Title of article :
Formation of hydroxyl and water layers on MgO films studied with ambient pressure XPS
Author/Authors :
Newberg، نويسنده , , John T. and Starr، نويسنده , , David E. and Yamamoto، نويسنده , , Susumu and Kaya، نويسنده , , Sarp and Kendelewicz، نويسنده , , Tom and Mysak، نويسنده , , Erin R. and Porsgaard، نويسنده , , Soeren and Salmeron، نويسنده , , Miquel B. and Brown Jr.، نويسنده , , Gordon E. and Nilsson، نويسنده , , Anders and Bluhm، نويسنده , , Hendrik، نويسنده ,
Issue Information :
هفته نامه با شماره پیاپی سال 2011
Pages :
6
From page :
89
To page :
94
Abstract :
To understand the interaction of water with MgO(100), a detailed quantitative assessment of the interfacial chemistry is necessary. We have used ambient pressure X-ray photoelectron spectroscopy (XPS) to measure molecular (H2O) and dissociative (OH) water adsorption on a 4 monolayer (ML) thick MgO(100)/Ag(100) film under ambient conditions. Since the entire 4 ML metal oxide (Ox) film is probed by XPS, the reaction of the MgO film with water can be quantitatively studied. Using a multilayer model (Model 1) that measures changes in Ox thickness from O 1s (film) and Ag 3d (substrate) spectra, it is shown that the oxide portion of the MgO film becomes thinner upon hydroxylation. A reaction mechanism is postulated in which the top-most layer of MgO converts to Mg(OH)2 upon dissociation of water. Based on this mechanism a second model (Model 2) is developed to calculate Ox and OH thickness changes based on OH/Ox intensity ratios from O 1s spectra measured in situ, with the known initial Ox thickness prior to hydroxylation. Models 1 and 2 are applied to a 0.15 Torr isobar experiment, yielding similar results for H2O, OH and Ox thickness changes as a function of relative humidity.
Keywords :
geochemistry , Catalysis , Magnesium oxide , Surface chemistry
Journal title :
Surface Science
Serial Year :
2011
Journal title :
Surface Science
Record number :
1685936
Link To Document :
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