Chemistry Letters 2000
605
adsorbed water. The supported sample exhibits an initial loss in
weight similar to that of FSM-16, but it shows further decrease
in weight as the temperature increases. It is evident that the rate
of weight loss above 300 °C is much more slower for
[NH ] SO /FSM-16. It was observed that in both cases (i.e., for A
and B) the Brønsted acid band was much more intense than the
Lewis acid band.
4
2
4
Among the method B catalysts, the sample evacuated at 300
C exhibited the largest Brønsted acid peak. This sample also
o
[
NH ] SO /FSM-16 than the unsupported [NH ] SO . This
4
2
4
4 2
4
indicates the relatively gradual decomposition of the salt in the
supported form.
showed a relatively larger peak than its counterpart prepared by
method A. These observations are partially in correlation with the
catalytic activity for the 1-butene isomerization reaction especially,
for the samples pretreated at 300 °C and above.
Figure 3 depicts the IR spectra of [NH ] SO /FSM-16 (A
4
2
4
-
1
and B). Absorption bands in the 1400-1415 cm region were
observed for both A and B samples thermally pretreated at 200-
Calcination of [NH ] SO /FSM-16 at 200 °C followed by
4
2
4
o
4
00 °C. These bands are assignable to the asymmetric stretching
evacuation at 300 C markedly leads to enhanced catalytic activity
for 1-butene and cyclopropane isomerization. Similar to our previ-
10
vibration of S=O bond of the sulfate species. The sample cal-
9
cined at 100 °C shows a very broad band centred around 1443
ous report, it is assumed that the high activity is due to sulfate
-
1
-1
cm , while a similar band is observed at 1437 cm . The bands
species so produced which interact with the SiOH group of FSM-
16 and transform them into Brønsted acid sites by their inductive
effect.
The authors wish to thank Toyota Central R&D Labs. Inc.,
Japan, for the kind provision of FSM-16.
+
11
may be attributed to the bending vibration band of NH . This
4
assignment is supported by the presence of broad bands in the
-1
3
000-3300 cm region (spectra not shown) associated with the
N-H stretching vibrations. It was noted that increasing calcina-
tion temperature caused the disappearance of the broad band
-1
while the 1400 cm region bands appeared. This can be related
to the gradual decomposition of the supported salt which pro-
ceeds by initial removal of ammonia. The S=O peak intensity
reached a maximum at 300 °C, after which it sharply decreased
in the case of the method A catalysts. As shown, after calcina-
tion at 500 °C, no visible peak ascribed to sulfate species is
observed.
References
1
2
3
4
5
6
7
8
9
1
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In contrast, the evacuation of [NH ] SO /FSM-16 (B) at
4
2
4
even higher temperatures, for example, 500 °C, did not result in
the complete disappearance of the S=O band (compare spectra
(d) and (e) of A with the corresponding ones of B in Figure 3.)
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Chem. Soc., Chem. Commun., 1995, 973.
R. Mokaya and W. Jones, Phys. Chem. Chem. Phys., 1, 207
This suggests that direct calcination of [NH ] SO /FSM-16 in air
4
2
4
facilitates the decomposition of the [NH ] SO above 300 °C.
4
2
4
2-
(1999).
Thus the thermal stability of the SO4 species heated in vacuum
is much higher than when calcined in air.
M. Sugioka, L. Andalaluna, and J. K. A. Dapaah, Stud. Surf.
Sci. Catal., 129, 823 (2000).
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Figure 4 shows the spectra of adsorbed pyridine on (method
A and B) catalysts after pyridine desorption by evacuation at 100
-
°
C for 30 min. Bands were observed at 1547, 1490 and 1446 cm
0
1
-1
in both cases. The 1547 cm peak is attributed to the pyridini-
-1
um ion associated with Brønsted acid site whilst 1446 cm corre-
sponds to coordinated pyridine at Lewis acid site. Thus both
Brønsted acid sites and Lewis acid sites are present on
11 S. Bodoardo, R. Chiappetta, B. Onida, F. Figueras, and E.
Garrone, Micropor. Mesopor. Mater., 20, 187 (1998).