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Spectroscopic Identification of Adsorbed Intermediates Derived from the CO+H2O Reaction on Zeolite-Encapsulated Gold Catalysts

โœ Scribed by Mohamed Mokhtar Mohamed; Tarek M. Salama; Masaru Ichikawa


Publisher
Elsevier Science
Year
2000
Tongue
English
Weight
123 KB
Volume
224
Category
Article
ISSN
0021-9797

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โœฆ Synopsis


Identification of reaction intermediates in the water-gas shift reaction (WGSR: H(2)O+CO-->H(2)+CO(2)) on Au(n+) (1</=n<3) incorporated into NaY, Na-mordenite, and Na-ZSM-5 zeolites has been studied by means of in situ FT-IR spectroscopy. Exposure of Au(n+)/zeolites to a gas mixture consisting of CO+H(2)O at 323 K produced IR carbonyl spectra characterized by Au(+)-CO at 2192 cm(-1) and Au(0)-CO at 2128 cm(-1). On Au(n+)/NaY, a unidentate formate species (1710, 1620, and 1340 cm(-1)) is produced as a surface intermediate, which was very readily removed upon evacuation at 323 K. The reduction of the catalyst by H(2) at 423 K prior to the admission of the reacting gas mixture caused inhibition of formate species formation. This result suggests that Au(+) is the dominant species on which the reaction took place. Au(+)/Na-mordenite displayed unidentate formate and organic carbonate species (1936 and 1850 cm(-1)). The latter bands showed a significant increase in intensity with time at the expense of the adsorbed CO(2) bands at 2384 and 2338 cm(-1). On the other hand, Au(+)/Na-ZSM-5 resulted in the formation of different carbonate-like species (1936, 1850, 1730, and 1400 cm(-1)) as well as the rapid appearance of deformation vibrations of adsorbed water molecules at 1630 cm(-1) that built up very quickly compared to that in the Au(+)/Na-mordenite sample. These results were consistent with the catalytic activity data that showed the highest formation rates of CO(2) on Au(+)/NaY compared to those on Au(+)/Na-mordenite and Au(+)/Na-ZSM-5 catalysts. Copyright 2000 Academic Press.


๐Ÿ“œ SIMILAR VOLUMES


Spectroscopic and Kinetic Studies of the
โœ Mohamed Mokhtar Mohamed; Masaru Ichikawa ๐Ÿ“‚ Article ๐Ÿ“… 2000 ๐Ÿ› Elsevier Science ๐ŸŒ English โš– 107 KB

The surface species formed from the reaction of CO + H 2 O and CO + O 2 and decomposition of HCOOH on Au incorporated into H-mordenite zeolite have been studied by means of in situ FTIR spectroscopy. On H-mordenite, a bidentate formate species (2912, 1536, and 1390 cm -1 ) is produced upon exposure