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Comparison of 18O Isotopic Exchange After and During the Interaction of N2O, NO, and NO2 with Fe Ions in Ferrierites

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Abstract

Nitrous oxide deposits its oxygens on Fe-ferrierites at 200–250 °C in contrast with nitric oxide and nitrogen dioxide. This oxygen is readily exchangeable for 18O2 at room temperature and the reaction proceeds via a single-step exchange mechanism. All three nitrogen oxides in a mixture with 18O labeled dioxygen undergo isotopic exchange (IE) at 200–250 °C, N2O via the same single-step mechanism, while NO and NO2 react via a multiple-step mechanism. Zeolitic oxygens participate in IE above 250 °C during temperature-programmed desorption of surface species formed in the reaction of nitrogen oxides with 18O2.

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Nováková, J., Sobalik, Z. Comparison of 18O Isotopic Exchange After and During the Interaction of N2O, NO, and NO2 with Fe Ions in Ferrierites. Catalysis Letters 89, 243–247 (2003). https://doi.org/10.1023/A:1025762714948

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