Mechanism of soil water regime formation of reclaimed territories
2015
Romanova,T.A. | Kapilevich,Zh.A. | Ivakhnenko,N.N. | Efimova,I.A.
In a course of the research there was studied the mechanism of soil water regime formation of reclaimed territories. The research was realized in the conditions of the Republic of Belarus on two melioration systems in the Luninets and Kobrin districts of Brest region and soil atmospheric moisture developed on water and glaciers greenhouse sands in the Berezinsky Biosphere Reserve in the central part of Belarus. As a result of research it was revealed that spatial vertical infiltration of precipitation occured only in conditions of excessive moisture and depending on the degree of its expressiveness. Wash water regime formed only in sod-podzolic swamped soils with illuvial humus horizon in soils developed on sands, in automorphic sod-podzolic soils formed nonflushing regime. Soil and ground water in the sandy sediments accumulate due to subsurface runoff from soil with maximize hydration. It was developed a functional model of soil combinations moisture at low flat watersheds and deep depressions on loose sediments.
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