“…In fact, non‐uniform flow fields can develop in porous media at any scale, provided that sufficiently strong spatial variations of permeability exist at that scale. In particular, pore‐scale preferential flow paths form in statistically stationary porous media owing to spatial fluctuations of pore size and connectivity (Adler, 1992; Adler & Berkowitz, 2000; Blunt, 2001; David, 1993; Bruderer‐Weng et al., 2004; Dai & Seol, 2014; Dullien, 1992; Fedorov & Adler, 2005; Moctezuma‐Berthier et al., 2004; see also Didari et al., 2020, in the case of non‐Newtonian fluid flow). As in reservoir‐scale flow, a greater non‐uniformity of the pore‐scale flow field is associated with enhanced dispersion of solute transport (Bernabé, Li, et al., 2015; Bernabé, Wang, et al., 2015; Bijeljic & Blunt, 2006; Kang et al., 2015; Li et al., 2018; Sahimi et al., 1986) and multi‐phase flow fingering (Blunt et al., 1992; Holtzman, 2016; Regaieg & Moncorgé, 2017; Tang et al., 2020).…”