tion activities can be enlarged when reduction of MoO pro-
3
ceeds through the formation of a H MoO phase, from which
x
the MoO H phase is derived presumably.
x y
3
Acknowledgements
This work has been supported in part by a Grant-in-Aid for
ScientiÐc Research on Priority Area A of ““New Protium
FunctionÏÏ from the Ministry of Education, Science, Sports
and Culture.
References
1
2
C. P. Huu, M. J. Ledoux and J. Guille, J. Catal., 1993, 143, 249.
E. A. Blekkam, C. P. Huu, M. J. Ledoux and J. Guille, Ind. Eng.
Chem. Res., 1994, 33, 1657.
Fig. 11 Relation between the heptane isomerization activity and the
propan-2-ol dehydration activity. MoO reduced at 573 (L), 623 (K)
3
and 673 K (|). Pt/MoO reduced at 523 (=), 573 (>), 623 (@), 673
3
3
M. J. Ledoux, C. P. Huu, P. Delporte, E. A. Blekkam, A. P. E.
York, E. G. Derouane and A. Fonseca, Stud. Surf. Sci. Catal.,
(
+), 723 (È) and 773 K ()).
1
994, 92, 81.
4
5
6
A. Katrib, P. LeÑaive, L. Hilaire and G. Maire, Catal. L ett., 1996,
and 2.7 ] 10~3 mol h~1 g~1, respectively. Thus, the results
shown in Fig. 11 can not be interpreted in terms of the di†er-
ence in the dehydrogenation activity. Hall and co-workers
reported that cyclopropane isomerization and propene hydro-
genation reactions on H -reduced Mo/Al O were poisoned
38, 95.
A. Katrib, V. Logie, N. Saurel, P. Wehrer, L. Hilaire and G.
Maire, Surf. Sci., 1997, 377–379, 754.
F. Barath, M. Turki, V. Keller and G. Maire, J. Catal., 1999, 185,
1.
2
2 3
with H O.27 The catalytic behavior of H -reduced MoO and
7
8
V. Keller, F. Barath and G. Maire, J. Catal., 2000, 189, 269.
T. Matsuda, Y. Hirata, M. Suzuki, H. Sakagami and N. Taka-
hashi, Chem. L ett., 1999, 873.
2
2
3
Pt/MoO in the isomerization of heptane seems to be some-
what di†erent from that in the conversion of propan-2-ol,
3
9
0
T. Matsuda, Y. Hirata, F. Uchijima, H. Itoh and N. Takahashi,
Bull. Chem. Soc. Jpn., 2000, 73, 1029.
T. Matsuda, H. Shiro, H. Sakagami and N. Takahashi, Catal.
L ett., 1997, 47, 99.
because H O is produced in the conversion of propan-2-ol.
2
The acidity of Mo/Al O has been explained by the induc-
1
2
3
tive e†ect.32,33 Since the average Sanderson electronegativity
of Al O is 3.72, while that of MoO is 3.89, hydroxy groups
on Al O which are near MoO can be made more acidic by
the inductive e†ect. When MoO is reduced to MoO , of
which the electronegativity is 3.53, Mo/Al O becomes less
acidic. Maire and co-workers6,7 recently reported the results
of alkene isomerization on H -reduced MoO /a-Al O . They
proposed from the correlation with XPS measurements that
coordinatively unsaturated sites, such as Mo4` and Mo2`,
will be responsible for dehydrogenation and hydrogenation
reactions, and Bronsted acidity can originate from hydroxy
groups coordinated to Mo5`. The dependencies of the isomer-
ization and dehydration activities on the reduction degree
were very similar to that of the surface area, suggesting an
11 T. Matsuda, Y. Hirata, S. Suga, H. Sakagami and N. Takahashi,
2
2
3
3
3
Appl. Catal. A: General, 2000, 193, 185.
T. Matsuda, Y. Hirata, H. Sakagami and N. Takahashi, Chem.
L ett., 1997, 1261.
3
1
2
3
2
2
3
13 T. Matsuda, Y. Hirata, H. Itoh, H. Sakagami and N. Takahashi,
Microporous Mesoporous Mater., 2001, 42, 337.
