DFT study of the adsorption of microsolvated glycine on a hydrophilic amorphous silica surfacew Dominique Costa,* ab Asma Tougerti, a Frederik Tielens, a Christel Gervais, c Lorenzo Stievano a and Jean Franc¸ois Lambert a Received 16th April 2008, Accepted 25th July 2008 First published as an Advance Article on the web 23rd September 2008 DOI: 10.1039/b806501b Density functional theory (DFT) periodic ab initio molecular dynamics calculations are used to study the adsorption of gaseous and microsolvated glycine on a hydroxylated, hydrophilic silica surface. The silica model is presented and the interaction of water with surface silanols is studied. The heat of interaction of water is higher with the associated silanols (be they terminal or geminal ones) studied here than with isolated silanols presented in past works. Glycine is stabilized in a parallel mode on the hydroxylated surface. Terminal silanols do not allow the stabilization of the zwitterionic form, whereas geminal silanols do. Molecular dynamics (MD) first-principle calculations show that microsolvated zwitterion glycine directly binds through the carboxylate function to a surface silanol rather than through water molecules. The adsorption mode, whether with or without additional water molecules, is parallel to the surface. The ammonium function does not interact directly with the silanol groups but rather through water molecules. Thus, the carboxylate and ammonium functions exhibit two different reactivities towards silanols. The calculated free energies, taking into account the chemical potentials of water and glycine in the gas phase, suggest the existence of a thermodynamic domain in which the glycine is present in the gas phase as well as strongly adsorbed on specific sites of the surface. Introduction Mineral surfaces have been suggested, already in the late 1950s, to play a role in the activation of amino acids polymerization that lead to the formation of peptides in early prebiotic chemistry. 1 In particular, clays and other oxides were present in large amounts on the prebiotic earth crust after the formation of hydrosphere, and may have played an important role in the process of chemical evolution (ref. 2 and references therein). The earth crust consists primarily of silicate minerals, containing a number of metal cations (e.g.aluminium, magnesium, calcium, iron etc.) mainly structured in frame- works of (SiO 4 ) tetrahedra connected by siloxane bonds. In spite of relevant differences with natural silicates, the study of the adsorption and reactivity of amino acids on a pure silica system can be considered as a ‘‘model’’ system for studying the role that such surfaces may have played in the activation of peptide bond formation. 3 For oxides such as silica, alumina or iron oxides, molecular- level studies remain scarce, even though it would be desirable to know, not only if such surfaces can exhibit significant selectivities (maybe even molecular recognition phenomena) for different biomolecules going from amino acids to proteins, but also whether the structure of the adsorption site may influence the reactivity of adsorbed biomolecules. Recently, theoretical ab initio tools have been successfully used to investigate the mode of interaction of small biofunctions with oxide and sulfide surfaces, in particular the adsorption of: glycine on a dry (110) rutile surface, 4 cysteine and serine on a dry (110) and a hydroxylated (100) rutile surface, 5 glycine on pyrite, 6 on alumina 7 and on crystalline silica. 8,9 We have undertaken a joint experimental and theoretical study of the adsorption of glycine on amorphous silica surfaces from the point of view of the surface, using knowledge pre- viously gained on the molecular identification of surface func- tional groups (such as silanols, silanolates, ‘‘nests’’ of silanols...) to better characterize their interaction with amino acids, both from the aqueous 10 and from the vapor phase. 11 We showed that glycine from the aqueous phase binds with specific surface sites at a coverage of 0.8 glycine nm 2 (10% of the physical monolayer). In the theoretical part of our work, we presented B3LYP results, obtained with minimal clusters of glycine interacting with a silica surface, with and without ref. 11–13 the presence of water molecules. It was found that glycine from the gas phase may form H-bond rings with silanols, and that additional water molecules are needed to stabilize zwitter- ionic glycine on the surface ref. 11 and 12. We focused our attention on comparing calculated and experimental vibration frequencies, namely the n COO and d HNH modes. A precise characterization of the glycine adsorption site was difficult, principally due to the overlapping of frequencies with d HOH of residual water, and also to the coupling of those frequencies a Laboratoire de Re ´activite´ de Surface, Universite´ Pierre et Marie Curie—Paris 6, 4, Place Jussieu, F-75252 ParisCedex 05 France b Laboratoire de Physico-Chimie des Surfaces, ENSCP, 11 rue P. et M. Curie, 75005 Paris, France. E-mail: [email protected]c Laboratoire de Chimie de la Matie `re Condense ´e, Universite´ Pierre et Marie Curie—Paris 6, 4, Place Jussieu, F-75252 ParisCedex 05 France w Electronic supplementary information (ESI) available: Further simulation details. See DOI: 10.1039/b806501b 6360 | Phys. Chem. Chem. Phys., 2008, 10, 6360–6368 This journal is c the Owner Societies 2008 PAPER www.rsc.org/pccp | Physical Chemistry Chemical Physics
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DFT study of the adsorption of microsolvated glycine on a hydrophilic
amorphous silica surfacew
Dominique Costa,*ab Asma Tougerti,a Frederik Tielens,a Christel Gervais,c
Lorenzo Stievanoaand Jean Francois Lambert
a
Received 16th April 2008, Accepted 25th July 2008
First published as an Advance Article on the web 23rd September 2008
DOI: 10.1039/b806501b
Density functional theory (DFT) periodic ab initio molecular dynamics calculations are used to
study the adsorption of gaseous and microsolvated glycine on a hydroxylated, hydrophilic silica
surface. The silica model is presented and the interaction of water with surface silanols is studied.
