3868 Inorganic Chemistry, Vol. 49, No. 8, 2010
Rosa et al.
like TauD and MMO are characterized by more oxygen than
nitrogen donor ligands.
Fe complexes show very high reactivity and produce the
same products via the same type of mechanism. For this
reason such materials were called “mineral enzymes” or
“zeozymes”.37,38
On the basis of the design principles put forward above,
EDTA has been proposed as a ligand that should be very
effective, combining equatorial oxygen donors with a weak
trans axial donor (two off-axis N lone pairs at large dis-
tance).16 In the present contribution we will propose that the
catalytic activity of the well-known R-oxygen in Fe-ZSM-5
can be considered from the same point of view: it possibly
owes its high oxidative power to the presence of a FeO2þ unit
in exactly the favorable ligand environment of equatorial
oxygen ligands and absence of a trans axial donor.
The location and nuclearity of R-sites (an R-site is defined
as an iron entity able to adsorb one atom of R-oxygen), have
been extensively debated.38 It is by now widely accepted that
the R-sites are located inside the channels of the zeolite
matrix.39-42 The nuclearity of the R-sites is less clear,
although significant evidence has been given that they are
monatomic and in a paired arrangement, with each of the Fe
ions in the binuclear structure being capable of generating
R-oxygen species independently.23 Although the oxygen
species involved in the C-H bond activation have not been
identified experimentally, [FeO]þ, [Fe(O)2]þ, [OFeO]þ, and
[FeO]2þ species have been proposed as the catalytically active
centers on the basis of quantum chemical calculations.43-48
Depending on the ironoxo species assumed as the catalytic
active center, different C-H bond activation mechanisms
have been theoretically proposed.
Iron exchanged ZSM-5 has been shown to be an active
catalyst for many reactions, a very interesting example being
the decomposition of N2O. This process has been suggested
to proceed via oxidation of Fe2þ to Fe3þ, forming active
oxygen species called by Panov and co-workers atomic R-
oxygen.22,23 This R-oxygen species is capable of selectively
and quantitatively converting benzene to phenol at ambient
temperature,24,25 similar to the active oxygen of monooxy-
genases (MMOs), forwhich the hydroxylation of aromaticsis
a typical reaction.26 The R-oxygens in Fe-ZSM-5 zeolites
react at room temperature even with methane, the most inert
organic molecule, giving quantitative yield of methanol,27
thus challenging the reactivity of the active oxygen of
methane monooxygenases (MMO).28-33 Dubkov et al.34
studied the kinetic isotope effect (KIE = kH/kD) for the
methane and benzene oxidations by R-oxygen and found
high KIE values (1.9-5.5, depending on the reaction tem-
perature) for methane oxidation and no isotopic effect for
benzene oxidation. This means that, similar to the MMO
case, methane oxidation by R-oxygen involves the cleavage of
the C-H bond as the rate-limiting step. The oxidation of
benzene proceeds somewhat differently. Understandably,
benzene is attacked by the electrophilic FeO2þ at its π elec-
tron cloud, as has been found for benzene hydroxylation with
biomimetic non-heme FeO2þ complexes35 and with a zeolite
[FeO]þ with a d5 Fe(III) has been assumed as the active
catalytic center by Yoshizawa et al.43 We wish to stress that
the [FeO]þ would have to accommodate the extra electron it
possesses compared to [FeO]2þ in the R-dz2 orbital, which we
view16,18 as the prime acceptor orbital of this moiety, respon-
sible for its extreme electrophilicity and high activity in C-H
functionalization. This will lead to much higher barriers than
expected for [FeO]2þ. The authors of ref 43 studied the
reaction pathways and the energetics for the direct hydro-
xylation of methane and of benzene over [FeO]þ in the Fe-
ZSM-5 zeolite surface. The barrier height computed for the
second transition state in the two-step process, TS2, is quite
high (41.6 and 31.1 kcal/mol in the case of methane and
benzene, respectively). The proposed mechanism does not
account for the high KIE values measured for methane
oxidation by zeolite R-oxygen.34 A d5 Fe(III) iron center
with occupied R-dz2 is also advocated in the theoretical work
by Malykhin et al.,48 who propose an electronic configura-
cluster with FeO2þ 36
. Therefore, in many respects, R-oxygen
in Fe-ZSM-5 zeolites exhibits an exciting analogy to the active
oxygen in MMO: in both cases oxygen species coordinated to
tion [Fe(III)O ]
- 2þ. These authors note however that in their
3
calculations on the model system FeO(OH)2, the lowest
energy configuration at the minimum energy geometry does
have a d4 Fe(IV) iron center, that is, empty R-dz2. Important
recent experimental evidence, based on resonant inelastic
(22) Panov, G. I.; Uriarte, A. K.; Rodkin, M. A.; Sobolev, V. I. Catal.
