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- W2358173899 abstract "The mechanism of grade erosion effect law with different slopes and ground vegetations in small watersheds was investigated, which showed that there is peak value in the slope erosion intensity on the system length of the slope size scale and that the peak value appeares in the middle or lower course of the system length of the slope. The process of dynamical evolution falled into six steps: slaps erosion, sheet erosion, near-slope rill development, rill development, slipping and gully erosion excretion, system erosion stability (to the datum plane). Every step had its own zone of scatter: the slope in the upper course was of mainly slaps erosion and sheet erosion, the slope in the upper middle course was of mainly rill erosion and the slope in the middle lower course was of mainly rill erosion. At the same time, erosion sediment run-off occurred, and the slope in the lower course was of mainly slash erasion and secondly some letdown surface erasion. In the process of system element erosion, the slope played a leading role in the place where the peak value occurred and had no effect on the law of erosion effect. The ground vegetation presented a stronger interference in the effect of slope erosion mainly by the way of impoundment for direct runoff." @default.
- W2358173899 created "2016-06-24" @default.
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- W2358173899 date "2011-01-01" @default.
- W2358173899 modified "2023-09-22" @default.
- W2358173899 title "Mechanism of grade element slop erosion in small watersheds based on (137)~Cs trace method" @default.
- W2358173899 hasPublicationYear "2011" @default.
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