Abstract
Soil is an absorber of different pollutants from water and the atmosphere. Their fate and migration depend, besides the external conditions, also on the conditions and the properties of the soil itself. One of the most important soil features in this context is soil redox status which decidedly influences solubility and the biotransformations of pollutants. The dynamics of the variation of the oxidation — reduction conditions depend on redox buffering capacity being an intrisnic property of a given soil.
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