I. R. Subbotina, A. L. Tarasov, B. N. Shelimov, and V. B. Kazansky
Zelinskii Institute of Organic Chemistry, Russian Academy of Sciences, Moscow, 117913 Russia
Received April 10, 1998
AbstractThe UV irradiation of the MoO3/Al2O3 catalyst in the CO atmosphere at room temperature results
in the reduction of the surface Mo6+ ions to Mo5+ and Mo4+. The average oxidation states of molybdenum ions
in photoreduced samples and ESR data suggest that Mo4+ ions dominate in 0.1% MoO3/Al2O3 samples, whereas
Mo4+ and Mo5+ are formed in nearly the same amounts in 1% MoO3/Al2O3. The Mo4+ ions are assumed to be
formed from the surface monomolybdates, whereas the Mo5+ ions are formed from polymolybdates, whose
fraction substantially increases with an increase in the concentration of the supported molybdenum. The heating
of photoreduced samples in a vacuum at 300°C results in a substantial decrease in the concentration of Mo4+
and in an increase in the concentration of Mo5+ due to the metathesis Mo4++ Mo6+
2Mo5+ in polymolyb-
date structures. The composition of Mo4+(CO)x complexes in photoreduced MoO3/Al2O3 is studied by IR spec-
troscopy. When MoO3/Al2O3 is UV-irradiated in the presence of the CO + NO mixtures, the photocatalytic
reduction of NO yields N2O and CO2.
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