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Title: Dissociation of water on oxygen-covered Rh(111)

Journal Article · · Journal of Chemical Physics
DOI:https://doi.org/10.1063/1.3266941· OSTI ID:21559812
; ;  [1]; ; ; ;  [2]
  1. Department of Chemistry, The University of Reading, Whiteknights, Reading RG6 6AD (United Kingdom)
  2. Department of Synchrotron Radiation Research, Institute of Physics, Lund University, P.O. Box 118, S-221 00 Lund (Sweden)

The adsorption of water and coadsorption with oxygen on Rh(111) under ultrahigh vacuum conditions was studied using synchrotron-based photoemission and photoabsorption spectroscopy. Water adsorbs intact on the clean surface at temperatures below 154 K. Irradiation with x-rays, however, induces fast dissociation and the formation of a mixed OH+H{sub 2}O layer indicating that the partially dissociated layer is thermodynamically more stable. Coadsorption of water and oxygen at a coverage below 0.3 monolayers has a similar effect, leading to the formation of a hydrogen-bonded network of water and hydroxyl molecules at a ratio of 3:2. The partially dissociated layers are more stable than chemisorbed intact water with the maximum desorption temperatures up to 30 K higher. For higher oxygen coverage, up to 0.5 monolayers, water does not dissociate and an intact water species is observed above 160 K, which is characterized by an O 1s binding energy 0.6 eV higher than that of chemisorbed water and a high desorption temperature similar to the partially dissociated layer. The extra stabilization is most likely due to hydrogen bonds with atomic oxygen.

OSTI ID:
21559812
Journal Information:
Journal of Chemical Physics, Vol. 131, Issue 21; Other Information: DOI: 10.1063/1.3266941; (c) 2009 American Institute of Physics; ISSN 0021-9606
Country of Publication:
United States
Language:
English