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- W2349371406 abstract "Experiments are carried out to study the movement of fine grains in soil and its effect on the landslide and debris flow.The grain series at different sections before and after experiments are compared.It is shown that the fine grains move downwards in the direction vertical to the slope surface and mostly are assembled in the middle.The fine grains are more at the tail than at the foreside at the same parallel to the slope surface. It may be thought that the fine grains are assembled at the lower part and foreside of the slope due to the raining and penetration of water,which causes decrease of the permeability at these places.Therefore,the pore pressure increases and pore water are blocked at these places,loading to formation of the sliding face and the landslide or debris flow occurs." @default.
- W2349371406 created "2016-06-24" @default.
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- W2349371406 date "2005-01-01" @default.
- W2349371406 modified "2023-09-22" @default.
- W2349371406 title "The Movement of Fine Grains and Its Effects on the Landslide and Debris Flow Caused by Raining" @default.
- W2349371406 hasPublicationYear "2005" @default.
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