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Investigation into a homogenous step-like rock slope response under wide-frequency seismic loads using a large-scale shaking table

Author

Listed:
  • Jianxian He

    (Southwest Jiaotong University
    Chinese Academy of Sciences
    University of Chinese Academy of Sciences
    Innovation Academy for Earth Science, Chinese Academy of Sciences)

  • Zhifa Zhan

    (China Renewable Energy Engineering Institute)

  • Shengwen Qi

    (Chinese Academy of Sciences
    University of Chinese Academy of Sciences
    Innovation Academy for Earth Science, Chinese Academy of Sciences)

  • Chunlei Li

    (China Institute of Water Resources and Hydropower Research)

  • Bowen Zheng

    (Chinese Academy of Sciences
    University of Chinese Academy of Sciences
    Innovation Academy for Earth Science, Chinese Academy of Sciences)

  • Guoxiang Yang

    (China University of Geoscience)

  • Songfeng Guo

    (Chinese Academy of Sciences
    University of Chinese Academy of Sciences
    Innovation Academy for Earth Science, Chinese Academy of Sciences)

  • Xiaolin Huang

    (Chinese Academy of Sciences
    University of Chinese Academy of Sciences
    Innovation Academy for Earth Science, Chinese Academy of Sciences)

  • Yu Zou

    (Chinese Academy of Sciences
    University of Chinese Academy of Sciences
    Innovation Academy for Earth Science, Chinese Academy of Sciences)

  • Ning Liang

    (Chinese Academy of Sciences
    University of Chinese Academy of Sciences
    Innovation Academy for Earth Science, Chinese Academy of Sciences)

Abstract

This paper studied the dynamic response of the homogeneous step-like rock slope under wide frequency and amplitude through a large-scale shaking table test. A homogenous rock slope with a length of 3.50 m, width of 0.68 m and height of 1.20 m was constructed in a rigid steel box. Results indicate that acceleration amplification factor in horizontal direction (AAF-X) along the slope surface is amplified with the increase in the slope height when loading frequency ≤ 45 Hz, while AAF-X decreases first then increases when loading frequency is 60 Hz and 75 Hz. The acceleration amplification factor in vertical direction (AAF-Z) increases first and then decreases with the increase in the slope height. The resonance frequency of slope near the slope crest decreases from 61.37 to 58.12 Hz, while the damping ratio increases from 5.8 to 8.8%, as the loading amplitude increases from 0.1 to 0.5 g. The AAF reminds linear increase with a loading amplitude of up to 0.4 g while decreases when the loading amplitude becomes larger than 0.5 g. It reveals that the loading amplitude has a “double-effect” on the seismic response of the homogeneous rock slope. That is, on the one hand, the larger the loading amplitude, the stronger the acceleration intensity, the greater deterioration of rock slope structure or material and the larger damping ratio of the slope; on the other hand, more energy will be dissipated due to plastic deformation or particle friction of high damping ratio and weaker slope structure. Such test result can be used for understanding the dynamic instability mechanism of the homogeneous slope in the field.

Suggested Citation

  • Jianxian He & Zhifa Zhan & Shengwen Qi & Chunlei Li & Bowen Zheng & Guoxiang Yang & Songfeng Guo & Xiaolin Huang & Yu Zou & Ning Liang, 2023. "Investigation into a homogenous step-like rock slope response under wide-frequency seismic loads using a large-scale shaking table," Natural Hazards: Journal of the International Society for the Prevention and Mitigation of Natural Hazards, Springer;International Society for the Prevention and Mitigation of Natural Hazards, vol. 116(2), pages 2645-2669, March.
  • Handle: RePEc:spr:nathaz:v:116:y:2023:i:2:d:10.1007_s11069-022-05782-1
    DOI: 10.1007/s11069-022-05782-1
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    Cited by:

    1. Xiuhong Zheng & Qihua Zhao & Sheqin Peng & Longke Wu & Yanghao Dou & Kuangyu Chen, 2024. "Analysis of Failure Mechanism of Medium-Steep Bedding Rock Slopes under Seismic Action," Sustainability, MDPI, vol. 16(17), pages 1-21, September.

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