Molecular reorientation of water adsorbed on charged Ag(1 1 1) surfaces Cristian G. Sanchez * Atomistic Simulation Group, School of Mathematics and Physics, Physics Building, QueenÕs University Belfast, University Road, BT7 1NN Belfast, Northern Ireland, UK Received 8 November 2002; accepted for publication 22 January 2003 Abstract In this work we present first principles calculations of water adsorption over charged Ag(1 1 1) surfaces. The ori- entation of the adsorbed water molecule with respect to the surface changes from oxygen pointing away from the surface at negative charges to oxygen pointing towards the surface at positive charges. At zero charge the water molecule is oriented approximately parallel to the surface plane. Complete orientation of the molecule in the direction of the field is achieved for a critical charge density of 15 lC cm 2 for both positive and negative charges. Ó 2003 Elsevier Science B.V. All rights reserved. Keywords: Density functional calculations; Chemisorption; Water; Silver; Low index single crystal surfaces; Solid–liquid interfaces 1. Introduction Double layer modelling plays a fundamental role in theoretical electrochemistry since an accu- rate knowledge of the double layer is needed in any attempt to describe other electrochemical phe- nomena such as charge transfer processes. Many different approaches have been applied to the study of this subject, ranging from first principles mo- lecular dynamics to Monte Carlo simulations. These works have been extensively reviewed re- cently [1–4]. In spite of the effort dedicated there is not a general consensus on a model for the elect- rochemical double layer, and existing models have difficulties to rationalise all of the abundant body of experimental data. This limited success can be ascribed to the inherent complexity of the problem. The interface is a highly anisotropic environment in which large changes of composition occur within a very narrow spatial extent. The abrupt difference in molecular structure between the phases on either side of the interface, that makes them so interest- ing, is extremely challenging from a theoretical point of view. Techniques for the study of both the charged metal surface [5,6] and water from first principles ([7] and references therein) have been made available only recently. No fully ab initio simulation yet exists of the charged interface, only for the neutral case [8,9]. The study of water adsorption over metallic surfaces provides valuable information that may help the understanding of the electrochemical interface and there is abundant experimental in- formation available [10,11]. A number of first * Tel.: +44-28-90273557; fax: +44-28-90241958. E-mail address: [email protected](C.G. Sanchez). 0039-6028/03/$ - see front matter Ó 2003 Elsevier Science B.V. All rights reserved. doi:10.1016/S0039-6028(03)00080-3 Surface Science 527 (2003) 1–11 www.elsevier.com/locate/susc
11
Embed
Molecular reorientation of water adsorbed on charged Ag(111) surfaces
This document is posted to help you gain knowledge. Please leave a comment to let me know what you think about it! Share it to your friends and learn new things together.
Transcript
Molecular reorientation of water adsorbed on chargedAg(1 1 1) surfaces
Cristi�aan G. S�aanchez *
Atomistic Simulation Group, School of Mathematics and Physics, Physics Building, Queen�s University Belfast, University Road,
BT7 1NN Belfast, Northern Ireland, UK
Received 8 November 2002; accepted for publication 22 January 2003
Abstract
In this work we present first principles calculations of water adsorption over charged Ag(1 1 1) surfaces. The ori-
entation of the adsorbed water molecule with respect to the surface changes from oxygen pointing away from the
surface at negative charges to oxygen pointing towards the surface at positive charges. At zero charge the water
molecule is oriented approximately parallel to the surface plane. Complete orientation of the molecule in the direction
of the field is achieved for a critical charge density of 15 lCcm�2 for both positive and negative charges.
� 2003 Elsevier Science B.V. All rights reserved.
Keywords: Density functional calculations; Chemisorption; Water; Silver; Low index single crystal surfaces; Solid–liquid interfaces
1. Introduction
Double layer modelling plays a fundamental
role in theoretical electrochemistry since an accu-
rate knowledge of the double layer is needed in any
attempt to describe other electrochemical phe-
nomena such as charge transfer processes. Manydifferent approaches have been applied to the study
of this subject, ranging from first principles mo-
lecular dynamics to Monte Carlo simulations.
These works have been extensively reviewed re-
cently [1–4]. In spite of the effort dedicated there is
not a general consensus on a model for the elect-
rochemical double layer, and existing models have
difficulties to rationalise all of the abundant body
of experimental data. This limited success can be
ascribed to the inherent complexity of the problem.
The interface is a highly anisotropic environment in
which large changes of composition occur within a
very narrow spatial extent. The abrupt difference in
molecular structure between the phases on either
side of the interface, that makes them so interest-ing, is extremely challenging from a theoretical
point of view. Techniques for the study of both the
charged metal surface [5,6] and water from first
principles ([7] and references therein) have been
made available only recently. No fully ab initio
simulation yet exists of the charged interface, only
for the neutral case [8,9].
The study of water adsorption over metallicsurfaces provides valuable information that may
Positive angles indicate that the oxygen atom is pointing towards the surface and negative ones that the oxygen atom is pointing away
from the surface. The acronyms used in the method column are as follows: MP2 ¼ Moller–Plesset second-order perturbation theory,PW ¼ plane wave basis set, BLYP ¼ density functional theory using BLYP GGA functional, B3LYP ¼ Becke 3 parameter hybrid
Hartree–Fock DFT functional, PBE ¼ DFT using PBE GGA functional.
ception of the Al(1 1 1) surface [17] for which theresults indicate orientation normal to the surface.
