Genesis and evolution of drained soils developed on lake-glacial deposits
Abstract
The drainage reclamation directed to remove excess moisture gives rise to substantial change both regime characteristics and basic properties of soils with a different degree of humidification. Thus, in-depth transformation of soil-formation process and gradual creation of drained soils having their inherent diagnostic signs and properties take place. Eluvial-illuvial processes accompanied with increase in mobility of a humus and also removal of it and elements significant physically for plants from upper soil horizons strengthen in a soil profile. The better structural organization, presence of pores-fractures, increase of a filtration coefficient is characteristic for subsurface horizons of drained soils in comparison with un-drained ones.
About the Authors
A. V. Visochenko
Institute for Land Reclamation and Grassland Cultivation
Belarus
Belarus
Zh. A. Kapilevich
Institute for Land Reclamation and Grassland Cultivation
Belarus
Belarus
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Review
For citations:
Visochenko A.V., Kapilevich Zh.A. Genesis and evolution of drained soils developed on lake-glacial deposits. Land Reclamation. 2006;(1):106-113. (In Russ.)
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