17 O NMR and Computational Study of a Tetrasiliconiobate Ion, [H 2+ x Si 4 Nb 16 O 56 ] (14− x )

Rates of oxygen‐isotope exchange were measured in the tetrasiliconiobate ion [H 2+ x Si 4 Nb 16 O 56 ] (14− x )− to better understand how large oxide ions interact with water. The molecule has 19 nonequivalent oxygen sites and is sufficiently complex to evaluate hypotheses derived from our previous work on smaller clusters. We want to examine the extent to which individual oxygen atoms react independently with particular attention given to the order of protonation of the various oxygen sites as the pH decreases from 13 to 6. As in our previous work, we find that the set of oxygen sites reacts at rates that vary over approximately 10 4 across the molecule at 6