中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
In-situ observations of damage-fracture evolution in surrounding rock upon unloading in 2400-m-deep tunnels

文献类型:期刊论文

作者Guo, Haosen2,4; Sun, Qiancheng2,3; Feng, Guangliang1; Li, Shaojun1; Xiao, Yaxun1
刊名INTERNATIONAL JOURNAL OF MINING SCIENCE AND TECHNOLOGY
出版日期2023-04-01
卷号33期号:4页码:437-446
关键词Deep tunnel Fractured zone Damaged zone In -situ observation Unloading of rock mass
ISSN号2095-2686
DOI10.1016/j.ijmst.2022.11.008
英文摘要The damage-fracture evolution of deep rock mass has obvious particularity, which is revealed in 2400-m -deep tunnels by field tests. The evolution of the excavation damaged zone depth is consistent with that of the fractured zone depth. The ratio of the excavation damaged zone depth to the excavation fractured zone depth is greater than 2.0 in a rock mass with both high strength and good integrity, but less than 1.5 in a rock mass with lower strength or poor integrity. Zonal disintegration in a rock mass with high strength and fair integrity is more likely to occur when it contains more than two groups of primary fractures in damaged zones. Fractures develop outward in zonal disintegration but are totally different from the single-zone fracture, in which the fractures develop inward, and it is the starting position of the fractured zone when the excavation surface of the middle pilot is 7-9 m close to the pre-set borehole and it stops after the excavation surface of the baseplate is 11-14 m away. The most intense evolution occurs around 2-4 m from the pre-set borehole in the sidewall expansion stage. The research results provide a reference for the monitoring scheme and support design of CJPL-III in its future construction.(c) 2023 Published by Elsevier B.V. on behalf of China University of Mining & Technology. This is an open access article under the CC BY-NC-ND license (http://creativecommons.org/licenses/by-nc-nd/4.0/).
资助项目National Natural Science Foundation of China[51909136] ; National Natural Science Foundation of China[42177168] ; Project of Youth Innovation Promotion Association of Chinese Academy of Sciences[2021326] ; Open Research Fund of Key Laboratory of Geological Hazards on Three Gorges Reservoir Area (China Three Gorges University) , Ministry of Education[2020KDZ03]
WOS研究方向Mining & Mineral Processing
语种英语
WOS记录号WOS:001090459400001
出版者ELSEVIER
源URL[http://119.78.100.198/handle/2S6PX9GI/39705]  
专题中科院武汉岩土力学所
通讯作者Sun, Qiancheng; Feng, Guangliang
作者单位1.Chinese Acad Sci, Inst Rock & Soil Mech, State Key Lab Geomech & Geotech Engn, Wuhan 430071, Peoples R China
2.Minist Educ, Key Lab Geol Hazards Three Gorges Reservoir Area, Yichang 443002, Peoples R China
3.China Three Gorges Univ, Coll Civil Engn & Architecture, Yichang 443002, Peoples R China
4.Jiangxi Key Lab Disaster Prevent mitigat & Emergen, Nanchang 330013, Peoples R China
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GB/T 7714
Guo, Haosen,Sun, Qiancheng,Feng, Guangliang,et al. In-situ observations of damage-fracture evolution in surrounding rock upon unloading in 2400-m-deep tunnels[J]. INTERNATIONAL JOURNAL OF MINING SCIENCE AND TECHNOLOGY,2023,33(4):437-446.
APA Guo, Haosen,Sun, Qiancheng,Feng, Guangliang,Li, Shaojun,&Xiao, Yaxun.(2023).In-situ observations of damage-fracture evolution in surrounding rock upon unloading in 2400-m-deep tunnels.INTERNATIONAL JOURNAL OF MINING SCIENCE AND TECHNOLOGY,33(4),437-446.
MLA Guo, Haosen,et al."In-situ observations of damage-fracture evolution in surrounding rock upon unloading in 2400-m-deep tunnels".INTERNATIONAL JOURNAL OF MINING SCIENCE AND TECHNOLOGY 33.4(2023):437-446.

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来源:武汉岩土力学研究所

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