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Effect of Strain Rate on Anisotropic Mechanical Behavior of the Shale Under Uniaxial Compression Conditions

文献类型：期刊论文

作者He, Jianming2,3,4; Afolagboye, Lekan Olatayo1; Zheng, Bo2,3,4; Mao, Tianqiao2,3; Wu, Yanfang2,3,4; Li, Guanfang2,3,4; Li, Shouding2,3,4; Li, Xiao2,3,4
刊名ROCK MECHANICS AND ROCK ENGINEERING
出版日期2022-06-06
页码9
关键词Anisotropy Bedding orientation Failure mode Shale Strain rate
ISSN号0723-2632
DOI10.1007/s00603-022-02892-x
英文摘要HighlightsIncrease in strain rate can shorten the mechanical response time of the shale and modify the stress-strain curves into linear form.The anisotropic strength and elastic modulus of the shale generally increased as the strain rate increases.Failure mode transform from shearing failure at low strain rate to combination of tensile split and shearing failure at high strain rate.
WOS关键词GAS ; ROCKS
资助项目National Natural Science Foundation of China[41877270] ; Key Research Program of the Institute of Geology and Geophysics, CAS[IGGCAS-201903] ; Second Tibetan Plateau Scientific Expedition and Research Program (STEP)[2019QZKK0904]
WOS研究方向Engineering ; Geology
语种英语
WOS记录号WOS:000806693000001
出版者SPRINGER WIEN
资助机构National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Key Research Program of the Institute of Geology and Geophysics, CAS ; Key Research Program of the Institute of Geology and Geophysics, CAS ; Key Research Program of the Institute of Geology and Geophysics, CAS ; Key Research Program of the Institute of Geology and Geophysics, CAS ; Second Tibetan Plateau Scientific Expedition and Research Program (STEP) ; Second Tibetan Plateau Scientific Expedition and Research Program (STEP) ; Second Tibetan Plateau Scientific Expedition and Research Program (STEP) ; Second Tibetan Plateau Scientific Expedition and Research Program (STEP) ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Key Research Program of the Institute of Geology and Geophysics, CAS ; Key Research Program of the Institute of Geology and Geophysics, CAS ; Key Research Program of the Institute of Geology and Geophysics, CAS ; Key Research Program of the Institute of Geology and Geophysics, CAS ; Second Tibetan Plateau Scientific Expedition and Research Program (STEP) ; Second Tibetan Plateau Scientific Expedition and Research Program (STEP) ; Second Tibetan Plateau Scientific Expedition and Research Program (STEP) ; Second Tibetan Plateau Scientific Expedition and Research Program (STEP) ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Key Research Program of the Institute of Geology and Geophysics, CAS ; Key Research Program of the Institute of Geology and Geophysics, CAS ; Key Research Program of the Institute of Geology and Geophysics, CAS ; Key Research Program of the Institute of Geology and Geophysics, CAS ; Second Tibetan Plateau Scientific Expedition and Research Program (STEP) ; Second Tibetan Plateau Scientific Expedition and Research Program (STEP) ; Second Tibetan Plateau Scientific Expedition and Research Program (STEP) ; Second Tibetan Plateau Scientific Expedition and Research Program (STEP) ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Key Research Program of the Institute of Geology and Geophysics, CAS ; Key Research Program of the Institute of Geology and Geophysics, CAS ; Key Research Program of the Institute of Geology and Geophysics, CAS ; Key Research Program of the Institute of Geology and Geophysics, CAS ; Second Tibetan Plateau Scientific Expedition and Research Program (STEP) ; Second Tibetan Plateau Scientific Expedition and Research Program (STEP) ; Second Tibetan Plateau Scientific Expedition and Research Program (STEP) ; Second Tibetan Plateau Scientific Expedition and Research Program (STEP)
源URL[http://ir.iggcas.ac.cn/handle/132A11/105999]  
专题地质与地球物理研究所_中国科学院页岩气与地质工程重点实验室
通讯作者He, Jianming
作者单位1.Ekiti State Univ, Dept Geol, Ado Ekiti, Nigeria
2.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Shale Gas & Geoengn, Beijing, Peoples R China
3.Chinese Acad Sci, Innovat Acad Earth Sci, Beijing, Peoples R China
4.Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing, Peoples R China
推荐引用方式
GB/T 7714		 He, Jianming,Afolagboye, Lekan Olatayo,Zheng, Bo,et al. Effect of Strain Rate on Anisotropic Mechanical Behavior of the Shale Under Uniaxial Compression Conditions[J]. ROCK MECHANICS AND ROCK ENGINEERING,2022:9.
APA He, Jianming.,Afolagboye, Lekan Olatayo.,Zheng, Bo.,Mao, Tianqiao.,Wu, Yanfang.,...&Li, Xiao.(2022).Effect of Strain Rate on Anisotropic Mechanical Behavior of the Shale Under Uniaxial Compression Conditions.ROCK MECHANICS AND ROCK ENGINEERING,9.
MLA He, Jianming,et al."Effect of Strain Rate on Anisotropic Mechanical Behavior of the Shale Under Uniaxial Compression Conditions".ROCK MECHANICS AND ROCK ENGINEERING (2022):9.

入库方式： OAI收割

来源：地质与地球物理研究所

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