Titlebook: Experimental Erosion; Theory and Practice Xiangzhou Xu,Tongxin Zhu,Lu Gao Book 2020 Science Press and Springer Nature Singapore Pte Ltd. 2

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Philip D. Truscott,Michael F. Kornsnd behavior of the mass failure on steep loess slopes. The results show that the quantity of soil loss caused by the avalanche and landslide was much more than that caused by the mudslide, and the avalanche was the most violent gravity erosion. As the slopes were eroded with five runs of rainfalls e

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Jason H. Moore,Nate Barney,Bill C. Whiteoccurrence and behavior. This chapter conducted a series of laboratory experiments to test the stability of different slope geometries and rainfalls and then performed a sensitivity analysis. The following three types of gravity erosion were observed: landslide, avalanche, and mudslide. In an event

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A. A. Almal,C. D. MacLean,W. P Worzeltal research in this area. In this chapter, a series of laboratory experiments were conducted to observe the failure geometries and volumes under rainfall simulations. The following six failure-scar types occurred: Tf, Cd, Cu, Ia, Ps, and Co. Tf, Cd, and Cu were the three major types of failure scar

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