JCompPhys 326 0222
JCompPhys 326 0222
JCompPhys 326 0222
School of Physics and Astronomy, University of Edinburgh, Peter Guthrie Tait Road, Edinburgh EH9 3FD, United Kingdom
National Physical Laboratory, Hampton Road, Teddington, Middlesex TW11 0LW, United Kingdom
IBM T. J. Watson Research Center, Yorktown Heights, NY 10598, USA
a r t i c l e
i n f o
Article history:
Received 20 March 2016
Received in revised form 10 August 2016
Accepted 24 August 2016
Available online 29 August 2016
Keywords:
Molecular dynamics
Force eld
Electronic coarse graining
Dispersion
Polarisation
Path integral
a b s t r a c t
One key factor that limits the predictive power of molecular dynamics simulations is
the accuracy and transferability of the input force eld. Force elds are challenged by
heterogeneous environments, where electronic responses give rise to biologically important
forces such as many-body polarisation and dispersion. The importance of polarisation
in the condensed phase was recognised early on, as described by Cochran in 1959
[Philosophical Magazine 4 (1959) 10821086] [32]. Currently in molecular simulation,
dispersion forces are treated at the two-body level and in the dipole limit, although the
importance of three-body terms in the condensed phase was demonstrated by Barker
in the 1980s [Phys. Rev. Lett. 57 (1986) 230233] [72]. One approach for treating both
polarisation and dispersion on an equal basis is to coarse grain the electrons surrounding a
molecular moiety to a single quantum harmonic oscillator (cf. Hirschfelder, Curtiss and Bird
1954 [The Molecular Theory of Gases and Liquids (1954)] [37]). The approach, when solved
in strong coupling beyond the dipole limit, gives a description of long-range forces that
includes two- and many-body terms to all orders. In the last decade, the tools necessary
to implement the strong coupling limit have been developed, culminating in a transferable
model of water with excellent predictive power across the phase diagram. Transferability
arises since the environment automatically identies the important long range interactions,
rather than the modeller through a limited set of expressions. Here, we discuss the role of
electronic coarse-graining in predictive multiscale materials modelling and describe the
rst implementation of the method in a general purpose molecular dynamics software:
QDO_MD.
2016 Elsevier Inc. All rights reserved.
1. Introduction
Molecular modelling has become an integral part of research in all areas of condensed matter, forming a new part of the
scientic method that elucidates scientic principles and accelerates the discovery of new materials [1]. This computational
revolution has been driven by the exponential scaling of computer hardware [2,3] along with the implementation of scalable
software on these platforms [47]. An important part of the equation remains to improve the accuracy and transferability of
Corresponding author.
E-mail address: aviu.cipcigan@ed.ac.uk (F.S. Cipcigan).
http://dx.doi.org/10.1016/j.jcp.2016.08.030
0021-9991/ 2016 Elsevier Inc. All rights reserved.
223
Fig. 1. Examples of environments studied using electronically coarse-grained methods and shown to match experiment: ice II, ambient temperature liquid
water and the surface of liquid water. The images illustrate the electronic responses of individual molecules, with red and blue isosurfaces corresponding to
regions of enhancement and depletion of electronic density, respectively. (For interpretation of the references to colour in this gure, the reader is referred
to the web version of this article.)
the employed force elds, which ultimately dene the accuracy of results, thereby laying the basis for predictive modelling,
given sucient sampling of phase space.
Standard force elds, designed to be numerically ecient, are created by tting a subset of thermodynamic and structural
properties to an analytic expression for the potential energy, typically consisting of sums of pairwise long-range terms [8].
In many systems, this approach has proved successful even if the accuracy of such force elds is at best around 1 kcal/mol.
