Okumura Kazu, Yoshimoto Ryosuke, Uruga Tomoya, Tanida Hajime, Kato Kazuo, Yokota Shigeru, Niwa Miki
Department of Materials Science, Faculty of Engineering, Tottori University, Koyama-cho, Tottori 680-8552, Japan, and Japan Synchrotron Radiation Research Institute, 1-1-1 Kouto, Mikazuki-cho, Sayo-gun, Hyogo 679-5198, Japan.
J Phys Chem B. 2004 May 20;108(20):6250-5. doi: 10.1021/jp037187b.
Spontaneous dispersion and clustering processes of Pd were measured by means of the energy-dispersive EXAFS method. The spontaneous dispersion of bulky metal Pd into highly dispersed PdO was directly observed on the H-type zeolite in the atmosphere of O2. In contrast to H-type zeolites, simple oxidation of the agglomerated Pd was observed on Na-ZSM-5. The structural change of Pd was followed in the atmosphere of hydrogen. The clustering processes of metal Pd depended on the kind of zeolite, and these were categorized into three groups. The first group, i.e., Na-ZSM-5 and H-beta, showed monotonic agglomeration of metal Pd by increasing the reduction temperature. The second group consisted of H-ZSM-5 and H-mordenite where the formation of Pd6 clusters was found. On these zeolites, the generation of Pd6 clusters was reversibly observed upon the repetition of reduction and oxidation treatments. The third group consisted of H-Y and USY zeolites where the formation of Pd13 clusters was observed. From these findings, it was concluded that the crystal structure and acid sites of zeolites had profound influences on the dynamic behavior and the genesis of Pd clusters with various structures.
采用能量色散扩展X射线吸收精细结构(EXAFS)方法测量了钯的自发分散和团聚过程。在O₂气氛中,直接观察到块状金属钯在H型沸石上自发分散为高度分散的PdO。与H型沸石不同,在Na-ZSM-5上观察到团聚钯的简单氧化。在氢气气氛中跟踪了钯的结构变化。金属钯的团聚过程取决于沸石的种类,可分为三组。第一组,即Na-ZSM-5和H-β,随着还原温度的升高,金属钯呈现单调团聚。第二组由H-ZSM-5和H-丝光沸石组成,在这些沸石上发现了Pd₆簇的形成。在这些沸石上,重复进行还原和氧化处理时,可逆地观察到Pd₆簇的生成。第三组由H-Y和USY沸石组成,在这些沸石上观察到了Pd₁₃簇的形成。从这些发现可以得出结论,沸石的晶体结构和酸位点对具有各种结构的钯簇的动态行为和生成有深远影响。