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  • . The study was carried out on chernozem-type soils during different hydrological years. The water content of the snow varied. Both the amount of snow and the type of land use influence the surface runoff volume. Slopes covered with perennial grasses
  • of southern West Siberia (Predsalairye, Priobye and Kuznetsk hollow). These areas have different geomorphological and climatic characteristics and soils. Observations were made from 1969 to 2007. Soil losses in high-snow and very high-snow years varied from