Abstract
We find that less than 0.01 monolayer of S can enhance surface self-diffusion on Cu(111) by several orders of magnitude. The measured dependence of two-dimensional island decay rates on S coverage () is consistent with the proposal that clusters are responsible for the enhancement. Unexpectedly, the decay and ripening are diffusion limited with very low and very high but not for intermediate . To explain this result we propose that surface mass transport in the intermediate region is limited by the rate of reaction to form clusters on the terraces.
- Received 28 May 2004
DOI:https://doi.org/10.1103/PhysRevLett.93.166101
©2004 American Physical Society