“…The Hele–Shaw cell, a simple apparatus built with a small aperture between two transparent flat plates, has been extensively used to visualize the Darcy flow, including density-driven CO 2 transport. Furthermore, by varying several parameters in the cell, such as aperture, porosity, and vertical or horizontal permeability, it is possible to mimic the transport mechanism similar to that of CO 2 storage in different geological structures. − These experimental studies have adopted different visualization techniques to investigate the finger morphology during density-driven CO 2 transport, such as the pH indicator-based method, Schlieren method, particle image velocimetry, laser-induced fluorescence, and interferometry method. ,,− Furthermore, several studies have investigated scaling relationships to characterize the convective dissolution rate of CO 2 in brine formations. − Mojtaba et al developed a relationship between Sherwood and Rayleigh numbers and CO 2 convective flux at different Rayleigh numbers under 3.45 MPa and 182 < Ra < 20,860. Mahmoodpour et al showed scaling relationships between compensated flux and transition times between successive regimes in the system for experimental fluid with different salt types (NaCl and CaCl 2 ).…”