Ferrallitisation is the process in which rock is changed into a soil consisting of clay (kaolinite) and sesquioxides, in the form of hydrated oxides of iron and aluminium. In humid tropical areas, with consistently high temperatures and rainfall for all or most of the year, chemical weathering rapidly breaks down the rock. This at first produces clays which later also break down to form silica. The silica is removed by leaching and the sesquioxides of iron and aluminium remain, giving the characteristic red colour of many tropical soils. Ferrallitisation is the reverse of podsolisation, where silica remains and the iron and aluminum are removed. In tropical rain forests with rain throughout the year, ferrallitic soils develop. In savanna areas, with altering dry and wet climates, ferruginous soils occur.
Further reading
- Lavelle, P.; Spain, A. (28 February 2002). Soil Ecology. Springer. p. 190. ISBN 9780792371236. Retrieved 28 October 2013.
- Kolay, A.K. (July 10, 2007). Soil Genesis, Classification Survey and Evaluation, Volume 1. New Delhi: Atlantic Publishers and Distributors. pp. 191ff. ISBN 9788126908028. Retrieved 28 October 2013.
 | This soil science–related article is a stub. You can help Wikipedia by expanding it. |
 | This geochemistry article is a stub. You can help Wikipedia by expanding it. |
This page was last edited on 18 July 2023, at 17:33