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Study of kinematic characteristics of a rock avalanche and subsequent erosion process due to a debris flow in Wenjia gully, Sichuan, China

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Listed:
  • Chao Kang

    (University of Northern British Columbia)

  • Dongxing Ren

    (Chengdu Surveying Geotechnical Research Institute Co., Ltd. of MCC)

  • Xiaofeng Gao

    (Chengdu Surveying Geotechnical Research Institute Co., Ltd. of MCC)

  • Chuntan Han

    (Chinese Academy of Sciences)

  • Yuxi Wang

    (Third Institute Geology and Mineral Exploration of Gansu Province Bureau of Geology and Mineral Resources)

Abstract

This paper aims to systematically study kinematic characteristics of Wenjiagou rock avalanche triggered by the M8.0 2008 Wenchuan earthquake and one of subsequent debris flows that occurred on August 13, 2010 (8.13 debris flow), using a numerical approach. The kinematic characteristics of the rock avalanche are back-calculated using an energy-based runout model. The erosion process of the subsequent rainfall-induced debris flow is analyzed using a progressive scouring entrainment model incorporated in the energy-based runout model. The results indicate that Wenjiagou rock avalanche traveled farther than most other rock avalanches with a maximum velocity of approximately 73 m/s detected at about 1700 m away from the source zone. The erosion of the 8.13 debris flow mainly occurred right after the dam failure which contributes to more than 97% of the total eroded volume. Besides, four different scenarios, including no blockage of the runoff (scenario I), no dam failure (scenario II), dam failure at the end of precipitation (scenario III), and no erodible material (scenario IV), are supposed to study the effect of the failure of a check dam on the erosion characteristics of the debris flow. The results reveal that the blockage of the channel without failure could reduce 86% of the total volume and the failure of check dams is the main reason for the destructive consequence of the 8.13 debris flow. This paper proposes an approach to explore kinematic characteristics of a rock avalanche and erosion process of the subsequent rainfall-induced debris flows and also innovatively provides a method to indirectly assess mitigation strategies that can be used for the design of mitigation projects.

Suggested Citation

  • Chao Kang & Dongxing Ren & Xiaofeng Gao & Chuntan Han & Yuxi Wang, 2021. "Study of kinematic characteristics of a rock avalanche and subsequent erosion process due to a debris flow in Wenjia gully, Sichuan, China," 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. 106(1), pages 937-964, March.
  • Handle: RePEc:spr:nathaz:v:106:y:2021:i:1:d:10.1007_s11069-021-04501-6
    DOI: 10.1007/s11069-021-04501-6
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    References listed on IDEAS

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    1. H. Ni & W. Zheng & Y. Tie & P. Su & Y. Tang & R. Xu & D. Wang & X. Chen, 2012. "Formation and characteristics of post-earthquake debris flow: a case study from Wenjia gully in Mianzhu, Sichuan, SW China," 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. 61(2), pages 317-335, March.
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    Cited by:

    1. Yao Shunyu & Nazir Ahmed Bazai & Tang Jinbo & Jiang Hu & Yi Shujian & Zou Qiang & Tashfain Ahmed & Guo Jian, 2022. "Dynamic process of a typical slope debris flow: a case study of the wujia gully, Zengda, Sichuan Province, China," 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. 112(1), pages 565-586, May.

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