“…Subsurface reactive fluid flow and solute transport is central to several pressing energy, environment, and societal challenges, including the geological storage of carbon dioxide (CO2). Mineral nucleation and growth is a prime example of interface-coupled dissolution and precipitation (ICDP) reactions giving rise to geometry evolution in porous media [1,[6][7][8][9][10][11]. When precipitation reactions are ample, crystal accumulations can dramatically reduce porosity (amount of void space) [8,10,12].…”