Wave generation, energy conversion, and sediment accumulation in a real-scale channel-like reservoir by landslide using a soil-water coupling SPH model
文献类型：期刊论文
| 作者 | Shi CQ(石传奇)2,4; Wang, Xiaoliang1,3; Liu, Qingquan3 |
| 刊名 | LANDSLIDES
 |
| 出版日期 | 2025-04-21 |
| 页码 | 15 |
| 关键词 | Landslide-generated impulse waves Soil-water coupling Huangtian landslide Channel-like reservoirs |
| ISSN号 | 1612-510X |
| DOI | 10.1007/s10346-025-02515-w |
| 通讯作者 | Wang, Xiao-liang(wangxiaoliang36@bit.edu.cn) ; Liu, Qing-quan(liuqq@bit.edu.cn) |
| 英文摘要 | For reservoirs located in mountainous regions, often referred to as channel-like reservoirs, the dynamics of landslide-generated impulse waves (LGIWs) differ considerably. The LGIW disaster resulted from the Huangtian landslide, which occurred in southwestern China, exemplifies a typical event in such channel-like reservoirs. However, survey data is limited due to the challenges of field observations. For instance, the evolution of LGIWs and the landslide movement process remain unknown. To investigate this practical event, a soil-water coupling model utilizing the Smoothed Particle Hydrodynamics (SPH) method is introduced. The results demonstrate a close alignment with actual observations. Notably, the evolution of the leading wave within the channel-like reservoir reveals significant differences, as the water body transitions from the common three-dimensional spreading propagation characteristic of reservoirs to a unidirectional movement along the river channel. This transition complicates the direct application of empirical formulas derived from conventional physical modeling experiments to wave phenomena in channel-like reservoirs. Moreover, the head velocity of the landslide diverges from its average velocity, offering a more accurate characterization of the landslide's impact on the water body. The energy conversion coefficient peaks at approximately 15% around the moment the landslide impacts the opposite bank, highlighting the substantial influence of topographic characteristics on the energy conversion process. The analysis also addresses the degree of siltation in the channel following the landslide and its implications for navigation. |
| 分类号 | 一类 |
| WOS关键词 | NUMERICAL-SIMULATION ; TSUNAMIS ; FLOWS ; DEFORMATION ; PARTICLES ; INSIGHT ; LONG |
| 资助项目 | National Natural Science Foundation of China |
| WOS研究方向 | Engineering ; Geology |
| 语种 | 英语 |
| WOS记录号 | WOS:001471147500001 |
| 资助机构 | National Natural Science Foundation of China |
| 其他责任者 | Wang, Xiao-liang，Liu, Qing-quan |
| 源URL | [http://dspace.imech.ac.cn/handle/311007/101070]  |
| 专题 | 力学研究所_流固耦合系统力学重点实验室(2012-) |
| 作者单位 | 1.Beijing Inst Technol, Zhuhai 519088, Peoples R China; 2.Univ Sci & Technol China, Dept Modern Mech, Hefei 230027, Peoples R China; 3.Beijing Inst Technol, Sch Aerosp Engn, Dept Mech, Beijing 100081, Peoples R China 4.Chinese Acad Sci, Inst Mech, Beijing 100190, Peoples R China; |
| 推荐引用方式 GB/T 7714 | Shi CQ,Wang, Xiaoliang,Liu, Qingquan. Wave generation, energy conversion, and sediment accumulation in a real-scale channel-like reservoir by landslide using a soil-water coupling SPH model[J]. LANDSLIDES,2025:15. |
| APA | 石传奇,Wang, Xiaoliang,&Liu, Qingquan.(2025).Wave generation, energy conversion, and sediment accumulation in a real-scale channel-like reservoir by landslide using a soil-water coupling SPH model.LANDSLIDES,15. |
| MLA | 石传奇,et al."Wave generation, energy conversion, and sediment accumulation in a real-scale channel-like reservoir by landslide using a soil-water coupling SPH model".LANDSLIDES (2025):15. |
入库方式： OAI收割
来源：力学研究所
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