River blockage and impulse wave evolution of the Baige landslide in October 2018: insights from coupled DEM-CFD analyses
On 11 October 2018, the Baige landslide in Southwest China blocked the Jinsha River and induced waves amplifying the landslide-affected area significantly. Devastating flood damage was caused by the consequent dam breach. Such a complex sequence can lead to catastrophic consequences but has rarely b...
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sg-ntu-dr.10356-1706612023-09-25T05:28:02Z River blockage and impulse wave evolution of the Baige landslide in October 2018: insights from coupled DEM-CFD analyses Li, Dongyang Nian, Tingkai Tiong, Robert Lee Kong Shen, Yueqiang Shao, Zhe School of Civil and Environmental Engineering Engineering::Civil engineering Baige Landslide Landslide-River Interaction On 11 October 2018, the Baige landslide in Southwest China blocked the Jinsha River and induced waves amplifying the landslide-affected area significantly. Devastating flood damage was caused by the consequent dam breach. Such a complex sequence can lead to catastrophic consequences but has rarely been fully reproduced. This paper investigates the landslide-river interaction of the first Baige landslide based on coupled discrete element method (DEM) and computational fluid dynamics (CFD) analyses. To this end, the volume of fluid (VOF) and virtual sphere model are adopted to realise impacted river tracing and accurate terrain modelling. The damming process and impulse wave evolution of the first event are well represented. In addition, the simulated cumulative landslide spreading path, deposit geometry, maximum wave elevation and cumulative wave erosion area satisfactorily match the survey results. Our findings further indicate that the movement path and deposit morphology of the Baige landslide are mainly affected by local terrain, while the propagation of impulse waves is driven by the sliding mass and modulated by the riverbank and hydrodynamic conditions. In particular, we discussed the evolution patterns of impulse waves caused by river damming landslides, encompassing run-up on the opposite bank and quasi-3D propagation along the river direction. This research provides a valuable guide for the practical simulation of river blockage and impulse wave evolution and supports the mitigation of landslide disasters in mountainous areas. This research was supported by the National Natural Science Foundation of China (52079020, 51579032), the LiaoNing Revitalization Talents Program (XLYC2002036) and the China Scholarship Council (CSC) (File No. 202006060115). 2023-09-25T05:28:02Z 2023-09-25T05:28:02Z 2023 Journal Article Li, D., Nian, T., Tiong, R. L. K., Shen, Y. & Shao, Z. (2023). River blockage and impulse wave evolution of the Baige landslide in October 2018: insights from coupled DEM-CFD analyses. Engineering Geology, 321, 107169-. https://dx.doi.org/10.1016/j.enggeo.2023.107169 0013-7952 https://hdl.handle.net/10356/170661 10.1016/j.enggeo.2023.107169 2-s2.0-85159551028 321 107169 en Engineering Geology © 2023 Elsevier B.V. All rights reserved. |
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Engineering::Civil engineering Baige Landslide Landslide-River Interaction Li, Dongyang Nian, Tingkai Tiong, Robert Lee Kong Shen, Yueqiang Shao, Zhe River blockage and impulse wave evolution of the Baige landslide in October 2018: insights from coupled DEM-CFD analyses |
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On 11 October 2018, the Baige landslide in Southwest China blocked the Jinsha River and induced waves amplifying the landslide-affected area significantly. Devastating flood damage was caused by the consequent dam breach. Such a complex sequence can lead to catastrophic consequences but has rarely been fully reproduced. This paper investigates the landslide-river interaction of the first Baige landslide based on coupled discrete element method (DEM) and computational fluid dynamics (CFD) analyses. To this end, the volume of fluid (VOF) and virtual sphere model are adopted to realise impacted river tracing and accurate terrain modelling. The damming process and impulse wave evolution of the first event are well represented. In addition, the simulated cumulative landslide spreading path, deposit geometry, maximum wave elevation and cumulative wave erosion area satisfactorily match the survey results. Our findings further indicate that the movement path and deposit morphology of the Baige landslide are mainly affected by local terrain, while the propagation of impulse waves is driven by the sliding mass and modulated by the riverbank and hydrodynamic conditions. In particular, we discussed the evolution patterns of impulse waves caused by river damming landslides, encompassing run-up on the opposite bank and quasi-3D propagation along the river direction. This research provides a valuable guide for the practical simulation of river blockage and impulse wave evolution and supports the mitigation of landslide disasters in mountainous areas. |
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School of Civil and Environmental Engineering |
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School of Civil and Environmental Engineering Li, Dongyang Nian, Tingkai Tiong, Robert Lee Kong Shen, Yueqiang Shao, Zhe |
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Article |
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Li, Dongyang Nian, Tingkai Tiong, Robert Lee Kong Shen, Yueqiang Shao, Zhe |
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Li, Dongyang |
title |
River blockage and impulse wave evolution of the Baige landslide in October 2018: insights from coupled DEM-CFD analyses |
title_short |
River blockage and impulse wave evolution of the Baige landslide in October 2018: insights from coupled DEM-CFD analyses |
title_full |
River blockage and impulse wave evolution of the Baige landslide in October 2018: insights from coupled DEM-CFD analyses |
title_fullStr |
River blockage and impulse wave evolution of the Baige landslide in October 2018: insights from coupled DEM-CFD analyses |
title_full_unstemmed |
River blockage and impulse wave evolution of the Baige landslide in October 2018: insights from coupled DEM-CFD analyses |
title_sort |
river blockage and impulse wave evolution of the baige landslide in october 2018: insights from coupled dem-cfd analyses |
publishDate |
2023 |
url |
https://hdl.handle.net/10356/170661 |
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1779156684691734528 |