Chemical-mechanical coupling effects on the permeability of shale subjected to supercritical CO2-water exposure

被引:48
作者
Yang, Kang [1 ,2 ]
Zhou, Junping [1 ,2 ]
Xian, Xuefu [1 ,2 ]
Zhou, Lei [1 ,2 ]
Zhang, Chengpeng [1 ,2 ]
Tian, Shifeng [1 ,2 ]
Lu, Zhaohui [3 ]
Zhang, Fengshou [4 ]
机构
[1] Chongqing Univ, State Key Lab Coal Mine Disaster Dynam & Control, Chongqing 400044, Peoples R China
[2] Chongqing Univ, Sch Resources & Safety Engn, Chongqing 400044, Peoples R China
[3] Chongqing Inst Geol & Mineral Resources, Natl Joint Engn Res Ctr Shale Gas Explorat & Dev, Chongqing 400042, Peoples R China
[4] Tongji Univ, Coll Civil Engn, Dept Geotech Engn, Shanghai 200092, Peoples R China
基金
中国国家自然科学基金;
关键词
Carbon dioxide sequestration; Shale gas; CO2 -Water-shale interaction; Permeability; Chemical-mechanical coupling effects; CO2-BRINE-ROCK INTERACTION; CO2; ADSORPTION; PORE STRUCTURE; STRESS; WATER; COAL; EVOLUTION; STORAGE; PHYSICS; MATRIX;
D O I
10.1016/j.energy.2022.123591
中图分类号
O414.1 [热力学];
学科分类号
摘要
The permeability of shale reservoir rock and caprock is the key parameters influencing the shale gas production and the storage security of CO2. During the CO2 enhanced shale gas recovery, the issue of how the coupled chemical-mechanical process control the evolution of porosity and permeability in shale remains undetermined. In this study, multiple tests were conducted to obtained the shale properties alteration induced by ScCO2-water exposure, including the mineral compositions measured by XRD, XRF and ICP-OES, the mechanical properties measured by uniaxial compression test, the pore structure and permeability of shale measured using nuclear magnetic resonance (NMR) at different confining stresses over a range of injection pressures. After ScCO2-water exposure, the contents of carbonate and clay minerals decreased, while the contents of quartz and feldspar increased. The geochemical reaction altered the pore structure and mechanical properties of shale, resulting in the enlargement of pore, the decrease in uniaxial compressive strength and elastic modulus of shale, which in turn impact the porosity and permeability evolution in shale. At the unstressed state, the pore in shale was enlarged by the pure chemical reaction, leading to the increase in porosity and the initial permeability of shale. At the stressed condition, the porosity and permeability of shale is controlled by the chemical-mechanical coupling effects, the permeability of CO2-water treated shale sample is lower than that of the untreated shale sample, which can be explained by the increase in stress sensitivity of shale permeability induced by the mechanical weakening, as the compressibility Cf and permeability change rate Dkc were increased after ScCO2-water exposure. In addition, the stress sensitivity of permeability in shale is stress dependent, for both untreated and ScCO2-water treated shale samples, the C-f and delta k(c) of shale shown a negative relation with effective stress. At a higher effective stress condition, the change in the permeability of ScCO2-water treated shale is more significantly enhanced. The results demonstrated that the ScCO2-water-shale interaction induced chemical-mechanical effect may decrease the permeability of shale at in-situ stress condition, and hence adversely affecting the efficiency of gas recovery and CO2 sequestration in shale formation. (C)& nbsp;2022 Published by Elsevier Ltd.
引用
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页数:16
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