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FORMATION OF SOILS ON LITOLOGICAL MONOMIAL PARENT ROCKS AND THEIR DEGRADATION UNDER THE INFLUENCE OF NATURAL AND ANTHROPOGENIC PROCESSES

Abstract

On example of sod-podzolic soils of Belarus formed on litological monomial moraine and loess-like loams, it is shown that modern soils are the final residual product of degradation of the parent substratum. At the given stage of pedogenesis development, in holocen time period, homogeneous moraine and loess-like loams degraded to loamy sand varieties under the influence of natural and anthropogenic processes.

For citations:


Lisitsa V.D., Bubnova T.V., Shul′gina S.V., Buben I.I. FORMATION OF SOILS ON LITOLOGICAL MONOMIAL PARENT ROCKS AND THEIR DEGRADATION UNDER THE INFLUENCE OF NATURAL AND ANTHROPOGENIC PROCESSES. Soil Science and Agrochemistry. 2010;(1):254-272. (In Russ.)

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ISSN 0130-8475 (Print)