahe or Ap) is evidence of earthworm invasion. These acid soils have a B horizon containing accumulations of amorphous materials composed of humified organic matter associated with aluminum and iron.

  6. USDA soil taxonomy - Wikipedia

    en.wikipedia.org/wiki/USDA_soil_taxonomy

    About 1,000 soil subgroups are defined in the United States. [6] A soil family category is a group of soils within a subgroup and describes the physical and chemical properties which affect the response of soil to agricultural management and engineering applications. The principal characteristics used to differentiate soil families include ...

  7. Soil morphology - Wikipedia

    en.wikipedia.org/wiki/Soil_morphology

    Field equipment for soil description. Soil morphology is the branch of soil science dedicated to the technical description of soil, [1] particularly physical properties including texture, color, structure, and consistence. Morphological evaluations of soil are typically performed in the field on a soil profile containing multiple horizons. [2]

  8. Berkshire (soil) - Wikipedia

    en.wikipedia.org/wiki/Berkshire_(soil)

    Berkshire soil series is the name given to a well-drained loam or sandy loam soil which has developed on glacial till in parts of southern Quebec, eastern New York State and New England south to Massachusetts.

  9. Charlottetown (soil series) - Wikipedia

    en.wikipedia.org/wiki/Charlottetown_(soil_series)

    Charlottetown soil series is the name given to a deep fine sandy loam soil which has developed under forest vegetation on glacial till. This series occurs only on Prince Edward Island , where it is widespread and so important for agriculture that it has been designated as the Provincial Soil.