中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Control Effect of a Large Geological Discontinuity on the Seismic Response and Stability of Underground Rock Caverns: A Case Study of the Baihetan #1 Surge Chamber

文献类型:期刊论文

作者Cui, Zhen1,2; Sheng, Qian2; Leng, Xianlun2
刊名ROCK MECHANICS AND ROCK ENGINEERING
出版日期2016
卷号49期号:6页码:2099-2114
关键词Underground cavern Seismic stability Structural control effect Discrete element method Continuously yielding model
ISSN号0723-2632
DOI10.1007/s00603-015-0908-6
英文摘要In this paper, the seismic stability of the #1 surge chamber of the Baihetan hydropower plant, which is influenced by a large dominating geological discontinuity [the interlayer shear weakness zone (ISWZ) C2)], is studied. An advanced, nonlinear, continuously yielding (CY) model was adopted to describe the complex mechanical properties of ISWZ C2. This model considers a power function type, normal stress dependent behavior and the progressive damage that occurred during shear tests. The applicability of the CY model is proved via a comparison with field test results and the theoretical solution. Verification work was conducted in 3DEC code to show that the 3DEC software is suitable for implementing this model. Three ground motion waveforms were utilized to conduct a seismic analysis of the #1 surge chamber after a special response spectrum matching process. The seismic analysis confirmed the control effect of ISWZ C2 on the seismic stability of the cavern. The majority of the cavern's seismic displacement consists of elastic body movement, while the plastic deformation is relatively limited. Further, most of the deformations were caused by the contact deformation of C2. For the contact deformation of C2, the magnitude of permanent shear deformation is larger than that of the normal deformation. The magnitude of permanent shear deformation is more notable along the strike direction of C2, and the permanent normal displacement n of C2 mainly occurs along the dip direction of C2. Finally, the seismic stability of the cavern is assessed via the overload method. The seismic safety factor of the cavern is approximately 2-3.
WOS研究方向Engineering ; Geology
语种英语
WOS记录号WOS:000377365400007
出版者SPRINGER WIEN
源URL[http://119.78.100.198/handle/2S6PX9GI/3878]  
专题岩土力学所知识全产出_期刊论文
国家重点实验室知识产出_期刊论文
作者单位1.PowerChina Huadong Engn Corp Ltd
2.Chinese Acad Sci, Inst Rock & Soil Mech, State Key Lab Geomech & Geotech Engn ;
推荐引用方式
GB/T 7714
Cui, Zhen,Sheng, Qian,Leng, Xianlun. Control Effect of a Large Geological Discontinuity on the Seismic Response and Stability of Underground Rock Caverns: A Case Study of the Baihetan #1 Surge Chamber[J]. ROCK MECHANICS AND ROCK ENGINEERING,2016,49(6):2099-2114.
APA Cui, Zhen,Sheng, Qian,&Leng, Xianlun.(2016).Control Effect of a Large Geological Discontinuity on the Seismic Response and Stability of Underground Rock Caverns: A Case Study of the Baihetan #1 Surge Chamber.ROCK MECHANICS AND ROCK ENGINEERING,49(6),2099-2114.
MLA Cui, Zhen,et al."Control Effect of a Large Geological Discontinuity on the Seismic Response and Stability of Underground Rock Caverns: A Case Study of the Baihetan #1 Surge Chamber".ROCK MECHANICS AND ROCK ENGINEERING 49.6(2016):2099-2114.

入库方式: OAI收割

来源:武汉岩土力学研究所

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