Abstract
The water- interaction is of paramount importance for many processes occurring on , and the rutile -() surface has often been considered as a test case. Yet, no consensus has been reached whether the well-studied surface O vacancies on the terraces are the only active sites for water dissociation on rutile -(), or whether another channel for the creation of H adatoms exists. Here we use high-resolution scanning tunneling microscopy and density functional theory calculations to tackle this long-standing question. Evidence is presented that a second water dissociation channel exists on the surfaces of vacuum-annealed crystals that is associated with the step edges. This second water dissociation channel can be suppressed by blocking of the step edges using ethanol.
- Received 18 December 2012
DOI:https://doi.org/10.1103/PhysRevLett.110.146101
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