Abstract

As a result of long-term researches it has been established, that creation of a friable blanket on leached chernozem in the conditions of Western Siberia leads to its gradual pauperisation by physical clay (<0.01mm) at the expense of washing away. Migrating on a soil profile, elementary soil particles accumulate in layers of 20-40 and 60-80cm., forming the recondensed horizons with the lowered water permeability. In a layer of 20-40cm. mainly collect an average and small silt, and in 60-80cm. - clay fraction. Speed infiltration the generated layers almost on 40% below values of a virgin soil. In the conditions of Siberia it can lead to stagnation of water in the top layers or to its unproductive loss at the expense of physical evaporation and a superficial drain. The received results can become a basis for optimisation of granulometric composition artificial ground and system engineering of preparation of the soil stabilising an ecological condition of anthropogenic-reformed territories.

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