Today 1998, 41, 365.
(23) Dubkov, K. A.; Ovanesyan, N. S.; Shteinman, A. A.; Starokon,
E. V.; Panov, G. I. J. Catal. 2002, 207, 341.
(24) Sobolev, V. I.; Kharitonov, A. S.; Paukshtis, Y. A.; Panov, G. I.
J. Mol. Catal. 1993, 84, 117.
(25) Panov, G. I.; Sobolev, V. I.; Dubkov, K. A.; Parmon, V. N.;
Ovanesyan, N. S.; Shilov, A. E.; Shteinman, A. A. React. Kinet. Catal. Lett.
1997, 61, 251.
(26) Shilov, A. E. Metal Complexes in Biomimetic Chemical Reactions;
CRC Press: New York, 1997.
(27) Panov, G. I.; Sobolev, V. I.; Dubkov, K. A.; Kharitonov, A. S. Stud.
Surf. Sci. Catal. 1996, 101, 493.
(28) Dewitt, J. G.; Bentsen, J. G.; Rosenzweig, A. C.; Hedman, B.; Green,
J.; Pilkington, S.; Papaefthymion, G. C.; Dalton, H.; Hodgson, K. O.;
Lippard, S. J. J. Am. Chem. Soc. 1991, 113, 9219.
(29) Shteinman, A. A. Russ. Chem. Bull. 2001, 50, 1795.
(30) Que, L. Pure Appl. Chem. 1998, 70, 947.
(31) Kopp, D. A.; Lippard, S. J. Curr. Opin. Chem. Biol. 2002, 6, 568.
(32) Siegbahn, P. E. M.; Crabtree, R. H.; Nordlund, P. J. Biol. Inorg.
Chem. 1998, 3, 314.
(37) Parton, R.; De Vos, D.; Jakobs, P. A. In Zeolite Micropores Solids:
Synthesis, Structure and Reactivity; Derouane, E. G., Ed.; Kluwer: The Nether-
lands, 1992; p 555.
(38) Panov, G. I. CATTECH 2000, 4, 18.
(39) Ribera, A.; Arends, I. W. C. E.; de Vries, S.; Perez-Ramires, J.;
Sheldon, R. A. J. Catal. 2000, 195, 287.
(40) Pirutko, L. W.; Parenago, O. O.; Lunina, E. V.; Kharitonov, A. S.;
Okkel, L. G.; Panov, G. I. React. Kinet. Catal. Lett. 1994, 52, 275.
(41) Panov, G. I.; Kharitonov, A. S.; Fenelonov, V. B.; Voskresenskaya,
T. P.; Rudina, N. A.; Molchanov, V. V.; Plyasova, M. L. Zeolites 1995, 15,
253.
(42) Pirutko, L. W.; Dubkov, K. A.; Solovjeva, L. P.; Panov, G. I. React.
Kinet. Catal. Lett. 1996, 58, 105.
(43) Yoshizawa, A. L.; Shiota, Y.; Yumura, T.; Yamabe, T. J. Phys.
Chem. B 2000, 104, 734.
(44) Kachurovskaya, N. A.; Zhidomirov, G. M.; Hensen, E. J. M.; van
Santen, R. A. Catal. Lett. 2003, 86, 25.
(33) Lieberman, R. L.; Rosenzweig, A. C. Nature 2005, 34, 177.
(34) Dubkov, K. A.; Sobolev, V. I.; Talsi, E. P.; Rodkin, M. A.; Watkins,
N. H.; Shteinman, A. A.; Panov, G. I. J. Mol. Catal. 1997, 123, 155.
(35) de Visser, S. P.; Oh, K.; Han, A.-R.; Nam, W. Inorg. Chem. 2007, 46,
4632.
(36) Fellah, M. F.; van Santen, R. A.; Onal, I. J. Phys. Chem. C 2009, 113,
15307.
(45) Kachurovskaya, N. A.; Zhidomirov, G. M.; van Santen, R. A.
J. Phys. Chem. B 2004, 108, 5944.
(46) Ryder, J. A.; Chakraborty, A. K.; Bell, A. T. J. Catal. 2003, 220, 84.
(47) Liang, W.-Z.; Bell, A. T.; Head-Gordon, M.; Chakraborty, A. K.
J. Phys. Chem. B 2004, 108, 4362.
(48) Malykhin, S.; Zilberberg, I.; Zhidomirov, G. M. Chem. Phys. Lett.
2005, 414, 434.