14 T. Matsuda, Y. Hirata, H. Sakagami and N. Takahashi, Micro-
porous Mesoporous Mater., 2000, 42, 345.
5
6
7
2
3
2 3
1
1
1
P. A. Sermon and G. C. Bond, J. Chem. Soc., Faraday T rans. 1,
1
976, 72, 730.
G. C. Bond and J. B. Tripathi, J. Chem. Soc., Faraday T rans. 1,
1
976, 72, 933.
P. G. Dickens, R. H. Jarman, R. C. T. Slade and C. J. Wright, J.
Chem. Phys., 1982, 77, 575.
18 R. Erre and J. J. Fripiat, Stud. Surf. Sci. Catal., 1983, 17, 285.
1
2
2
2
2
2
2
2
9
0
1
2
3
4
5
6
T. Matsuda, F. Uchijima, S. Endo and N. Takahashi, Appl. Catal.
A: General, 1999, 176, 91.
important role of the MoO H phase in generating the acid
x y
sites. Although we have no spectroscopic data at present, we
F. Uchijima, T. Takagi, H. Itoh, T. Matsuda and N. Takahashi,
Phys. Chem. Chem. Phys., 2000, 2, 1077.
deduce that interaction of Mon`ÈOH in the MoO H phase
x y
and Mo(n`1)` can create the acid sites that are responsible for
P. Arnoldy, J. C. M. de Jonge and J. A. Moulijin, J. Phys. Chem.,
1985, 89, 4517.
heptane isomerization and propan-2-ol dehydration.
A. Lofberg, A. Frennet, G. Leclercq, L. Leclercq and J. M. Girau-
don, J. Catal., 2000, 189, 170.
Conclusion
T. Ressler, O. Timpe, T. Neisius, J. Find, G. Mestl, M. Dieterle
and R. Schlogl, J. Catal., 2000, 191, 75.
H reduction of Pt/MoO was accompanied by an increase in
2
3
P. Delporte, F. Meunier, C. P. Huu, P. Vennegues, M. J. Ledoux
and J. Guille, Catal. T oday, 1995, 23, 251.
the surface area, which reached the maximum value of 250 m2
g~1 at a reduction degree of 60È70%. The surface area of
MoO reduced at 573 and 623 K was similarly dependent on
the reduction degree as that of H -reduced Pt/MoO . In con-
trast, reduction of MoO at 673 K changed the surface area
C. Bouchy, C. Pham-Huu, B. Heirich, C. Chaumont and M. J.
Ledoux, J. Catal., 2000, 190, 92.
3
E. A. Lombardo, M. Houalla and W. K. Hall, J. Catal., 1978, 51,
256.
2
3
3
little. The formation of pores is likely to be a reason for the
27 E. A. Lombardo, M. Jacono and W. K. Hall, J. Catal., 1980, 64,
1
50.
enlargement of surface area. H -reduced MoO and Pt/MoO
2
3
3
28 R. B. Quincy, M. Houalla, A. Proctor and D. A. Hercules, J.
with large surface areas contained the MoO H phase, which
x y
Phys. Chem., 1990, 94, 1520.
M. Yamada, J. Yasumaru, M. Houalla and D. A. Hercules, J.
Phys. Chem., 1991, 95, 7037.
was derived, presumably, from the H MoO phase. The activ-
2
9
x
3
ity for heptane isomerization was well related to that for
propan-2-ol dehydration, suggesting that the isomerization
activity of H -reduced MoO and Pt/MoO can be controlled
30 T. Kataoka and J. A. Dumesic, J. Catal., 1988, 112, 66.
31 Yu. V. Belokopytov, K. M. Kholyavenko and S. V. Gerei, J.
Catal., 1979, 60, 1.
2
3
3
by the ability to act as an acid catalyst. The dependencies of
the isomerization and dehydration activities on the reduction
degree were very similar to that of the surface area. We
suggest from these results that the isomerization and dehydra-
3
2
W. Suarez, J. A. Dumesic and C. G. Hill, Jr., J. Catal., 1985, 94,
08.
4
3
3
R. T. Sanderson, Chemical Bonds and Bond Energy, Academic
Press, New York, 1976.
4436
Phys. Chem. Chem. Phys., 2001, 3, 4430È4436