The heat of interaction of water is higher with the associated silanols (be they terminal or geminal
ones) studied here than with isolated silanols presented in past works. Glycine is stabilized in a
parallel mode on the hydroxylated surface. Terminal silanols do not allow the stabilization of the
calculations show that microsolvated zwitterion glycine directly binds through the carboxylate
function to a surface silanol rather than through water molecules. The adsorption mode, whether
with or without additional water molecules, is parallel to the surface. The ammonium function
does not interact directly with the silanol groups but rather through water molecules. Thus, the
carboxylate and ammonium functions exhibit two different reactivities towards silanols. The
calculated free energies, taking into account the chemical potentials of water and glycine in the
gas phase, suggest the existence of a thermodynamic domain in which the glycine is present in the
gas phase as well as strongly adsorbed on specific sites of the surface.
Introduction
Mineral surfaces have been suggested, already in the late 1950s, to
play a role in the activation of amino acids polymerization that
lead to the formation of peptides in early prebiotic chemistry.1
In particular, clays and other oxides were present in large
amounts on the prebiotic earth crust after the formation of
hydrosphere, and may have played an important role in the
process of chemical evolution (ref. 2 and references therein).
The earth crust consists primarily of silicate minerals,
containing a number of metal cations (e.g.aluminium,
magnesium, calcium, iron etc.) mainly structured in frame-
works of (SiO4) tetrahedra connected by siloxane bonds. In
spite of relevant differences with natural silicates, the study of
the adsorption and reactivity of amino acids on a pure silica
system can be considered as a ‘‘model’’ system for studying the
role that such surfaces may have played in the activation of
peptide bond formation.3
For oxides such as silica, alumina or iron oxides, molecular-
level studies remain scarce, even though it would be desirable
to know, not only if such surfaces can exhibit significant
selectivities (maybe even molecular recognition phenomena)
for different biomolecules going from amino acids to proteins,
but also whether the structure of the adsorption site may
influence the reactivity of adsorbed biomolecules.
Recently, theoretical ab initio tools have been successfully
used to investigate the mode of interaction of small biofunctions
with oxide and sulfide surfaces, in particular the adsorption of:
glycine on a dry (110) rutile surface,4 cysteine and serine on a
dry (110) and a hydroxylated (100) rutile surface,5 glycine on
pyrite,6 on alumina7 and on crystalline silica.8,9
We have undertaken a joint experimental and theoretical
study of the adsorption of glycine on amorphous silica surfaces
from the point of view of the surface, using knowledge pre-
viously gained on the molecular identification of surface func-
tional groups (such as silanols, silanolates, ‘‘nests’’ of
silanols. . .) to better characterize their interaction with amino
acids, both from the aqueous10 and from the vapor phase.11 We
showed that glycine from the aqueous phase binds with specific
surface sites at a coverage of 0.8 glycine nm�2 (10% of the
physical monolayer). In the theoretical part of our work, we
presented B3LYP results, obtained with minimal clusters of
glycine interacting with a silica surface, with and without ref.
