Abstract

The paper presents the results of research on the formation of melt water runoff and its qualitative composition in the conditions of the anti-erosion complex "Novonikulinskoe". It was found that during the twenty-one-year period, there was no runoff for nine years, the runoff was weak for seven years, and very weak for six years. Analyzing the average results of runoff formation for 1969-1978 with the results obtained in the following years 2000-2021, it can be noted that the volume of runoff decreased by 5.8 mm, and the runoff coefficient decreased three times. Moreover, the amount of snow water in the catchment area has increased by 26.84% in recent years. The developed and implemented complex of anti-erosion measures made it possible to minimize the runoff and flushing of batteries in catchments.

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