“…Studies for a long time mainly focused on zeolites of the FAU and MOR structural types. 5,8,29,31,34,38,40,47,52,71,[169][170][171]173,175,177,178,182,184,185,187,188 The interest in these two types of zeolites can be explained by their large pore openings, which allow easier diffusion of iodine (I 2 , CH 3 I) and non-iodine (NO x , CO x , H 2 O, etc.) compounds inside the zeolites.…”