Abstract
Transmission electron diffraction (TED) combined with direct methods have been used to study the reconstruction on the polar (111) surface of MgO and refine the valence charge distribution. The surface is nonstoichiometric and is terminated by a single magnesium atom. A charge-compensating electron hole is localized in the next oxygen layer and there is a nominal charge transfer from the oxygen atoms to the top magnesium atom. The partial charges that we obtain for the surface atoms are in reasonable agreement with empirical bond-valence estimations.
- Received 25 June 2003
DOI:https://doi.org/10.1103/PhysRevLett.92.026101
©2004 American Physical Society