Pedogenesis

CLIMATE

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..

ORGANISMS

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 .

PARENT MATERIAL

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.

REFERENCES

Buol, Stanley W., F.D. Hole and R.W. McCracken. 1997. Soil Genesis and Classification, 4th ed. Iowa State Univ. Press, Ames ISBN 0-81382-873-2

Hole Francis D., J.B. Campbell. 1985. Soil landscape analysis. Totowa Rowman & Allanheld, 214 p. ISBN 0-86598-140-X

Jenny, Hans (1994) Factors of Soil Formation. A System of Quantitative Pedology. New York: Dover Press. (Reprint, with Foreword by R. Amundson, of the 1941 McGraw-Hill publication). pdf file format.

Pluijm, Ben van der, et al. Fall, 2005. Soils, Weathering, and Nutrients from the Global Change 1 Lectures. University of Michigan. Url last accessed on 2006 - 04-18

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Pedogenesis