Classical molecular dynamics and Grand Canonical Monte Carlo simulations are carried out for sorbates (CO 2 and N 2 ) in zeolite NaKA using a universal type ab initio force field. By combining the results of these simulations, we reproduce the CO 2 uptake as a function of the K + content in the zeolite NaKA as measured experimentally by Liu et al.1 The experiment yielded an exceptionally high CO 2 -over-N 2 selectivity of >200 at a specific K + /(K + + Na + ) ratio of 17 atom %. This high selectivity could be attributed to the nonlinear uptake dependency of the K + /(K + + Na + ) ratio measured for both CO 2 and N 2 . Additionally, our simulations show a strong coupling between the self-diffusion of CO 2 and the site-to-site jumping rate of the extra-framework cations. These results show that this nonlinear uptake dependency of CO 2 is the result of molecular sieving. Following this, our simulations conclude that both thermodynamic and kinetic contributions must be taken into account when modeling the uptake of this and similar materials with the same functionalities.
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Mace et al. (2013) studied this question.
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