“…They showed that dipolar reorientation is due to Na + , and the TSDC spectrum analysis leads to an assessment of the interaction energies (70-90 kJ/ mol) between the hopped Na + ions and the zeolitic lattice. According to the Na + exchange degree and the nature of the occupied Na + sites, a quantitative and qualitative characterization of each site was given for dehydrated and hydrated Namordenite.The authors [153] determined characteristic terms dependent on (i) the hydration state, (ii) the site selectivity of sodium ions and water molecules, and (iii) the sodium/network interaction energy [154][155][156]. Upon hydration, half of the Na + ions remain embedded in site A, whereas the other Na + ions are extracted from the main channel sites (sites D and E).…”