n-BUTANE OVER Pt(100) AND Pt(111)
29
150, the rate can be expressed as the competitive adsorption
of H2 and n-butane with the cleavage of C C bonds being
CONCLUSIONS
–
The activities and selectivities for the hydrogenolysis and
isomerization of n-butane have been measured for poly-
crystalline Pt and Pt(100) and Pt(111) single crystals. The
experiments were performed over wide ranges of reaction
temperatures and H2 partial pressures. The open (100) sur-
face was approximately an order of magnitude more ac-
tive than the close-packed (111) surface, in accordance with
what has been reported for Rh and Ni single crystals. Pro-
duct distributions for the single crystals were different in
that the (100) face had a higher methane selectivity, indi-
cating more multiple hydrogenolysis. Neither surface pro-
duced substantial amounts of iso-butane, as the quantity
of hydrogenolysis products was always much higher than
thatofisomerization. Bothsingle-crystalsurfacesshowcon-
siderable deactivation at low H2 pressures due to carbon de-
position, withslightchangesintheselectivityatlowH2 pres-
sures. Also, both surfaces demonstrate a loss in activity as a
function of reaction time and concomitantly there is an in-
crease in the amount of carbon on the surface. These results
will be used to provide a baseline for determining the effect
of supported particle microstructure for a silica-supported
Pt catalyst where the morphology can be controlled by ther-
mal treatment in different gaseous atmospheres.
the rate-limiting step. This has also been reported to be
the case for n-butane hydrogenolysis over Ir single crystals,
but for H2 : nC4 ratios greater than 20. The decrease in the
concentration of surface hydrogen is regarded to be respon-
sible for this change in rate limiting step. On Pt surfaces, it
appears that the carbon deposited at low H2/n-butane ra-
tios acts to block or modify the available reaction sites. For
Pt(111), not only is the amount of surface carbon at low H2
pressures causing a decrease in activity but it changes the
product distribution as well. One possible explanation for
this observation is that the carbon preferentially blocks the
–
sites where internal C C bond cleavage takes place, thus
yielding the higher methane concentration. A second pos-
sibility is that the surface carbon is being hydrogenated and
desorbing as methane. This change in selectivity is not seen
on either the Pt(100) or polycrystalline Pt surface, where
the amount of methane is already high.
As seen from Fig. 5, there is a maximum in activity with
increasing H2 pressure, and such a maximum has also been
reported to occur over supported Pt/silica catalysts (3, 29).
Competition between the parent hydrocarbon and H2 for
surface sites leads to a drop in activity at high H2 pressures.
Comparison of Figs. 5 and 6 shows that the TOF begins
to roll over at a higher hydrogen pressure for the Pt(111)
surface than for the Pt(100) surface. This clearly supports
the evidence that the (100) surface has a higher concen-
tration of hydrogen than the close-packed (111) surface, at
an equivalent temperature. Both surfaces exhibit a loss in
activity as a function of reaction time, for a given temper-
ature. This loss in activity correlates well with a increase
in the amount of carbon on the surface. In addition to the
change in activity, in Pt(111) surface also shows a change
in selectivity with the more deactivated surface producing
an increased amount of methane. What is not clear yet is
whether the increased rate of methane formation is a result
of the hydrogenation of the accumulated surface carbon
or an enhancement in the terminal bond scission pathway
relative to the internal bond scission pathway.
Two important aspects have emerged from this study, the
first is that neither Pt(100) or (111) are capable of the iso-
merization of n-butane to iso-butane under the experimen-
tal conditions of this study. The second aspect is that dif-
ferences in hydrogenolysis activities and selectivities exist
between the two crystal faces and these differences are sig-
nificant enough to help in the study of supported Pt catalysts
with known particle morphology. The aim of this study has
been to establish the effect of temperature and H2 partial
pressure on the catalytic behavior of unsupported, well-
defined Pt surfaces for the reaction of n-butane and hydro-
gen. These results will be used to elucidate the effect of
particle microstructure on the reaction of n-butane and H2
for silica supported Pt catalysts.
ACKNOWLEDGMENTS
This research has been supported by the American Chemical Society,
Petroleum Research Fund Grant 28656-AC5. S. L. Anderson would like
to thank the Los Alamos Graduate Research Program.
REFERENCES
1. Bond, G. C., and Hui, L., J. Catal. 137, 462 (1992).
2. Bond, G. C., and Paal, Z., Appl. Catal. 86, 1 (1992).
3. Bond, G. C., Chem. Soc. Rev. 20, 441 (1991).
4. Yates, D. J. C., and Sinfelt, J. H., J. Catal. 8, 348 (1967).
5. Yao, H. C., Yu Yao, Y.-F., and Otto, K., J. Catal. 56, 21 (1979).
6. Lee, C., and Schmidt, L. D., J. Catal. 101, 123 (1986).
7. Shi, A.-C., and Masel, R. I., J. Catal. 120, 421 (1989).
8. Lee, W. H., Vanloon, K. R., Petrova, V., Woodhouse, J. B., Loxton,
C. B., and Masel, R. I., J. Catal. 126, 658 (1990).
9. Ramachandran, A., Anderson, S. L., and Datye, A. K., Ultrami-
croscopy 51, 282 (1993).
10. Davis, S. M., Zaera, F., and Somorjai, G. A., J. Am Chem. Soc. 104,
7453 (1982).
11. Davis, S. M., Zaera, F., and Somorjai, G. A., J. Catal. 77, 439 (1982).
12. Davis, S. M., Zaera, F., and Somorjai, G. A., J. Catal. 85, 206 (1984).
13. Logan, A. D., Sharoudi, K., and Datye, A. K., J. Phys. Chem. 95, 5568
(1991).
14. Campbell, C. T., and Paffett, M. T., Surf. Sci. 139, 396 (1984).
15. Somorjai, G. A., “Chemistry in Two Dimensions.” Cornell Univ. Press,
Ithaca, NY, 1981.
16. Christmann, K., Ertl, G., and Pignet, T., Surf. Sci. 54, 365 (1975).
17. Bond., G. C., Cunningham, R. H., and Short, E. L., Stud. Surf. Sci.
Catal. 75, 849 (1993).
18. Kalakkad, D., Anderson, S. L., Logan, A. D., Pena, J., Braunschweig,