For example, Schames et al. [9] used molecular dynamics simulations to discover a hidden binding site in HIV integrase,
a molecule that enables the integration of HIVs genetic material into the host cell DNA. This discovery led to experimental
conrmation [10] and subsequent development of raltegravir, a successful medicine that halts the progression of HIV into
AIDS. Another success was the simultaneous discovery by simulation [11] and experiment [12] of the molecular basis of
mutations in a gene responsible for Gauchers disease, a genetic disease causing the build-up of fatty substances in the
organism.
Nonetheless, strategies based on tting to a xed functional are not guaranteed to be transferable to heterogeneous
environments far from the region of parametrisation and validity of terms selected. One such environment is, for example,
a bacterial membrane penetrated by a peptide. The shape of the peptide inside the membrane depends strongly on the
force elds used [13], with only experiments currently being able to distinguish between possibilities.
Here we present our recent development of a class of force elds for materials modelling [1420] that are transferable,
physically motivated, and implemented in the general purpose molecular dynamics software QDO_MD. The technique treats
many-body polarisation and many-body dispersion on the same footing by representing electronic distributions of individual
atoms and molecular moieties using a single coarse grained particle. This particle, known as a Quantum Drude Oscillator
[19,20] (QDO), consists of a negative charge bound to a positive centre by a quantum harmonic oscillator. QDOs generate
many-body polarisation, many-body dispersion interactions and cross terms beyond the dipole limit [21] and represent a
non-perturbative approach that generates all long-range forces within Gaussian statistics when sampled in strong coupling.
The QDO approach has been employed to construct a general purpose water model (QDO-water) that is transferable
without tting to any condensed phase data (at present neglecting bond breaking and making, which could however be
included using a TersoffPettifor approach [17,22,23]). QDO-water consists of a rigid molecular geometry (decorated with
xed charges), short-range empirical repulsion and a QDO. The model is parametrised using the static multiple moments of
an isolated molecule, its polarisability, the dipoledipole dispersion coecient (C 6 ) and one cut through the dimer energy
surface [14] used to set the short-range repulsion. Its properties have been studied in a diverse set of environments (depicted in Fig. 1), ranging from high-pressure ice (ice II), liquid water, steam, the liquidvapour interface, and supercritical
water. The model predicts density, surface tension, enthalpy of vaporisation and dielectric constant across these wide range
of environments, demonstrating a formerly unrealised level of transferability.
2. Predictive materials modelling using electronically coarse grained methods
Fig. 2 presents the spectrum of modelling techniques, with the QDO technique occupying a previously vacant place
between ab initio methods and all-atom molecular dynamics. QDOs guiding philosophy is instead of treating an exact
system in an approximate way, treat an approximate system in an exact way.
In a physical sense, the QDO model is solvable in strong coupling, allowing for an approach that contains all long-range,
many-body interactions to all orders. The absence of truncation means that the modeller does not pick the symmetry by
choice of truncation but rather the environment picks the key terms. This type of simplied but rich model is at the heart
of modern theories because its lack of bias allows the essential physics to emerge naturally without the modeller choosing
the important interactions a priori.
224
Fig. 2. Various simulation techniques arranged according to the timescales and lengthscales which they sample. The left-most image, originally by Chaplin
[24], represents electron densities of the water pentamer obtained via ab initio calculations. The next is the electronically coarse grained representation
of the air-water surface, where red and blue isosurfaces depict regions of enhancement and depletion of electronic density. This is followed by a classical
molecular dynamics simulation and an atomically coarse grained study of the same interface. The right-most image represents a particle-based realtime
simulation of water ow over complex landscape using a method developed by Chentanez and Mller [25]. The left and right-most images are used with
permission from their respective authors while the rest are original work by the authors of this paper. (For interpretation of the references to colour in this
gure, the reader is referred to the web version of this article.)
