Experimental investigation on the formation and failure of landslide dams considering the landslide mobility and river flow

被引:0
|
作者
Luo, Hongwei [1 ,2 ]
Zhou, Gordon G. D. [1 ,2 ,3 ]
Lu, Xueqiang [1 ,2 ]
Cui, Kahlil F. E. [1 ,2 ]
Zhao, Yuting [1 ]
Xie, Yunxu [1 ,2 ]
Zhong, Wei [1 ,2 ]
Zhou, Jiawen [4 ]
Pasuto, Alessandro [5 ]
机构
[1] Chinese Acad Sci, Inst Mt Hazards & Environm, Key Lab Mt Hazards & Engn Resiliences, Chengdu 610000, Peoples R China
[2] Univ Chinese Acad Sci, Beijing 100000, Peoples R China
[3] CAS HEC, China Pakistan Joint Res Ctr Earth Sci, Islamabad, Pakistan
[4] Sichuan Univ, State Key Lab Hydraul & Mt River Engn, Chengdu 610065, Peoples R China
[5] CNR, Res Inst Geohydrol Protect CNR IRPI, I-35127 Padua, Italy
基金
中国国家自然科学基金;
关键词
Landslide; River blockage; Froude number; Landslide dam; Dam faliure; Erosion rate; SOIL ERODIBILITY; MECHANISM; EROSION;
D O I
10.1016/j.enggeo.2024.107873
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
River blockage by landslides is a common geological disaster in mountainous regions that threaten the safety of human lives. Therefore, it is necessary to better understand the formation and failure of landslide dams. In this work, flume experiments are conducted to study the influence of landslide mobility and river flow dynamics, both characterized by the Froude number, on the formation process of landslide dams and the degree of river blockage. Here, river blockage is classified as either complete or partial depending on the ratio between the minimum dam height over the river flow depth. A criterion based on the relative Froude numbers of landslides and rivers is proposed to judge the degree of river blockage. We further found that during breaching, the erosion rate is still mainly controlled by the Froude number of the breaching flood and less so by the degree of blockage. The results of this work are expected to enhance the understanding of the formation and failure of landslide dams.
引用
收藏
页数:13
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