Maxence Valla1, Aaron J Rossini2, Maxime Caillot3,4, Céline Chizallet4, Pascal Raybaud4, Mathieu Digne4, Alexandra Chaumonnot4, Anne Lesage5, Lyndon Emsley2, Jeroen A van Bokhoven3,6, Christophe Copéret1. 1. Department of Chemistry and Applied Biosciences, Laboratory of Inorganic Chemistry, ETH Zürich , Vladimir Prelog Weg 1-5, CH-8093 Zürich, Switzerland. 2. Institut des Sciences et Ingénierie Chimiques, Ecole Polytechnique Fédérale de Lausanne (EPFL) , CH-1015 Lausanne, Switzerland. 3. Department of Chemistry and Applied Biosciences, Institute for Chemical and Bioengineering, ETH Zürich , Vladimir Prelog Weg 1, CH-8093 Zürich, Switzerland. 4. IFP Energies nouvelles , Rond-point de l'échangeur de Solaize, BP 3, 69360 Solaize, France. 5. Centre de RMN à Très Hauts Champs, Institut de Sciences Analytiques (CNRS/ENS Lyon/UCB Lyon 1), Université de Lyon , 69100 Villeurbanne, France. 6. Paul Scherrer Institut , CH-5232 Villigen PSI, Switzerland.
Abstract
Despite the widespread use of amorphous aluminosilicates (ASA) in various industrial catalysts, the nature of the interface between silica and alumina and the atomic structure of the catalytically active sites are still subject to debate. Here, by the use of dynamic nuclear polarization surface enhanced NMR spectroscopy (DNP SENS) and density functional theory (DFT) calculations, we show that on silica and alumina surfaces, molecular aluminum and silicon precursors are, respectively, preferentially grafted on sites that enable the formation of Al(IV) and Si(IV) interfacial sites. We also link the genesis of Brønsted acidity to the surface coverage of aluminum and silicon on silica and alumina, respectively.
Despite the widespread use of amorphous aluminosilicates (ASA) in various industrial catalysts, the nature of the interface between silica and alumina and the atomic structure of the catalytically active sites are still subject to debate. Here, by the use of dynamic nuclear polarization surface enhanced NMR spectroscopy (DNPSENS) and density functional theory (DFT) calculations, we show that on silica and alumina surfaces, molecular aluminum and silicon precursors are, respectively, preferentially grafted on sites that enable the formation of Al(IV) and Si(IV) interfacial sites. We also link the genesis of Brønsted acidity to the surface coverage of aluminum and silicon on silica and alumina, respectively.
Amorphous
aluminosilicates (ASAs) are ubiquitous in catalysis and
are used both as a catalyst and as a catalyst support for single sites,
metal sulfides, and metal nanoparticles because they have high surface
areas, combined with mild acidic properties alternative to zeolite
in industrial reaction conditions.[1−3] They are known to dehydrate
ethanol to ethylene, as well as to catalyze the isomerization of m-xylene.[4] They are also industrially
used in refining technology to convert heavy fractions of crude oil
and as supports for hydrotreating catalysts thanks to the tolerance
of their acid sites to heteroelements containing organic molecules.[5−8] They also show promising properties in the production of fine chemicals[1,2,9,10] and
the conversion of biomass.[11,12]Their activity
arises from their acid/base properties. The presence
of both aluminum and silicon atoms at the surface of the materials
induces Brønsted acidity to the surface hydroxyls.[2,13−16] However, the complex distribution of silicon and aluminum and the
amorphous character of the material make the correlation between structure
and activity very difficult to establish; the structure of the catalytically
active sites are still a matter of debate.[14,17−20] The original structural models of ASA proposed that the Brønsted
acidity arises from protons compensating the electronic charge of
the surface[21,22] or from HO–Al groups close
to silanol groups.[23] Since these original
pioneering works, numerous additional structural models have been
proposed. Based on probe molecule adsorption, it has been suggested
that the acidic sites are similar to those of zeolites, that is, bridging
Si–OH–Al groups.[14,20,24] In contrast to depositing aluminum or silicon precursors, coimpregnation
yields sites of similar strength as zeolites.[16] Other studies have concluded that the acidic sites are silanol groups
in the vicinity of aluminum atoms (but not bridging the OH). In this
case, the nature of Al atoms in the vicinity of the acidic groups
is also a subject of discussion: tetrahedral Al(IV), five-coordinate
Al(V),[18,25] and unsaturated Al(III) sites have all been
proposed.[17,18] All these structural propositions are based
on interpretation of complex spectral data. For instance, the assignments
of OH infrared stretching frequencies have been debated.[26−28] In particular, the vibrational properties of probes such as CO and
pyridine are not unambiguously specific to given ASA surface sites.[29,30] Additionally, the numerous preparation routes give rise to a broad
range of materials with varying structure, acidity, and active sites.[16] Even the surfaces that are formed using well-defined
methods are heterogeneous in nature.[16] More
recently, pseudo-bridging silanol groups have also been proposed to
be active sites based on DFT calculations.[19]An efficient synthesis of ASA materials involves the controlled
grafting of aluminum alkoxide or silicon alkoxide precursors onto
a silica or alumina surface under anhydrous conditions at low temperatures,
thus forming Al2O3 on SiO2 (Al/SiO2) and SiO2 on Al2O3 (Si/Al2O3), respectively.[16,31−33] This approach has the advantage of providing a homogeneous and regular
deposition. The anhydrous conditions prevent the prehydrolysis of
the precursor and inhomogeneous deposition. In addition, the amount
of precursor grafted on the surface is mainly directed by the size
of the alkyl chain of the precursor used. High Al and Si loadings
may be achieved through successive grafting steps for both Al/SiO2 and Si/Al2O3. The stoichiometric adsorption
and further dehydration of ethanol enabled the quantification of the
surface density of active sites.[33] Even
with a controlled deposition synthesis of ASA materials, Si/Al2O3 and Al/SiO2 still have multiple types
of Brønsted acid sites on their surface. Comparing these data
to the catalytic activity for m-xylene isomerization
revealed a moderate intrinsic acidity of these materials with respect
to zeolites, Si/Al2O3 being the more reactive.[33] Grafting of the silicon precursor occurred first
on the (100) surface. Brønsted acidity only appeared upon grafting
the (110) surface.[8,32−34]While
NMR spectroscopy is a valuable tool to obtain insights into
the nature of Al and Si species on ASA,[18,35−39] unambiguous identification of the most relevant surface sites has
not been achieved yet, one reason being the small amount of surface
sites combined with the low sensitivity of NMR. Dynamic nuclear polarization
surface enhanced spectroscopy (DNPSENS)[40−42] has recently
been introduced to characterize materials and in particular their
