Study on the Energy Evolution and Damage Mechanism of Fractured Rock Mass Under Stress-Seepage Coupling

被引:1
|
作者
Shuang, Haiqing [1 ,2 ,3 ]
Liu, Xiangxiang [1 ,2 ]
Zhou, Bin [1 ,2 ,3 ]
Cheng, Liang [1 ,2 ,3 ]
Lin, Haifei [1 ,2 ,3 ]
Hu, Biao [1 ,2 ,3 ]
Liu, Zijia [1 ,2 ]
机构
[1] Xian Univ Sci & Technol, Coll Safety Sci & Engn, Xian 710054, Peoples R China
[2] Xian Univ Sci & Technol, Minist Educ, Key Lab Western Mine Exploitat & Hazard Prevent, Xian 710054, Peoples R China
[3] Shaanxi Prov Key Lab Gas Disaster Prevent & Contro, Xian 710054, Peoples R China
基金
中国博士后科学基金; 中国国家自然科学基金;
关键词
stress-seepage coupling; intermittent fissure; energy evolution; damage characteristics; FAILURE; COAL;
D O I
10.3390/pr13010270
中图分类号
TQ [化学工业];
学科分类号
0817 ;
摘要
In the process of deep mining, the dynamic disasters of coal and rock occur frequently under the action of high stress and high seepage pressure, the essence of which is energy-driven coal rock failure. In order to explore the energy evolution law and damage mechanism of sandstone with intermittent cracks under the coupling effect of stress and seepage, in this paper, by comparing the differences in mechanical characteristics between fractured rock and intact rock, the energy evolution characteristics, crack propagation, and micro-damage mechanism of fractured rock under different confining pressures and seepage pressures are analyzed. The research shows that: (1) The local stress drop phenomenon occurs in the fractured rock during the loading process, and the stress-strain shape is 'bimodal'. At the same time, there is stress concentration at both ends of the fracture. (2) The energy conversion of the fractured rock changes in stages during loading. As confining pressure rises, the energy storage limit and the maximum dissipation energy go up. The increase in seepage pressure reduces the energy storage limit, while the dissipation energy shows an upward trend. The energy consumption ratio curve shows 'concave' evolution during the loading process. (3) Based on the dissipation energy and residual stress, the damage state of the specimen is analyzed, and the proposed damage variable can reasonably explain the whole process of the damage evolution of intermittent fractured rock under stress and seepage. (4) The increase in confining pressure increases the friction between the particles inside the sample and promotes the transformation of the sample from tensile failure to shear failure. The seepage pressure reduces the friction between the particles in the sample through the air wedge effect to deepen the damage degree, thus promoting the tensile failure of the sample.
引用
收藏
页数:25
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