Russian Chemical Bulletin, International Edition, Vol. 54, No. 5, pp. 1185—1188, May, 2005
1185
Catalytic isomerization of allylbenzene on organomagnesium clusters
ꢀ
D. A. Potapov, L. A. Tjurina, and V. V. Smirnov
Department of Chemistry, M. V. Lomonosov Moscow State University,
1 Leninskie Gory, 119992 Moscow, Russian Federation.
Fax: +7 (095) 932 8846. Eꢀmail: smirnov@kinet.chem.msu.ru, tyurina@kinet.chem.msu.ru
Catalytic isomerization of allylbenzene to form transꢀβꢀmethylstyrene quantitatively ocꢀ
curs on the magnesium—anthracene cluster adduct under mild conditions. A lowꢀstability
organomagnesium compound, presumably of the cluster nature and active in catalytic
allylbenzene isomerization, is formed by cocondensation of magnesium and allylbenzene vaꢀ
pors at the liquid nitrogen temperature. The products of lowꢀtemperature solidꢀphase reactions
of magnesium with hydrocarbons containing aromatic rings exhibit high catalytic activity in
the allyl isomerization of allylbenzene.
Key words: catalysis, isomerization, allylbenzene, magnesium, metal vapor synthesis, magꢀ
nesium—anthracene adduct.
Magnesium compounds exhibit no catalytic activity in
hydrocarbon transformations under conventional condiꢀ
tions, although some data indicate the activity of magneꢀ
siumꢀcontaining products of metal vapor synthesis (MVS)
in hydrocarbon conversion. For instance, the study of the
magnesium cocondensates with propylene1,2 revealed
deuterioꢀhydrogen exchange. On heating the magnesium
cocondensates with hexene, anthracene, indene, and
1ꢀmethylindene the isomerization of the starting olefins
and products of their autohydrogenation occurs.3,4 In
many cases, the product : magnesium ratio is higher than
unity, indicating the catalytic character of the processes.
The catalytic isomerization and hydrogenation of unsatꢀ
urated hydrocarbons are characteristic of strong acids or
systems based on transition metals. It was assumed4,5 that
the catalytic activity of samples containing only magneꢀ
sium and hydrocarbon is caused by the formation of acꢀ
tive magnesium clusters.
It has previously6—8 been shown that the Grignard
reagent cluster containing the Mg4 core can be formed in
magnesium—halohydrocarbon systems at low temperaꢀ
tures. The quantumꢀchemical calculations9,10 show that
Mg4 is the most stable of the small magnesium clusters. It
has recently been shown that cluster compounds are also
formed by the reactions of magnesium with some hydroꢀ
carbons. For instance, derivatives containing the Mg4 clusꢀ
ter appear in the magnesium—anthracene system. Their
formation was proved by MALDI TOFꢀMS mass specꢀ
trometry.11
catalytic conversion of hydrocarbons in the presence of
preliminarily prepared individual organomagnesium clusꢀ
ter derivatives has not been proved reliably to date.
The purpose of the present work is to carry out the
catalytic isomerization of olefins (using allylbenzene as
an example) in the presence of the preliminarily prepared
organomagnesium cluster adduct and to reveal conditions
for the reaction to proceed quantitatively.
Experimental
Cocondensates of magnesium with organic compounds were
obtained by the simultaneous precipitation of magnesium and
organic reactant vapors on a vacuumꢀactivated reactor surface
cooled from outside with liquid nitrogen. Reactors of two types
were used: "immerse" (A) and "spectral" (B). In reactor A, conꢀ
densation is conducted on the internal surface of the vacuum
reactor cooled from outside with liquid nitrogen. Reactor B is a
glass vacuum vessel applied for IR spectroscopic studies of the
cocondensates. The vessel has a potassium bromide window,
and a polished copper unit cooled with liquid nitrogen is placed
into the reactor. Reagents are condensed on this unit. When
IR spectra are recorded, a beam from a spectrometer is directed
by a system of mirrors through the KBr window and a condenꢀ
sate film onto the copper unit, reflected, again passed through
the KBr window, and directed to the spectrometer detector.12
Cocondensation was carried out under a pressure of ~10–4 Torr
inside the reactors. Magnesium was evaporated from a quartz
evaporator at 400—450 °C. The evaporation temperatures of
anthracene (AN) and allylbenzene (AB) were selected to ensure
the AN/Mg ratio of 50—200 and AB/Mg ratio of 10—110 during
condensation. Reagents Mg, AN, and AB were condensed with
rates of (1.6—4.0)•10–5, (0.9—8.5)•10–3, and (0.1—3.8)•10–3
mol h–1, respectively. The condensation duration in reactors A
and B was 0.5—1.5 h and 10—30 min, respectively.
All these data agree with our previous4,5 supposition
that the catalytic activity of the MVS products involving
magnesium is caused by the presence of magnesium clusꢀ
ters with unsaturated coordination sites. At the same time,
Published in Russian in Izvestiya Akademii Nauk. Seriya Khimicheskaya, No. 5, pp. 1155—1158, May, 2005.
1066ꢀ5285/05/5405ꢀ1185 © 2005 Springer Science+Business Media, Inc.