“…The scCO 2 migration and storage in the natural sandstone or glass beads at the core scale, either homogeneous or heterogeneous, during the drainage process of the core flooding experiments are widely studied using many physical experimental tools: (1) the traditional optical technique by examining thin-sections in transmitted and reflected light or microscopic simulation model (e.g., a pore-scale network model, rock etching model) (Mattax, 1961;Jamaloei et al, 2010;Al-Shalabi and Ghosh, 2016); (2) scanning electron microscopy to observe the wettability of scCO 2 film on the surface of mineral grains, while considering the impacts of composition, size and distribution on micro-scale fluid flow (Combes et al, 1998;Kareem, 2015); (3) confocal laser scanning microscopy; (4) the greatly developed computed tomography (CT) technology, which can realize the three-dimensional (3D) visualization with a high resolution (several µm) and has already been widely used in investigating the distribution of residual oil (Turner et al, 2004;Youssef et al, 2010;Iglauer et al, 2012) or scCO 2 (Perrin and Benson, 2010;Krevor et al, 2012;Wang et al, 2013;Wei et al, 2014;Zhang et al, 2014;Miao et al, 2019;Xu et al, 2020); and (5) nuclear magnetic resonance imaging that is also widely used in studying fluid distribution in porous or fractured media at mm or µm resolution (Baldwin and Yamanashi, 1989;Suekane et al, 2009;Song et al, 2012;Yu et al, 2014;Prather, 2015).…”