Quantitative analysis of microscopic structure and gas seepage characteristics of low-rank coal based on CT three-dimensional reconstruction of CT images and fractal theory

被引:170
|
作者
Wang, Gang [1 ,2 ]
Qin, Xiangjie [2 ]
Shen, Junnan [2 ]
Zhang, Zhenyu [3 ]
Han, Dongyang [2 ]
Jiang, Chenghao [2 ]
机构
[1] Shandong Univ Sci & Technol, Mine Disaster Prevent & Control Minist, State Key Lab Breeding Base, Qingdao 266590, Shandong, Peoples R China
[2] Shandong Univ Sci & Technol, Coll Min & Safety Engn, Qingdao 266590, Shandong, Peoples R China
[3] Chongqing Univ, State Key Lab Coal Mine Disaster Dynam & Control, Chongqing 400044, Peoples R China
基金
中国国家自然科学基金;
关键词
Micro-CT; 3D reconstruction; Fractal dimension; Porosity and permeability; Connectivity; PORE STRUCTURE CHARACTERIZATION; MU-CT; NUMERICAL-SIMULATION; FLOW; FRACTURES; DIMENSION; CONNECTIVITY; RESERVOIR; PERMEABILITY; SCALES;
D O I
10.1016/j.fuel.2019.115900
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
The pores/fractures are places for gas migration and storage in coal. Their structure complexity will directly influence the pore structure parameters and gas seepage properties of coal. Therefore, we selected 6 low-rank coal samples and quantitatively studied these influences utilizing the high-resolution micro computed tomography (mu CT) and fractal theory. The total pore structure and connected pore structure parameters of 6 samples were acquired from three-dimensional (3D) reconstruction of CT images. The fractal dimensions of total pore structures (D-f), solid structures (D-s) and connected pore structures (D-c) were calculated using 3D box-counting method. The relationship between D-f and porosity was analyzed through the 3D total pore model, and the relationships between D-c and connectivity as well as permeability were analyzed through the 3D connected pore model. The results show that D-f, which is between 2.10 and 2.43, could accurately describe the fractal characteristics of coal and the solid structure of coal is not fractal. The porosities of the 6 samples are between 3.33% and 12.18% and their relationship with D-f can be defined by a monotonically increasing power function. The larger the D-f is, the larger the porosity of the tested coal sample. D-c is between 2.28 and 2.32, the connectivity is between 0.54 and 0.83, and the permeability is in the range of 1.76-11.63 x 10(-8) m(2) (except samples 1 and 6). D-c is negatively correlated with connectivity and permeability and its relationship with connectivity and permeability can be represented by the quadratic function and monotone decreasing power function, respectively.
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页数:11
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