中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Crack initiation stress of brittle rock with different porosities

文献类型:期刊论文

作者Tang, Minghao3; Wang, Guibin2; Chen, Shiwan1; Yang, Chunhe2,3
刊名BULLETIN OF ENGINEERING GEOLOGY AND THE ENVIRONMENT
出版日期2021-04-23
页码16
关键词Crack initiation stress Lateral strain Brittle rocks Lateral strain response Cyclic stressing Acoustic emissions
ISSN号1435-9529
DOI10.1007/s10064-021-02187-5
英文摘要Accurately determining the crack initiation stress (CI) is of great importance to evaluate the stability of deep underground openings and the permeability of host rock in the near field. For this paper, uniaxial compression tests and increasing amplitude cyclic stressing tests were performed on four kinds of rocks with different porosities. The stress-strain data and acoustic emission (AE) data of these tests are analyzed to evaluate the applicability and accuracy of the existing methods for determining the CI. The results demonstrate that for marble and Beishan granite with low porosity, the lateral strain (LS) method is the simplest and most direct method to obtain the CILS. For high porosity sandstone, the result of lateral strain response (LSR) method is significantly smaller than that obtained by AE. The cumulative AE hits (CAEH) method heavily depends on the "S-shaped" characteristic of the cumulative AE hits curve, which limits its scope of application. The cumulative AE hits curve slope (CAHS) method, which determines the key inflection point of the cumulative AE hits curve by slope variation to determine the CICAHS, possesses the widest applicability and highest accuracy. The CI/UCS ratios of rocks with similar grain sizes decreases with increasing porosity. For Beishan granite, the average CICAHS is less than that of CILS. They are 0.43 UCS and 0.53 UCS, respectively. According to the residual strain data from the cyclic loading tests, the two crack initiation thresholds of Beishan granite can be clearly identified. These two crack initiation thresholds represent different crack initiation sequences in grain boundaries and different minerals.
资助项目National Natural Science Foundation of China[51234004] ; Project of Decommissioning of Nuclear Facilities and Radioactive Waste Management ; National Key Research and Development Program of China[2017YFC0804601] ; National Key Research and Development Program of China[2018YFC0808403]
WOS研究方向Engineering ; Geology
语种英语
WOS记录号WOS:000642839800003
出版者SPRINGER HEIDELBERG
源URL[http://119.78.100.198/handle/2S6PX9GI/27230]  
专题中科院武汉岩土力学所
通讯作者Wang, Guibin
作者单位1.Guizhou Univ, Coll Resources & Environm Engn, Guiyang 550025, Guizhou, Peoples R China
2.Chinese Acad Sci, Inst Rock & Soil Mech, State Key Lab Geomech & Geotech Engn, Wuhan 430071, Hubei, Peoples R China
3.Chongqing Univ, Sch Resources & Safety Engn, State Key Lab Coal Mine Disaster Dynam & Control, Chongqing 400044, Peoples R China
推荐引用方式
GB/T 7714
Tang, Minghao,Wang, Guibin,Chen, Shiwan,et al. Crack initiation stress of brittle rock with different porosities[J]. BULLETIN OF ENGINEERING GEOLOGY AND THE ENVIRONMENT,2021:16.
APA Tang, Minghao,Wang, Guibin,Chen, Shiwan,&Yang, Chunhe.(2021).Crack initiation stress of brittle rock with different porosities.BULLETIN OF ENGINEERING GEOLOGY AND THE ENVIRONMENT,16.
MLA Tang, Minghao,et al."Crack initiation stress of brittle rock with different porosities".BULLETIN OF ENGINEERING GEOLOGY AND THE ENVIRONMENT (2021):16.

入库方式: OAI收割

来源:武汉岩土力学研究所

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