Study on the failure mechanism of high-temperature granite under two cooling modes

被引:0
|
作者
Li, Chun [1 ]
Feng, Gan [2 ]
Zhang, Xinran [3 ,4 ]
Zhang, Chunwang [5 ]
Hu, Yaoqing [6 ]
Meng, Tao [7 ]
机构
[1] Taiyuan Univ Technol, Sch Min Engn, Taiyuan 030024, Shanxi, Peoples R China
[2] Sichuan Univ, Coll Water Resource & Hydropower, State Key Lab Hydraul & Mt River Engn, Chengdu 610065, Peoples R China
[3] Heilongjiang Commun Investment Grp Co Ltd, Harbin 150090, Peoples R China
[4] Nenjiang Kunyuan Min Co Ltd, Heihe 161400, Peoples R China
[5] Taiyuan Univ Technol, Ctr Shanxi Engn Res Coal Mine Intelligent Equipmen, Taiyuan 030024, Peoples R China
[6] Taiyuan Univ Technol, Key Lab Insitu Property Improving Min, Minist Educ, Taiyuan 030024, Shanxi, Peoples R China
[7] Taiyuan Univ Sci & Technol, Coll Chem & Biol Engn, Oil & Gas Storage & Transportat Engn Lab, Taiyuan 030024, Shanxi, Peoples R China
来源
SCIENTIFIC REPORTS | 2024年 / 14卷 / 01期
基金
中国国家自然科学基金;
关键词
FRACTURE-TOUGHNESS; HIGH-PRESSURE; ROCK; PERMEABILITY; BEHAVIOR; TRANSITION; SANDSTONE; CRACKS; DAMAGE;
D O I
10.1038/s41598-024-66073-2
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
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 600degree celsius, 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.
引用
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页数:12
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