Moyano et al.
TABLE 1. F la sh Va cu u m P yr olysis Rea ction s of 1
for N-aryl-substituted pyrazoles,1 but this case with
zeolites was the first one described in fvp of an unsub-
stituted pyrazole. On the other hand, it was observed that
pyrazole isomerization was present only in protonic
zeolites with strong acid sites (Bro¨nsted sites), while
extrusion and fragmentation reactions were catalyzed on
materials having Bro¨nsted and Lewis sites or Lewis sites
only.3
As an extension of these studies on fvp reactions over
solid catalysts, anionic clays such as hydrotalcites were
chosen as catalytic materials. It is known that hydrotal-
cites or calcined hydrotalcites have been used extensively
as catalysts in many organic processes due to their basic
properties and mainly for their ability to exchange
anions.5 Thus, it is possible to find these materials as
efficient basic catalysts for the epoxidation of various
olefins6 and also for aldol condensation reactions.7
T (°C)
catalyst
% 1
T (°C)
catalyst
% 1
400
none
HT-1
HT-2
HT-3
none
HT-1
100a
95
88
500
HT-2
HT-3
none
HT-1
HT-2
HT-3
90
88
600
100a
89
70
500
100a
91
87
83
a
From ref 2a.
The aim of this study is to research the effect of the
basic sites as well as the hydrotalcite structure on
thermal reactions of NH-pyrazoles and product selectivity
in the process. This study may be a significant contribu-
tion in the development of heterogeneous fvp systems,
since the existing literature does not provide any com-
parative studies between zeolites and hydrotalcites with
the same substrates.
Therefore, some hydrotalcites having different struc-
tures and interlayer spaces were chosen with carbonate
(HT-1), nitrate (HT-2), and silicate (HT-3). The substrates
employed are NH-pyrazole (1) and 3,5-diphenylpyrazole
(2), which afford nitrogen extrusion in the homogeneous
systems.1e,2a
It is important to point that the name anionic clay is
applied to natural or synthetic layered hydroxides con-
taining anionic species in the interlayer space. The
general formula describing the chemical composition of
III
anionic clays is [MII
M )x/n‚mH2O. When
x(OH)2](An-
1-X
MII is Mg, MIII is Al, and the interlaminar anion (A) is
carbonate, the compound is usually known as hydrotal-
cite [Mg6Al2(OH)16CO3‚4H2O]. The structure consists of
brucite layers, which are positively charged because of
partial substitution by trivalent cations, with the inter-
layer space filled with anions (to balance the positive
charge of the layers) and water molecules.
Resu lts a n d Discu ssion
F la sh Va cu u m P yr olysis of NH-P yr a zole (1). The
fvp experiments were carried out between 400 and 600
°C using hydrotalcites HT-1, HT-2, and HT-3 as solid
catalysts. The results here obtained, as well as the ones
previously reported in the homogeneous system,1,2 are
shown in Table 1. It can be seen that 1 has very low
reactivity under the experimental conditions, and high
amounts of unreacted material were recovered. Some
unidentified volatile products were formed, probably
arising from ring fragmentation or coke reactions, and
also starting material was adsorbed on the catalyst
surface. No propyne, was detectedsthe expected product
from a nitrogen extrusion reaction. This is an important
difference when comparing these reactions with the ones
over zeolites.3
In reactions where HT-2 was used, loss of the inter-
layer anion as gaseous NO2 was observed. This elimina-
tion is accompanied by an increase of the surface area,
which results in the collapse of the layered structure and,
after the thermolysis, the material became useless for
other experiments. It is worthwhile to mention here that
this loss was also detected when HT-2 was submitted to
experimental conditions without substrates, showing the
instability of this material.
As can be seen, these solids show anion-exchange
properties5,8 and, depending on the nature of the cations
and the calcination temperature, the recovery of the
structure is possible.9
Anionic clays may be synthesized by different methods
such as precipitation, hydrothermal synthesis, anion
exchange, and others. However, they are usually pre-
pared by coprecipitacion of metal hydroxides of divalent
and trivalent cations in a basic aqueous solution in the
presence of the anions that will be located in the
interlayer. Physicochemical and structural properties of
the resulting solids depend on the precipitation pH,
temperature, aging, washing, drying, and crystallization
conditions. When the clays are calcined at moderate
temperatures, new materials are formed, and a mixture
of the oxides of the starting cations is developed. These
new materials are used as catalysts in different relevant
processes.5,10 Previous studies on these materials showed
that these systems are usually more effective as catalyst
after calcinations where the layered structure is lost
starting from 350 °C and large specific areas are devel-
oped, the largest being with silicate.11
It was also seen that the decomposition of 1 was
greater when HT-3 was used. In this case, a small
amount (20%) of substrate was adsorbed by the catalyst.
This adsorption was low at 500 °C, due probably to a
partial saturation of the material. Since the catalysts
underwent continuous deactivation during the reaction,
it was impossible to recover the total amount of the
catalytic material employed as a result of a carbonaceous
deposit (coke), which restricted their lifetime.
(5) Roy, A.; Forano, C.; El Malki, K.; Besse, J . Expanded Clays and
Other Microporous Solids, Occelli, M. L., and Robson, V. N. R., Eds.;
New York, 1992; p 108.
(6) Ueno, S.; Yamaguchi, K.; Yoshida, K.; Ebitani, K.; Kaneda, K.
Chem. Commun. 1998, 3, 295.
(7) Rao, K. K.; Gravelle, M.; Valente, J . S.; Figueras, F. J . Catal.
1998, 173, 1, 115.
(8) (a) Bennani, M. N.; Tichit, D.; Figueras, F.; Abouarnadasse, S.
J . Chim. Phys. Phys.Chim. Biol. 1999, 96, 1498. (b) Cavani, F.; Trifiro,
F.; Vaccari, A. Catal. Today 1991, 11, 1.
(9) (a) Chibwe, K.; J ones, W. Chem. Mater. 1989, 1, 489. (b) Del Arco,
M.; Malet, P.; Trujillano, R.; Rives, V. J . Mater. Chem. 1999, 9, 1499.
(10) (a) Uzunova, E.; Klissurski, D.; Kassabov, J . J . Mater. Chem.
1994, 4, 153. (b) Uzunova, E.; Klissurski, D.; Mitov, I.; Stefanov, P.
Chem. Mater. 1993, 5, 576.
(11) Del Arco, M.; Gutierrez, S.; Martin, C.; Rives, V. Phys. Chem.
Chem. Phys. 2001, 3 (1), 119.
8148 J . Org. Chem., Vol. 67, No. 23, 2002