On the nature of Pd species formed upon exchange of H-ZSM5 with Pd(NH3)42+ and calcination in O2

被引:33
|
作者
Pommier, B [1 ]
Gélin, P [1 ]
机构
[1] Univ Lyon 1, Lab Applicat Chim Environm, CNRS, UMR 5634, F-69622 Villeurbanne, France
关键词
D O I
10.1039/a808792j
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 chemistry of a high Pd loading Pd-H-ZSM-5 prepared by exchanging H-ZSM-5 with an aqueous solution of Pd(NH3)(4)(NO3)(2) and calcined in O-2 was studied by FTIR and TPD experiments. Acidic protons were found to readily exchange with Pd(NH3)(2)(2+) complexes and NH4+ ions arising from the partial decomposition of Pd(NH3)(4)(2+) possibly at the surface of H-ZSM-5 crystallites. The interaction of the Pd(II) ammine complexes with the MFI framework induced a strong absorption band at 928 cm(-1) attributed to the vibration of distorted T-O bonds (T = Si, Al). Slow calcination in O-2 at 653 K allowed the complete removal of NH3 Ligands from Pd(NH3)(2) entities and the decomposition of ammonium ions into protons. Despite the high Pd loading, no large PdO particles formed and the final oxidized Pd entities could be represented by the mean formula Pd(II)(OH)(1.3)(0.7+), suggesting the formation of isolated oxo and/or hydroxo Pd(II) complexes. A sharp IR band at 932 cm(-1) indicated that most of these complexes were anchored to the oxygen atoms of the zeolite framework. On the contrary, calcination in O-2 at 773 K led to the partial sintering of isolated Pd(II) species into large PdO particles. The possible formation of mobile Pd(OH)(2) moieties in O-2 at 773 K, migrating along the MFI channels, is discussed.
引用
收藏
页码:1665 / 1672
页数:8
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