Experimental study on the methane desorption-diffusion behavior of Longmaxi shale exposure to supercritical CO2

被引:12
|
作者
Qin, Chao [1 ,2 ]
Jiang, Yongdong [1 ]
Cao, Mengyao [2 ]
Zhou, Junping [1 ]
Song, Xiao [1 ]
Zuo, Shuangying [2 ]
Chen, Shiwan [2 ]
Luo, Yahuang [3 ]
Xiao, Siyou [4 ]
Yin, Hong [5 ]
Du, Xidong [6 ]
机构
[1] Chongqing Univ, State Key Lab Coal Mine Disaster Dynam & Control, Chongqing 400044, Peoples R China
[2] Guizhou Univ, Coll Resources & Environm Engn, Key Lab Karst Georesources & Environm, Minist Educ, Guiyang 550025, Peoples R China
[3] Chongqing Construct Engn Qual Supervis & Inspect C, Chongqing 400000, Peoples R China
[4] Liupanshui Normal Univ, Coll Mines & Civil Engn, Liupanshui 553000, Peoples R China
[5] Chongqing Technol & Business Univ, Engn Res Ctr Waste Oil Recovery Technol & Equipmen, Minist Educ, Chongqing 400067, Peoples R China
[6] Kunming Univ Sci & Technol, Fac Land Resources Engn, Kunming 650093, Yunnan, Peoples R China
基金
中国国家自然科学基金;
关键词
Shale gas; Supercritical carbon dioxide; Desorption kinetics; Diffusion coefficient; CO2 enhanced shale gas recovery; ENHANCED GAS RECOVERY; ADSORPTION-KINETICS; TREATMENT TIME; PRESSURE; STORAGE; COAL; TEMPERATURE;
D O I
10.1016/j.energy.2022.125456
中图分类号
O414.1 [热力学];
学科分类号
摘要
Desorption-diffusion behaviors of CH4 in shale after supercritical CO2 (ScCO2) injection are closely related to CO2 enhanced shale gas recovery (CO2-ESGR). A self-developed gas desorption test system was used to measure the desorption kinetics of CH4 in shale collected from Sichuan Basin at different ScCO2 exposure pressures (8, 12, 16 MPa) and temperatures (40, 60, 80 degrees C), and the low-pressure N-2 adsorption was performed to evaluate the variations of pore structure of shale. Results indicate that the desorption kinetics curves of CH4 in shale exhibit typical Langmuir characteristics under different desorption pressures, and the kinetics data were fitted by unipore and bidisperse diffusion models, manifesting that the diffusion of CH4 in the shale samples are dominated by macroporous channel (>95%). With increasing desorption pressure, the desorption capacity of CH4 in shale (n(de)) increased, while the diffusion coefficient of CH4 in shale (D) decreased. Additionally, the n(de) and D increased after ScCO2 exposure, and exhibited a slight exposure pressure and temperature dependence, which is mainly caused by the decrease of specific surface area and the widening of microstructure in shale, implying that the ScCO2-shale interaction can promote the desorption-diffusion of CH4 in shale. This study provides a theoretical reference for CO2-ESGR.
引用
收藏
页数:12
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