“…In a different context, over the last few years, the geological storage of CO 2 has been increasingly considered a promising approach toward a green environment where CO 2 is permanently immobilized in deep underground formations of the earth’s subsurface, for instance, depleted oil/gas reservoirs, aquifers, or coal bed seams. ,,− Here, the injected CO 2 dissolves in the formation brine and establishes acidic conditions, , which in turn induces geochemical interactions with the formed minerals that lead to the dissolution of minerals, for example, carbonates, feldspar, kaolinite, calcite, chlorite, or clays . These interactions directly affect the reservoir permeability, porosity, rock strength, and capillary pressure, and hence, the flow of CO 2 through the porous media along with CO 2 storage capacity.…”