Polyoxometalate grafting onto silica: stability diagrams of H3PMo12O40 on {001}, {101}, and {111}...
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This journal is c the Owner Societies 2011 Phys. Chem. Chem. Phys., 2011, 13, 15955–15959 15955
Cite this: Phys. Chem. Chem. Phys., 2011, 13, 15955–15959
Polyoxometalate grafting onto silica: stability diagrams of H3PMo12O40
on {001}, {101}, and {111} b-cristobalite surfaces analyzed by DFTw
Xavier Rozanska,z*a Philippe Sautet,*aFrancoise Delbecq,
aFrederic Lefebvre,
b
Sergei Borshch,aHenri Chermette,
cJean-Marie Bassetyb and Eva Grinenval
b
Received 13th April 2011, Accepted 8th July 2011
DOI: 10.1039/c1cp21171d
The process of grafting H3PMo12O40 onto silica surfaces is studied using periodic density
functional theory methods. For surfaces with a high hydroxyl coverage, the hydroxyl groups are
consumed by the polyoxometalate protons, resulting in water formation and the creation of a
covalent bond between the polyoxometalate and the surface, and mostly no remaining acidic
proton on the polyoxometalate. When the surfaces are partially dehydroxylated and more
hydrophobic, after temperature pretreatment, less covalent and hydrogen bonds are formed and
the polyoxometalate tends to retain surface hydroxyl groups, while at least one acidic proton
remains. Hence the hydroxylation of the surface has a great impact on the chemical properties of
the grafted polyoxometalate. In return, the polyoxometalate species affects the compared stability
of the partially hydroxylated silica surfaces in comparison with the bare silica case.
1. Introduction
Polyoxometalates (POM) are molecular transition metal oxide
compounds with a structure built upon MOn and sometimes
with inclusion of XOm polyhedra, where M and X are a
transition metal and an heteroatom, respectively, and that
can present Brønsted acidity.1–4 Counter-ions are present to
balance the system charge in the solid state. The immobiliza-
tion of POM onto surfaces is of great interest from a chemical
point of view because it allows an additional control over their
physical and physico-chemical properties opening further use
in heterogeneous catalysis processes.1,2,5 Recently, Grinenval
et al.5 showed that it is possible to obtain well-defined mono-
dispersed H3PMo12O40 (H3POM) species onto silica surfaces,
allowing the accessibility to efficient heterogeneous catalysts.
Particularly, their grafting procedure permits us to get
H3POM units that retain seven times more protons than when
a classical impregnation procedure is employed.5
In this study, we focus on the grafting process of
H3PMo12O40 Keggin polyoxometalate onto silica surfaces.
This POM carries three protons and is approximately sphe-
rical with a diameter of ca. 1 nm (Fig. 1). The silica surface is
terminated with hydroxyl groups with a surface density that
depends on the temperature and water partial pressure.6–8 The
bonding between the POM molecule and the silica surface
occurs in two ways, namely via the formation of hydrogen
bonds between the acidic protons of H3POM and the surface
hydroxyl groups, be it accompanied or not by proton transfer
from H3POM to the surface hydroxyl groups, or via the
formation of covalent bond(s) between POM oxygen and
surface silicon(s), with release of water according to the
successive reactions:
RSi–OH�H3POM - H2O(g) + H2POM–SiR, (1a)
RSi–OH�H2POM–SiR - H2O(g) + HPOMQ(SiR)2,
(1b)
RSi–OH�HPOMQSiR - H2O(g) + POMR(SiR)3,
(1c)
where ‘SiR’ represents a surface Si atom bonded to three
oxygens of the silica surface, ‘–’, ‘Q’, and ‘R’ represent one,
two and three covalent bonds, respectively, and ‘�’ an hydrogen-
bonded complex. The study of this reaction is not trivial
because reaction (1) can enter in competition with the silica
surface dehydroxylation reaction:
HO–SiR + HO–SiR - H2O(g) + RSi–O–SiR, (2)
and reactions (1) and (2) can couple in:
aUniversite de Lyon, Institut de Chimie de Lyon, CNRS, EcoleNormale Superieure de Lyon, Laboratoire de Chimie, Laboratoire deChimie, Ecole Normale Superieure de Lyon, 46 Allee d’Italie, 69046Lyon, France. E-mail: [email protected],[email protected]
bUniversite de Lyon, Institut de Chimie de Lyon, C2P2 UMR 5265,CNRS–CPE–Universite de Lyon I, LCOMS, France
cUniversite de Lyon, Institut de Chimie de Lyon, CNRS UMR 5180Sciences Analytiques Chimie Physique Theorique–Universite de Lyon I,Francew Electronic supplementary information (ESI) available. See DOI:10.1039/c1cp21171dz Present address: Materials Design, 18 rue de Saisset, 92120Montrouge, France.y Present address: KAUST Catalysis Center (KCC), Thuwal,Kingdom of Saudi Arabia.
