To investigate long-term CO 2 behavior in geological formations and quantification of possible CO 2 leaks, it is crucial to investigate the potential mobility of CO 2 dissolved in brines over a wide range of spatial and temporal scales and density distributions in geological media. In this work, the mass transfer of aqueous CO 2 in brines has been investigated by means of a chemical potential gradient model based on non-equilibrium thermodynamics in which the statistical associating fluid theory equation of state was used to calculate the fugacity coefficient of CO 2 in brine. The investigation shows that the interfacial concentration of aqueous CO 2 and the corresponding density both increase with increasing pressure and decreasing temperature; the effective diffusion coefficients decrease initially and then increase with increasing pressure; and the density of the CO 2 -disolved brines increases with decreasing CO 2 pressure in the CO 2 dissolution process. The aqueous CO 2 concentration profiles obtained by the chemical potential gradient model are considerably different from those obtained by the concentration gradient model, which shows the importance of considering non-ideality, especially when the pressure is high.