surfaces. In a DNPSENS experiment, the sample is impregnated with
a small volume of a solution containing a persistent radical that
acts as the DNP polarizing agent.[40−42] Impregnation brings
the solvent and DNP polarizing agent (usually a nitroxide biradical)[43] into contact with the surface. DNP at low temperatures[44,45] (ca. 100 K) is then used to enhance the polarization of protons
of the solvent and surface functionality.[43−45] The DNP enhanced
proton polarization is then transferred to the surface heteronuclei
by cross-polarization (CP)[46] or other coherence
transfer methods.[40−42,46−48] For inorganic materials, signals from NMR active nuclei residing
at the surface of the material are selectively enhanced since only
the surface nuclei are in proximity to the protons of the solvent
or surface functionalities. DNPSENS routinely provides sensitivity
enhancements of 2 orders of magnitude,[49,50] enabling NMR
experiments that would normally require isotopic labeling or prohibitively
long signal averaging periods.[40−42,48]Here, we apply DNPSENS for the detailed characterization
of ASA
materials prepared via controlled grafting approach, so as to provide
an unambiguous characterization of the interface between silica and
alumina for two well-defined series of samples: silica deposited on
alumina (Si/Al2O3) and alumina deposited on
silica (Al/SiO2) materials.[16] DNP NMR has recently been applied to characterize materials such
as alumina, silica, and β-zeolite surfaces.[51−57] Here DNPSENS allows sensitivity enhancements of several orders
of magnitude, thus enabling the acquisition of natural abundance 29Si–27Al scalar and dipolar heteronuclear
correlation spectra, providing structural insight into the alumina/silica
interface of these materials. Calculations of NMR signatures of surface
sites of Si/Al2O3 on a aluminosilicate model
by periodic density functional theory (DFT) calculations, which have
proven to be efficient for the assignment of NMR spectra of various
oxides,[58−66] allow us not only to propose a structure for the interface between
the alumina and the silica but also to propose structural models of
the Brønsted acid sites of ASA.
Experimental
and Computational Details
Samples were prepared by chemical
liquid deposition (CLD) and exhibit
different concentrations of SiO2 on Al2O3 (Si/Al2O3) and Al2O3 on SiO2 (Al/SiO2) (Table ).[32] Si/Al2O3 samples were prepared by contacting
excess tetraethyl-orthosilicate dissolved in dry toluene with alumina
(resulting from calcination at 540 °C of Pural SB3, Sasol) in
inert atmosphere (argon). After elimination of the unreacted precursor
molecules, the samples were dried at 100 °C and further calcined
at 500 °C under flow of air for 4 h. The 7.3 wt % of SiO2Si/Al2O3 sample was obtained after
one grafting step; 12.0 and 17.1 wt % of SiO2Si/Al2O3 samples were obtained after completion of two
and three grafting steps, respectively. In all cases, the final composition
was determined by X-ray fluorescence spectroscopy. A similar procedure
was applied for the preparation of the Al/SiO2 samples.
Aluminum isopropoxide dissolved in dry toluene was contacted with
silica in inert atmosphere (silica gel beads from Grace). The amount
of aluminum precursor was adapted to obtain either 5.7 wt % of Al2O3 or 15.0 wt % of Al2O3 after
one grafting step; 24.8 wt % Al/SiO2 was obtained after
a second grafting step.
Table 1
Properties of Synthesized
ASA Materials[16]
number of grafting
cycles
wt % of Al2O3 grafted
on SiO2 (Al/SiO2)
wt % of SiO2 grafted on Al2O3 (Si/Al2O3)
1
5.7
7.3
2
15.0
12.0
3
24.8
17.1
For DNPSENS[40,42] experiments, the nitroxide
biradical
polarizing agents bCTbK[47] or TEKPol were
used.[67] Incipient wetness impregnation
with 1,1,2,2-tetrachloroethane (TCE) biradical solution[42,68] with a concentration of 14–16 mM biradical was used to prepare
the samples for DNP experiments. The impregnated samples were packed
into sapphire rotors, and the sample was frozen at 100 K inside the
low temperature 3.2 mm MAS probe head. Samples were typically subjected
to multiple insert–eject cycles and left under an eject gas
flow prior to insertion in order to reduce the amount of oxygen in
the TCE solution and increase DNP enhancements.[69] Experiments were performed with a 400 MHz (9.4 T)/263 GHz
Bruker DNP system or a 600 MHz (14.1 T)/395 GHz Bruker DNP system.[70] The sweep coil of the main magnetic field was
set so that microwave irradiation occurred at the 1H positive
enhancement maximum of nitroxide biradicals. Standard ramped cross-polarization
(CP)[46] was then used to transfer polarization
from the 1H nuclei to the nucleus of interest (29Si or 27Al). For 1H–27Al
CP experiments, a low 27Al spin lock radiofrequency field
less than 20 kHz was employed in order to maximize the efficiency
of the CP transfers. Two-dimensional 29Si–27Al scalar correlation spectra were acquired with a refocused INEPT
pulse sequence (Figure S1). 29Si–27Al dipolar correlation spectra were acquired
with a dipolar refocused R3-INEPT pulse sequence[71] where first order rotary resonance recoupling
(R3)[72] was employed to recouple 29Si–27Al dipolar couplings. In all cases,
initial 29Si magnetization was generated with 1H–29Si CP with a 6 ms contact time. We also tested
a 29Si–27Al population transfer-HMQC
pulse sequences[73] (with detection of 29Si) to obtain scalar correlation spectra; however, the INEPT
type sequences (with 27Al detection) were found to provide
superior sensitivity. 1H–27Al and 1H–29Si HETCOR experiments were performed
with e-DUMBO1–22 homonuclear decoupling
applied during the t1 evolution period.[74] The States-TPPI procedure was applied to achieve
quadrature detection in the indirect dimension. The one-dimensional 27Al DNPSENSCPMAS spectra were fit to a Cjzek model implemented
in DMFit program in order to model the broad and featureless 27Al resonances characteristics of distributions of quadrupole
and chemical shift parameters.[75] The fits
enabled the determination of the relative ratio of each species, the
isotropic chemical shift (δiso), the Gaussian distribution
of the chemical shifts (Δδiso), and the quadrupolar
coupling constant.Density functional theory (DFT) calculations
were performed starting
from the periodic ASA model previously established,[19] according to a SiO2/Al2O3 type, for θOH = 5.4 nm–2 and
θSi = 6.5 nm–2. This model was
obtained by calculating the interaction of silicic compounds (silicic
acid and a silica film) on a γ-Al2O3 model
previously described by Digne et al.[76,77] Molecular
dynamics simulations revealed amorphization as well as mixing between
the silica and alumina phases, by extraction of some aluminum atoms
from the alumina layer to the silica one. The step-by-step simulation
of hydration led to models containing OH groups. Shielding tensor
computations were carried out with the CASTEP code,[78] using the generalized gradient approximation of Perdew,
Burke, and Ernzerhof (PBE)[79] and ultrasoft
pseudopotentials[80] (cutoff energy 550 eV).
