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Study on the failure mechanism of high-temperature granite under two cooling modes.
Li, Chun; Feng, Gan; Zhang, Xinran; Zhang, Chunwang; Hu, Yaoqing; Meng, Tao.
Affiliation
  • Li C; School of Mining Engineering, Taiyuan University of Technology, Taiyuan, 030024, Shanxi, China.
  • Feng G; State Key Laboratory of Hydraulics and Mountain River Engineering, College of Water Resource & Hydropower, Sichuan University, Chengdu, 610065, China.
  • Zhang X; Heilongjiang Geology and Mineral Resources Investment Group Co., Ltd., Harbin, 150090, China. 13796061286@163.com.
  • Zhang C; Nenjiang Kunyuan Mining Co., Ltd., Heihe, 161400, China. 13796061286@163.com.
  • Hu Y; Center of Shanxi Engineering Research for Coal Mine Intelligent Equipment, Taiyuan University of Technology, Taiyuan, 030024, China.
  • Meng T; Key Laboratory of In-situ Property-improving Mining of Ministry of Education, Taiyuan University of Technology, Taiyuan, 030024, Shanxi, China.
Sci Rep ; 14(1): 15630, 2024 Jul 07.
Article in En | MEDLINE | ID: mdl-38972905
ABSTRACT
In the geothermal development of hot dry rock (HDR), both the drilling of the wellbore and the heat exchange of the heat reservoir involve the effects of different cold and hot conditions on the high-temperature rock mass. The testing machine for rock mechanics was used to conduct a uniaxial compression test and carry out micro testing on the treated samples; furthermore, with the help of scanning electron microscopy the fracture mechanism of granite subjected to different temperatures and cooling methods was studied. The results show (1) With the gradual increase in temperature, the compressive strength of granite under the two cooling methods gradually decreases. (2) The failure modes of the samples under the two cooling methods are mainly shear failure of the "Y" type. The degree of damage of the sample under water cooling is significantly greater than that under natural cooling. Electron micrographs could confirm these results. (3) It can be obtained by testing the mineral composition and element changes of granite at different temperatures. When the temperature reaches 600℃, its change is more pronounced. The results of this study can provide a theoretical reference for the failure of the wellbore and the degree of fracture of the thermal reservoir rock mass during geothermal development.

Full text: 1 Collection: 01-internacional Database: MEDLINE Language: En Journal: Sci Rep Year: 2024 Document type: Article Affiliation country: China Country of publication: Reino Unido

Full text: 1 Collection: 01-internacional Database: MEDLINE Language: En Journal: Sci Rep Year: 2024 Document type: Article Affiliation country: China Country of publication: Reino Unido