Communications
cofeeding of water leads to a substantial increase of the
propane conversion. The conversion passes a maximum at
bered ring of the wall of the sinusoidal channel of MFI zeolite.
The cluster approach was chosen, because modeling of the
unit cell of MFI zeolite with 96 T atoms is computationally
prohibitive. On the other hand, the cluster with 14 T atoms is
large enough to account for all significant interactions
between the cationic species and the zeolite framework as
well as to describe activation of small molecules such as H2
and H2O. This conclusion is supported by recent quantum-
chemical calculations with this cluster.[12] Water dissociation
at cluster I is exothermic (DE = ꢀ102 kJmolꢀ1, Figure 1) and
pH O of 0.3 kPa. Catalyst performance in the presence of
2
steam (0.3 kPa) was found to be stable over a period of at
least 4 h. The very different product composition between
Ga+/ZSM-5 in the absence of steam and HZSM-5 points to a
change in the mechanism from protolytic hydrocarbon
ꢀ
ꢀ
activation involving C H and C C bond cleavage for
ꢀ
HZSM-5 to dominant C H activation by the Lewis acidic
Ga cations.[8]
Addition of water to the feed strongly increases the
activity. The main product remains propylene, although with
increasing water content slightly increased amounts of
methane and ethylene are formed. The formation of methane
and ethylene is due to protolytic cracking of propane. This
finding indicates some regeneration of Brønsted acid protons,
which are formed upon hydrolysis of gallium species.[6] More
ethylene than methane is formed because of additional
proton-catalyzed oligomerization/cracking reactions of pro-
pylene. The carbon selectivity to dehydrogenated products
remains well over 85%. The increased dehydrogenation
activity of Ga/ZSM-5 compared to HZSM-5 is obvious from
the increased amount of hydrogen formed. No carbon oxides
were detected in the reactor effluent. The activity decrease at
higher pH O is likely due to more complete hydrolysis of the
2
active intrazeolitic Ga sites. 27Al NMR spectroscopy meas-
urements indicate that prolonged steam exposure does not
lead to massive redistribution of tetrahedral aluminium
species (see the Supporting Information).
The promoting effect of water is due to the formation of
reactive partly hydrolyzed gallium species. For mononuclear
gallium sites, the catalytic cycle is initiated by desorption of
H2 from [Ga3+(Hꢀ)(OHꢀ)]+ to form the GaO+ ion. However,
Table 2 shows that the energy barrier for hydrogen recombi-
Figure 1. Relative stability of binuclear cationic Ga species stabilized
by the eight-membered ring of ZSM-5 zeolite. For clarity, the zeolite
clusters are not included in the depicted structures. All of the
structures involve bidentate coordination of each Ga cation to two
zeolite-framework oxygen anions of the 14-T-atom zeolite cluster (see
the Supporting Information).
Table 2: Comparison of reaction energies (DE) and activation barrier
energies (DE°) for H2 and H2O desorption over various Ga clusters.
leads to formation of structure II, which contains
a
[Ga3+(Hꢀ)(OHꢀ)]+ ion in which the hydroxyl group coordi-
nates to the neighboring Ga+ ion. This structure can rearrange
by migration of the hydroxyl H atom to the Ga+ ion to give
structure III, an oxygen-bridged binuclear [{Ga3+(Hꢀ)}2O]2+
ion. The latter rearrangement allows an additional stabiliza-
tion energy of 44 kJmolꢀ1. Reaction of a second water
molecule with structure III results in further stabilization of
the extraframework gallium dimer by 69 kJmolꢀ1 and gives
structure IV (Figure 1). Structure IV contains an almost
square and planar Ga2O2 core with hydride ions and protons
bound to the extraframework Ga cations and O anions,
respectively. Rearrangement of structure IV to the conven-
tional situation with two isolated [Ga3+(Hꢀ)(OHꢀ)]+ ions
(structure V) interacting through a hydrogen bond costs
68 kJmolꢀ1.
Reaction[a]
DE [kJmolꢀ1
]
DE° [kJmolꢀ1
]
II!VI+H2
147
102
127
113
242
128
263
230
211
142
305
259
II!I+H2O
IV!VII+H2
IV!II+H2O
[Ga3+(Hꢀ)(OHꢀ)]+!GaO+ +H2
[b]
[Ga3+(Hꢀ)(OHꢀ)]+!Ga+ +H2O[b]
[a] Roman letters refer to structures in Figure 1; [b] reference [10].
nation is prohibitively high (305 kJmolꢀ1), which is due to the
very low acidity of the hydrogen atom attached to the oxygen
atom. In agreement with earlier computations,[11] water
formation is strongly favored. We propose that multinuclear
Ga sites are formed. To clarify whether such species can be
generated upon water adsorption and whether their forma-
tion facilitates hydrogen desorption, we studied the inter-
action of two distantly placed Ga+ ions with H2O by quantum-
chemical cluster calculations in the DFT formalism. The
Ga+ ions are stabilized by two negatively charged Al-con-
taining oxygen tetrahedra embedded in a cluster of 14
T atoms (T= Si, Al) representing the elongated eight-mem-
Since hydrogen-atom recombination at the hydroxylated
structures II and IV is required to initiate alkane dehydrogen-
ation, the corresponding energetics were evaluated. Reaction
energies and activation barriers are listed in Table 2. Coor-
dination of the hydroxyl group of the [Ga(Hꢀ)(OHꢀ)]+ ion to
the neighboring gallium cation results in a significant decrease
of the reaction energy for H2 recombination (147 kJmolꢀ1)
7274
ꢀ 2007 Wiley-VCH Verlag GmbH & Co. KGaA, Weinheim
Angew. Chem. Int. Ed. 2007, 46, 7273 –7276