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15956 Phys. Chem. Chem. Phys., 2011, 13, 15955–15959 This journal is c the Owner Societies 2011
RSi–OH�H3POM + RSi–O–SiR
- H2POM–SiR + HO–SiR + HO–SiR, (3a)
RSi–OH�H2POM–SiR + RSi–O–SiR
- HPOMQ(SiR)2 + HO–SiR + HO–SiR, (3b)
RSi–OH�HPOMQSiR + RSi–O–SiR
- POMR(SiR)3 + HO–SiR + HO–SiR, (3c)
which implies that the silica surface reconstruction could be
affected by the presence of the POM. Hence, POM grafting
onto silica surfaces cannot be studied independently of the
hydroxylation/dehydroxylation processes of the silica surfaces.
Theoretical chemistry is of great help for an atomistic scale
understanding of the structure and stability of metal
complexes grafted on oxide supports.9 After the presentation
of the computational methods, we explore the stability
diagrams as a function of temperature and water partial
pressure for the grafting of H3PMo12O40 on three different
surfaces of b-cristobalite and we compare them with the
corresponding diagrams obtained on bare silica.
2. Methods
All calculations are performed in the framework of density
functional theory (DFT) for periodic systems, as implemented in
VASP.10–13 We use the PBE exchange–correlation functional14,15
with the following calculation parameters: (i) Van der Bilt
ultra-soft pseudopotentials16 for all atoms, (ii) an associated
energy cut-off for the plane wave basis set of 400 eV, (iii) a
K-point sampling restricted to the G-point owing to the
relatively large unit cells. The electronic wave-functions
Fig. 1 Geometry of the PMo12O403� polyoxometalate: the core of the
Keggin complex is a PO43 tetrahedron that is sheltered inside an
Mo12O36 shell that is constituted of twelve OQMoO4/2 distorted
pyramids, where O1/2 designates an oxygen atom that is shared by
two pyramids. Three protons are required to balance the negative
charge: they are located on bridging oxygen atoms between two Mo
for an isolated POM3,4 but migrate to maximize the number of strong
hydrogen bonds when in contact with the silica surface.5 These
protons show strong acidic properties.
Table 1 Dimensions of the unit cells and energies of the systemsa
Label Dimensions of the unit cell Composition of the unit cell Energy
H2O 2 � 2 � 2 O, 2H �14.27b-cristobalite bulk 0.73 � 0.73 � 0.73 8Si, 16O �190.28001-1:POM 1.47 � 1.47 � 3 12Mo, 1P, 40Si, 136O, 35H �1625.67001-1–POM 1.47 � 1.47 � 3 12Mo, 1P, 40Si, 135O, 33H �1610.92001-2:POM 1.47 � 1.47 � 3 12Mo, 1P, 40Si, 132O, 27H �1566.92001-2–POM 1.47 � 1.47 � 3 12Mo, 1P, 40Si, 131O, 25H �1552.39001-2QPOM 1.47 � 1.47 � 3 12Mo, 1P, 40Si, 130O, 23H �1537.70001-3:POM 1.47 � 1.47 � 3 12Mo, 1P, 40Si, 132O, 27H �1566.44001-3–POM 1.47 � 1.47 � 3 12Mo, 1P, 40Si, 131O, 25H �1552.15001-3QPOM 1.47 � 1.47 � 3 12Mo, 1P, 40Si, 130O, 23H �1537.30001-6:POM 1.47 � 1.47 � 3 12Mo, 1P, 43Si, 136O, 23H �1602.68001-6–POM 1.47 � 1.47 � 3 12Mo, 1P, 43Si, 135O, 21H �1587.92001-6QPOM 1.47 � 1.47 � 3 12Mo, 1P, 43Si, 134O, 19H �1572.72101-1:POM 2.08 � 1.47 � 3 12Mo, 1P, 48Si, 152O, 35H �1813.00101-1–POM 2.08 � 1.47 � 3 12Mo, 1P, 48Si, 151O, 33H �1797.92101-1QPOM 2.08 � 1.47 � 3 12Mo, 1P, 48Si, 150O, 31H �1783.30101-1RPOM 2.08 � 1.47 � 3 12Mo, 1P, 48Si, 149O, 29H �1769.21101-2:POM 2.08 � 1.47 � 3 12Mo, 1P, 52Si, 156O, 