The price paid for the richness of the QDO model at low computational cost (order N log N [26,27] or N [28]) is the
approximation made in coarse graining: assuming localised electrons in an insulator respond according to Gaussian statistics
and the neglect of exchange effects, which are taken to be short range. This is consistent with the general spirit of coarse
grained approaches where exactness is sacriced while maintaining sucient accuracy for the problem at hand. Basically,
QDOs are a coarse graining of a full high level electronic structure without truncating the long range interaction, while
standard force elds can be thought of as a coarse graining of QDOs, with a truncation to dipole limit pair-wise dispersion
and a neglect of polarisation or its inclusion at the many-body dipole level. As demonstrated in the next section, systems
of single QDOs per atom or molecular moiety solved in strong coupling are sucient to model molecules that are isotropic
(such as noble gases) or close to isotropic (such as simple hydrides like methane and water). To model anisotropic responses,
multiple interacting QDOs can be pinned to individual points in the molecular frame [29].
The quantum Drude oscillator model has a rich history dating back to London [30], who used it to derive from quantum
mechanical principles the 1/ R 6 functional form of the dispersion interaction between atoms and molecules and of course
Drude himself, who used the classical limit of the model to understand the dispersion of light passing through insulators
[31]. In more details, the classical limit describes dipole many-body polarisation and has been successfully employed in theory and simulation for many years following the work of Cochran [3236]. In the quantum dipole limit, the Drude oscillator
has been employed as an exemplar model for dispersion in the 1950s [37,38], following Londons initial calculations. The
quantum dipole limit model has been used to simulate xenon clusters [35] via an N 3 scaling method and electron attachment to water clusters using a Conguration Integral approach with high order polynomial scaling [39]. The full model was
examined as an approximate treatment for dispersion of one valance electron systems by Fontana in the 1960s [40]. In a
series of papers beginning in 2006, the tools to simulate the full model with order N to N log N complexity (depending
on the method used to treat long-range interactions) via non-perturbative path integral techniques [20,17,21] were developed. Applications begun with rare gases [19,21] and moved forward to liquid water [18,1416]. In related work, the
dipole-limit quantum model has been embedded within density functional theory (within the local density approximation)
by Tkachenko et al. [41] to treat many-body dipole dispersion beyond empirical potentials using the adiabatic connection
formula [42]. This merger of embedded dipole-limit quantum oscillators and density functional theory lead to applications
to heterogeneous systems such as benzene adsorbed onto metal surfaces [43] or DNAgraphene interactions [44].
Water is an ideal system in which to illustrate the importance of a complete treatment of electronic responses. Waters
structure arises due to a competition between directional hydrogen bonds, which favour an open ice-like local structure and
van der Waals forces, which favour a close-packed local structure. Many-body polarisation and dispersion interaction are
key to distinguishing the dominant motifs under the conditions of interest.
Hydrogen bonds are known to be cooperative, meaning that their interaction strength changes depending on environment
thus leading to the emergence of a wide variety of motifs. A simple reporter of this cooperation is the molecular dipole
moment, which changes from a value of 1.85 D in the gas phase to an estimated value of 2.53.6 D in the condensed phase
[18,45], where four hydrogen bonded motifs are dominant. This sensitivity to local structure can be used as a ngerprint of
various local motifs, as we have reported in Ref. [15]. There, we showed that a cusp in the dipole moment as a function
of temperature coincides with experimental maxima in heat capacity, separating the supercritical region in gas-like and
liquid-like regions [46] and revealing the Widom line [47] at a molecular level. We also have shown that such cooperation
makes hydrogen bonds more asymmetric than previously thought [16], with a molecule favouring the loss of an acceptor
bond (on the side of the oxygen) over that of a donor bond (on the side of the hydrogen) in both the liquid phase and at
the liquidgas interface.
Dispersion interactions are also important in water. Including these responses is essential to generate even the basic
structure of water at room temperature. An illustrative example of this balance is the overstructuring of room-temperature
225
water by local approximations to DFT [48], where including the electron correlations that lead to accurate van der Waals
interactions is challenging (although, there have been promising results using the similar technique of embedded quantum
harmonic oscillators at the dipole level [41]). In our water model, it is possible to increase the dispersion coecients linearly
while keeping the polarisabilities constant and vice versa, allowing the study to the effect of both contributions to water
structure independently. In Ref. [18], we showed that by tuning only the strength of van der Waals interactions, the density
of liquid water can be decreased by 15% while still maintaining the desired hydrogen bonded local structure.
