中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
MPM evaluation of the dynamic runout process of the giant Daguangbao landslide

文献类型:期刊论文

作者Li, Xinpo1,2; Tang, Xiong1,2; Zhao, Shuxi1,2; Yan, Qiwei1,2; Wu, Yong1,2
刊名LANDSLIDES
出版日期2020
页码1438-1451
ISSN号1612-510X
关键词Landslide Runout analysis Material point method Friction degradation
DOI10.1007/s11629-019-5831-y
通讯作者Li, Xinpo(lixinpo@imde.ac.cn) ; Wu, Yong(wyhongyu@163.com)
产权排序1
文献子类Article;Early Access
英文摘要Giant landslides can cause significant damage to their dynamic runout processes. Understanding the mechanics of the runout process is essential for landslide risk assessment and mitigation design. This paper investigates the runout process of the 1.16 x 10(9) m(3) giant Daguangbao landslide triggered by the 2008 Ms 8.0 Wenchuan earthquake. The Daguangbao landslide is a typical bedding-plane slide and the properties of basal sliding surface play a key role in the runout behaviors of the landslide. The material point method (MPM) is adopted as a numerical tool of the simulations. A thermal-based velocity-weakening friction law is used to simulate the contact between the sliding body and the basal sliding surface. A strain-softening constitutive model is used to evaluate the damages inside the landslide body and their effects on the runout behaviors of the landslide. Numerical results reveal that landslide mass slides along the bedding-plane as a whole body initially and then disintegrates during the runout process. The calculated duration of sliding is 64 s and the maximum velocity reaches 60 m/s. The friction coefficient of the slip surface decreases sharply as the landslide body starts to move, and a steady-state friction coefficient mu approximate to 0.06 is reached when the velocity exceeds approximately 20 m/s. Friction degradation of the slip surface shows a sensible influence on the final runout distance and the depth of the deposit zone. The dynamic fragmentation of the landslide body, the final runout distance, and deposition topography are also significantly affected by material softening.
电子版国际标准刊号1993-0321
WOS关键词MATERIAL-POINT METHOD ; IN-CELL METHOD ; EARTHQUAKE ; FLOW ; SIMULATION ; VELOCITY ; FORCE ; DEFORMATION ; LUBRICATION ; IMPACT
资助项目NSFC[41877291] ; NSFC[41672356] ; National Key R&D Program of China[2020YFC1512005] ; Belt & Road international cooperation team for the Light of West program of CAS ; Key Research Program of the Chinese Academy of Sciences[KFZD-SW-424]
WOS研究方向Engineering ; Geology
语种英语
出版者SPRINGER HEIDELBERG
WOS记录号WOS:000538038700012
资助机构NSFC ; National Key R&D Program of China ; Belt & Road international cooperation team for the Light of West program of CAS ; Key Research Program of the Chinese Academy of Sciences
源URL[http://ir.imde.ac.cn/handle/131551/50740]  
专题成都山地灾害与环境研究所_山地灾害与地表过程重点实验室
通讯作者Li, Xinpo; Wu, Yong
作者单位1.Chinese Acad Sci, Inst Mt Hazards & Environm, Key Lab Mt Hazards & Earth Surface Proc, Chengdu, Peoples R China;
2.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
推荐引用方式
GB/T 7714
Li, Xinpo,Tang, Xiong,Zhao, Shuxi,et al. MPM evaluation of the dynamic runout process of the giant Daguangbao landslide[J]. LANDSLIDES,2020:1438-1451.
APA Li, Xinpo,Tang, Xiong,Zhao, Shuxi,Yan, Qiwei,&Wu, Yong.(2020).MPM evaluation of the dynamic runout process of the giant Daguangbao landslide.LANDSLIDES,1438-1451.
MLA Li, Xinpo,et al."MPM evaluation of the dynamic runout process of the giant Daguangbao landslide".LANDSLIDES (2020):1438-1451.

入库方式: OAI收割

来源:成都山地灾害与环境研究所

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