XPS study of Pt ammine decomposition in K faujasites: Comparison with bulk behavior

Z. Bastl, L. Kubelková, J. Nováková
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引用次数: 4

Abstract

The XPS method is employed to compare the behavior of [Pt(NH3)4]2+ ions in the surface layers of KX and KY zeolites with that in the zeolite bulk. FT i.r. and MS-t.p.d. methods are used to characterize the bulk properties. XPS and FT i.r. reveal the formation of different intermediate NHx species during the decomposition of the ammine complex in a vacuum. They are interpreted as Pt-diammine, framework ammine, and immine complexes. The maximum evolution of ammonia occurs in the temperature interval ranging from 150°C to 250°C. Positive shifts of Pt: (4f) photoelectrons, observed for samples with a decomposed Pt-ammine complex, are explained by a decrease of the population of Pt 5d levels in encaged metallic clusters. The surface concentration of Pt decreases with increasing temperature due to the inward diffusion of Pt atoms.

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铂胺在山竹石中分解的XPS研究:与散装行为的比较
采用XPS方法比较了[Pt(NH3)4]2+离子在KX和KY沸石表层与沸石体中的行为。FT . i.r.和ms . t.p.d.。方法是用来表征体积性质。XPS和FT ir揭示了在真空条件下胺配合物分解过程中不同中间体NHx的形成。它们被解释为pt -二胺、框架胺和亚胺配合物。氨的最大演化发生在150 ~ 250℃的温度区间。对于分解Pt-胺配合物的样品,观察到Pt: (4f)光电子的正位移,可以用包裹金属团簇中Pt 5d水平的下降来解释。由于Pt原子向内扩散,Pt的表面浓度随温度升高而降低。
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