Abstract
Anatase is a metastable polymorph of . In contrast to the more widely studied rutile, O vacancies (’s) are not stable at the anatase (101) surface. Low-temperature STM shows that surface ’s, created by electron bombardment at 105 K, start migrating to subsurface sites at temperatures . After an initial decrease of the density, a temperature-dependent dynamic equilibrium is established where ’s move to subsurface sites and back again, as seen in time-lapse STM images. We estimate that activation energies for subsurface migration lie between 0.6 and 1.2 eV; in comparison, density functional theory calculations predict a barrier of ca. 0.75 eV. The wide scatter of the experimental values might be attributed to inhomogeneously distributed subsurface defects in the reduced sample.
- Received 12 July 2012
DOI:https://doi.org/10.1103/PhysRevLett.109.136103
© 2012 American Physical Society