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Revision 3975 by kstocke1, Thu Nov 21 21:10:22 2013 UTC vs.
Revision 3977 by gezelter, Fri Nov 22 22:27:38 2013 UTC

# Line 79 | Line 79 | We have adapted the Velocity Shearing and Scaling Reve
79   %%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%
80   \section{Introduction}
81  
82 + Non-equilibrium Molecular Dynamics (NEMD) methods impose a temperature
83 + or velocity {\it gradient} on a
84 + system,\cite{ASHURST:1975tg,Evans:1982zk,ERPENBECK:1984sp,MAGINN:1993hc,Berthier:2002ij,Evans:2002ai,Schelling:2002dp,PhysRevA.34.1449,JiangHao_jp802942v}
85 + and use linear response theory to connect the resulting thermal or
86 + momentum flux to transport coefficients of bulk materials.  However,
87 + for heterogeneous systems, such as phase boundaries or interfaces, it
88 + is often unclear what shape of gradient should be imposed at the
89 + boundary between materials.
90  
91 + \begin{figure}
92 + \includegraphics[width=\linewidth]{VSS2}
93 + \caption{Schematics of periodic (left) and non-periodic (right)
94 +  Velocity Shearing and Scaling RNEMD. A kinetic energy or momentum
95 +  flux is applied from region B to region A. Thermal gradients are
96 +  depicted by a color gradient. Linear or angular velocity gradients
97 +  are shown as arrows.}
98 + \label{fig:VSS}
99 + \end{figure}
100 +
101 + Reverse Non-Equilibrium Molecular Dynamics (RNEMD) methods impose an
102 + unphysical {\it flux} between different regions or ``slabs'' of the
103 + simulation
104 + box.\cite{MullerPlathe:1997xw,ISI:000080382700030,Kuang:2010uq} The
105 + system responds by developing a temperature or velocity {\it gradient}
106 + between the two regions.  The gradients which develop in response to
107 + the applied flux are then related (via linear response theory) to the
108 + transport coefficient of interest. Since the amount of the applied
109 + flux is known exactly, and measurement of a gradient is generally less
110 + complicated, imposed-flux methods typically take shorter simulation
111 + times to obtain converged results. At interfaces, the observed
112 + gradients often exhibit near-discontinuities at the boundaries between
113 + dissimilar materials.  RNEMD methods do not need many trajectories to
114 + provide information about transport properties, and they have become
115 + widely used to compute thermal and mechanical transport in both
116 + homogeneous liquids and
117 + solids~\cite{MullerPlathe:1997xw,ISI:000080382700030,Maginn:2010} as
118 + well as heterogeneous
119 + interfaces.\cite{garde:nl2005,garde:PhysRevLett2009,kuang:AuThl}
120 +
121 +
122   %%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%
123   % **METHODOLOGY**
124   %%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%
125 < \section{Methodology}
125 > \section{Velocity Shearing and Scaling (VSS) for non-periodic systems}
126 > The VSS-RNEMD approach uses a series of simultaneous velocity shearing
127 > and scaling exchanges between the two slabs.\cite{2012MolPh.110..691K}
128 > This method imposes energy and momentum conservation constraints while
129 > simultaneously creating a desired flux between the two slabs.  These
130 > constraints ensure that all configurations are sampled from the same
131 > microcanonical (NVE) ensemble.
132  
133 + We have extended the VSS method for use in {\it non-periodic}
134 + simulations, in which the ``slabs'' have been generalized to two
135 + separated regions of space.  These regions could be defined as
136 + concentric spheres (as in figure \ref{fig:VSS}), or one of the regions
137 + can be defined in terms of a dynamically changing ``hull'' comprising
138 + the surface atoms of the cluster.  This latter definition is identical
139 + to the hull used in the Langevin Hull algorithm.
140 +
141 + We present here a new set of constraints that are more general than
142 + the VSS constraints.  For the non-periodic variant, the constraints
143 + fix both the total energy and total {\it angular} momentum of the
144 + system while simultaneously imposing a thermal and angular momentum
145 + flux between the two regions.
146 +
147 + After each $\Delta t$ time interval, the particle velocities
148 + ($\mathbf{v}_i$ and $\mathbf{v}_j$) in the two shells ($A$ and $B$)
149 + are modified by a velocity scaling coefficient ($a$ and $b$) and by a
150 + rotational shearing term ($\mathbf{c}_a$ and $\mathbf{c}_b$).
