482
PATER, JACOBS, AND MARTENS
There is one main difference between the behavior of
ACKNOWLEDGMENTS
the zeolite and the clay. The ultrastable Y zeolite deacti-
vates faster in dodecane than in octane (Fig. 3), while the
opposite is observed for beidellite (Fig. 2). The zeolite con-
tains micropores and mesopores, while the clay material is
essentially meso and macroporous. On beidellite, as well
as ultrastable Y, hydrogen transfer reactions to produce
saturates are more important in dodecane than in octane
(Tables 2 and 3). It can be speculated that in the zeolite,
the hydrogen deficient molecules cause deactivation by mi-
cropore blockage, whereas in the clay with its larger pores
they are more easily desorbed. It remains to be explained
why the hydrogen transfer reactions are less important in
octane, compared to dodecane, and this is independent of
the nature of the catalyst.
This work has been sponsored by Total Raffinage Distribution S.A.
Stimulating discussions with J. M. Colin, R. Loutaty, A. Pantazidis,
G. Szabo (CERT TOTAL, Harfleur-France), and C. Naccache (IRC,
Villeurbanne-France) were greatly appreciated.
REFERENCES
1. Ipatieff, V. N., Corson, B. B., and Egloff, G., Ind. Eng. Chem. 27, 1077
(1935).
2. Jones, E. K., in “Advances in Catalysis” (Frankenburg & Komarewsky,
Eds.), Vol. VIII, p. 219. Academic Press, New York, 1956.
3. Oblad, A. G., Mills, G. A., and Heinemann, H., in “Catalysis” (Emmet,
Ed.), Vol. VI, p. 341. Reinhold, New York, 1958.
4. van den Berg, J. P., Wolthuizen, J. P., and van Hooff, J. H. C., J. Catal.
80, 139 (1983).
5. van den Berg, J. P., Wolthuizen, J. P., Clague, A. D. H., Hays, G. R.,
Huis, R., and van Hooff, J. H. C., J. Catal. 80, 130 (1983).
6. Quann, R. J., Green, L. A., Tabak, S. A., and Krambeck, F. J.,
Ind. Eng. Chem. Res. 27, 565 (1988).
4. CONCLUSIONS
7. Gricus Kofke, T. J., and Gorte, R. J., J. Catal. 115, 223 (1989).
8. Sealy, S. J., Fraser, D. M., Mo¨ller, K. P., and O’Connor, C. T., Chem.
Eng. Sci. 49, 3307 (1994).
The activity, stability, and selectivity of beidellite and ul-
trastable Y zeolite in 1-hexene oligomerization are strongly
influenced by the physical state of the hydrocarbons under
9. Knifton, J. F., and Sanderson, J. R., Catal. Lett. 28, 223 (1994).
reaction conditions. With both catalysts, liquid phase re- 10. Dai, P-S. E., Sanderson, J. R., and Knifton, J. F., in “Studies in Surface
Sciences and Catalysis” (J. Weitkamp et al., Eds.), Vol. 84, p. 1701.
Elsevier, Amsterdam, 1994.
11. Stepanov, A. G., Luzgin, M. V., Romannikov, V. N., and Zamaraev,
action conditions achieved by using octane and dodecane
solvents are most appropriate with respect to catalytic ac-
tivity, oligomerization selectivity, and stability. Under liq-
K. I., Catal. Lett. 24, 271 (1994).
uid phase conditions, the molecular weight of the solvent
has a strong influence on the selectivity and the stability of
the catalyst. On beidellite as well as on ultrastable zeolite
Y, hydrogen transfer reactions resulting in the formation
of C6 saturates are the main side reactions. These hydro-
gen transfer reactions are more abundant in dodecane than
in octane. Deactivation seems to be linked to the forma-
tion of large hydrogen deficient molecules, blocking micro-
and mesopores in ultrastable Y zeolites but not the larger
pores in beidellite. It explains why the beidellite catalyst is
most stable in dodecane, the ultrastable Y zeolite catalyst in
octane.
12. Muthukumaru Pillai, S., and Ravindranathan, M., J. Chem. Soc. Chem.
Commun., 1813 (1994).
13. Garwood, W. E., in “Intrazeolite Chemistry” (D. Stucky and F. G.
Dwyer, Eds.), A.C.S Symp. Ser., Vol. 218, p. 383. Am. Chem. Soc.,
Washington, DC, 1983.
14. Tabak, S. A., U.S. Patent 4,254,295 (1981).
15. Miehe, J., Le Dred, R., Baron, J., and Saehr, D., in “Synthesis of Porous
Materials” (M. L. Occelli and H. Kessler, Eds.), p. 523. Dekker, New
York, 1996.
16. Poncelet, G., and Schutz, A., in “Chemical Reactions in Organic
and Inorganic Constrained Systems” (R. Setton, Ed.), p. 165. Reidel,
Dordrecht, 1986.
17. Molina, R., Moreno, S., Vieira-Coelho, A., Martens, J. A., Jacobs,
P. A., and Poncelet, G., J. Catal. 148, 304 (1994).