PARAMAGNETIC SILVER CLUSTERS IN MOLECULAR SIEVES: ZEOLITE RHO J. Michalik, J. Sadlo and M. Danilczuk Institute of Nuclear Chemistry and Technology Dorodna16, 03-195 Warsaw, POLAND
It is assumed that materials containing metal nanoparticles will be playing important role in future electronics, optics and heterogeneous catalysis. Nanoparticle properties depend strongly on particle size, however usually metal clusters are produced with broad distribution of nuclearity. Zeolite frameworks offer excellent conditions for stabilization of nanoparticles with uniform nuclearity and shape. Although paramagnetic silver metal clusters have been generated radiolytically in several types of molecular sieves Ag agglomerates produced in zeolite rho and sodalites show unique stability even above room temperature. In AgCs-rho zeolite silver agglomeration process was followed by EPR in temperature range 77 - 370 K. In dehydrated samples the EPR doublet of silver atoms is observed at 77 K. The Ag0 atoms decay during thermal annealing is correlated with the formation of silver dimmers Ag[2]+ (A[iso]=29 mT, g[iso]=1.983). At higher temperature the Ag[2]+ triplet is replaced by Ag[3]2+ quartet. Finally, at room temperature the EPR quintet (A[iso]=13.9 mT, g[iso]=1.970) of silver tetramer Ag[4]3+ is recorded1. The results prove univocally that in gamma irradiated AgCs-rho zeolites silver clusters are formed by the reactions between Ag0 atoms or cationic Ag cluster and Ag+ cations. Although Ag[4]3+ clusters in AgCs-rho are exceptionally stable they are accessible for the small molecular adsorbates. When irradiated AgCs-rho containing Ag[4]3+ clusters is exposed to ammonia the hyperfine splitting is decreasing from 13.9 mT to 10.7 mT. This indicates the significant shift of spin density from Ag nuclei to the ammonia ligands. Additionally, in the presence of ammonia the outer lines of Ag[4]3+ quintet show secondary structure. It was proved by experiments with 15NH[3] that this structure is due to the superhyperfine interaction with nitrogen nuclei. The simulation of the spectra recorded in the presence of 14NH[3] and 15NH[3] indicated that Ag[4]3+ coordinates two close and four more distant NH[3] molecules forming multicore Ag[4]3+(NH[3])[2]'(NH[3])[4]" complex 2.
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