A 1 × 1 × 2 k-points mesh was used. The
gauge including projector augmented wave (GIPAW) algorithm[81] was applied. Due to computer memory constraints,
the size of the systems modeled was reduced compared with the original
geometry, by removing the lowermost atoms from the cell and saturating
the resulting dangling bonds with water molecules to avoid unphysical
electrostatic effects (Figure S2). The
isotropic shielding (σiso), quadrupolar coupling
constants (CQ), and asymmetry parameters
(η) of 1H, 27Al, and 29Si were
calculated. Tetramethylsilane (for 1H and 29Si) and α-Al2O3 (for 27Al)
were used as references for chemical shift calculations.
Results and Discussion
Probing
the Structure of Aluminum on SiO2
The samples
with increasing loadings of aluminum (i.e., 5.7, 15,
and 24.8 wt % of Al2O3 on SiO2 noted
Al/SiO2) were analyzed with 1H–27Al cross-polarization magic angle spinning (CPMAS) solid-state NMR
spectroscopy. Indirect 1HDNP coupled with CPMAS enables
the selective enhancement of the NMR signals of the surface 27Al nuclei that are nearby to 1H nuclei of the surface
hydroxyl groups and solvent molecules.[51] Here a short contact time of 0.6 ms was employed in 1H–27Al CPMAS experiments since it is well-known
that with short contact times the CP experiment is very selective
and only nuclei in close proximity to protons will be excited. CP
transfers to more distant subsurface will also be less efficient due
to dipolar truncation, ensuring that only surface nuclei are detected.[55]1HDNP enhancements were measured
with CP to 27Al (εAl-CP) and were
between 5 and 8 for the different samples at 600 MHz/395 GHz (Figure A, spectra a–c).
Note that previous studies indicate that the overall sensitivity enhancement,
compared with a dry sample at room temperature, is usually similar
to the ε value under these conditions.[49] DNP enhanced 1H–27Al CPMAS spectra
were also acquired at 400 MHz/263 GHz, and higher (εAl-CP) signal enhancements between 51 and 80 were observed (Figure S3). The resolution of the 27Al solid-state NMR spectra is greatly improved at higher magnetic
field, as expected for quadrupolar nuclei such as 27Al.
Therefore, our analysis of 1D spectra focuses on the high field spectra.
Figure 1
(A) DNP
enhanced 1H–27Al CPMAS solid-state
NMR spectra acquired at 600 MHz/395 GHz: (a) 24.8 wt % Al/SiO2, (b) 15.0 wt % Al/SiO2, (c) 5.7 wt % Al/SiO2. Spectra for all of these samples were also measured on a
400 MHz DNP spectrometer (Figure S3, ESI). The recycle delay was 3.5 s. (B) DNP SENS (400 MHz/263 GHz) 1H–29Si CPMAS solid-state NMR spectra: (d)
24.8 wt % Al/SiO2, (e) 15.0 wt % Al/SiO2, (f)
5.7 wt % Al/SiO2. For 29Si measurement, DNP
enhancement was measured by directly observing the 1H spectrum,
since the acquisition of a 29Si CPMAS spectrum without
DNP required too long for signal averaging. All spectra were acquired
with a 12.5 kHz spinning frequency and a CP contact time of 0.6 ms
for 27Al and 3.0 ms for 29Si. 1H–29Si CPMAS spectrum of the starting silica is available Figure S7. (C) DNP SENS (400 MHz/263 GHz) scalar
refocused INEPT (black traces/contours) and dipolar refocused R3-INEPT (red traces/contours) 29Si–27Al heteronuclear correlation spectra: (g) 5.7 wt % Al/SiO2, (h) 15.0 wt % Al/SiO2, (i) 24.8 wt % Al/SiO2. All spectra were acquired with a 12.5 kHz MAS frequency. Projections
of the 2D spectra are shown along the horizontal and vertical axes.
For dipolar correlation experiments, 96 total rotor cycles (N, Figure S1) of recoupling were
used, while for scalar correlation experiments, 420 total rotor cycles
of evolution were used. Spectra were acquired with between 16 and
80 scans per increment, 28 t1 increments,
and a rotor synchronized t1 increment
of 80 μs. Recycle delays were optimized for sensitivity and
were between 3.8 and 5.0 s. The pulse sequences used to acquire the
2D spectra are illustrated in Figure S1.
(A) DNP
enhanced 1H–27Al CPMAS solid-state
NMR spectra acquired at 600 MHz/395 GHz: (a) 24.8 wt % Al/SiO2, (b) 15.0 wt % Al/SiO2, (c) 5.7 wt % Al/SiO2. Spectra for all of these samples were also measured on a
400 MHz DNP spectrometer (Figure S3, ESI). The recycle delay was 3.5 s. (B) DNPSENS (400 MHz/263 GHz) 1H–29SiCPMAS solid-state NMR spectra: (d)
24.8 wt % Al/SiO2, (e) 15.0 wt % Al/SiO2, (f)
5.7 wt % Al/SiO2. For 29Si measurement, DNP
enhancement was measured by directly observing the 1H spectrum,
since the acquisition of a 29SiCPMAS spectrum without
DNP required too long for signal averaging. All spectra were acquired
with a 12.5 kHz spinning frequency and a CP contact time of 0.6 ms
for 27Al and 3.0 ms for 29Si. 1H–29SiCPMAS spectrum of the starting silica is available Figure S7. (C) DNPSENS (400 MHz/263 GHz) scalar
refocused INEPT (black traces/contours) and dipolar refocused R3-INEPT (red traces/contours) 29Si–27Al heteronuclear correlation spectra: (g) 5.7 wt % Al/SiO2, (h) 15.0 wt % Al/SiO2, (i) 24.8 wt % Al/SiO2. All spectra were acquired with a 12.5 kHz MAS frequency. Projections
of the 2D spectra are shown along the horizontal and vertical axes.
