Abstract
The stabilities of the humus in different soil types (a soddy-podzolic soil from Moscow oblast, a deep typical chernozem from Kursk oblast, and a typical sierozem) have been compared on the basis of long-term studies of the composition, structural features, and properties of the humus acids formed under contrasting climatic conditions. The transformation features of the humic substances under agrogenic impacts of different intensities and durations have been studied by the example of a soddy-podzolic soil as a soil susceptible to environmental changes. The features of degradation of the humus quality and their manifestation at different levels of the structural organization of the humus system have been characterized.
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