Impact of the Si/Al ratio on the selective capture of iodine compounds in silver-mordenite: a periodic DFT study

Silver modified zeolites with a mordenite structure can capture volatile iodine compounds (I 2 and ICH 3 ) which can be released during a severe nuclear accident. However under these particular conditions, molecules such as CO and H 2 O present in the containment atmosphere are expected to inhibit the adsorption of iodine compounds. In the present work, periodic density functional theory calculations have been carried out to investigate the interaction of I 2 , ICH 3 , H 2 O and CO molecules in silver-exchanged mordenite with various Si/Al ratios with the aim of finding values that favor a selective adsorption of I 2 and ICH 3 . Computational results show that the interaction energies of CO and H 2 O remain of the same order of magnitude (from −120 to −140 kJ mol −1 for CO and from −90 to −120 kJ mol −1 for H 2 O) for all the investigated Si/Al ratios. In contrast, ICH 3 is increasingly strongly adsorbed as the Si/Al ratio decreases, from around −145 kJ mol −1 when Si/Al = 47 to −190 kJ mol −1 for Si/Al = 5. The same trend is observed for I 2 with a larger amplitude: from −135 kJ mol −1 for Si/Al = 47 to −300 kJ mol −1 for Si/Al = 5. Therefore, the use of silver-exchanged mordenite with Si/Al ratios of 5 or 11 would drastically limit the inhibiting effect of contaminants on the adsorption of volatile iodine species. Also for the same ratios, a spontaneous dissociation of I 2 during its adsorption is observed, leading to the formation of AgI complexes which are prerequisite for the immobilization of iodine in the long term. Decreasing the Si/Al ratio in silver exchanged mordenite drastically limits the potential inhibiting effect of H 2 O and CO on the adsorption of I 2 and ICH 3 , and allows a spontaneous dissociation of I 2 leading to the formation of AgI complexes.