Snowmelt-induced soil erosion on gentle slopes in the southern Cis-Ural region

被引：0
|
作者：
M. A. Komissarov
I. M. Gabbasova
机构：
[1] Russian Academy of Sciences,Institute of Biology, Ufa Scientific Center
来源：
Eurasian Soil Science | 2014年 / 47卷
关键词：
soil erosion; snow reserves; snowmelt stages; suspended sediments; freezing depth;
D O I：
暂无
中图分类号：
学科分类号：
摘要：
It has been revealed that, in the years when the freezing depth of leached chernozems on slopes in the southern Cis-Ural region is in the range of 30–38 cm, no surface runoff is observed in the spring regardless of the snow cover, soil wetting, or vegetation; the critical freezing depth under forest is half that on the open surfaces. When the freezing depth is deeper, the critical volume of the spring runoff is mainly determined by the meteorological conditions, the water permeability of the soil, and its protection by plants.
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页码：598 / 607
页数：9
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