Author
Listed:
- Qifeng Guo
(School of Civil and Resource Engineering, University of Science and Technology Beijing, Beijing 100083, China
Key Laboratory of the Ministry of Education of China for High-Efficient Mining and Safety of Metal Mines, Beijing 100083, China)
- Jiliang Pan
(School of Civil and Resource Engineering, University of Science and Technology Beijing, Beijing 100083, China
Key Laboratory of the Ministry of Education of China for High-Efficient Mining and Safety of Metal Mines, Beijing 100083, China)
- Meifeng Cai
(School of Civil and Resource Engineering, University of Science and Technology Beijing, Beijing 100083, China
Key Laboratory of the Ministry of Education of China for High-Efficient Mining and Safety of Metal Mines, Beijing 100083, China)
- Ying Zhang
(School of Civil and Resource Engineering, University of Science and Technology Beijing, Beijing 100083, China
Key Laboratory of the Ministry of Education of China for High-Efficient Mining and Safety of Metal Mines, Beijing 100083, China)
Abstract
Progressive failure in rock bridges along pre-existing discontinuities is one of the predominant destruction modes of rock slopes. The monitoring and prediction of the impending progressive failure is of great significance to ensure the stability of the rock structures and the safety of the workers. The deformation and fracture of rocks are complex processes with energy evolution between rocks and the external environment. Regarding the whole slope as a system, an energy evolution equation of rock slope systems during progressive failure was established by an energy method of systemic stability. Then, considering the weakening effect of joints and the locking effect of rock bridges, a method for calculating the safety factor of rock slopes with a locked section was proposed. Finally, the energy evolution equation and the calculation method of safety factor are verified by a case study. The results show that when the energy dissipated in the progressive failure process of rock bridges is less than the energy accumulated by itself, the deformation energy stored in the slope system can make the locked section deform continuously until the damage occurs. The system energy equal to zero can be used as the critical criterion for the dynamic instability of the rock slope with locked section. The accumulated deformation energy in the slope system can promote the development of the cracks in the locked section, and the residual energy in the critical sliding state is finally released in the form of kinetic energy, which is the main reason for the progressive dynamic instability of rock slopes.
Suggested Citation
Qifeng Guo & Jiliang Pan & Meifeng Cai & Ying Zhang, 2020.
"Analysis of Progressive Failure Mechanism of Rock Slope with Locked Section Based on Energy Theory,"
Energies, MDPI, vol. 13(5), pages 1-18, March.
Handle:
RePEc:gam:jeners:v:13:y:2020:i:5:p:1128-:d:327654
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