494
LIU ET AL.
within cavities by an initial hydrogen abstraction followed
by addition of NO2 to the resulting radical.
3. Beutel, T., Adelman, B., and Sachtler, W. M. H., Catal. Lett. 37, 125
(1996).
4. Wu, J., and Larsen, S. C., J. Catal. 182, 244 (1999).
5. Rebrov, E. V., Simakov, A. V., Sazonova, N. N., and Stoyanov, E. S.,
Catal. Lett. 64, 129 (2000).
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(1999).
7. Gerlach, T., and Baerns, M., Chem. Eng. Sci. 54, 4379 (1999).
8. Chen, H.-Y., Voskoboinikov, T., and Sachtler, W. M. H., J. Catal. 186,
91 (1999).
It is significant that NO2 formation during the SCR re-
action at 296 C is much less than that with NO/O2 alone
at a lower temperature (Table 1). Furthermore, the NO2
concentration first declines with temperature above 300 C
during SCR to a minimum near 365 C where ethane con-
sumption is complete. The implication is that NO2 is being
consumed by a reaction involving ethane that has a higher
activation energy than NO oxidation. Thus NO2 does ap-
9. Cant, N. W., Cowan, A. D., Liu, I. O. Y., and Satsuma, A., Catal. Today
54, 473 (1999).
pear to be a key reactant in this system in agreement with 10. Liu, I. O. Y., unpublished results.
11. Cant, N. W., Cowan, A. D., Doughty, A., Haynes, B. S., and Nelson,
current views concerning hydrocarbon-SCR reactions over
transition metal zeolites.
P. F. , Catal. Lett. 46, 207 (1997).
12. Cowan, A. D., Cant, N. W., Haynes, B. H., and Nelson, P. F., J. Catal.
176, 329 (1998).
CONCLUSIONS
13. Lombardo, E. A., Sill, G. A., d’Itri, J. L., and Hall, W. K., J. Catal. 173,
440 (1998).
14. Cant, N. W., Chambers, D. C., Cowan, A. D., Liu, I. O. Y., and Satsuma,
A., Top. Catal. 10, 13 (2000).
15. Szanyi, J., and Paffett, M. T., J. Chem. Soc. Faraday Trans. 92, 5165
(1996).
16. Radtke, F., Koeppel, R. A., and Baiker, A., Appl. Catal. A 107, L125
(1994).
17. Radtke, F., Koeppel, R. A., and Baiker, A., Environ. Sci. Technol. 29,
2703 (1995).
18. Radtke, F., Koeppel, R. A., and Baiker, A., J. Chem. Soc. Chem. Com-
mun., 427 (1995).
19. Radtke, F., Koeppel, R. A., and Baiker, A., Catal. Today 26, 159
(1995).
20. Burch, R., and Scire, S., Appl. Catal. B 3, 295 (1994).
21. Obuchi, A., Wo¨gerbauer, C., Ko¨ppel, R. A., and Baiker, A., Appl.
Catal. B 19, 9 (1998).
22. March, J., “Advanced Organic Chemistry,” p. 807. Wiley, New York,
1985.
Nitroethane reacts readily in NO/O2 over Cu-MFI with
initial conversion to CO2 and N2. Deactivation due to de-
posited material occurs below 330 C with the eventual
emergence of isocyanates, principally CH3NCO by dehy-
dration, but with some HNCO, by deposit decomposition,
as well. Nitromethane reacts in a similar way but deacti-
vation is much slower. While HNCO is then the only iso-
cyanate formed, significant amounts of HCN and NH3 are
also seen. With both systems nitrogen can arise either by hy-
drolysis of isocyanate to amine (or ammonia) on Brønsted
sites and subsequent SCR reactions involving transition
metal ions or through reaction of NO2 with deposits. The
rates of these processes are sufficiently fast for nitroethane
to be feasible as an intermediate during the selective cat-
alytic reduction of NO by ethane on Cu-MFI.
23. Du¨mpelmann, R., Cant, N. W., and Trimm, D. L., J. Catal. 162, 96
(1996).
24. Chambers, D. C., Angove, D. E., and Cant, N. W., J. Catal. in press.
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Trans. 91, 1841 (1995).
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ACKNOWLEDGMENTS
This work has been supported by grants from the Australian Research
Grants Committee. We are grateful to Mr. A. Asano for provision of the
starting zeolite sample.
27. Satsuma, A., Cowan, A. D., Cant, N. W., and Trimm, D. L., J. Catal.
181, 165 (1999).
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