Abstract

The initial stages of the oxidation of the (100) and (110) surfaces of iron caused by the adsorption of water have been investiagted using ab initio local-spin-density functional calculations including generalized gradient corrections. It is shown that at low coverages water dissociates spontaneously into hydrogen atoms and hydroxyl groups. Further adsorption of water molecules in the presence of preadsorbed H and OH does not lead to spontaneous dissociation. On both surfaces dissociation is a weakly activated process. This explains the presence of molecular water as observed experimentally. Especially on the (110) surface ${\mathrm{H}}_{2}\mathrm{O}$ dissociation in the presence of preadsorbed H and OH is found to be a complex process involving the formation of an intermediate molecular species.

Full Text
Paper version not known

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call

Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.