Hydrogenated zinc oxide gives rise to complex vibrational spectra with many prominent features that remain unexplained. Our calculations have unambiguously shown that the presence of vacant oxygen and zinc interstitial surface sites is the only way to rationalize the observed spectra, notably the 1710 cm−1 zinc hydride stretching mode. The large number of such sites, which expose low-coordinated surface ions, are inherent at ionically reconstructed polar surfaces. The thermal stability of the sorbed hydrogen and the infrared activity of the resulting species are correlated with site coordination and coverage.
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French et al. (2002) studied this question.
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