中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
首页 机构 成果 学者
  
  1. CAS IR Grid
  2. 地质与地球物理研究所
  3. 中国科学院地质与地球物理研究所
Acoustic emission pattern of shale under uniaxial deformation

文献类型：期刊论文

作者Wang, Y.1; Li, C. H.1; Hu, Y. Z.2; Miao, S. J.1
刊名GEOTECHNIQUE LETTERS
出版日期2017-12-01
卷号7期号:4页码:323-329
关键词Anisotropy Laboratory Tests Rocks/rock Mechanics
ISSN号2049-825X
DOI10.1680/jgele.17.00056
文献子类Article
英文摘要The brittle fracture mechanism of shale is an important issue to both borehole stability and hydraulic fracturing. A number of experimental studies on shale macroscopic mechanical properties have been carried out; however, the acoustic emission (AE) patterns of anisotropic shale are not fully understood. In this paper, a series of uniaxial compressive strength tests were conducted on cylindrical shale obtained by drilling at different orientations to the bedding plane. The anisotropic failure modes of shale samples have been monitored by real-time AE monitoring and stress-strain response, under ambient conditions and uniaxial stresses. The experimental results suggest that the pronounced bedding planes of shale have a significant influence on the mechanical properties and the AE responses. The AE counts and AE accumulative energy release curves clearly indicate the initiation and propagation of cracks during compression, and the 'U' shaped curves well reflect the anisotropic failure mechanism. The sounded foliation in the shale formation results in the anisotropy of elasticity, strength, AE counts and accumulated energy release from which the changes in strength dominate the entire failure pattern of shale samples. It is suggested that the AE activities monitored during deformation can provide good information to grasp the anisotropic failure mechanism of shale.
WOS关键词MECHANICAL-PROPERTIES ; CONFINING PRESSURES ; BRITTLENESS ; ANISOTROPY ; FAILURE ; ROCKS
WOS研究方向Engineering
语种英语
WOS记录号WOS:000419274900008
出版者ICE PUBLISHING
资助机构National Natural Science Foundation of China(41502294 ; National Natural Science Foundation of China(41502294 ; Fundamental Research Funds for the Central Universities(2302017FRF-TP-17-027A1) ; Fundamental Research Funds for the Central Universities(2302017FRF-TP-17-027A1) ; National Key Basic Research Program of China (973 Program)(2015CB060200) ; National Key Basic Research Program of China (973 Program)(2015CB060200) ; National Key Technologies Research & Development programme(2017YFC0804609) ; National Key Technologies Research & Development programme(2017YFC0804609) ; 51574014) ; 51574014) ; National Natural Science Foundation of China(41502294 ; National Natural Science Foundation of China(41502294 ; Fundamental Research Funds for the Central Universities(2302017FRF-TP-17-027A1) ; Fundamental Research Funds for the Central Universities(2302017FRF-TP-17-027A1) ; National Key Basic Research Program of China (973 Program)(2015CB060200) ; National Key Basic Research Program of China (973 Program)(2015CB060200) ; National Key Technologies Research & Development programme(2017YFC0804609) ; National Key Technologies Research & Development programme(2017YFC0804609) ; 51574014) ; 51574014) ; National Natural Science Foundation of China(41502294 ; National Natural Science Foundation of China(41502294 ; Fundamental Research Funds for the Central Universities(2302017FRF-TP-17-027A1) ; Fundamental Research Funds for the Central Universities(2302017FRF-TP-17-027A1) ; National Key Basic Research Program of China (973 Program)(2015CB060200) ; National Key Basic Research Program of China (973 Program)(2015CB060200) ; National Key Technologies Research & Development programme(2017YFC0804609) ; National Key Technologies Research & Development programme(2017YFC0804609) ; 51574014) ; 51574014) ; National Natural Science Foundation of China(41502294 ; National Natural Science Foundation of China(41502294 ; Fundamental Research Funds for the Central Universities(2302017FRF-TP-17-027A1) ; Fundamental Research Funds for the Central Universities(2302017FRF-TP-17-027A1) ; National Key Basic Research Program of China (973 Program)(2015CB060200) ; National Key Basic Research Program of China (973 Program)(2015CB060200) ; National Key Technologies Research & Development programme(2017YFC0804609) ; National Key Technologies Research & Development programme(2017YFC0804609) ; 51574014) ; 51574014)
源URL[http://ir.iggcas.ac.cn/handle/132A11/82474]  
专题中国科学院地质与地球物理研究所
通讯作者Wang, Y.
作者单位1.Univ Sci & Technol Beijing, Sch Civil & Resource Engn, Dept Civil Engn, Beijing Key Lab Urban Underground Space Engn, Beijing, Peoples R China
2.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Shale Gas & Geoengn, Beijing, Peoples R China
推荐引用方式
GB/T 7714		 Wang, Y.,Li, C. H.,Hu, Y. Z.,et al. Acoustic emission pattern of shale under uniaxial deformation[J]. GEOTECHNIQUE LETTERS,2017,7(4):323-329.
APA Wang, Y.,Li, C. H.,Hu, Y. Z.,&Miao, S. J..(2017).Acoustic emission pattern of shale under uniaxial deformation.GEOTECHNIQUE LETTERS,7(4),323-329.
MLA Wang, Y.,et al."Acoustic emission pattern of shale under uniaxial deformation".GEOTECHNIQUE LETTERS 7.4(2017):323-329.

入库方式： OAI收割

来源：地质与地球物理研究所

浏览0
下载0
收藏0
其他版本

除非特别说明，本系统中所有内容都受版权保护，并保留所有权利。