27H �1844.32101-2-POM 2.08 � 1.47 � 3 12Mo, 1P, 52Si, 155O, 25H �1829.67101-2QPOM 2.08 � 1.47 � 3 12Mo, 1P, 52Si, 154O, 23H �1815.13101-3:POM 1.56 � 1.47 � 3 12Mo, 1P, 40Si, 128O, 19H �1497.98101-3–POM 1.56 � 1.47 � 3 12Mo, 1P, 40Si, 127O, 17H �1483.23101-3QPOM 1.56 � 1.47 � 3 12Mo, 1P, 40Si, 126O, 15H �1468.54111-1:POM 2.08 � 2.08 � 3 12Mo, 1P, 64Si, 184O, 35H �2194.16111-1–POM 2.08 � 2.08 � 3 12Mo, 1P, 64Si, 183O, 33H �2179.37111-1QPOM 2.08 � 2.08 � 3 12Mo, 1P, 64Si, 182O, 31H �2164.94111-1RPPOM 2.08 � 2.08 � 3 12Mo, 1P, 64Si, 181O, 29H �2150.24111-3:POM 2.08 � 2.08 � 3 12Mo, 1P, 68Si, 188O, 27H �2224.64111-3–POM 2.08 � 2.08 � 3 12Mo, 1P, 68Si, 187O, 25H �2210.19111-3QPOM 2.08 � 2.08 � 3 12Mo, 1P, 68Si, 186O, 23H �2195.30a The dimensions are in nm and the energies in eV. All unit cells possess orthorhombic symmetry (a = 901, b = 901, g = 901) except 111 systems,
which are hexagonal (a = 901, b = 901, g = 1201, b in the xy direction).
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are restricted to close-shell configurations in agreement with
the nature of the system. All atomic positions are allowed to
relax in the geometry optimization. The geometries are
considered optimized when forces on all atoms are below
0.03 eV A�1. The vectors and atomic formula of the unit cells
are reported in Table 1.
The Gibbs free energies are evaluated with the usual
thermochemical equations (see ref. 1 and 17 and electronic
supporting information) to analyze the stable POM-silica
surface structures as a function of T and PH2O. The surface
labels used here are the same as in ref. 17 for easier comparison.
The atomic coordinates of all silica surfaces can be found in the
supporting information of ref. 17.
3. Results and discussion
We analyzed previously the structures, reconstruction, and
stability of b-cristobalite surfaces during a dehydroxylation
process following reaction (2) and their comparison with
experimental amorphous silica surfaces.17 This permits us to
access silica surface models that cover a large range of hydro-
xyl group coverage, associated with more or less severe pre-
treatment conditions. In the current study, we chemisorb
H3PMo12O40 onto our b-cristobalite surface models and define
the subsequent systems by removing one to three H2O, when
possible, following reaction (1). In the hydrogen-bonded
POM�complex, the number of hydrogen bonds is not only
based on the number of protons in the POM but also on the
availability of neighboring surface hydroxyl groups to interact
with it. The formation of three covalent bonds (after dehydration)
between the POM and the surface is sometimes not permitted
due to topological inadequacy (Fig. 2 and 3). Our investigation
of the POM�silica surface systems is not limited to the
thermodynamically most stable bare silica surfaces in the
absence of the POM but also includes metastable terminations
that could be stabilized by the presence of the POM (Table 1,
Fig. 4).17 With this procedure, we consider all reactions from
(1) to (3). We describe now the POM�surface systems that are
the most stable. The determination of the Gibbs free energies
of the reactions5,17 allows the construction of the stability
diagrams as a function of water partial pressure and temperature.
