期刊
PHYSICAL CHEMISTRY CHEMICAL PHYSICS
卷 13, 期 15, 页码 6892-6900出版社
ROYAL SOC CHEMISTRY
DOI: 10.1039/c0cp02088e
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The results of a DRIFT study of carbon monoxide molecular adsorption and hydrogen dissociative adsorption on gallium-modified mordenite and MFI (ZSM-5) zeolites are presented. It was found that in the reduced gallium-modified mordenite (Ga-MOR) both Ga3+ and Ga+ exchanged cations are present and can be detected by CO adsorption. Ga3+ cations in Ga-MOR dissociatively adsorb molecular hydrogen at elevated temperatures, resulting in the formation of gallium hydride species and acidic hydroxyl groups. In the reduced Ga-MFI evacuated at 823 K under medium vacuum conditions only Ga+ exchanged intrazeolite cations were detected. It was found, however, that Ga3+ intrazeolite exchanged cations which form upon high-temperature disproportionation of Ga+ cations in the reduced Ga-MFI and Ga-MOR can be stabilized by high-temperature oxidation of these zeolites.
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