a State Key Laboratory of Geohazard Prevention and Geoenvironment Protection, Chengdu University of Technology, Chengdu, China
b College of Environment and Civil Engineering, Chengdu University of Technology, Chengdu, China
c Institute of Mountain Hazards and Environment, Chinese Academy of Sciences (CAS), Chengdu, China
d Institute for Transport Studies, University of Leeds, 34-40 University Rd, Leeds, LS2 9JT, UK
2025, 17(4): 2009-2030. doi:10.1016/j.jrmge.2024.03.031
Received: 2024-01-05 / Revised: 2024-01-29 / Accepted: 2024-03-17 / Available online: 2024-07-10
2025, 17(4): 2009-2030.
doi:10.1016/j.jrmge.2024.03.031
Received: 2024-01-05
Revised: 2024-01-29
Accepted: 2024-03-17
Available online: 2024-07-10
Bedding parallel stepped rock slopes exist widely in nature and are used in slope engineering. They are characterized by complex topography and geological structure and are vulnerable to shattering under strong earthquakes. However, no previous studies have assessed the mechanisms underlying seismic failure in rock slopes. In this study, large-scale shaking table tests and numerical simulations were conducted to delineate the seismic failure mechanism in terms of acceleration, displacement, and earth pressure responses combined with shattering failure phenomena. The results reveal that acceleration response mutations usually occur within weak interlayers owing to their inferior performance, and these mutations may transform into potential sliding surfaces, thereby intensifying the nonlinear seismic response characteristics. Cumulative permanent displacements at the internal corners of the berms can induce quasi-rigid displacements at the external corners, leading to greater permanent displacements at the internal corners. Therefore, the internal corners are identified as the most susceptible parts of the slope. In addition, the concept of baseline offset was utilized to explain the mechanism of earth pressure responses, and the result indicates that residual earth pressures at the internal corners play a dominant role in causing deformation or shattering damage. Four evolutionary deformation phases characterize the processes of seismic responses and shattering failure of the bedding parallel stepped rock slope, i.e. the formation of tensile cracks at the internal corners of the berm, expansion of tensile cracks and bedding surface dislocation, development of vertical tensile cracks at the rear edge, and rock mass slipping leading to slope instability. Overall, this study provides a scientific basis for the seismic design of engineering slopes and offers valuable insights for further studies on preventing seismic disasters in bedding parallel stepped rock slopes.
Keywords: Rock slope stability, Shaking table test, Numerical simulation, Permanent displacement, Acceleration amplification factor
Chunlei Xin
Chunlei Xin has been engaged in teaching and research in the field of seismic interaction in geotechnical engineering and underground structural engineering. He obtained his Master degree and PhD in Bridge and Tunnel Engineering from Southwest Jiaotong University in 2011 and 2016, respectively. He pursued joint PhD studies at Rensselaer Polytechnic Institute from 2013 to 2014. Since 2022, he has been working as a researcher at the State Key Laboratory of Geological Hazard Prevention and Geological Environment Protection. He was recognized as a high-level talent in overseas studies from Sichuan Province and the transportation industry. He was also regarded as a key teacher at Chengdu University of Technology. Throughout his career, he has successfully led and participated in over 10 research projects funded by the National Natural Science Foundation of China and provincial-level research programs. He has published more than 20 SCI-indexed papers as the first author or corresponding author. His contributions have been acknowledged with a second-class prize for scientific and technological progress at the provincial and ministerial levels.