In addition, three-body effects account for as much as 25% of the binding energy of water, according to the estimates
of Keutsch et al. [49]. Thus, monoatomic two-body potentials for the water molecule can only reproduce waters condensed
phase properties if their parameters are allowed to vary with state point [50,51]. Even a full-atom description of water
cannot be transferable if its electrostatics is xed. Vega and Abascal [52] showed that a nonpolarisable model of water
cannot simultaneously reproduce the melting temperature and temperature of maximum density.
Therefore, in order to create a truly transferable energy surface for molecular simulations, which is therefore predictive
outside the regime of parametrisation, the electronic effects need to be taken into account since they give rise to non-trivial
many-body polarisation and dispersion. QDOs do so while keeping eciency close to that of all-atom molecular dynamics
and scaling as N log N with the number of atoms N (assuming the use of particle mesh type Ewald summation techniques;
the scaling can be further reduced to order N via the use of cell multipole methods [28]). This strategy can be used to
create models that are parametrised without any condensed phase input, yet generate the properties of condensed phases.
3. Electronic coarse graining using Quantum Drude Oscillators
3.1. Dispersion interactions between quantum harmonic oscillators
In order to gain intuition into how quantum harmonic oscillators reproduce electronic responses, consider a simple
model proposed rst by London [30,37]: a negative charge q of mass m, free to move in a dimension x. The charge is
localised by connecting it by a spring of frequency to a positive charge +q xed at the origin.
Consider adding a positive, xed test charge Q at a distance R x from the origin. The system is in equilibrium when
the Coulomb force Eq on the negative charge equals the spring force m2 x. Balancing the two forces results in the oscillator
acquiring a dipole moment = qx = q2 E /(m2 ) and thus having a dipole polarisability dened as:
1 :=
q2
m 2
(1)
In order to account for dispersion effects, the system has to be treated quantum mechanically. Consider two identical
oscillators separated by a distance R interacting via a term c ( R ). The leading order interaction is dipoledipole, meaning
that the term c ( R ) is proportional to R 3 . Thus, the Hamiltonian is:
=
H
p 21
2m
p 22
2m
1
+ m2 x21 + x22 + c ( R ) x1 x2 .
2
Changing coordinates to = 1
monic oscillators of frequency
=
H
p 2+
2m
1 c.
(2)
+ m (1 + c ) + +
2
p 2
2m
2
+ m (1 c )
2
(3)
The ground state energy of the coupled system is hence given by, to leading order in c:
E0 =
1
2
1+c+
1c
1
h 1 c 2 + O (c 3 ) .
(4)
Fig. 3 shows the ground state probability distribution 2 (x1 , x2 ) in the independent (c = 0) and correlated (c > 0) cases.
When c increases, it becomes more probable for
x1 and x2 to have the opposite sign and less probable for them to have the
same sign. Since the energy is proportional to dx1 dx2 2 (x1 , x2 )x1 x2 c ( R ), this correlation leads to the attractive force between two neutral molecules proportional to c ( R )2 R 6 , just as the leading order term in the van der Waals potential.
This analysis shows that even a one dimensional quantum harmonic oscillator can capture two basic effects of long range
forces: polarisation and dispersion. In this case, these interactions are limited to dipole-limit forces. To capture the full set
of interactions one has to consider the full three dimensional system.
226
Fig. 3. The ground state probability density of two one dimensional quantum harmonic oscillators interacting via a c ( R )x1 x2 term. The left panel illustrates
the non-interacting case, with c ( R ) = 0. The right panel illustrates the interacting case, with c ( R ) > 0. The spread of the wavefunction across the diagonal
represents the electron correlation the gives rise to attractive van der Waals forces in real systems.
=
H
p 2
2m
+ m 2 x2 .