151 + \begin{displaymath}
152 + \begin{array}{rclcl}
153 + & \underline{~~~~~~~~\mathrm{scaling}~~~~~~~~} & &
154 + \underline{\mathrm{rotational~shearing}} \\  \\
155 + \mathbf{v}_i $~~~$\leftarrow &
156 +  a \left(\mathbf{v}_i - \langle \omega_a
157 +  \rangle \times \mathbf{r}_i\right) & + & \mathbf{c}_a \times \mathbf{r}_i \\
158 + \mathbf{v}_j $~~~$\leftarrow &
159 +  b  \left(\mathbf{v}_j - \langle \omega_b
160 +  \rangle \times \mathbf{r}_j\right) & + & \mathbf{c}_b \times \mathbf{r}_j
161 + \end{array}
162 + \end{displaymath}
163 + Here $\langle\mathbf{\omega}_a\rangle$ and
164 + $\langle\mathbf{\omega}_b\rangle$ are the instantaneous angular
165 + velocities of each shell, and $\mathbf{r}_i$ is the position of
166 + particle $i$ relative to a fixed point in space (usually the center of
167 + mass of the cluster).  Particles in the shells also receive an
168 + additive ``angular shear'' to their velocities.  The amount of shear
169 + is governed by the imposed angular momentum flux,
170 + $\mathbf{j}_r(\mathbf{L})$,
171 + \begin{eqnarray}
172 + \mathbf{c}_a & = & - \mathbf{j}_r(\mathbf{L}) \cdot
173 + \overleftrightarrow{I_a}^{-1} \Delta t   + \langle \omega_a \rangle \label{eq:bc}\\
174 + \mathbf{c}_b & = & + \mathbf{j}_r(\mathbf{L}) \cdot
175 + \overleftrightarrow{I_b}^{-1}  \Delta t  + \langle \omega_b \rangle \label{eq:bh}
176 + \end{eqnarray}
177 + where $\overleftrightarrow{I}_{\{a,b\}}$ is the moment of inertia tensor for
178 + each of the two shells.
179 +
180 + To simultaneously impose a thermal flux ($J_r$) between the shells we
181 + use energy conservation constraints,
182 + \begin{eqnarray}
183 + K_a - J_r \Delta t & = & a^2 \left(K_a - \frac{1}{2}\langle
184 + \omega_a \rangle \cdot \overleftrightarrow{I_a} \cdot \langle \omega_a
185 + \rangle \right) + \frac{1}{2} \mathbf{c}_a \cdot \overleftrightarrow{I_a}
186 + \cdot \mathbf{c}_a \label{eq:Kc}\\
187 + K_b + J_r \Delta t & = & b^2 \left(K_b - \frac{1}{2}\langle
188 + \omega_b \rangle \cdot \overleftrightarrow{I_b} \cdot \langle \omega_b
189 + \rangle \right) + \frac{1}{2} \mathbf{c}_b \cdot \overleftrightarrow{I_b} \cdot \mathbf{c}_b \label{eq:Kh}
190 + \end{eqnarray}
191 + Simultaneous solution of these quadratic formulae for the scaling
192 + coefficients, $a$ and $b$, will ensure that the simulation samples
193 + from the original microcanonical (NVE) ensemble.  Here $K_{\{a,b\}}$
194 + is the instantaneous translational kinetic energy of each shell.  At
195 + each time interval, we solve for $a$, $b$, $\mathbf{c}_a$, and
196 + $\mathbf{c}_b$, subject to the imposed angular momentum flux,
197 + $j_r(\mathbf{L})$, and thermal flux, $J_r$ values.  The new particle
198 + velocities are computed, and the simulation continues. System
199 + configurations after the transformations have exactly the same energy
200 + ({\it and} angular momentum) as before the moves.
201 +
202 + As the simulation progresses, the velocity transformations can be
203 + performed on a regular basis, and the system will develop a
204 + temperature and/or angular velocity gradient in response to the
205 + applied flux.  Using the slope of the radial temperature or velocity
206 + gradients, it is quite simple to obtain both the thermal conductivity
207 + ($\lambda$) and shear viscosity ($\eta$),
208 + \begin{equation}
209 +  J_r = -\lambda \frac{\partial T}{\partial
210 +    r} \hspace{2in} j_r(\mathbf{L}_z) = -\eta \frac{\partial
211 +    \omega_z}{\partial r}
212 + \end{equation}
213 + of a liquid cluster.
214 +
215   %%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%
216   % NON-PERIODIC DYNAMICS
217   %%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%

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