The diffusion of hydrogen atoms across solid oxide surfaces is often assumed to be accelerated by the presence of water molecules. Here we present a high-resolution, high-speed scanning tunneling microscopy (STM) study of the diffusion of H atoms on an FeO thin film. STM movies directly reveal a water-mediated hydrogen diffusion mechanism on the oxide surface at temperatures between 100 and 300 kelvin. Density functional theory calculations and isotope-exchange experiments confirm the STM observations, and a proton-transfer mechanism that proceeds via an H3O+-like transition state is revealed. This mechanism differs from that observed previously for rutile TiO2(110), where water dissociation is a key step in proton diffusion.
Revised: October 15, 2012 |
Published: May 18, 2012
Citation
Merte L.R., G. Peng, R. Bechstein, F. Rieboldt, C.A. Farberow, L.C. Grabow, and W. Kudernatsch, et al. 2012.Water-Mediated Proton Hopping on an Iron Oxide Surface.Science 336, no. 6083:889-893. doi:10.1126/science.1219468