11–13 the presence of water molecules. It was found that glycine
from the gas phase may form H-bond rings with silanols, and
that additional water molecules are needed to stabilize zwitter-
ionic glycine on the surface ref. 11 and 12. We focused our
attention on comparing calculated and experimental vibration
frequencies, namely the nCOO and dHNH modes. A precise
characterization of the glycine adsorption site was difficult,
principally due to the overlapping of frequencies with dHOH
of residual water, and also to the coupling of those frequencies
a Laboratoire de Reactivite de Surface, Universite Pierre et MarieCurie—Paris 6, 4, Place Jussieu, F-75252 ParisCedex 05 France
b Laboratoire de Physico-Chimie des Surfaces, ENSCP, 11 rue P. etM. Curie, 75005 Paris, France. E-mail: [email protected]
c Laboratoire de Chimie de la Matiere Condensee, Universite Pierre etMarie Curie—Paris 6, 4, Place Jussieu, F-75252 ParisCedex 05Francew Electronic supplementary information (ESI) available: Furthersimulation details. See DOI: 10.1039/b806501b
6360 | Phys. Chem. Chem. Phys., 2008, 10, 6360–6368 This journal is �c the Owner Societies 2008
PAPER www.rsc.org/pccp | Physical Chemistry Chemical Physics
with those of water molecules. Therefore, further theoretical
efforts are necessary to gain more precise insights into the
specific adsorption site.
However, the cluster calculations performed do not take into
account the long-range interactions and the information on the
constraints induced by the surface. Density functional theory
(DFT) periodic calculations of glycine adsorption on a crystal-
line silica were also performed.9 It was shown that the heat of
interaction of glycine with an isolated silanol is 56.9 kJ mol�1.9
However, isolated silanols are expected from experimental
results to exhibit a different reactivity versus probe molecules
than associated ones.14,15 H-Bonded silanols in silanol nests
have been suggested to be more reactive to water than isolated
ones and to allow water clustering.14–16 In addition, our own
works suggest that glycine, a hydrophilic amino-acid, should
adsorb on a silanol nest.11–13
We thus present here a study of the adsorption of glycine
(neutral or zwitterionic) on a model of silica surface exhibiting
OH clustering on the surface and also different types of OH
groups (terminal and geminal).
The scope of the present work is to explore briefly the
water/silica, glycine/silica, and microsolvated glycine/silica
interfaces at low coverages of amino acid (AA) on the surface,
as is found experimentally. In addition, we calculated thermo-
dynamical values (DG1) of the interface as a function of the
temperature and partial pressure, and we deduce desorption
temperatures of water and glycine from the surface.
Computational details
Every geometry optimization and minimization of the total
energy has been performed using the VASP code.17,18 In the
periodic density functional theory framework used,
the Kohn–Sham equations have been solved by means of the
A Hydroxylated silica surface—choice, description of the
model and geometry optimization
The silica model consists of a three-layer slab, with a
dehydroxylated surface and bottom oxygen atoms terminated
with H atoms (see Fig. 1a and b). Our strategy was to use this
‘‘healed plane of oxygen’’ to model a hydroxylated surface.
The resulting surface (obtained after reoptimization at 0 K of
the ‘‘Bernasconi slab’’) is shown in Fig. 1b. The atomic density
is 2.35 g cm�3. This density corresponds well to that reported
for real silica (2.2 g cm�3). The cell surface is 1.56 nm2. All Si
atoms have their complete coordination shell and all surface
Si atoms are hydroxylated and posses one or two SiOH
hydroxyl group (silanols). The SiOH density is 7.66 OH per
nm2. While this value is significantly higher than the generally
accepted silanol density for fumed silicas (4 to 5 per nm2), we
believe that it may be representative of precipitated silicas,
where SiOH densities between 7 and 8 per nm2 have been
reported;32 precipitated silicas are most probably relevant as
materials that may have been present in the prebiotic earth.
Also, the figure of 6.2 silanols per nm2 has been quoted for
biogenic silicas,33 indicating that these quite high silanol
density values are not unrealistic for silicas formed in
conditions of high water activity.
On silicas of lower OH density as commercial Degussa
Aerosil 380 which presents 5.1 silanols per nm2, these values
are average values taken over the whole surface and high
silanol density nano-zones on the surface are not unlikely to
exist. Indeed, experimental works on amorphous silica suggest
the coexistence of hydrophilic zones and hydrophobic ones,15
a hypothesis recently substantiated by a theoretical work.34
In the latter work, a silica surface of mean silanol density of
3.7 OH nm�2 is shown to exhibit zones free of silanols
coexisting with zones containing up to 7.5 silanols nm�2.