In this diagram, only the most stable surface system is shown, for
given conditions of temperature and pressure. The comparison
of these diagrams in the presence and absence of the POM is
particularly revealing (Fig. 5). In Fig. 5, we also include the
hydroxyl coverage of the silica surface prior to grafting and,
between parentheses, the hydroxyl coverage after the POM
grafting reaction (1).
As mentioned earlier, reactions (1) and (2) are in competi-
tion because they both lead to dehydroxylation and H2O
release from the surface. Considering the stability diagrams
at low temperature and high water partial pressure in Fig. 5,
the presence of the POM has a rather equivalent effect on the
{001}, {101}, and {111} surfaces: it lowers the temperature or
increases the water partial pressure for the first water release in
comparison to surfaces without POM. The easier water for-
mation in presence of the POM could be related to the more
acidic character of the POM in comparison to the surface
hydroxyl groups. The extent of this effect, which results from
the POM grafting through reaction (1), is different for the
three surfaces. For the {111} surface, three hydroxyl groups
are consumed at PH2O/P1 = 1 and T = 300 K, and H3POM
has lost its three protons, forming three covalent bonds with
the surface in return. In the same conditions two hydroxyl
groups are consumed and the POM forms two covalent bonds
on the {101} surface. The case of the {001} surface is slightly
different. Without the POM, this surface has already a
different behavior from the two other ones: it undergoes a
first dehydration according to reaction (2) in ambient conditions
of pressure and temperature, whereas {101} and {111} surfaces
require harder conditions. When the POM is present on {001},
the dehydrated form is still favored but the shift in pressure
and temperature for dehydration is much less pronounced
than for the other surfaces. The grafting of the POM occurs
through two covalent bonds.
Furthermore, as suggested by reaction (3), the POM pre-
sence alters the very local topology of the silica surface while
Fig. 2 Front and side views of POM grafted with two covalent bonds
onto partially dehydroxylated {001} silica surface (product of reaction
1b, 001-2QPOM in Fig. 5). The Si–O–Mo angles usually do not have
much flexibility: they are close in Fig. 2 and 3. The value for all systems
(Fig. 5) is 155+21/�71. The unavailability of hydroxyl to anchor the
POM while conserving this Si–O–Mo angle prevents here the forma-
tion of a third covalent bond, although both POM’s proton and
surface hydroxyl groups are present and interact via hydrogen bonds.
Fig. 3 View of tricovalently grafted POM onto {111} surface
(111-1RPOM in Fig. 5). The formation of three covalent bonds
between the POM and the surface is favorable in ambient conditions
of temperature and water partial pressure when the topologies of the
accessible silica surface hydroxyl groups permit it.
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conserving the hydroxyl coverage. In the case of the {001}
surface for an hydroxyl coverage of 3.71 nm�2, the honeycomb
arrangement of the hydroxyl is ca. 20 kJ mol�1 nH2O�1 less
stable than a row-pattern.17 After the POM grafting, the
stability becomes reversed. This is explained by the most
favorable fitting of H3PMo12O40 in the honeycomb nests of
the surface, allowing a larger number of hydrogen bonds
between POM and surface.
Similarly, the maximum number of covalent bonds that can
be formed between the POM and the silica surface depends on
the local disposition of the surface hydroxyl groups. Only two
covalent bonds can be formed in the case of the {001}
honeycomb pattern surface, whereas three can be formed with
{101} and {111} surfaces over a large range of water partial
pressure and temperature.
When silica surface dehydroxylation is considered at higher
temperature and/or lower water partial pressure than
previously, it appears in contrast that the POM presence slowsFig. 4 Definition of the silica surfaces used in this work and their
labels (silicon: light grey, oxygen: dark grey, hydrogen: white).
Fig. 5 Stability diagrams of {001} (top), {101} (middle), and {111}
(bottom) b-cristobalite surfaces in absence (left) and presence (right) of
H3PMo12O40 as a function of the water partial pressure and tempera-
ture. The bonding between the POM and the surface is labeled as
follow: ‘:’, ‘–’, ‘Q’, and ‘R’ stand for hydrogen-bonds, one, two, and
three covalent bonds between the POM and the surface (reaction (1)),
respectively. The numbers are hydroxyl coverage in nm�2. For the
POM�surfaces (right), two values are given when relevant: the first
corresponds to the hydroxyl coverage of the corresponding silica
surface in the absence of POM, whereas the value in parentheses
is calculated by subtracting the surface hydroxyl groups that are
consumed in reaction (1).
