A new insight into the role played by water molecules in the crystalline framework of type-A zeolites is
demonstrated. The effect of dehydration on the effective free aperture dimension, D
f, is studied by utilizing
temperature-programmed decapsulation of He and Ne. The interplay between the various known mechanisms
governing D
f is directly sensed by the decapsulation behavior of differently sized inert atoms. The results are
qualitatively interpreted using pure dimensional considerations, revealing the occurrence of a strict relation
between the content of water molecules and the redistribution of zeolitic cations in determining D
f. Water
content is shown to have a strong effect on the blocking state of the O8 and O6 zeolitic windows, which in
turn, governs gas accessibility to the α and β cages. It is proposed that D
f is regulated via a subtle balance
between two coupled principal mechanisms. One involves direct lattice adjustments, where two opposite
sub-mechanisms seem to play competitive roles. Removal of water molecules by simultaneous heating and
pumping enlarges D
f, while hydroxyl groups elimination from within the zeolitic channels results in their
partial collapse, thus reducing D
f. The second mechanism involves the regulation of aperture blocking via
relocations of the counterions initiated by increasing vacancies due to removal of water molecules. While
dehydration continuously contracts the O6 apertures, a two-stage effect is observed for the wider O8 windows.
Upon dehydration at large water contents, O8 apertures are reduced; then, beyond a critical extent of dehydration,
the net effect is reversed, widening the O8 windows.