Also, the small size of the glycine molecule allows focusing
on a small proportion of the surface without formation of
chemical bonds with other surface groups. Finally, this high
density model is conserved because high silanol density zones,
with a known hydrophilic character, are the adsorption of
glycine, an amino acid of known hydrophilic character, or in
general a biofunction which contains few hydrophobic groups
on its interacting surface.
The repartition of the surface silanols in the model used is
5.1 geminal silanols (66%) per nm2, 2.5 terminal-associated
(44%). The silanol groups are H-bonded to each other or are
H-donating to a bridging O atom in a siloxane group. The
O–H bond lengths in the H bonds vary from 1.7 to 2.7 A.
Experimentally, the measured proportion of geminal silanols
depends on the type of silica and of the degree of humidity of
the atmosphere. Geminal silanols are expected to be stabilized
Table 1 Stabilization energies (from neutral glycine, NG) of the neutral (NG) and zwitterion (ZG) forms of glycine on vicinal silanols andgeminal silanol groups. Comparison with the stabilization energies of NGn, ZGn (G, n water molecules) complexes. Values in parenthesis indicatethe energies of G–water interaction calculated with B3LYP, 6-311++G** (kJ mol�1)
(c) Energy versus time (fs), blue: perpendicular orientation, pink:
parallel orientation. (d) Conformation obtained after standard
geometry optimization of the local minima in the MD run.
6366 | Phys. Chem. Chem. Phys., 2008, 10, 6360–6368 This journal is �c the Owner Societies 2008
rather high value (the mean value of H bonds between water
molecules in several water clusters was evaluated as
23 kJ mol�1). Again, as observed for water, this higher energy
of interaction may be attributed to the associated character of
the geminal silanols and to cooperative hydrogen bindings.
The displacement of the water molecules to allow a direct
interaction of glycine (as found through the MD runs) with a
silanol group is also in agreement with this higher energy of
adsorption calculated for glycine as compared to water on
hydroxylated silica. This result may seem rather counter-
intuitive, as H bonds are expected to be weak bonds. However,
there is experimental evidence that glycine is strongly adsorbed
onto the silica surface through a H-bond network.10,11
The results presented here support our previous works
performed at the B3LYP level on small clusters: indeed, the
interaction energy of glycine with free silanols was calculated
at �110 kJ mol�1: it was found that those free silanols do not
solvate glycine and that water acts as a ZG co-stabilizing
agent. Using a periodic approach, an interaction energy of
�98 kJ mol�1 for neutral glycine on terminal silanols was
obtained. This value is in good agreement with that found
using small clusters and B3LYP approach.
The relaxation energy of the surface in the presence of glycine
was calculated to be equal to DErelax = �12 kJ mol�1.44 This
rather low energy of surface rearrangement is in agreement with
the expected flexibility of amorphous silica, and shows that even
within the periodic scheme, the size of the cell was big enough to
ensure a low energetic cost surface reconstruction.
Rimola et al.9 reported that the COO(H) function does not
bind to a unique SiOH, but bridges two silanols, despite their
rather long distance. Their result is in agreement with our
findings using clusters to mimic the silanols on silica.11 Our
present results are in line with this trend, as neither 0 K
calculations nor MD studies report the binding with one single
silanol as a local minimum. Such a result is also found when
studying the adsorption of glycine on an a-alumina surface:
multi-site adsorption on hydroxyls is favored over adsorption
on one single site.7 As a consequence, the glycine molecule lies
parallel to the surface (silica or alumina). We also showed here
that the presence of additional water molecules does not
change the orientation of glycine, parallel to the surface.
Moreover, glycine interacts preferentially through the carboxy-
late function directly with the silanol groups rather than
through water molecules. This suggests that glycine is able to
displace water molecules on the surface to form a bond
between the carboxylate function and the silanols. In contrast,
the ammonium does not exhibit the ability to substitute water
molecules on the surface. This is understandable when one
considers that silanol groups are acidic in nature, and that they
mostly interact with the basic carboxylate group than the acidic
ammonium. Interestingly, a similar trend was also found in the
case of glycine adsorption on a-alumina: even on m1-OH
groups, which have been characterized as rather basic groups,45
the ammonium group does not form H bonds, whereas the
carboxylate function makes H bonds with one or two
hydroxyls.7 Thus, it seems to be a general trend that there is
no perpendicular binding of glycine, but rather a parallel
adsorption mode where the carboxylate function interacts with
several hydroxyls, on the one hand, and the ammonium group
may also build H bonds with the surface. Our present
calculations show that the presence of water does not change
this tendency.
