Abstract

A series of metal/bimetal catalysts has been prepared from molecular carbonyl clusters such as Rh6–x Irx(CO)16(x= 0–6) and Rh4Fe2(CO)162– which were synthesized inside NaY zeolite supercages. Na Y-entrapped Rh6, Ir6, Rh4Ir2, Rh3Ir3 and Rh2Ir4 crystallites derived from the precursor carbonyl clusters have been well characterized by f.t.i.r., EXAFS, 129Xe n.m.r. and CO/H chemisorption on their metallic structures and electronic states. The results suggested that the reduced crystallites inside NaY zeolite consist of cluster ensembles < 10 Å in size with controlled metal compositions. These ensembles are fairly stable through several cycles of oxidation, reduction and alkane hydrogenolysis. As the probing reactions, hydrogenolysis of n-butane and ethane, and benzene hydrogenation were conducted. There is a dramatic decrease of hydrogenolysis activity by four orders of magnitude across the series of clusters on increasing the number of Ir atoms in the active Rh ensembles, while a slight enhancement of activity is observed for benzene hydrogenation. The remarkable activity suppression of hydrogenolysis has been interpreted not simply in terms of the geometric Rh ensemble-size effect with a small amount of Ir atoms but of the different electronic states of the RhIr bimetallic clusters in decreasing the electron deficiency through the series clusters. This was demonstrated by the unusually large chemical shifts of n.m.r. signals of 129Xe adsorbed on NaY-Rh-rich clusters in reflecting the higher electron deficiency. For butane hydrogenolysis, the smaller Rh ensembles in bimetallic RhIr clusters gave the maximum selectivities towards the central C—C bond scission to give C2H6, higher than those on the Rh6 and Ir6 inside zeolites. In contrast, RhFe/NaY derived from [Rh4Fe2(CO)16]2–/NaY exhibited conversely a high selectivity towards terminal C—C bond scission to give CH4+ C3H8. The Fe promotion for the terminal C—C bond scission is suggested to be associated with the electronic ligand effect on the heteronuclear sites consisting of Rh–Fe3+ located on the internal zeolite cages.

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