A new anisotropic coal permeability model under the influence of stress, gas sorption and temperature: Development and verification

被引:37
|
作者
Zhou, H. W. [1 ,3 ]
Rong, T. L. [2 ]
Wang, L. J. [4 ]
Mou, R. Y. [5 ]
Ren, W. G. [5 ]
机构
[1] China Univ Min & Technol, Sch Energy & Min Engn, Beijing 100083, Peoples R China
[2] Henan Polytech Univ, Sch Energy Sci & Engn, Jiaozuo 454003, Henan, Peoples R China
[3] China Univ Min & Technol, State Key Lab Coal Resources & Safe Min, Beijing 100083, Peoples R China
[4] Natl Inst Clean & Low Carbon Energy, State Key Lab Water Resource Protect & Utilizat C, Beijing 100011, Peoples R China
[5] China Univ Min & Technol, Sch Mech & Civil Engn, Beijing 100083, Peoples R China
基金
中国国家自然科学基金;
关键词
Anisotropic permeability; Directional fracture strain; Three-dimensional stress; Matrix-fracture interaction; Thermal internal swelling coefficient; DEEP COAL; EVOLUTION; IMPACT; STRAIN; DEFORMATION; PROPAGATION; ADSORPTION; DESORPTION; PRESSURES; MOVEMENT;
D O I
10.1016/j.ijrmms.2020.104407
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
Modeling approach to permeability especially anisotropic permeability of coal in front of working face is of significance for gas extraction in coal mining. Considering three-dimensional stress condition and multi-field influence, in this study, an anisotropic permeability model was suggested for coal in front of working face. The anisotropic permeability was assumed to be controlled by the directional fracture strain under the condition of multi-field influence caused by effective stress, adsorption-desorption and thermal stress. The directional fracture strain induced by effective stress was governed by the generalized Hooke constitutive model. Based on the matrix-fracture interaction, the constitutive model of directional fracture strain induced by adsorption-desorption was established from the improved Langmuir equation. Assuming that the coal matrix was connected by the matrix bridge, the constitutive model of directional fracture strain induced by thermal stress was constructed by proposing the thermal internal swelling coefficient. Consequently, a new anisotropic coal permeability model was developed based on the directional fracture strain under the influence factor of stress, gas sorption and temperature. Moreover, the new permeability model was verified by laboratory tests under different effective stresses, gas pressures, temperatures and their combined influence. The theoretical results of proposed anisotropic permeability model may provide a better understanding of permeability evolution in multi-field coupling geological environment during coal mining.
引用
收藏
页数:15
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