Conclusion
The interaction of glycine with an amorphous hydrophilic
silica surface, containing a high density of associated terminal
and geminal silanols, was investigated by means of periodic
DFT. It was found that the heat of interaction of glycine with
geminal silanols is higher than with terminal silanols. The
comparison with previous data suggests that the associated
silanols (either terminal or geminal) have an increased affinity
towards glycine than isolated ones. At room temperature,
glycine was predicted to bind to geminal groups through the
carboxylate function, lying parallel to the surface. Micro-
solvated glycine binds to the surface via its COO� function
rather than through water molecules. Through the combina-
tion of H bonds formation, the energy of adsorption is high
enough to ensure thermal stability until 400 K.
Finally it was shown that the presence of silanols of different
reactivities allows the coexistence of glycine grafted at the
surface and gaseous glycine in the gas phase.
Acknowledgements
The authors thank Prof. C. F. Bernasconi for kindly supplying
his amorphous silica model. The computation facilities
provided by national computational center IDRIS and by
CCRE (Universite Pierre et Marie Curie) are acknowledged.
References
1 J. D. Bernal, Phys. Basis Life, 1951, 1.2 R. Hazen, Elements, 2005, 1, 135.3 J. F. Lambert, Origins Life Evol. Biosphere, 2008, 38, 211.4 L. Ojamae, C. Aulin, H. Pedersen and P. O. Kall, J. ColloidInterface Sci., 2006, 296, 71.
5 W. Langel and L. Menken, Surf. Sci., 2003, 538, 1.6 C. Boehme and D. Marx, J. Am. Chem. Soc., 2003, 125, 13362.7 C. Arrouvel, B. Diawara, D. Costa and P. Marcus, J. Phys. Chem.C, 2007, 111, 18164.
8 A. Rimola, S. Tosoni, M. Sodupe and P. Ugliengo,ChemPhysChem, 2006, 7, 157.
9 A. Rimola, M. Sodupe, S. Tosoni, B. Civalleri and P. Ugliengo,Langmuir, 2006, 22, 6593.
10 M. Meng, L. Stievano and J.-F. Lambert, Langmuir, 2004, 20, 914.11 C. Lomenech, G. Bery, D. Costa, L. Stievano and J.-F. Lambert,
ChemPhysChem, 2005, 6, 1061.12 D. Costa, C. Lomenech, M. Meng, L. Stievano and J.-F. Lambert,
THEOCHEM, 2007, 806, 253.13 L. Stievano, I. Lopes, L.-Y. Piao, M. Meng, D. Costa and
J.-F. Lambert, Eur. J. Mineral., 2007, 19, 321.14 V. Bolis, A. Cavenago and B. Fubini, Langmuir, 1997, 13(5), 895.15 B. Fubini, V. Bolis, A. Cavengo, E. Garrone and P. Ugliengo,
Langmuir, 1993, 9, 2712.16 T. Takei and M. Chikazawa, J. Colloid Interface Sci., 1998, 208,
570.17 G. Kresse and J. Hafner, Phys. Rev. B, 1994, 49, 14251.18 G. Kresse and J. Furthmuller, Comput. Mater. Sci., 1996, 6, 15.19 J. P. Perdew, J. A. Chevary, S. H. Vosko, K. A. Jackson, M. R.
Penderson, D. J. Singh and C. Fiolhais, Phys. Rev. B, 1992, 46, 6671.20 J. P. Perdew and Y. Wang, Phys. Rev. B, 1992, 45, 13244.21 P. E. Blochl, Phys. Rev. B, 1994, 50, 17953.22 G. Kresse and J. Joubert, Phys. Rev. B, 1999, 59, 1758.
This journal is �c the Owner Societies 2008 Phys. Chem. Chem. Phys., 2008, 10, 6360–6368 | 6367
23 P. Masini and M. Bernasconi, J. Phys.: Condens. Matter, 2002, 14,4133.
24 S. G. Stepanian, I. D. Reva, E. D. Radchenko, M. T. S. Rosado,G. Wada, E. Tamura, M. Okina and M. Nakamura, Bull. Chem.Soc. Jpn., 1982, 55, 3064.
