Thermal behavior of minerals in shale and its influence on evolution of gas-flow channels under thermal shock

被引:2
作者
Jiang, Changbao [1 ]
Xu, Ling [1 ]
Chen, Yufei [2 ]
Liu, Wei [3 ]
Wang, Botao [1 ]
Liu, Ping [4 ]
Deng, Bozhi [1 ]
机构
[1] Chongqing Univ, Sch Resources & Safety Engn, State Key Lab Coal Mine Disaster Dynam & Control, Chongqing 400030, Peoples R China
[2] Southwest Petr Univ, Sch Geosci & Technol, Chengdu 610500, Sichuan, Peoples R China
[3] Jining 3 Mine, Yankuang Energy Grp Co Ltd, Jining 272169, Peoples R China
[4] Guizhou Univ, Min Coll, Guiyang 550025, Peoples R China
来源
GAS SCIENCE AND ENGINEERING | 2024年 / 121卷
关键词
Shale gas; Reservoir thermal treatment; Mineral thermal behavior; Gas -flow channel evolution; Threshold temperature; ORGANIC-RICH SHALE; HIGH-TEMPERATURE; PERMEABILITY; ADSORPTION; PORE; SICHUAN; COALS; MODEL;
D O I
10.1016/j.jgsce.2023.205183
中图分类号
TE [石油、天然气工业]; TK [能源与动力工程];
学科分类号
0807 ; 0820 ;
摘要
Thermal shock-induced damage can significantly enhance the connectivity of the rock's fracture network. Thermal Enhanced Recovery (TER) technology holds promising potential for application in shale gas production. Nevertheless, there is still a lack of direct experimental studies focusing on the evolution of shale's gas-flow channels and the mechanism of thermal fracturing in shale under the influence of thermal shock. In this study, we initially investigated the impact of thermal shock on various minerals in shale through X-ray diffraction (XRD) analysis and scanning electron microscope (SEM) imaging, and examined the mass and heat variation with temperature using Thermogravimetry-Differential Scanning Calorimetry (TG-DSC) testing. Subsequently, we assessed the alterations in shale's internal structure due to thermal shock through low-temperature gas (N2) adsorption (LTGA) analysis, and observed the distribution and expansion patterns of shale fractures under thermal shock using computed tomography (CT). Finally, we evaluated the changes in shale permeability before and after thermal shock. The findings indicate that quartz, feldspar, and clay exhibit relatively stable behavior in shale under thermal shock, whereas carbonate and pyrite are prone to crack. Under the combined influence of mineral cracking and thermal stress, the internal pore structure of shale tends to enlarge in size while reducing in surface area. The substantial decrease in pore specific surface area highlights the considerable reduction in gas adsorption capacity. Furthermore, fractures expand along the bedding planes as surface fractures. The expansion of pores and fractures promotes the formation of primary gas-flow channels. In addition, the aforementioned test results demonstrate a high level of consistency, specifically highlighting a distinct threshold temperature (500 degrees C) for the alteration of various physical parameters of shale during thermal shock. This study is anticipated to offer insights into the implementation of TER technology in the oil and gas industry.
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页数:14
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