Experimental Study of the Pore Structure Characterization in Shale With Different Particle Size

被引:18
|
作者
Zhang, Shuwen [1 ]
Xian, Xuefu [1 ]
Zhou, Junping [1 ]
Liu, Guojun [1 ]
Guo, Yaowen [1 ]
Zhao, Yuan [1 ]
Lu, Zhaohui [2 ]
机构
[1] Chongqing Univ, Coll Resource & Environm Sci, State Key Lab Coal Mine Disaster Dynam & Control, 174 Sha Zheng St, Chongqing 400044, Peoples R China
[2] Chongqing Inst Geol & Mineral Resources, 177-9 Changjiang 2nd Rd, Chongqing 400042, Peoples R China
基金
中国国家自然科学基金;
关键词
LOW-PRESSURE N-2; SILURIAN LONGMAXI SHALES; UPPER YANGTZE PLATFORM; GAS-ADSORPTION; FRACTAL CHARACTERISTICS; LACUSTRINE SHALE; SICHUAN BASIN; CHINA; POROSITY; COAL;
D O I
10.1115/1.4039022
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
In order to study the effects of particle size on the determination of pore structure in shale, the outcrop of Ordovician Wufeng (WF) and Silurian Longmaxi shale (LMX) samples from Sichuan basin were chosen and crushed into various particle sizes. Then, pore structure was analyzed by using low-pressure gas adsorption (LPGA) tests. The results show that the pore of shales is mainly composed of slit-type pores and open pores. The specific surface areas of shale are mainly contributed by micropores, while the largest proportion of the total pore volume in shale is contributed by mesopores. With the decreasing of particle size, the specific surface area of both samples is decreased, while average pore diameter and the total pore volume are increased gradually. The influences of particle size on the pore structure parameters are more significant for micropore and macropore, as the particle sizes decrease from 2.36 mm to 0.075 mm, the volume of micropores in Longmaxi shale increases from 0.283 cm(3) / 100 g to 0.501 cm(3) / 100 g with an increment almost 40%, while the volume of macropores decreases from 0.732 cm(3) / 100 g to 0.260 cm(3) / 100 g with a decrement about 50%. This study identified the fractal dimensions at relative pressures of 0-0.50 and 0.50-0.995 as D-1 and D-2, respectively. D-1 increases with the decrease of particle size of shale, while D-2 shows an opposite tendency in both shale samples.
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页数:10
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