中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Analysis of a retrogressive landslide with double sliding surfaces: a case study

文献类型:期刊论文

作者Zheng, Yun3; Chen, Congxin3; Liu, Tingting2,3; Xia, Kaizong3; Sun, Chaoyi3; Chen, Longlong1
刊名ENVIRONMENTAL EARTH SCIENCES
出版日期2020
卷号79期号:1页码:23
关键词Retrogressive landslide Weak intercalation Mechanism Excavation Numerical simulation
ISSN号1866-6280
DOI10.1007/s12665-019-8741-y
英文摘要In 2014, a cutting slope was excavated in Guizhou Province in China during the construction of the YanDe highway when a previously unknown ancient landslide was encountered. It has subsequently been named the 'Longjiayan ancient landslide'. Large surface cracks and severe building damage occurred, as well as apparent ground subsidence. This work reports the results of a comprehensive investigation performed to identify the mechanism and process of reactivation of the ancient landside. In situ surveys and mapping activities were first carried out to obtain a preliminary delineation of the landslide surface, and 19 boreholes were set up in the reactivation area to determine the landslide structure, as well as create a picture of the sliding surfaces involved. Then, 41 surface cracks and deep displacements in eleven boreholes were monitored for over 40 days. A numerical 2D analysis was also undertaken to back analyze the landside. A conceptual model is proposed for interpreting the mechanisms responsible for reactivation of ancient landslides based on the Longjiayan landslide. Thereafter, based on the formation mechanism of the landslide, detailed reinforcement measures were proposed to control it. The results reveal that the landslide was a retrogressive soil-mass slide involving two sliding surfaces. These surfaces have different depths: one is shallow and located in a silty clay layer; the other is deep and lies in a completely weathered shale layer. The soil mass primarily slid towards the free surface along the deep sliding surface. Up to three failure stages have been identified in the landslide which was triggered by excavation in the toe region. Rainfall and adverse dip direction of weak intercalations further promoted the development of the landslide. During this process, the shallow landslide played a key role in the formation of the deep landslide. Appropriate use of anti-slide piles and water interception/drainage is an effective approach to controlling such landslides.
资助项目National Natural Science Foundation of China[11602284] ; National Natural Science Foundation of China[11472293] ; National Natural Science Foundation of China[51609183]
WOS研究方向Environmental Sciences & Ecology ; Geology ; Water Resources
语种英语
WOS记录号WOS:000502759700003
出版者SPRINGER
源URL[http://119.78.100.198/handle/2S6PX9GI/23186]  
专题中科院武汉岩土力学所
通讯作者Zheng, Yun; Sun, Chaoyi
作者单位1.China Univ Geosci Beijing, Sch Engn & Technol, Beijing 100083, Peoples R China
2.Wuhan Univ Technol, Key Lab Roadway Bridge & Struct Engn, Wuhan 430070, Hubei, Peoples R China
3.Chinese Acad Sci, Inst Rock & Soil Mech, State Key Lab Geomech & Geotech Engn, Wuhan 430071, Hubei, Peoples R China
推荐引用方式
GB/T 7714
Zheng, Yun,Chen, Congxin,Liu, Tingting,et al. Analysis of a retrogressive landslide with double sliding surfaces: a case study[J]. ENVIRONMENTAL EARTH SCIENCES,2020,79(1):23.
APA Zheng, Yun,Chen, Congxin,Liu, Tingting,Xia, Kaizong,Sun, Chaoyi,&Chen, Longlong.(2020).Analysis of a retrogressive landslide with double sliding surfaces: a case study.ENVIRONMENTAL EARTH SCIENCES,79(1),23.
MLA Zheng, Yun,et al."Analysis of a retrogressive landslide with double sliding surfaces: a case study".ENVIRONMENTAL EARTH SCIENCES 79.1(2020):23.

入库方式: OAI收割

来源:武汉岩土力学研究所

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