- ISSN 0258-2724
- CN 51-1277/U
- EI Compendex
- Scopus
- Indexed by Core Journals of China, Chinese S&T Journal Citation Reports
- Chinese S&T Journal Citation Reports
- Chinese Science Citation Database
| Citation: | YANG Bing, ZHOU Zihong, TAO Long, FU Guanxi, ZHUO Linbo. Experimental Study on Instability Characteristic and Bearing Capacity of Slope with Bedrock under Rainfall[J]. Journal of Southwest Jiaotong University, 2022, 57(4): 910-918. doi: 10.3969/j.issn.0258-2724.20200355
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In order to investigate the characteristics of slope with bedrock induced by rainfall, the failure process and mechanism of slope with bedrock under rainstorm were studied systematically by laboratory model test. The variation characteristics of soil moisture content and pore water pressure in time and space before and after rainfall were discussed to reveal the mechanism of slope instability induced by rainfall. Besides, the variation law of slope bearing capacity after rain was studied by loading at the top of slope. The results show that with the development of rainfall, the liquefaction flow of soil appears first at the foot of the slope, and then the local shedding of the soil occurs there. With the continuous rainfall, the scope of soil shedding damage gradually increases, which leads to the increase of the free surface of the upper soil. After the soil is damaged, it is saturated and softened by the rain and slides downward, and the rear soil is further eroded, resulting in the slope failure of a certain depth and width. The increase of soil moisture content and pore water pressure in the slope are the main factors leading to the instability and failure of the slope. After the rainfall stops, the ultimate load that the slope can bear increases at first and then decreases, and finally tends to be stable, while the failure of the slope with bedrock shows either a global slip mode or a local slip mode under the top static load.
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