“…Displacement of one fluid by another within a porous medium is relevant to many processes such as oil and gas recovery from hydrocarbon reservoirs, CO 2 storage in deep saline aquifers, gas transport in fuel cells, nonaqueous phase liquid contaminant transport in groundwater aquifers, and water infiltration into soils. Immiscible displacement encountered in these applications is influenced, at the pore scale, by the properties of the grains (size distribution, roughness, mineralogy) and how they are arranged (pore topology and geometry) [e.g., [1][2][3][4][5], the properties of the fluids (chemical and physical constituents, which in turn alter fluid-fluid-grain contact angle, fluid-fluid interfacial tension, viscosity, and density) [e.g., [6][7][8], the fractional volumes of the fluids initially occupying the pores [e.g., 6,9,10], and the velocity of the fluids [e.g., 11,12].…”