The classification is based mainly on soil morphology as an expression pedogenesis.
2.
The classification is based mainly on soil morphology as an expression of pedogenesis.
3.
Pedogenesis is studied as a branch of soil geography ) and past ( paleopedology ) geologic periods.
4.
Porosity in finer material below the aggregating influence of pedogenesis can be expected to approximate this value.
5.
They can contribute to processes such as pedogenesis, seed dispersal, and either increases or decreases in biodiversity.
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Soil series consist of pedons that are grouped together because of their similar pedogenesis, soil chemistry, and physical properties.
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Differing concepts of pedogenesis, and differences in the significance of morphological features to various land uses can affect the classification approach.
8.
This dehydration or " aging " process has been found to be intimately associated with pedogenesis in alluvial floodplains and desert environments.
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A rate of pedogenesis of 1 / 10 mm per year is in order of magnitude of the global soil production estimates .,
10.
The product of pedogenesis, it commonly occurs as dark red redox concretions that usually form platy, polygonal, or reticulate patterns.
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