Abstract
When adsorbed (at a low temperature) on alkali-metal-exchanged zeolites, CO forms both M(CO)+ and M(OC)+ carbonyl species with the extra-framework alkali-metal cation of the zeolite. Both quantum chemical and experimental results show that C-bonded adducts are characterized by a C-O stretching IR band at a frequency higher than that of 2143 cm-1 for free CO, while for O-bonded adducts this IR band appears below 2143 cm -1. The cation-CO interaction energy is higher for M(CO)+ than for M(OC)+ carbonyls, although the corresponding difference decreases substantially when going from Li+ to Cs+. By means of variable-temperature FTIR spectroscopy, this energy difference was determined for several alkali-metal cations, and the existence of a thermal equilibrium between M(CO)+ and M(OC)+ species was established. The current state of research in this field is reviewed here, with a view to gain more insight into the thermal isomerization process.
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Areán, C. O., Palomino, G. T., Tsyganenko, A. A., & Garrone, E. (2002). Quantum chemical and FTIR spectroscopic studies on the linkage isomerism of carbon monoxide in alkali-metal-exchanged zeolites: A review of current research. International Journal of Molecular Sciences. MDPI AG. https://doi.org/10.3390/i3070764
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