Abstract
The differentiation of the soils under study in terms of the bulk chemical composition of the solid phase was mainly manifested along the profile and decreased with depth, because it was primarily ensured by the different aspects of the biogenic accumulative processes. The bulk composition parameters of the solid phase were of higher information value for determining the type of soil horizon, and the composition of the water-soluble compounds (in water extracts and natural soil solutions) reflected the features characteristic of the soil type.
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