In situ XPS study of Pd(111) oxidation at elevated pressure, Part 2:: Palladium oxidation in the 10-1 mbar range

被引:146
|
作者
Gabasch, Harald
Unterberger, Werner
Hayek, Konrad
Kloetzer, Bernhard
Kleimenov, Evgueni
Teschner, Detre
Zafeiratos, Spiros
Haevecker, Michael
Knop-Gericke, Axel
Schloegl, Robert
Han, Jinyi
Ribeiro, Fabio H.
Aszalos-Kiss, Balazs
Curtin, Teresa
Zemlyanov, Dmitry
机构
[1] Purdue Univ, Birck Nanotechnol Ctr, W Lafayette, IN 47907 USA
[2] Univ Innsbruck, Inst Phys Chem, A-6020 Innsbruck, Austria
[3] Max Planck Gesell, Fritz Haber Inst, Abt Anorgan Chem, D-14195 Berlin, Germany
[4] Purdue Univ, Sch Chem Engn, W Lafayette, IN 47907 USA
[5] Univ Limerick, Mat & Surface Sci Inst, Limerick, Ireland
[6] Univ Limerick, Phys Dept, Limerick, Ireland
关键词
x-ray photoelectron spectroscopy; chemisorption; oxidation; surface chemical reaction; palladium; single crystal surfaces; low index single crystal surfaces; oxygen; high-pressure XPS;
D O I
10.1016/j.susc.2006.05.029
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
The oxidation of the Pd(1 1 1) surface was studied by in situ XPS during heating and cooling in 0.4 mbar O-2. The in situ XPS data were complemented by ex situ TPD results. A number of oxygen species and oxidation states of Palladium were observed in situ and ex situ. At 430 K, the Pd(1 1 1) surface was covered by a 2D oxide and by a supersaturated O-ads layer. The supersaturated O-ads layer transforms into the Pd5O4 phase upon heating and disappears completely at approximately 470 K. Simultaneously, small clusters of PdO, PdO seeds, are formed. Above 655 K, the bulk PdO phase appears and this phase decomposes completely at 815 K. Decomposition of the bulk oxide is followed by oxygen dissolution in the near-surface region and in the bulk. The oxygen species dissolved in the bulk is more favoured at high temperatures because oxygen cannot accumulate in the near-surface region and diffusion shifts the equilibrium towards the bulk species. The saturation of the bulk "reservoir" with oxygen leads to increasing the uptake of the near-surface region species. Surprisingly, the bulk PdO phase does not form during cooling in 0.4 mbar O-2, but the Pd5O4 phase appears below 745 K. This is proposed to be due to a kinetic limitation of PdO formation because at high temperature the rate of PdO seed formation is compatible with the rate of decomposition. (c) 2006 Elsevier B.V. All rights reserved.
引用
收藏
页码:2980 / 2989
页数:10
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