Influence of reservoir properties on the methane adsorption capacity and fractal features of coal and shale in the upper Permian coal measures of the South Sichuan coalfield, China

被引:25
|
作者
Bao, Yuan [1 ,2 ]
Ju, Yiwen [2 ]
Yin, Zhongshan [3 ]
Xiong, Jianlong [3 ]
Wang, Guochang [4 ]
Qi, Yu [2 ]
机构
[1] Xian Univ Sci & Technol, Coll Geol & Environm, 58 Yanta Rd, Xian 710054, Shaanxi, Peoples R China
[2] Univ Chinese Acad Sci, Chinese Acad Sci, Coll Earth & Planetary Sci, Key Lab Computat Geodynam, 19 Yuquan Rd, Beijing 100049, Peoples R China
[3] Sichuan Prov Coalfield Geol Engn Invest & Design, Chengdu, Sichuan, Peoples R China
[4] St Francis Univ, Sch Sci, Loretto, PA USA
基金
中国国家自然科学基金;
关键词
Coal and shale; pore structure; methane adsorption; coal measures; South Sichuan coalfield; PORE STRUCTURE CHARACTERISTICS; GAS-ADSORPTION; EAST MARGIN; ORDOS BASIN; TRANSITIONAL SHALE; BEARING STRATA; BLACK SHALES; NORTH CHINA; ACCUMULATION; DIMENSIONS;
D O I
10.1177/0144598719877527
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
Pore structure plays an essential role in the reservoir heterogeneity and methane adsorption capacity. Significant progress has been made in the pore structure classification of porous materials (such as coal and shale). Considering the pore structure characterization of the coal measures and the measuring range of high-pressure mercury intrusion porosimetry and low-pressure N-2/CO2 gas adsorption, an integrated classification for coal and shale is provided. They are micropore (<2 nm), mesopore (2-100 nm), macropore A (100 nm-1 mu m), macropore B (1-10 mu m), and micro-fracture (>10 mu m). For coal and shale samples from Guxu mining area, the micropores and mesopores largely control the gas adsorption while micro-fractures and macropore B are significant for the storage and flow of free gas. The fractal dimensions calculated from limited N-2 adsorption data are not suitable for the coal samples which are not developed in mesopore and macropore A; these samples are precisely corresponding to the N-2 adsorption/desorption isotherms of group B (reversible isotherm). Furthermore, the main factors influencing the methane adsorption capacity of coal and shale in the coal measures are micropore frequency, micro-fracture width, clay mineral composition, and total organic carbon content.
引用
收藏
页码:57 / 78
页数:22
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