“…The Brønsted acidity of zeolites, which results from the non-equivalent substitution of T-atoms (e.g., the substitution of Si by Al in TO 4 units as shown in Figure 3) and the subsequent charge-balancing by external, exchangeable cations (Na + , NH 4 + , H + , etc.) at the adjacent oxygen sites within the pore space, enables several characteristic functions, such as ion-exchange capacity, proton donating ability and ionic conductivity [3,[40][41][42]. These properties allow zeolites to be used as adsorbents, separators, ionic conductors, sensors, or catalysts [3,[40][41][42].…”