For dipolar correlation experiments, 96 total rotor cycles (N, Figure S1) of recoupling were
used, while for scalar correlation experiments, 420 total rotor cycles
of evolution were used. Spectra were acquired with between 16 and
80 scans per increment, 28 t1 increments,
and a rotor synchronized t1 increment
of 80 μs. Recycle delays were optimized for sensitivity and
were between 3.8 and 5.0 s. The pulse sequences used to acquire the
2D spectra are illustrated in Figure S1.In all samples, three peaks centered
around 6, 33, and 60 ppm are
assigned, respectively, to hexa-coordinated Al(VI), penta-coordinated
Al(V), and tetra-coordinated Al(IV)aluminum sites, similarly to what
is observed for γ-alumina, albeit with a larger component of
Al(V),[51,66,82−84] in agreement with previous NMR measurements.[18,35,37,38] The shape
of the peaks in the spectra evolves as the concentration of alumina
on SiO2 changes. We also note that as the Al loading increases,
the intensity of the 27Al CPMAS spectra also substantially
increases (Figure S3). The one-dimensional 27Al DNPSENSCPMAS spectra were fit to a Cjzek model implemented
in DMFit program to model the broad and featureless 27Al
resonances characteristics of distributions of quadrupole and chemical
shift parameters (Figure S4).[75] The fits enabled the determination of the relative
ratio of each species, the isotropic chemical shift, and the quadupolar
constant (Table S1 and Figure S5). The
fits show that for Al/SiO2 the relative amount of Al(V)
(2%, 11%, and 17%) increases with higher aluminum loading.For
Al/SiO2, all of the 1D DNP enhanced 29SiCPMAS
NMR spectra show a major peak centered at around −100
ppm and a reduced intensity “tail” at around −85
ppm (Figure B, spectra
d–f). The major peak at −100 ppm indicates that most
silicon atoms are present as Q4 sites.
As the aluminum loading increases the intensity of the tail increases
and moves toward more positive chemical shift. Silicon with multiple
neighboring aluminum atoms or protons bound to the coordinating oxygen
atoms should exhibit more positive chemical shifts (see next section, regarding Si/Al2O3 samples).[4,85,86] It is indeed well-known from experiments on crystalline materials
that substitution of aluminum atoms into neighboring tetrahedral sites
around tetrahedral silica induces a positive displacement of the 29Si chemical shift.[85−89] From solid-state NMR experiments performed on amorphous silica,
it is also known that Si atoms with protons bound to coordinating
oxygen atoms are also displaced to higher 29Si chemical
shifts.[4,85,86,90] Finally, we note that 1D 29SiCPMAS experiments
and 2D 29Si–27Al INEPT-HETCOR experiments
used 3 and 6 ms contact times, respectively, since these relatively
long contact times gave the most signal. However, 29SiCPMAS spectra of 17.1% Si/Al2O3 acquired with
contact times of 1–6 ms showed only minor variation in the
observed 29Si chemical shifts with contact time (Figure S6). This suggests that even at relatively
long contact times only the surface of the material is probed.In addition, with increasing Al-loading, the relative number of
Al(IV) sites decreases. We suspect that at high loading, the conversion
of Al(IV) species into Al(V) is due to the increased ionicity of the
framework, leading to preferred higher coordination number. Indeed,
intrinsically, the Al–O bond is more ionic than the Si–O
bond as expected from the respective electronegativity values of Al,
Si, and O and the definition of ionicity given by Pauling.[91−93] Simultaneously, the ratio of six-coordinate Al sites remains at
around 60% of the total aluminum atoms.To obtain direct insight
into the bonding between Al and SiO2, DNPSENS29Si–27Al INEPT was
used to obtain two-dimensional 29Si and 27Al
heteronuclear correlation (HETCOR) spectra of Al/SiO2 (Figure C, spectra g–i).
We note that the 29Si–27Al correlation
experiments are very challenging due to the low natural isotopic abundance
of 29Si (natural abundance of 4.7%) and inefficient polarization
transfer to or from quadrupolar 27Al nuclei. Therefore,
2D 29Si–27Al correlation experiments
were performed at 400 MHz/263 GHz where substantially higher DNP enhancements
and NMR sensitivity were obtained. The HETCOR spectra were obtained
with 29Si–27Al scalar couplings to selectively
observe scalar coupled aluminum and silicon atoms linked by bridging
oxygen (black traces). HETCOR spectra were also obtained with 29Si–27Al dipolar couplings by applying dipolar
recoupling during the evolution period to observe both bonded and
nonbonded but proximate aluminum and silicon atoms (red contours/traces).
The scalar HETCOR spectra (black contours/traces) indicate that in
all cases the silica tetrahedra are primarily bound to aluminum tetrahedra
in Al/SiO2 (fits of the projected 27Al dimension
for both scalar and dipolar spectrum are provided in the SI, see Figures S8 and S9 and Tables S2 and S3). The
dipolar 29Si–27Al correlation spectra
(Figure C, spectra
g–i, red traces) show correlations between 29Si Q4 sites with 27Al(IV) and additional
weak correlations between silicon and octahedral aluminum Al(VI) in
all cases (Figure S9 and Table S3). This
result is consistent with earlier NMR analysis on cogelled ASA samples
with high silica content.[36] The relative
intensity of the latter correlations increases as the aluminum loading
level is increased. As the dipolar correlation experiment gives correlations
through space, the observed correlations to the octahedral Al-sites
are very weak and likely arise from coupling to proximate nonbonded
Al-octahedra. Note that at this stage, the correlation with Al(V)
nuclei cannot be excluded but does not appear on the correlation plots
probably due to low sensitivity of 29Si–27Al correlation experiments and the reduced resolution of the 27Al spectra at 9.4 T. We note that DNP enhanced 1H–27Al and 1H–29Si
dipolar HETCOR spectra were also acquired (Figure S10 and S11). However, both the 1H–29Si and 1H–27Al HETCOR spectra generally
show correlations to a very broad range of 1H chemical
shifts (ca. 0.5 to 10 ppm), which likely reflects the diverse range
of proton environments at the surface (hydroxyl, water, adsorbed solvent
molecules, acidic protons, etc.). The most intense 1H peaks
in the HETCOR spectra are centered around 4.5–5 ppm and ca.
6.2 ppm. These 1H chemical shifts likely correspond to
adsorbed H2O and TCE solvent molecules, respectively. The 1H peaks in the HETCOR spectra are also rather featureless,
which prevents useful structural information from being obtained.In summary, the scalar and dipolar DNPSENS29Si–27Al HETCOR spectra indicate that the majority of aluminum
species that are bound to the silica surface via Si Q4 sites are Al(IV) and as the loading increases the number
of Al(VI) proximate to the silica surface increases (Scheme ).
