Oxygen migration in silicon corresponds to an apparently simple jump between
neighboring bridge sites. Yet, extensive theoretical calculations have so far
produced conflicting results and have failed to provide a satisfactory account
of the observed 2.5 eV activation energy. We report a comprehensive set of
first-principles calculations that demonstrate that the seemingly simple oxygen
jump is actually a complex process involving coupled barriers and can be
properly described quantitatively in terms of an energy hypersurface with a
``saddle ridge'' and an activation energy of ∼2.5 eV. Earlier
calculations correspond to different points or lines on this hypersurface.Comment: 4 Figures available upon request. Accepted for publication in Phys.
Rev. Let