Na+/K+ ion exchange in silicate glasses: Results from 17O 3QMAS NMR

The effect of Na+/K+ ion exchange on the distribution of the modifier ions and on their interaction with the oxygen atoms in the network is investigated in ternary Na,Mg- and Na,Ca- silicate glasses using 17O triple-quantum magic-angle-spinning nuclear magnetic resonance spectroscopy. The results indicate that the K+ ions preferentially exchange with the Na+ ions present in {Na,Ca}-NBO and {Na,Mg}-NBO environments, while the Na-NBO environment is not significantly affected. Remelting of the ion-exchanged glasses leads to a homogenization of the modifier ion distribution around the NBO sites. The dynamical site preference for the Na+/K+ ion exchange has far-reaching implications in our understanding of the alkali ion transport and more specifically of the mixed-alkali effect in silicate glasses.SCOPUS: ar.jinfo:eu-repo/semantics/publishe

Structural modifications induced by Na+/K+ ion exchange in silicate glasses: A multinuclear NMR spectroscopic study

The structural mechanisms of stress relaxation during Na+/K+ ion exchange is studied in a variety of Na silicate glasses with and without alkaline-earth modifiers, using one and two-dimensional 23Na and 29Si nuclear magnetic resonance (NMR) spectroscopy. The results suggest that significant structural modifications accompany the Na+/K+ ion exchange process in the form of a shortening of the average Na[sbnd]O and Si[sbnd]NBO distances and an opening of the Si[sbnd]O[sbnd]Si angles without any detectable change in the Qn speciation. These trends are similar to those observed in analogous mixed Na,K glasses derived via the melt-quench route, with increasing K:Na ratio. Consequently, the ion-exchange-induced reorganization of the glass network is accompanied by a partial relaxation of the stress generated by the exchange of smaller Na+ by the larger K+ and better accommodation of the latter ion as a modifier.SCOPUS: ar.jinfo:eu-repo/semantics/publishe