Scheme 1
Representation of the Al/SiO2 Interface Depicting Direct
Bonding between Tetrahedral Aluminum and Silicon Sites and the Proximity
of Octahedral Aluminum Sites
X = Al, Si, or H. Homocondensation
of the alkoxides is possible leading to the formation Al–O–Al-type
species.
Representation of the Al/SiO2 Interface Depicting Direct
Bonding between Tetrahedral Aluminum and Silicon Sites and the Proximity
of Octahedral Aluminum Sites
X = Al, Si, or H. Homocondensation
of the alkoxides is possible leading to the formation Al–O–Al-type
species.
Probing the Structure of Silicon on Al2O3
Si/Al2O3 prepared
by the deposition
of SiO2 on Al2O3 via a molecular
approach was also investigated by DNPSENS. 1H–27Al CPMAS spectra were recorded for the Si/Al2O3 samples (Figure A, spectra a–c). Higher DNP enhancements of 7–20
were obtained for Si/Al2O3 compared with enhancements
of 5–8 observed for Al/SiO2 at 600 MHz/395 GHz.
The larger enhancements observed for Si/Al2O3 samples (51–80 at 400 MHz/263 GHz) compared with Al/SiO2 (εAl-CP of 114–153 at 400
MHz/263 GHz) could reflect more suitable dielectric properties of
alumina.[69] However, other factors such
as the degree of oxygen removal[69] or interaction
or aggregation of the radicals could also impact the observed DNP
enhancements. Once again, three distinct resonances centered around
9, 36, and 65 ppm were observed in the 1H–27Al CPMAS spectra and are assigned to Al(VI), Al(V), and Al(IV)aluminum
atoms in agreement with DFT calculations (Table S4). Given the sensitivity of the 27Al NMR chemical
shifts and quadrupole parameters to hydration and the challenge of
accurately modeling water coordination/hydration of the surface, we
did not consider the calculated 27Al NMR spectra.[66]
Figure 2
(A) DNP enhanced 1H–27Al
CPMAS solid-state
NMR spectra acquired at 600 MHz/395 GHz: (a) 17.1 wt % Si/Al2O3, (b) 12 wt % Si/Al2O3, and (c)
7.3 wt % Si/Al2O3. Spectra for all of these
samples were also measured on a 400 MHz DNP spectrometer (Figure S3, ESI). (B) DNP SENS (400 MHz/263 GHz) 1H–29Si CPMAS solid-state NMR spectra: (d)
17.1 wt % Si/Al2O3, (e) 12 wt % Si/Al2O3, and (f) 7.3 wt % Si/Al2O3. For 29Si measurement, DNP enhancement was measured by directly
observing the 1H spectrum, since the acquisition of a 29Si CPMAS spectrum without DNP required too long for signal
averaging. (g) DFT calculated spectrum for all 29Si nuclei,
independently of their proximity to 1H. The model corresponds
to a 14% Si/Al2O3. All spectra were acquired
with a 12.5 kHz spinning frequency and a CP contact time of 0.6 ms
for 27Al and 3.0 ms for 29Si. 1H–27Al CPMAS of the starting alumina is available, Figure S12. (C) DNP SENS (400 MHz/263 GHz) scalar
refocused INEPT (black traces/contours) and dipolar refocused R3-INEPT (red traces/contours) 29Si–27Al heteronuclear correlation spectra of (h) 17.1 wt % Si/Al2O3, (i) 12 wt % Si/Al2O3, and (j)
7.3 wt % Si/Al2O3. All spectra were acquired
with a 12.5 kHz MAS frequency. Projections of the 2D spectra are shown
along the horizontal and vertical axes. For dipolar correlation experiments,
96 total rotor cycles (N, Figure S1) of recoupling were used, while for scalar correlation experiments,
420 total rotor cycles of evolution were used. Spectra were acquired
with 16–80 scans per increment, 28 t1 increments, and a rotor synchronized t1 increment of 80 μs. Recycle delays were optimized for sensitivity
and were between 3.8 and 5.0 s. The pulse sequences used to acquire
the 2D spectra are illustrated in Figure S1.
(A) DNP enhanced 1H–27Al
CPMAS solid-state
NMR spectra acquired at 600 MHz/395 GHz: (a) 17.1 wt % Si/Al2O3, (b) 12 wt % Si/Al2O3, and (c)
7.3 wt % Si/Al2O3. Spectra for all of these
samples were also measured on a 400 MHz DNP spectrometer (Figure S3, ESI). (B) DNPSENS (400 MHz/263 GHz) 1H–29SiCPMAS solid-state NMR spectra: (d)
17.1 wt % Si/Al2O3, (e) 12 wt % Si/Al2O3, and (f) 7.3 wt % Si/Al2O3. For 29Si measurement, DNP enhancement was measured by directly
observing the 1H spectrum, since the acquisition of a 29SiCPMAS spectrum without DNP required too long for signal
averaging. (g) DFT calculated spectrum for all 29Si nuclei,
independently of their proximity to 1H. The model corresponds
to a 14% Si/Al2O3. All spectra were acquired
with a 12.5 kHz spinning frequency and a CP contact time of 0.6 ms
for 27Al and 3.0 ms for 29Si. 1H–27Al CPMAS of the starting alumina is available, Figure S12. (C) DNPSENS (400 MHz/263 GHz) scalar
refocused INEPT (black traces/contours) and dipolar refocused R3-INEPT (red traces/contours) 29Si–27Al heteronuclear correlation spectra of (h) 17.1 wt % Si/Al2O3, (i) 12 wt % Si/Al2O3, and (j)
7.3 wt % Si/Al2O3. All spectra were acquired
with a 12.5 kHz MAS frequency. Projections of the 2D spectra are shown
along the horizontal and vertical axes. For dipolar correlation experiments,
96 total rotor cycles (N, Figure S1) of recoupling were used, while for scalar correlation experiments,
420 total rotor cycles of evolution were used. Spectra were acquired
with 16–80 scans per increment, 28 t1 increments, and a rotor synchronized t1 increment of 80 μs. Recycle delays were optimized for sensitivity
and were between 3.8 and 5.0 s. The pulse sequences used to acquire
the 2D spectra are illustrated in Figure S1.Fits of the 27Al CPMAS
spectra show that the relative
ratio of the Al(VI)/Al(V)/Al(IV) sites is approximately 75:5:20 for
all silica loading levels. There is not a strong variation in the
relative intensities of the different aluminum sites with increasing
SiO2 loading level (Figure S13 and Table S5). However, as the loading of SiO2 is increased
and the alumina surface becomes covered, the absolute intensity of
the 27Al CPMAS spectra is observed to decrease (Figure S3). In addition, we may also expect a
different intrinsic behavior of Al/SiO2 and Si/Al2O3 interfaces. In Si/Al2O3, we expect
that Al(V) sites result from the reconstruction–amorphization
process as reported in ref (19); the rigid alumina framework imposes structural constraints
and likely limits the formation of a large number of Al(V) even at
