Soil production function

From Wikipedia, the free encyclopedia

Soil production function refers to the rate of bedrock weathering into soil as a function of soil thickness.

300px Soil production function

A general model suggested that the rate of physical weathering of bedrock (de/dt) can be represented as an exponential decline with soil thickness:

de/dt = P_0 \exp{[-k h]}\

where h is soil thickness [m], P0 [mm/year] is the potential (or maximum) weathering rate of bedrock and k [m-1] is an empirical constant.

The reduction of weathering rate with thickening of soil is related to the exponential decrease of temperature amplitude with increasing depth below the soil surface, and also the exponential decrease in average water penetration (for freely-drained soils). Parameters P0 and k are related to the climate and type of parent materials. Arjun Heimsath found the value of P0 ranges from 0.08 to 2.0 mm/year for sites in Northern California, and 0.05- 0.14 mm/year for sites in Southeastern Australia. Meanwhile values of k do not vary significantly ranging from 2 – 4 m-1.

A number of landscape evolution models have adopted the so-called humped model. This model dates back to Grove Karl Gilbert (G.K. Gilbert)'s Report on the Geology of the Henry Mountains (1877). Gilbert reasoned that the weathering of bedrock was fastest under an intermediate thickness of soil and slower under exposed bedrock or under thick mantled soil. This is because chemical weathering requires the presence of water. Under thin soil or exposed bedrock water tends to run off, reducing the chance of the decomposition of bedrock.

[edit] See also

[edit] References

  • Ahnert, F., 1977. Some comments on the quantitative formulation of geomorphological process in a theoretical model. Earth Surface Processes 2, 191-201.
  • Heimsath, A.M., Dietrich, W.E. Nishiizumi, K., Finkel, R.C., 1997. The soil production function and landscape equilibrium. Nature 388, 358-388.
  • Humphreys, G. S., and Wilkinson, M. T., 2007, The soil production function: a brief history and its rediscovery: Geoderma, v. 139, p. 73-78.[1]
  • Wilkinson, M. T., Chappell, J., Humphreys, G. S., Fifield, K., Smith, B., and Hesse, P. P., 2005, Soil production in heath and forest, Blue Mountains, Australia: influence of lithology and palaeoclimate: Earth Surface Processes and Landforms, v. 30, p. 923–934.[2]
  • Wilkinson, M. T., and Humphreys, G. S., 2005, Exploring pedogenesis via nuclide-based soil production rates and OSL-based bioturbation rates: Australian Journal of Soil Research, v. 43, p. 767-779.[3]