(5)
Perturbing this Hamiltonian via a point charge Q at a distance R gives a rst order correction to the energy of zero and
a second order correction of [21]:
E (2 ) ( R ) =
Q 2 l
l =0
2R 2l+2
(6)
l are given by
l1
(2l 1)!!
h
l =
q2
m 2
2m
(7)
Considering two QDOs separated by a distance R gives a rst order correction to the energy of zero and a second order
correction of [21,40]:
E (2 ) ( R ) =
C 2n R 2n
(8)
n =3
with
C6 =
1 1 h ,
4
C 8 = 51 2 h ,
(9)
...
Therefore, the full model has a complex and rich set of long range responses, which are replicated with only three
parameters. This means the responses are correlated and thus one needs to check whether these correlations are satised
in real atoms and molecules.
3.3. Invariant relationships between response coecients
As the responses of QDOs depend only on three parameters, these parameters can be eliminated, resulting in the following invariants that can be used to verify the accuracy of the QDO approximation [21]:
227
Fig. 4. Three types of invariant ratios between polarisation and dispersion coecients, predicted by Quantum Drude Oscillators. Polarisation ratios involve
only polarisabilities and analogously for dispersion ratios. Mixed ratios involve both polarisation and dispersion coecients. Deviation from theory is shown
for three types of atoms and molecules: noble gases, alkali metals and small hydrides.
20
9
49
40
2
= 1,
1 3
C8
C 6 C 10
C 6 1
4C 9
= 1,
(10)
= 1.
Comparing these ratios with the responses of real molecules gives the results shown in Fig. 4 (adapted from Ref. [21]).
The agreement is good for the noble gases, with ratios within 10% of experiment, as their shells are fully lled and thus
the distribution of electrons is nearly spherical. The agreement is also within 10% for most alkali metals, for which the last
electron contributes mostly to polarisation. Small hydrides such as water and methane agree within 15%. This agreement is
due to the electronegativity of atoms such as oxygen, which centres most of the electronic charge on them thus resulting in
charge distributions and responses that are close to spherical. For example, the dipole polarisability tensor of water exhibits
a 4% deviation from spherical symmetry.
The agreement shows that, in the case of the materials illustrated in Fig. 4, QDOs produce a dispersion and induction
series that matches experiments and ab initio calculations. This agreement also means that, in real materials, the individual
terms in these series are not independent, but related by symmetry constraints, with spherically symmetric materials having
responses approximated well by a Gaussian model. However, a spherical model has its limitations. For instance, the dipole
hyperpolarisability is identically zero due to the use of the on-site harmonic interactions. In order to move beyond the
response of (approximately) spherically symmetric systems, more QDOs can be placed the molecular frame to break the
symmetry. Enriching the model by changing the on-site interaction or introducing multiple QDOs per molecular moiety,
forms the basis for future work.
3.4. Parametrisation of the full quantum model
Invariants aside, the responses of a QDO can be inverted to give its properties as a function of the responses. The relevant
relations, which are used to parametrise a QDO are as follows:
1 4C 6
h 312
h 31
h 5C 6
or m =
,
42
C8
q = m 2 1 .
m=
(11)
(12)
(13)
4. Simulating Quantum Drude Oscillators via two temperature path integral molecular dynamics
Path integral molecular dynamics, shortened to PIMD, is a method of sampling a quantum mechanical partition function
such as that of a QDO, using classical methods [53,54]. This section highlights its basic derivation, with the full, QDO-based
method being described in Refs. [20,17].
228
Consider a quantum mechanical system (such as electrons sampling the BornOppenheimer surface of a nuclear conguration), with degrees of freedom x. The state of this system is described by a density matrix (x, x ; D ). The partition
function at inverse temperature D = 1/kT D is thus [55]:
Z ( D ) = tr e D H =
(14)
where dx represents a small volume element in the dim(x)-dimensional space spanned by the systems degrees of freedom.