high silica content. In contrast for Al/SiO2, monomeric
aluminum species deposited on the silica surface are intrinsically
more flexible, thus allowing the formation of Al(V) from Al(IV) species
(vide supra).Once again, high-quality 1H–29SiCPMAS
spectra could be rapidly acquired (ca. 5 min for a one-dimensional
spectrum). The DNP enhanced 1H–29SiCPMAS
spectra of Si/Al2O3 are shown for three different
silicon loadings of 7.3, 12.0, and 17.1 wt % (Figure B, spectra d–f). The 29SiDNPSENSCPMAS spectra of Si/Al2O3 can be
decomposed into three components at −83, −93, and −100
ppm (Figure S14 and S15).The calculated 29Si chemical shifts of the various surface
sites are distributed between −78 and −99 ppm, consistent
with the experimental observations. Applying Gaussian broadening to
this distribution leads to the simulated spectrum reported in Figure B, trace g. The position
of the maximum is enclosed between those of the experimental spectra
of the 12% and 17.1% Si/Al2O3 sample. The DFT
model is representative of a perfectly dispersed silica overlayer,
without multilayers, which may explain the slightly different shape
of the simulated spectrum compared with the experiment; the DFT simulated
spectrum is slightly more intense at negative chemical shifts and
less intense at the more positive chemical shift tail (Figure S16). Reducing the broadening for the
simulated spectrum leads to a three-component spectrum (Figure S17), centered at around −80, −92,
and −97 ppm. Excluding the Si atoms that do not have any hydrogen
as second neighbors from the simulation does not affect the shape
of the spectrum. All surface Si are likely observed since the contact
time used for the 1H–29SiCPMAS experiment
is long (3 ms).On the basis of DFT calculations, we can propose
an assignment
of the spectra of the Si/Al2O3 samples. Note
however that the presence of various environments around similar 29Si (Figure ), for example, various Si–O–Si and Si–O–Al
angles and bond lengths, coordination numbers of Al atoms, presence
of additional Al atoms noncovalently bonded but in close proximity
to Si–O, will lead to a distribution of chemical shifts, only
modeled in part here. In agreement with previous empirical assignments,
based on the analysis of crystalline and amorphous aluminosilicates,[85−89] both H and Al second neighbors are at the origin of the increase
of the chemical shift of 29Si nucleus (Figure ): the Z2 site, corresponding to −78 ppm chemical shift, is
surrounded by the highest number of Al neighbors (n = 4) together with a proton.[85−88] Considering that all oxygen atoms surrounding a Si
atom are 2-fold coordinated (as in silica), an empirical assignment
(Figure S18) and model (Figure ) can be drawn for each Si
atom in silicates based on the number of H (i) and
Al (n) neighbors, where the chemical shift of a specific
Si site is positively shifted by (10i + 5n) ppm from the chemical shift of pure SiO2 (Q4 sites, δiso = −110
ppm) as a reference (see eq ).[85−88]
Figure 3
On the top,
top view of the Si/Al2O3 DFT
model employed with θOH = 5.4 nm–2, constructed from the silication of the (100) γ-Al2O3 surface. The terminology for Si and outermost surface
Al atoms is given in black and blue, respectively. See Figure S2 and Table S4 (ESI) for more details
on local environments and side views. On the bottom, schematic representation
of each Si site with the DFT-computed 29Si chemical shifts
in parentheses and the number and the nature of second neighbors for
each Si atom on the ASA model employed. The environment of Si is noted
Si(nAl, iH, pSi), by extension of the terminology from previous work;[89]n + i + p can be larger than four because of the significant ionicity
of the framework (some oxygen are more than 2-fold coordinated). According
to the decomposition, DFT calculated peaks were lumped into three
subgroups centered around the experimental peaks: δ < −96
ppm; −96 ppm ≤ δ ≤ −88 ppm; −88
ppm < δ.
Figure 4
Comparison of 29Si chemical shifts calculated by DFT
and an empirical model (see Figure S18),
derived from the analysis of the literature data available, assuming
2-fold coordination for all O atoms, and constant chemical shift variation
by +10 ppm for each 1H and +5 ppm for each Al second neighbor.[85−89] The experimental 29Si chemical shifts of our Si/Al2O3 samples are represented with the dotted vertical
lines. The plain line depicts the diagonal of the parity plot.
On the top,
top view of the Si/Al2O3 DFT
model employed with θOH = 5.4 nm–2, constructed from the silication of the (100) γ-Al2O3 surface. The terminology for Si and outermost surface
Al atoms is given in black and blue, respectively. See Figure S2 and Table S4 (ESI) for more details
on local environments and side views. On the bottom, schematic representation
of each Si site with the DFT-computed 29Si chemical shifts
in parentheses and the number and the nature of second neighbors for
each Si atom on the ASA model employed. The environment of Si is noted
Si(nAl, iH, pSi), by extension of the terminology from previous work;[89]n + i + p can be larger than four because of the significant ionicity
of the framework (some oxygen are more than 2-fold coordinated). According
to the decomposition, DFT calculated peaks were lumped into three
subgroups centered around the experimental peaks: δ < −96
ppm; −96 ppm ≤ δ ≤ −88 ppm; −88
ppm < δ.Comparison of 29Si chemical shifts calculated by DFT
and an empirical model (see Figure S18),
derived from the analysis of the literature data available, assuming
2-fold coordination for all O atoms, and constant chemical shift variation
by +10 ppm for each 1H and +5 ppm for each Al second neighbor.[85−89] The experimental 29Si chemical shifts of our Si/Al2O3 samples are represented with the dotted vertical
lines. The plain line depicts the diagonal of the parity plot.However, in the presence of alumina,
a more ionic support than
silica, oxygen atoms can adopt higher than 2-fold coordination. In
alumina, the coordination number of oxygen atoms can be as high as
four, so that higher coordination may be expected at the Si/Al interface.
