Fractal characteristics and significances of the nanopores in oil shales during hydrous pyrolysis

被引:2
作者
Sun, Lina [1 ]
Fu, Deliang [2 ]
Chai, Shunqi [3 ]
Yang, Wenxia [3 ]
Zhou, Kai [3 ]
Li, Wei [3 ]
机构
[1] Yangtze Univ, Hubei Cooperat Innovat Ctr Unconvent Oil & Gas, Wuhan 430100, Peoples R China
[2] Minist Land & Resources, Key Lab Coal Resources Explorat & Comprehens Util, Xian 710021, Peoples R China
[3] Yangtze Univ, Sch GeoSci, Wuhan 430100, Peoples R China
基金
中国国家自然科学基金;
关键词
Oil shales; Hydrous pyrolysis; Nitrogen adsorption method; FHH model; Pore structure; Fractal dimension; NORTHEASTERN BRITISH-COLUMBIA; CH4 ADSORPTION CAPACITY; FRACTURED VERTICAL WELL; PORE STRUCTURE; ORGANIC POROSITY; GAS; COAL; BASIN; DIMENSIONS; CHINA;
D O I
10.1007/s13202-019-00785-4
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 explore the pore characterizations in shales during organic matter evolution, a series of simulation experiments were conducted. The artificial hydrous pyrolysis was conducted on the same seven columned oil-shale samples at 250 degrees C, 300 degrees C, 350 degrees C, 375 degrees C, 400 degrees C, 450 degrees C and 500 degrees C, respectively. To obtain the characteristics of pore structures in shales, the unheated and the residual solid samples were analyzed by low-pressure nitrogen adsorption method. Based on the nitrogen adsorption isotherms, fractal dimensions were calculated by the model of Frenkel-Halsey-Hill, which also contained the fractal dimension of D-1 and D-2 before and after the relative pressure P/Po = 0.5, respectively. And then the relationships of simulation temperatures (thermal maturity), total-, macro-, meso- and micro-pores volumes, specific surface areas and diameters to fractal dimensions were investigated. The results showed that the average value of D-2 (2.6110) was higher than D-1 (2.4147) and there was a positive relationship between them (R-2 = 0.9237), which indicated that though D-2 and D-1 were more related to pore structures and surfaces, the better linear relationships suggested that both of them could be used in the representation of pore structures and surfaces in shales. With the thermal maturity increasing, the obvious fractal characteristics were, the complexity of pore structures were, which may be associated with the following cause-and-effect relationships. During the pyrolysis, the generation of hydrocarbons increased, as well as the consumption of TOC may increase the volume and surface area of total-, macro-, meso- and micro-pores but decrease the corresponding average diameter and then the quantities of smaller pores occurred and led to the strengthening of pore heterogeneity in shales. Based on the fractal characteristics, we also found the higher thermal maturity would result in the better connections among pores but worse permeability in shale, which further increased the gas adsorption quantity. Therefore, analyzing the fractal characteristics in shales could provide help for clarifying the characteristics of reservoirs as well as the comprehensive exploration and development of shale gas.
引用
收藏
页码:557 / 567
页数:11
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