Adsorption of CO at ambient temperature on NaX zeolite produces four distinct infrared absorption bands at around 2207, 2192, 2178 and 2165 cm-'. The relative intensities of these bands depend on sample crystallinity and vary considerably when sodium is exchanged with other Group 1 or Group 2 cations. These bands are ascribed to weakly held (CO), molecular clusters trapped in supercages and stabilized under cation fields. In addition, two pairs of bands are also observed in the 1200-1800 cm-' region, the frequencies and the relative intensities of which depend on the cation, CO exposure temperature and the sample crystallinity. These bands are stable under ambient-temperature evacuation and show a uniform isotopic shift corresponding to a frequency ratio V ( ' ~C / ' ~C ) of ca. 0.973 on using 13C0 as adsorbate. The possible origins of these bands are discussed in detail.The catalytic properties of synthetic zeolites are closely related to their capacity to adsorb a variety of molecular species into structural cages and in the inter-connecting channels. The adsorption characteristics are in turn influenced by framework composition and the nature of charge-balancing cations.'-4 A number of studies have been devoted, particularly using probe molecules such as CO, CO,, CH, and C6H6, to understand the mode of adsorption in zeolitic cages.'-' ' In the previous thermal desorption spectroscopy studies on X-type zeolites, we have demonstrated the existence of multiple C O binding states which were found to be modified by charge balancing cation^.'^"^ C O at some of these sites was found to convert to CO, during adsorption as well as on subsequent heat treatment. The Fourier-transform infrared (FTIR) spectroscopy studies reported here were undertaken to investigate further the identity of various CO adsorption modes on cationexchanged X-zeolites and to identify the multiple sites if possible. The effect of temperature on the species formed in the C O interaction was investigated in detail for this purpose. Parallel studies were also performed on NaY zeolite, alumina and silica for comparative evaluation. 3C isotope substitution experiments were also carried out to examine the isotopic shifts. The results of these studies are presented and discussed below.
ExperimentalThe high-temperature, high-pressure stainless steel cell used in these transmission mode IR studies has been described earlier." The cell having a pathlength of ca. 6 cm was fitted with water-cooled CaF, windows. It had a provision for in situ evacuation (10-3-10-4 Torrt) and for pretreatment of the sample under inert or reactive gas media at temperatures in the range 300-625 K.The zeolite-X sample, NaX (Si : A1 = 1.25, from Union Carbide, USA), was washed repeatedly with hot water and then dried under vacuum for several hours before use. The representative samples of cation-exchanged zeolites were prepared by substituting H', K', Li+, Mg2+ and Ca2' for sodium, using conventional ion-exchange procedures as reported earlier.17 HX, LiX, KX, MgX and CaX were ex...