If we denote the environment of a given Si as Si(nAl, iH, pSi) to note the number
of its second neighbors, DFT calculations show that n + i + p can exceed four. This
can be related to the so-called “O tricluster” suspected
for aluminosilicate glasses.[4,65,94−96] We can extend this concept to an “O tetracluster”
on our silicate alumina surface model. This leads to a deviation (below
10 ppm) of the empirical model chemical shifts (Figure ) since the 29Si chemical shift
cannot be simply related to the nature and number of second neighbors.To assign the experimental 29SiCPMAS NMR spectra, we
compared the DFT calculated chemical shifts to the three experimental
chemical shifts obtained from deconvolution of the 29SiCPMAS spectrum of 17.1% Si/Al2O3 (Figure ). The −93 and −100
ppm peaks are clearly related to a higher number of Si atoms as second
neighbors than the −83 ppm peak. The −83 and −93
ppm peaks correspond generally, but not necessarily, to a high number
of Al as second neighbors (for example, X2), since several
H as second neighbors can also lead to increase in chemical shifts.[88] Experimental evaluation of the peak intensities
shows that at high silicon loading, Si species giving a signal around
−93 ppm (and to a lower extent, −100 ppm) become dominant,
whereas the −83 ppm signal vanishes, consistent with the existence
of more numerous Si as second neighbors. This can be related to the
formation of a SiO2 multilayer and a pure silica network
(Figure S14). At low loading, the −83
ppm peak increases dramatically, consistent with the first layer of
silicate bonding directly to the surface of Al2O3.Scalar two-dimensional 29Si–27Al DNPSENS INEPT HETCOR spectra of Si/Al2O3 (Figure C, spectra h–j)
show that the silica tetrahedra are primarily bonded to the aluminum
tetrahedra (decompositions of the projection of the 27Al
dimension for both scalar and dipolar HETCOR spectra are given in Figures S8 and S9 and Tables S2 and S3). However,
in the scalar HETCOR spectra, weak correlations to octahedral aluminum
sites are observed, and the relative intensities of these correlations
are constant (within the uncertainty of the measurement) with increasing
loading of Si on alumina (Figure S8 and Table S2). This is consistent with the high intensity of the octahedral
aluminum sites observed in the 1D 27Al CPMAS spectra of
Si/Al2O3. The dipolar 29Si–27Al HETCOR spectra of Si/Al2O3 show
more intense correlations to octahedral aluminum sites and penta-coordinate
aluminum, in particular for the lowest Si loading. The relative intensity
of the correlations to the octahedral and penta-coordinate aluminum
sites is also increased in Si/Al2O3 compared
with the corresponding HETCOR spectra of Al/SiO2 due to
the presence of 6- and 5-fold coordination of aluminum sites on the
alumina surface and therefore the close proximity with the 29Si nuclei (Figure S9 and Table S3). To
explain this, we analyzed the Si to Al proximity in our DFT model
(Figure S19). From this, we expect correlations
with all types of Al atoms (IV, V, VI), but clearly the environment
of Si is richer in Al(IV) than a priori expected
from the structure of the alumina surface (on the (100) alumina orientation
used for the simulation, no Al(IV) are exposed at the surface).[76,77] This can be interpreted as an Al(VI) to Al(IV) and Al(V) to Al(IV)
conversion induced by silica. This conversion is likely driven by
the higher degree of covalence of silica compared with alumina, which
favors lower coordination numbers. This is in line with the higher
Al(IV)/Al(VI) ratio observed as silica content increases in ASA, which
was known from classical 27Al NMR.[18,37,38] Note that the Al(IV) giving signal in the 29Si–27Al HETCOR spectra (Figures C and 2C) appears at slightly lower isotropic chemical shifts (62–66
ppm, Figure S9 and Table S3) than in the
1D DNP enhanced 27Al CPMAS NMR spectra (66–73 ppm, Figure S13 and Table S5). This can be related
to the DFT results, which show that the isotropic chemical shift of
Al(IV) is reduced when silicon is present as second neighbor (Figure ). This is qualitatively
comparable to observations from calculations on aluminosilicate glasses,
even if the strength of the effect is different.[90] Note also that the 29Si nuclei detected in 29Si–27Al HETCOR appear at more positive
chemical shifts than those in the 1D 29SiCPMAS NMR spectrum.
This is because Si sites that neighbor Al will give rise to more positive 29Si chemical shifts than Si near to only Si.
Figure 5
DFT calculated dependence
on Al(IV) isotropic chemical shift as
a function of the number of Si as second neighbors of Al. γ-Al2O3 serves as reference with no Si as second neighbors.
In AlIV–(OSi), IV refers
tetracoordinate aluminum and x to the number of (OSi)
bound to Al.
DFT calculated dependence
on Al(IV) isotropic chemical shift as
a function of the number of Si as second neighbors of Al. γ-Al2O3 serves as reference with no Si as second neighbors.
In AlIV–(OSi), IV refers
tetracoordinate aluminum and x to the number of (OSi)
bound to Al.In summary, the 1D 27Al and 29Si and 2D 29Si–27Al correlation spectra suggest that
grafting of silica onto alumina primarily results in the formation
of bonds between SiO4 tetrahedra and tetrahedral Al(IV)
sites; however, some SiO4 tetrahedra are bonded to octahedral
Al sites. Since SiO2 is deposited onto Al2O3, most Si atoms will be proximate to the aluminum surface
resulting in more intense correlations between Si and octahedral and
penta-coordinated aluminum atoms. The observation of more negative 29Si chemical shifts with increasing Si loading level is also
consistent with formation of a SiO2 multilayer at higher
loading level.Taken together, the variation in the intensities
of the DNPSENS
1D and 2D NMR with the loading levels can be used to propose some
simple structural models (Scheme ). On Si/Al2O3, the population
of Al(VI) is more abundant than on Al/SiO2 (from 27Al DNPSENS). Many Si nuclei are bonded to OH groups and are connected
to Al(IV) as second neighbors, being also quite close to Al(VI) and
Al(V) species. This strong connection to Al(IV) atoms is linked to
the locally strong covalence of ASA compared with alumina. As the
silica loading increases, there is an overall increase in the intensity
of signal with more negative chemical shifts. This suggests that increasing
loading of SiO2 results in the formation of a SiO2 multilayer, likely a pure silica network. On the other hand, when
Al is grafted onto silica in Al/SiO2, the relative intensity
of the tetrahedral sites is higher, due to the high covalence of the
host matrix (silica). However, as the Al-loading increases, an Al2O3 overlayer begins to form and relative ratio
of tetrahedral to six-coordinate sites decreases to converge toward
that of pure γ-alumina (3/1). Interestingly, the relative amount
of penta-coordinated aluminum sites at the surface increases with
the grafting of alumina, suggesting that more defected alumina surface
sites may result as the loading level is increased, thereby confirming
previous propositions.[32]
Scheme 2
Representation of
the Si/Al2O3 Interface Depicting
Direct Bonding between Tetrahedral Aluminum Silicon Sites and Close
Proximity of Octahedral Aluminum Sites
X = Al, Si, or H. Homocondensation
of the alkoxides is possible leading to the formation Si–O–Si-type
species.