Since we are interested in the ground state electronic surface of insulators, the inverse temperature D associated with the
electronic degrees of freedom is taken as large as possible while ensuring the ground state dominates the statistics. For
harmonic systems, D h > 8.
Since the density matrix is an exponential of the Hamiltonian, it can be factorised into higher temperature (smaller
= D / P ) slices to give the following path integral representation,
Z ( D ) =
P
(15)
i =1
The reason for this factorisation is that increasing the temperature, thus decreasing D makes density matrices more
classical and thus easier to approximate. Hence the use of the smallest D (or largest electronic temperature) that still
keeps the system close to the ground state serves to reduce P . The approximation used comes from a Trotter factorisation
0 = e H 0 , and a perturbation
(16)
In the case of QDOs it is convenient to set H 0 as the Hamiltonian of the isolated oscillator, with the following reference
density matrix:
0 (x, x ; ) =
P ( ) 2
P ( )
exp P ( )(x x )2 +
(x + (x )2 ) .
(17)
Z ( D ) =
P
i =1
P
i
du
3N /2
i =1
exp
2i2
i =1
2i
u
V (xi )
exp
2i2
V (xi (
u i ))
(18)
i =1
staging coordinates
external potential
One step remains in order to make the partition function isomorphic to a ctitious classical system: the addition of
i with corresponding faux masses m.
This transforms the partition function to:
conjugate momenta p
Z ( D ) =
P
i =1
i
du
1
2i2
3N /2
exp
2i
u
2i2
exp
P
i =1
2i
p
i exp
V (xi (
u i )) C
dp
.
2m
(19)
This nal transformation leads to a partition function with the effective classical Hamiltonian H (faux) , which can be sampled
via existing methods to sample classical systems [54,19,20].
H (faux) =
P
2i
2i
p
u
V (xi (
u i ))
+
+
.
2
2m
P
2 i
i =1
(20)
of the
When adding the motion of the nuclei, the adiabatic principle needs to be invoked and the ctitious mass m
electronic degrees of freedom selected such that they evolve on a time scale a factor of smaller than that of the nuclear
degrees of freedom. This selection of masses results in two effects: it allows the electronic degrees of freedom to be thermostatted at a higher temperature than the nuclei, and reduces energy transfer between the hot electrons and cold nuclei,
allowing the dynamics of these two subsystems to be evolved simultaneously [54,19,20,17]. Further energy transfer between
the two subsystems can be reduced by using an adaptive thermostat that dissipates excess heat induced by Brownian motion [57]. It is important to recognise that the canonical ensemble must be generated for the electronic degrees of freedom
in order for the model to have physical meaning, since the path integral method is explicitly derived to sample a canonical
ensemble.
229
Table 1
The free parameters of QDO-water. E h 27.211 eV is the Hartree energy,
a0 0.5292 is the Bohr radius and e 1.60 1019 C is the electron
charge.
Parameter
Value
Molecular geometry
R OH
0.9572
HOH
104.52
Ground state electrostatics
qH
0.605|e |
R OM
0.2667
Quantum Drude Oscillator
mD
0.3656 me
D
0.6287 E h /h
qD
1.1973|e |
Parameter
D
C
1
1
2
2
Value
Coulomb damping
= H = M
0.1 a 0
1.2 a0
Short range repulsion
613.3 E h
2.3244 a01
10.5693 E h
1.5145 a01
230
In more detail, the frame is xed in the experimental molecular geometry, with charges and distances chosen to give
an exact dipole moment for the isolated molecule (1.85 D) and a best t to the quadrupole moment. The parameters of
the QDO are t using the relations in equation (13) to the dipole and quadrupole polarisabilities and the C 6 induceddipoleinduced-dipole dispersion coecient. The repulsive potential is t by calculating the interaction energy between two
molecules using ab initio and the repulsion-free model and tting the difference to a double exponential 1 e 1 r + 2 e 2 r
[18,14]. The Coulomb interaction between charges is regularised by replacing each point charge X by a Gaussian distribution
of width X .
