“…Quantifying the local capillary trapped fraction has proved difficult as it depends on the exact geometry of the geologic depositional pattern (fabric), and the grain size contrast between depositional layers (Krishnamurthy et al., 2019; Meckel et al., 2017; Mishra & Haese, 2020). Numerical simulations have provided estimates of the effect of heterogeneities at different scales (Gershenzon et al., 2017; Jackson & Krevor, 2020; Shao et al., 2022; Trevisan, Krishnamurthy, & Meckel, 2017; Zahasky et al., 2020), but analogous laboratory experiments to corroborate these results have been lacking. Experiments have been limited to cores (Krishnamurthy et al., 2017; Manoorkar et al., 2021; Moreno & Rabinovich, 2021; Ni et al., 2019; Oh et al., 2015) where the depositional patterns are underrepresented due to size limitation (Huang et al., 1995; Ringrose & Bentley, 2015; Ringrose et al., 1993), and/or intermediate scale physical models (Trevisan et al., 2014; Trevisan et al., 2015; Trevisan, Pini, et al., 2017) which have heretofore been simplistic and blocky.…”