Representation of
the Si/Al2O3 Interface Depicting
Direct Bonding between Tetrahedral Aluminum Silicon Sites and Close
Proximity of Octahedral Aluminum Sites
X = Al, Si, or H. Homocondensation
of the alkoxides is possible leading to the formation Si–O–Si-type
species.
Relation to Brønsted acidity
The present NMR data,
in particular the correlation experiments, yield new insight into
the atomistic structure of the Brønsted acid sites of ASA materials. Table quantifies the Brønsted
acid sites.[16,31−33] On Al/SiO2 samples, the occurrence of Si(IV)–Al(IV) connectivity
as the aluminum loading increases is associated with a higher concentration
of acid sites per Al atom on these samples.[33] Previous measurements of the concentration of Brønsted acid
sites have shown that there are more Brønsted acid sites per
deposited aluminum at low Al loading levels. The DNPSENS 27Al CPMAS spectra also show that there is an increase in the relative
amount of Al(IV) sites at low loading levels. Taken together, these
two results strongly suggest that the formation of Brønsted acid
sites is related to the presence of Al(IV) on the Al/SiO2 surface. This finding substantiates previous observations.[97] Silicon connected to aluminum with higher coordination
number would be inefficient in forming Brønsted acid sites.
Table 2
Coverage by Aluminum Species and Surface
Density of Brønsted Acid Sites[31,33]
sample
Brønsted acid sites (nm–2)
Brønsted acid sites per Al atom (× 10–2, Al exposed–1)
5.7% Al2O3/SiO2
0.20
15.4
15% Al2O3/SiO2
0.39
6.7
24.8% Al2O3/SiO2
0.52
7.3
7.3% SiO2/Al2O3
0.04
0.5
12% SiO2/Al2O3
0.11
1.5
17.1% SiO2/Al2O3
0.19
5.2
The
results on Al/SiO2 materials show that the low coordination
of the aluminum atoms and the presence of silica as a matrix are both
crucial parameters for obtaining Brønsted acid sites in ASAs.
Gathering such conditions by grafting silicon species on the Al2O3 surface is more difficult for two main reasons.
On the one hand, the coordination of the aluminum atoms populating
the Al2O3 surface is on average closer to six
than to four, higher than that of the first aluminum species deposited
in Al/SiO2 samples. On the other hand, a significant amount
of deposited silicon species is required so as to change the covalence
of the surface aluminum species in such a way that it induces the
formation of reactive sites. Hence the number of Brønsted acid
sites per exposed aluminum atom in Si/Al2O3 samples
increases with the silica loading and consequent coverage of aluminum
surface species.Hensen et al.[20] categorized
the acid
sites of ASAs in two main types, the strongest ones being bridging
acid sites such as in zeolites and the milder ones being specific
to ASAs with different structures. Experimental and computational
data combined suggest that the structures of the acid sites of ASAs
are bridging hydroxyl between Si(IV) and Al(IV), possibly associated
with pseudo-bridging silanols (PBS) for Si/Al2O3 materials (Scheme ).[19,29,93,98] Such sites are defined as silanols being noncovalently
bonded to aluminum atoms (electrostatic interaction between aluminum
atoms and oxygen of the silanol, shown as dashed line in Scheme ). According to calculations,
such species can be protonated by basic probe molecules (B) such as
lutidine, by closing the Si–O···Al bridge, yielding
Si–O–Al anionic species and BH+, in agreement
with ref (17).[30,93] Moreover, the intrinsic protonation and cracking abilities of such
PBS sites have recently been compared with bridging acid sites of
a zeolite in DFT calculations, and these specific structures would
account for the milder acidity of PBS and corroborate the main role
of the interaction between the alumina support and deposited silicon
species.[98] In the present work, on the
basis of the NMR spectra, we suggest that the acceptor Al atom is
likely in tetrahedral coordination and that the silicon bearing the
silanol is covalently bonded to other Al(IV) ions (Scheme ). However, all PBS sites are
covalently connected to only Al(VI) and Al(V) in the DFT model discussed
here, due to the high aluminum content. While it is hard to make an
unambiguous prediction of the 29Si NMR chemical shift for
sites depicted in Scheme , the two PBS sites, V1 and Z2 in Figure , can be considered
as prototypical examples: they are characterized by very distinct
calculated chemical shifts of −96 and −78 ppm, respectively.
This large difference of calculated chemical shifts for similar species
shows that 1D NMR cannot be used to identify the Brønsted acid
sites of ASA. In contrast, NMR correlation experiments, which probe
Al(IV) to Si(IV) proximity, a requirement for Brønsted acidity,
are therefore better suited to characterize such species.
Scheme 3
Proposal
for a Possible Structure of Brønsted Acid Sites on
ASA (Si/Al2O3): Pseudo-Bridging Silanol in Connection
with Al(IV) Species
Conclusions
Combining DNPSENS NMR, including 2D scalar
and dipolar 29Si–27Al INEPT, and DFT
calculations on ASA materials
has allowed for a detailed atomic level description of (i) the connectivity
between Si and Al nuclei on ASA surfaces, as a function of their coordination
number and local environment, and (ii) structural insight into the
nature of Brønsted acid sites, which unifies the behavior of
solids obtained by grafting either Al on silica or Si on alumina.On silica and alumina surfaces, molecular Si and Al precursors
are preferentially grafted as “(IV)-to-(IV)”-coordinated
mixed layer: the deposited silicon species are preferentially attached
to Al(IV) sites issued from Al atoms of various coordinations of γ-alumina,
with strong Si(IV)–Al(IV) connectivity. Similarly, the first
deposited aluminum species on silica in Al/SiO2 are Al(IV)
tetrahedrally coordinated species. This specific surface site connectivity
eventually enables the formation of Brønsted acid sites. Such
acid sites may be formulated as bridging hydroxyls in connection with
Al(IV) species, such as pseudo-bridging silanol in Al/SiO2. While an atomic level description of the interface of ASAs remains
complex because each preparation technique makes a unique structure,
the present study lays the foundation for the determination of the
structure of the Brønsted active sites in the large family of
aluminosilicates with the ultimate goal to establish structure–activity
relationships and to use more rational development of solid acid catalysts.
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