中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Effects of thawing-induced softening on fracture behaviors of frozen rock

文献类型:期刊论文

作者Wang, Ting2; Jia, Hailiang3; Sun, Qiang2; Tan, Xianjun1; Tang, Liyun3
刊名JOURNAL OF ROCK MECHANICS AND GEOTECHNICAL ENGINEERING
出版日期2024-03-01
卷号16期号:3页码:979-989
关键词Frozen sandstone Different thawing temperature Fracture toughness Microcrack propagation process Unfrozen water content
ISSN号1674-7755
DOI10.1016/j.jrmge.2023.07.016
英文摘要Due to the presence of ice and unfrozen water in pores of frozen rock, the rock fracture behaviors are susceptible to temperature. In this study, the potential thawing-induced softening effects on the fracture behaviors of frozen rock is evaluated by testing the tension fracture toughness ( K IC ) of frozen rock at different temperatures (i.e. - 20 degrees C, - 15 degrees C, - 12 degrees C, - 10 degrees C, - 8 degrees C, - 6 degrees C, - 4 degrees C, - 2 degrees C, and 0 degrees C). Acoustic emission (AE) and digital image correlation (DIC) methods are utilized to analyze the microcrack propagation during fracturing. The melting of pore ice is measured using nuclear magnetic resonance (NMR) method. The results indicate that: (1) The K IC of frozen rock decreases moderately between - 20 degrees C and - 4 degrees C, and rapidly between - 4 degrees C and 0 degrees C. (2) At - 20 degrees C to - 4 degrees C, the fracturing process, deduced from the DIC results at the notch tip, exhibits three stages: elastic deformation, microcrack propagation and microcrack coalescence. However, at - 4 degrees C-0 degrees C, only the latter two stages are observed. (3) At - 4 degrees C-0 degrees C, the AE activities during fracturing are less than that at - 20 degrees C to - 4 degrees C, while more small events are reported. (4) The NMR results demonstrate a reverse variation trend in pore ice content with increasing temperature, that is, a moderate decrease is followed by a sharp decrease and - 4 degrees C is exactly the critical temperature. Next, we interpret the thawing-induced softening effect by linking the evolution in microscopic structure of frozen rock with its macroscopic fracture behaviors as follow: from - 20 degrees C to - 4 degrees C, the thickening of the unfrozen water film diminishes the cementation strength between ice and rock skeleton, leading to the decrease in fracture parameters. From - 4 degrees C to 0 degrees C, the cementation effect of ice almost vanishes, and the filling effect of pore ice is reduced signi ficantly, which facilitates microcrack propagation and thus the easier fracture of frozen rocks. (c) 2024 Institute of Rock and Soil Mechanics, Chinese Academy of Sciences. Production and hosting by Elsevier B.V. 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[42271148]
WOS研究方向Engineering
语种英语
WOS记录号WOS:001234779200001
出版者SCIENCE PRESS
源URL[http://119.78.100.198/handle/2S6PX9GI/41521]  
专题中科院武汉岩土力学所
通讯作者Jia, Hailiang
作者单位1.Chinese Acad Sci, Inst Rock & Soil Mech, State Key Lab Geomech & Geotech Engn, Wuhan 430064, Peoples R China
2.Xian Univ Sci & Technol, Coll Geol & Environm, Xian 710054, Peoples R China
3.Xian Univ Sci & Technol, Coll Architecture & Civil Engn, Xian 710054, Peoples R China
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Wang, Ting,Jia, Hailiang,Sun, Qiang,et al. Effects of thawing-induced softening on fracture behaviors of frozen rock[J]. JOURNAL OF ROCK MECHANICS AND GEOTECHNICAL ENGINEERING,2024,16(3):979-989.
APA Wang, Ting,Jia, Hailiang,Sun, Qiang,Tan, Xianjun,&Tang, Liyun.(2024).Effects of thawing-induced softening on fracture behaviors of frozen rock.JOURNAL OF ROCK MECHANICS AND GEOTECHNICAL ENGINEERING,16(3),979-989.
MLA Wang, Ting,et al."Effects of thawing-induced softening on fracture behaviors of frozen rock".JOURNAL OF ROCK MECHANICS AND GEOTECHNICAL ENGINEERING 16.3(2024):979-989.

入库方式: OAI收割

来源:武汉岩土力学研究所

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