Since QDO-water is parameterised from the properties of a single molecule and the dimer, condensed phase properties are a prediction rather than a tting target. The model was studied in the following environments: high pressure ice (ice II) [14], liquid water [14], steam [14], the liquidvapour interface [16] and supercritical water [15]. The
agreement with experiment was good, with densities within few percent of experiment. The model predicts the temperature of maximum density of 5.5(2) C (compared to the experimental value of 3.98 C [67]) and the critical point of
{ T C = 649(2) K, C = 0.317(5) g/cm3 } (compared to the experimental value of { T C = 647.096 K, C = 0.322 g/cm3 } [67]). It
also accurately tracks the dielectric constant, enthalpy of vaporisation and surface tension between T = 300 K and T = 600 K
[14].
QDO water also provided insights into the local structure at the liquidvapour interface [16] and in supercritical water
[15]. At the liquidvapour interface the orientation of the water molecules is inuenced by an intrinsic asymmetry in the
way water molecules hydrogen bond. When losing a hydrogen bond, molecules prefer to lose it on the side of the oxygen
(an acceptor bond) rather than on the side of the hydrogen (a donor bond) [16]. This leads to a surface with more oxygen
than hydrogen atoms, which is negatively charged.
In supercritical water [15], the dipole moment was discovered to be a reliable ngerprint of the Widom line extending
the liquidgas transition [15] into the supercritical region. The phase diagram locus where the heat capacity is maximum
coincides with a cusp in the dipole moment as a function of density. This cusp separates liquid-like from gas-like scaling,
tracking the Widom line. This conclusion is general to any polar uid, showing the importance of polarisation in characterising highly heterogeneous materials.
At this stage of development, we have studied a classical molecular model using a rigid geometry for the water
molecules. It has been shown that the rigid frame forms a much better approximation to a fully exible model including nuclear quantum effects than a classical exible model [6870]. Also as noted in [15], the critical constants, melting
point and other thermodynamic quantities do not show strong isotope effects. It is feasible to combine QDO with PIMD to
examine a fully exible model with quantum nuclei, a subject of current interest [71].
7. Conclusion
This paper summarises our recent progress in signicantly enhancing the transferability of force elds describing complex systems of insulators by coarse graining the electrons of a molecular moiety to a single quantum harmonic oscillator, an
approach we call the Quantum Drude Oscillator method. This technique generates, naturally and to all orders, many-body
forces such as dispersion, polarisation and mixed interactions beyond the dipole limit. These interactions are important
in modelling heterogeneous environments such as those occurring in biological systems, where the symmetry of key interactions depends strongly on environment. To demonstrate the application of the model, we highlight the successful
construction of a transferable model of a water molecule. The model is parametrised using only the properties of a single
molecule and those of a dimer yet has excellent predictive power across the phase diagram, from high pressure ice to
231
supercritical water. To encourage the adoption of the method, we present its rst implementation in the general purpose
molecular dynamics software QDO_MD.
Acknowledgements
This work was supported by the NPL Strategic Research programme. FSC acknowledges the Scottish Doctoral Training
Centre in Condensed Matter Physics (grant number EP/G03673X/1), NPL and EPSRC for funding under an Industrial CASE
studentship. We acknowledge use of Hartree Centre resources in this work, including those from the Intel Parallel Computing Centre.
Appendix A. Coecients
For a quantum Drude oscillator of mass m, charge q and frequency
following values,
P () =
P () =
f =
2h sinh( f )
2m tanh( f /2)
h
P
(A.1)
1 = x1 ,
u
i = xi xi ,
u
xi =
sinh( h )
sinh[i h ]
x1 +
sinh((i 1) h )
sinh(i h )
(A.2)
x P +1 = x1
12 =
i2 =
xi +1 ,
2m tanh( h /2)
h sinh[(i 1) h ] sinh( h )
m sinh[i h ]
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