Pedogenesis or soil evolution (formation) is the process by which soil is created. It is the major topic of the science of pedology, whose other aspects include the soil morphology, classification (taxonomy) of soils, and their distribution in nature, present and past (soil geography and paleopedology).
Climate regulates soil formation. Soils are more developed in areas with higher rainfall and more warmth. As the rate of chemical weathering increases 2-3 times when the temperature increases 10 degree cel..
The organisms living in and on the soil form distinct soil types. Coniferous forests have acidic leaf litter and form Inceptisols. Mixed or deciduous forests leave a larger layer of humus, changing the elements leached and accululated in the soil, forming Alfisols. Praries have very high humus accumulation, creating a dark, thick A horizon characteristic of Mollisols.
The rock from which soil is formed is called parent material. The main types are: eolian, glacial till, glacial outwash, alluvium, lacustrine depositional parent material and residual parent material, or bedrock. Hans Jenny (pedologist) uses the following formula for understanding soil formation:
s = f (cl, o, r, p, t, ...)
where s - soil properties; cl - regional climate; o - potential biota, r - topography; p - parent material; t - time; ... - additional variables.
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"Pedogenesis".
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