Abstract
In situ band gap mapping of the crystal surface revealed a reversible metal-to-insulator transition at 350–400 K, which occurs inhomogeneously across the surface and expands preferentially in the direction of the vanadyl () double rows. Supported by density functional theory and Monte Carlo simulations, the results are rationalized on the basis of the anisotropic growth of vanadyl-oxygen vacancies and a concomitant oxygen loss driven metal-to-insulator transition at the surface. At elevated temperatures irreversible surface reduction proceeds sequentially as .
- Received 25 May 2007
DOI:https://doi.org/10.1103/PhysRevLett.99.226103
©2007 American Physical Society