Previous first principles results for the Ag(1 1 1)
surface are inconclusive with respect to the ad-
sorption geometry. In Ref. [14], as mentioned in
Section 1, the tilting angle could not be obtained
because of the small energy difference between
different orientations, and this was attributed to a
limitation of the cluster model. Most cluster cal-culations avoid full geometry optimisation; nor-
mally the internal geometry of the adsorbate and
the adsorption site are constrained in order to save
computational time and no attempt to relax the
substrate is made. Furthermore, the experimental
lattice constant of the metal is used, which can be
different from the optimum lattice constant for the
model used. These approximations may be im-portant to determine the final water configuration.
The result that is more comparable to ours in
terms of the model used is that of Ref. [9]. Thegeometry obtained by these authors differs from
ours in that their results show the water molecule
tilted outwards at an angle of 30 degrees with re-
spect to the surface plane. This discrepancy might
be attributed to the lower (less accurate) plane
wave cutoff energy used in Ref. [9] (60 Ry). In our
experience cutoffs of over 90 Ry are needed in
order to ensure proper convergence of the forceswhen norm conserving Troullier–Martins pseudo-
potentials are used for oxygen. We have performed
plane wave calculations using the CPMD code
with a plane wave energy cutoff of 70 Ry and ob-
tained an adsorption geometry very similar to the
one presented here. All of this can be rationalised
from the fact that the potential energy surface for
water adsorption over Ag is a relatively shallowfunction of the tilt angle and molecular position
Fig. 2. Water orientation with respect to the substrate. For the sake of clarity only a ð1� 1Þ surface unit cell of substrate is shown(note that the unit cell used for the calculation is a ð2� 2Þ cell, 4 times larger, as shown in Fig. 1). (a) Zero charge, top view; (b) zerocharge, side view; (c) charge density of 15.7 lCcm�2, top view; (d) charge density of 15.7 lCcm�2, side view; (e) charge density of )15.7lCcm�2, top view; (f) charge density of )15.7 lCcm�2, side view.
where /ujðk; rÞ represents the basis set orbital j onatom u, wiðk; rÞ the i Kohn–Sham orbital with ei-genvalue �iðkÞ and the integration on k runs over
the Brillouin zone. In practice, the integration over
the Brillouin zone is replaced by a finite sum, andDirac�s d function is replaced by a Gaussian ofwidth r (0.25 eV was used for the PDOS shownhere):
guð�Þ ¼Xi;j;k
Zwk
1
rffiffiffiffiffiffi2p
p
� exp �� �iðkÞ2r2
� �hwiðk; rÞj/ujðk; rÞid�
ð2Þ
guð�Þ represents the portion of the total density ofstates due to orbitals on atom u. In Fig. 5b thedensity of states of the water molecule is shown,the three highest occupied molecular orbitals can
be seen. Iso-surface plots for these orbitals are
shown in Fig. 4. In Fig. 5b the total DOS is di-
vided into H and O contributions. From this we
can see that orbital 1B2 is formed from almost
equal contributions from oxygen and hydrogen
atomic orbitals. Orbital 3A1 (the r lone pair) has asmall contribution from H orbitals which is evensmaller for 1B1 (the p lone pair). 1B2 is the main rbonding orbital between O and H atoms, orbitals
3A1 and 1B1 are basically oxygen lone pairs. Upon
adsorption on the neutral surface (Fig. 5d) both
1B2 and 3A1 orbitals are stabilised but the most
important changes occur in the 1B1 orbital. This
orbital interacts mainly with the d-band (shown in
Fig. 5a) producing significant stabilisation andwidening. This fact explains that the most stable
orientation of the water molecule over the neutral
surface is almost horizontal. This is the orientation
that allows maximum overlap of the 1B1 orbital
with the surface. Integration of the OþH PDOSfrom )7 eV up to the Fermi level indicates that theoccupation of these orbitals increases, henceforth asmall negative charge (�0.02 electrons) is trans-ferred to the water orbitals. The localisation of this
charge is however, difficult to assess from the
analysis of the PDOS. Upon charging of the sur-
face the interaction with the electric field is even-
tually dominant and a perpendicular orientation is
attained. In this orientations the overlap between
the 1B1 orbital with the surface is smaller and itremains almost unchanged. The interaction is not
equivalent for positive and negative charges (com-
pare 4c and 4e) and some mixing can be appreci-
ated for positive charges when the orbital is closer
to the surface. Other differences exist between
positive and negative charges. While orbital 3A1energy remains almost unchanged the 1B2 orbital
energy is higher with respect to neutral charge andthis effect is more important for positive charges.
The same trend is observed for the 1B1 orbital.
This changes in orbital energies may be a result of
the combination of both orientation change and
charge effects. From the integration of the PDOS
in Fig. 5a change in occupation of around 0.1
electrons can be observed for both 3A1 and 1B1orbitals. This occupation increase is positive fornegative charge and the opposite holds for positive
surface charge.
In Fig. 7 of Ref. [40] Valette shows a plot of the
inner layer capacity of the water/Ag(1 1 1) interface
as a function of charge density. The inner layer
capacitance has a maximum at the potential of
zero charge (pzc) and levels off at about the same
Fig. 4. The three highest occupied molecular orbitals of H2O. The energy order is 1B1 > 3A1 > 1B2.