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Alumina surfaces and interfaces under non-ultrahigh vacuum conditions

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SURFACE SCIENCE REPORTS
卷 62, 期 7, 页码 271-303

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DOI: 10.1016/j.surfrep.2006.12.003

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This paper is a review of studies of the structures and reactivities of ordered alumina surfaces under ultrahigh vacuum (UHV; < 10(-8) Torr), ambient (>1 Torr), and intermediate (10(-7)-10(-1) Torr) pressure conditions. Most ordered alumina films-including alpha-Al2O3(0001) and transitional phase thin films grown on single-crystal substrates, are Al-terminated, but do not dissociate H2O or mAny other small molecules (e.g., CH3OH, NH3) at room temperature under UHV conditions. Under ambient conditions, the alpha-Al2O3(0001) suifa e becomes OH-terminated, with an overlayer of physisorbed molecular H2O stabilized by hydrogen bonding interactions with the OH substrate layer. The reactivity under ambient conditions is consistent with theoretical predictions of cooperative dissociation pathways for H20 on this surface with low activation barriers, and is also consistent with desorption studies indicating that high fractional surface coverages of H2O (theta H2O similar to 1) should only be observed at pressures of similar to 1 Torr or higher. Surprisingly, cooperative H2O interactions have also been observed at the surfaces of ordered films grown on Ni3Al(111) and (110), and on NiAI(100) substrates at intermediate pressures orders of magnitude below ambient; PH2O > 10(-7) Torr, 300 K. Under these conditions, a cooperative reaction is apparently initiated at defect sites, resulting in strong surface rearrangement. NO appears to exhibit analogous behavior to H2O, albeit at UHV pressures and at 100 K, where NO dimers form at surface defect sites. These data indicate that cooperative surface reactions occur at transitional phase alumina surfaces at pressures that are orders of magnitude below what one would expect based on straightforward thermodynamics and kinetics calculations, and point to the importance of surface defect sites for initiating reactions that eventually affect the entire surface. There is suggestive evidence that H2O exposure also leads to the incorporation of interstitial atomic hydrogen in transitional phase alumina films. Results at ambient and intermediate pressures indicate that these pressure regimes form distinct reaction environments, with reaction pathways on alumina that differ qualitatively from each other as well as from results observed in UHV (c) 2007 Published by Elsevier B.V.

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