25 R. Ramaekers, J. Pajak, B. Lambie and G. Maes, J. Chem. Phys.,2004, 120, 4182.
26 C. M. Aikens and M. S. Gordon, J. Am. Chem. Soc., 2006, 128,12835.
27 C. Chizallet, G. Costentin, M. Che, F. Delbecq and P. Sautet,J. Am. Chem. Soc., 2007, 129, 6442.
28 M. Digne, P. Sautet, P. Raybaud, P. Euzen and H. Toulhoat,J. Catal., 2002, 211, 1.
29 E. Kaxiras, Y. Bar-Yam, J. D. Joannopoulos and K. C. Pandey,Phys. Rev. B, 1987, 35, 9625.
30 G. X. Qian, R. M. Martin and D. J. Chadi, Phys. Rev. B, 1988, 38,7649.
31 M. J. Frisch, G. W. Trucks, H. B. Schlegel, G. E. Scuseria, M. A.Robb, J. R. Cheeseman, J. A. Montgomery, Jr., T. Vreven, K. N.Kudin, J. C. Burant, J. M. Millam, S. S. Iyengar, J. Tomasi, V.Barone, B. Mennucci, M. Cossi, G. Scalmani, N. Rega, G. A.Petersson, H. Nakatsuji, M. Hada, M. Ehara, K. Toyota, R.Fukuda, J. Hasegawa, M. Ishida, T. Nakajima, Y. Honda, O. Kitao,H. Nakai, M. Klene, X. Li, J. E. Knox, H. P. Hratchian, J. B. Cross,V. Bakken, C. Adamo, J. Jaramillo, R. Gomperts, R. E. Stratmann,O. Yazyev, A. J. Austin, R. Cammi, C. Pomelli, J. Ochterski, P. Y.Ayala, K.Morokuma, G. A. Voth, P. Salvador, J. J. Dannenberg, V.G. Zakrzewski, S. Dapprich, A. D. Daniels, M. C. Strain, O. Farkas,D. K. Malick, A. D. Rabuck, K. Raghavachari, J. B. Foresman, J.V. Ortiz, Q. Cui, A. G. Baboul, S. Clifford, J. Cioslowski, B. B.Stefanov, G. Liu, A. Liashenko, P. Piskorz, I. Komaromi, R. L.Martin, D. J. Fox, T. Keith, M. A. Al-Laham, C. Y. Peng, A.
Nanayakkara, M. Challacombe, P. M. W. Gill, B. G. Johnson, W.Chen, M. W. Wong, C. Gonzalez and J. A. Pople, GAUSSIAN 03(Revision B.03), Gaussian, Inc., Wallingford, CT, 2004.
32 A. Tuel, H. Hommel, A. P. Legrand, Y. Chevallier and J. C.Morawski, Colloids Surf., 1990, 45, 413.
33 S. Dixit and P. Van Cappellen, Geochim. Cosmochim. Acta, 2002,66, 2559.
34 A. A. Hassanali and S. J. Singer, J. Phys. Chem. B, 2007, 111,11181.
35 C. C. Liu and G. E. Maciel, J. Am. Chem. Soc., 1996, 118, 5103.36 D. W. Sindorf and G. E. Maciel, J. Phys. Chem., 1982, 86, 5208.37 X. Xue and M. Kanzaki, Phys. Chem. Miner., 1998, 26, 14.38 F. Tielens, W. Langenaeker and P. Geerlings, THEOCHEM, 2000,
496, 153.39 V. Murashov, J. Mol. Struct., 2003, 650, 141.40 F. Tielens, C. Gervais, J.-F. Lambert, F. Mauri and D. Costa,
Chem. Mater., 2008, 20, 3336.41 T. W. Dijkstra, R. Duchateau, R. van Santen, A. Meetsma and G.
P. A. Yap, J. Am. Chem. Soc., 2002, 124, 9856.42 H. Landmesser, H. Kosslick, U. Kurschner and R. Fricke,
J. Chem. Soc., Faraday Trans., 1998, 94, 971.43 A. Rimola, S. Tosoni, M. Sodupe and P. Ugliengo, Chem. Phys.
Lett., 2005, 408, 295.44 In this case, the energy of interaction (or binding energy) is
calculated as: DEint = E(G/Sil) � E(G) � E(Silgly), whereE(G/Sil) is the energy of the optimized G/Sil, E(G) is the referenceenergy of glycine in the gas phase, and E(Silgly) is the energy of thesilica surface frozen in the geometry-optimized in presence ofglycine. The difference of energy E1 � Eint gives the relaxationenergy of the silica surface, Erel.
45 M. Digne, P. Sautet, P. Raybaud, P. Euzen and H. Toulhoat,J. Catal., 2002, 211, 1.
6368 | Phys. Chem. Chem. Phys., 2008, 10, 6360–6368 This journal is �c the Owner Societies 2008