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down silica surface dehydroxylation and reconstruction in
comparison to the situation in the absence of the POM. Hence,
deep dehydration following reaction (2) is inhibited albeit the
initial dehydration following reaction (1) is favored by the
POM. For instance, the reconstructed {101} surface with an
hydroxyl coverage of 2.62 nm�2 is reached at a temperature of
ca. 600 and 725 K at PH2O = 10�5 bar in absence and presence
of the POM, respectively. Similar results are found with all
surfaces.
Overall, the size of the surface stability domains is different
in the presence or absence of the POM. With high hydroxyl
coverage surfaces, the surface hydroxyl groups are consumed
by the acid protons of the POM, forming water and a covalent
bond linkage. The resulting hydroxyl coverage is then lower
than in the absence of the POM. When the surfaces become
partially dehydroxylated and more hydrophobic, less covalent
and hydrogen bonds are formed between the POM and the
surface and reaction (3) comes into play to permit the POM to
retain surface hydroxyl groups in comparison to the bare silica
surfaces.
Further dehydroxylation, which we do not show here
because this goes beyond the experimental hydroxyl coverage
of ca. 1.5 nm�2,5 would lead to surface hydroxyl rarefaction
which eventually prevents the forming of more than one
covalent bond between the POM and surfaces. However,
one should keep in mind that hydroxyl group distribution
on the silica surfaces is not uniform,5,8 which can lead to the
possibility of multiple covalent bond formation even at relatively
low hydroxyl group coverage. For totally dehydroxylated
silica surfaces, a covalent bond could still be formed
between the POM and the silica surface following a reaction
equivalent to (3). Fully dehydroxylated silica surfaces are
experimentally obtained below PH2O = 105 Torr and above
T = 1473 K.6,7
The stability diagrams are insightful in interpreting the
experimental data.5 Under thermochemical equilibrium and
for moderate dehydration pretreatment conditions, e.g. 105 bar
and 500 K, the number of covalent bonds between the
POM and the silica surfaces should be two or three depending
on the surface topology. The POM should hence retain only a
very small number of protons (one or zero). This situation
corresponds to the ‘classical impregnation’ in ref. 5. The
temperature that is employed in this impregnation procedure
permits surface and POM covalent grafting to respect the
thermochemistry of the system (Fig. 5).
In the surface organometallic chemistry (SOMC) strategy,
the silica surface is pretreated at high temperature (T = 773 K)
under high vacuum (P = 10�5 Torr) before POM introduction.
The surfaces show hydroxyl coverage of ca. 1.4 nm�2 under
these conditions. The POM is then grafted at 298 K
in anhydrous conditions, which prevents silica surface
reconstruction and rehydration. Calculations suggest that only
dehydrated surfaces like 001-6, 101-2, and 111-4 exist under
these conditions (Fig. 5, left). The number of covalent bonds
between the POM and these surfaces is at most two (Fig. 5,
right), hence preserving at least one acidic proton on the POM.
The calculations hence clearly explain the influence of the
silica preparation conditions and surface hydroxyl density on
the final Brønsted acidity of the grafted POM.
4. Conclusions
We studied the grafting of H3PMo12O40 onto surfaces of
b-cristobalite by means of DFT, which permits us to construct
the stability diagrams as a function of temperature and water
partial pressure. The comparison with the diagrams of the bare
surface is particularly revealing and shows the full complexity
of the system. Indeed, silica dehydroxylation couples with the
covalent bonding of the acidic POM onto the surface, which
leads to a modification of the stability diagram of silica. The
dehydration following the POM grafting occurs at lower
temperature and at higher water partial pressure than the first
dehydration of the bare surface. In contrast, the second
dehydration is less easy on POM grafted surface than on bare
surface. Our results are compared with experimental data,
which greatly helps in their interpretation and comprehension.
In particular, our results explain the number of remaining
POM protons after grafting, and the superior density of
protons obtained by the SOMC approach.
Acknowledgements
This research was supported by the Agence Nationale de la
Recherche, research project METHANOX. CINES, IDRIS
(CNRS), and PSMN (ENS de Lyon) are greatly acknowledged
for the granted CPU time allocations.
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