“…Some researchers studied both thepores and fractures in coals. They characterized such complex natural pores and fractures by many experimental, numerical and analytical methods, including X‐ray micro‐computed tomography (micro‐CT) (Ju et al., 2018; Oleszko et al., 2015; Shah, Crawshaw, & Boek, 2017; Zhou et al., 2018), thin section (Lyu et al., 2019), nuclear magnetic resonance (NMR) (Sun et al., 2017), scanning electron microscope (SEM), focused ion beam scanning electron microscopy (FIB‐SEM) (Nie et al., 2015), fractal geometry methods (Cai et al., 2016; Chen & Yao, 2017; Jin et al., 2019; Pandey & Harpalani, 2018), acoustic emission and ultrasonic techniques (Kong et al., 2017; Zhang & Li, 2017), digital drilling imaging technology (Jin et al., 2015; Xie et al., 2015), 2D particle flow code (PFC2D) (Z. Lu et al., 2019; T. Wang et al., 2014, 2017), the discrete element method (Han et al., 2012; McLennan et al., 2010; Shimizu et al., 2011), finite element method, and boundary element method (Hossain & Rahman, 2008) from fracture to matrix, from 2D to 3D, from real scanning to reconstructed realization, and from static to dynamic. For porous media without microfractures, such as sandstone, due to the high self‐similarity of the pores, the fractal theory has been applied well in structure characterization (Chen & Yao, 2017; Chen et al., 2017).…”