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Podsolisation is an extreme form of leaching which causes the eluviation of iron and aluminium sesquioxides. The process generally occurs in areas where
Podsolisation
red colour of many tropical soils. Ferrallitisation is the reverse of podsolisation, where silica remains and the iron and aluminum are removed. In tropical
Ferrallitisation
Deterioration of rocks and minerals through exposure to the elements
compounds can easily affect surrounding rocks and soils, and may lead to podsolisation of soils. The symbiotic mycorrhizal fungi associated with tree root
Weathering
Landform in Lower Saxony, Germany
far as the iron buffer-region at pH 3, which initiates the process of podsolisation. Soil life is severely damaged, which results in a hard layer of earth
Lüneburg_Heath
Forest in Russia
different soil types are distinguished. They differ on the degree of podsolisation and the humus content. All floors of the Forest on the Vorskla are based
Worskla_Forest
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