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# Line 6 | Line 6 | behind classical mechanics. Firstly, One can determine
6   Closely related to Classical Mechanics, Molecular Dynamics
7   simulations are carried out by integrating the equations of motion
8   for a given system of particles. There are three fundamental ideas
9 < behind classical mechanics. Firstly, One can determine the state of
9 > behind classical mechanics. Firstly, one can determine the state of
10   a mechanical system at any time of interest; Secondly, all the
11   mechanical properties of the system at that time can be determined
12   by combining the knowledge of the properties of the system with the
# Line 17 | Line 17 | Newton¡¯s first law defines a class of inertial frames
17   \subsection{\label{introSection:newtonian}Newtonian Mechanics}
18   The discovery of Newton's three laws of mechanics which govern the
19   motion of particles is the foundation of the classical mechanics.
20 < Newton¡¯s first law defines a class of inertial frames. Inertial
20 > Newton's first law defines a class of inertial frames. Inertial
21   frames are reference frames where a particle not interacting with
22   other bodies will move with constant speed in the same direction.
23 < With respect to inertial frames Newton¡¯s second law has the form
23 > With respect to inertial frames, Newton's second law has the form
24   \begin{equation}
25 < F = \frac {dp}{dt} = \frac {mv}{dt}
25 > F = \frac {dp}{dt} = \frac {mdv}{dt}
26   \label{introEquation:newtonSecondLaw}
27   \end{equation}
28   A point mass interacting with other bodies moves with the
29   acceleration along the direction of the force acting on it. Let
30   $F_{ij}$ be the force that particle $i$ exerts on particle $j$, and
31   $F_{ji}$ be the force that particle $j$ exerts on particle $i$.
32 < Newton¡¯s third law states that
32 > Newton's third law states that
33   \begin{equation}
34 < F_{ij} = -F_{ji}
34 > F_{ij} = -F_{ji}.
35   \label{introEquation:newtonThirdLaw}
36   \end{equation}
37
37   Conservation laws of Newtonian Mechanics play very important roles
38   in solving mechanics problems. The linear momentum of a particle is
39   conserved if it is free or it experiences no force. The second
# Line 46 | Line 45 | N \equiv r \times F \label{introEquation:torqueDefinit
45   \end{equation}
46   The torque $\tau$ with respect to the same origin is defined to be
47   \begin{equation}
48 < N \equiv r \times F \label{introEquation:torqueDefinition}
48 > \tau \equiv r \times F \label{introEquation:torqueDefinition}
49   \end{equation}
50   Differentiating Eq.~\ref{introEquation:angularMomentumDefinition},
51   \[
# Line 59 | Line 58 | thus,
58   \]
59   thus,
60   \begin{equation}
61 < \dot L = r \times \dot p = N
61 > \dot L = r \times \dot p = \tau
62   \end{equation}
63   If there are no external torques acting on a body, the angular
64   momentum of it is conserved. The last conservation theorem state
65 < that if all forces are conservative, Energy
66 < \begin{equation}E = T + V \label{introEquation:energyConservation}
65 > that if all forces are conservative, energy is conserved,
66 > \begin{equation}E = T + V. \label{introEquation:energyConservation}
67   \end{equation}
68 < is conserved. All of these conserved quantities are
69 < important factors to determine the quality of numerical integration
70 < scheme for rigid body \cite{Dullweber1997}.
68 > All of these conserved quantities are important factors to determine
69 > the quality of numerical integration schemes for rigid bodies
70 > \cite{Dullweber1997}.
71  
72   \subsection{\label{introSection:lagrangian}Lagrangian Mechanics}
73  
74 < Newtonian Mechanics suffers from two important limitations: it
75 < describes their motion in special cartesian coordinate systems.
76 < Another limitation of Newtonian mechanics becomes obvious when we
77 < try to describe systems with large numbers of particles. It becomes
78 < very difficult to predict the properties of the system by carrying
79 < out calculations involving the each individual interaction between
80 < all the particles, even if we know all of the details of the
82 < interaction. In order to overcome some of the practical difficulties
83 < which arise in attempts to apply Newton's equation to complex
84 < system, alternative procedures may be developed.
74 > Newtonian Mechanics suffers from two important limitations: motions
75 > can only be described in cartesian coordinate systems. Moreover, it
76 > becomes impossible to predict analytically the properties of the
77 > system even if we know all of the details of the interaction. In
78 > order to overcome some of the practical difficulties which arise in
79 > attempts to apply Newton's equation to complex system, approximate
80 > numerical procedures may be developed.
81  
82 < \subsubsection{\label{introSection:halmiltonPrinciple}Hamilton's
83 < Principle}
82 > \subsubsection{\label{introSection:halmiltonPrinciple}\textbf{Hamilton's
83 > Principle}}
84  
85   Hamilton introduced the dynamical principle upon which it is
86 < possible to base all of mechanics and, indeed, most of classical
87 < physics. Hamilton's Principle may be stated as follow,
88 <
89 < The actual trajectory, along which a dynamical system may move from
90 < one point to another within a specified time, is derived by finding
91 < the path which minimizes the time integral of the difference between
96 < the kinetic, $K$, and potential energies, $U$ \cite{tolman79}.
86 > possible to base all of mechanics and most of classical physics.
87 > Hamilton's Principle may be stated as follows: the actual
88 > trajectory, along which a dynamical system may move from one point
89 > to another within a specified time, is derived by finding the path
90 > which minimizes the time integral of the difference between the
91 > kinetic, $K$, and potential energies, $U$,
92   \begin{equation}
93 < \delta \int_{t_1 }^{t_2 } {(K - U)dt = 0} ,
93 > \delta \int_{t_1 }^{t_2 } {(K - U)dt = 0}.
94   \label{introEquation:halmitonianPrinciple1}
95   \end{equation}
101
96   For simple mechanical systems, where the forces acting on the
97 < different part are derivable from a potential and the velocities are
98 < small compared with that of light, the Lagrangian function $L$ can
99 < be define as the difference between the kinetic energy of the system
106 < and its potential energy,
97 > different parts are derivable from a potential, the Lagrangian
98 > function $L$ can be defined as the difference between the kinetic
99 > energy of the system and its potential energy,
100   \begin{equation}
101   L \equiv K - U = L(q_i ,\dot q_i ) ,
102   \label{introEquation:lagrangianDef}
# Line 114 | Line 107 | then Eq.~\ref{introEquation:halmitonianPrinciple1} bec
107   \label{introEquation:halmitonianPrinciple2}
108   \end{equation}
109  
110 < \subsubsection{\label{introSection:equationOfMotionLagrangian}The
111 < Equations of Motion in Lagrangian Mechanics}
110 > \subsubsection{\label{introSection:equationOfMotionLagrangian}\textbf{The
111 > Equations of Motion in Lagrangian Mechanics}}
112  
113 < For a holonomic system of $f$ degrees of freedom, the equations of
114 < motion in the Lagrangian form is
113 > For a system of $f$ degrees of freedom, the equations of motion in
114 > the Lagrangian form is
115   \begin{equation}
116   \frac{d}{{dt}}\frac{{\partial L}}{{\partial \dot q_i }} -
117   \frac{{\partial L}}{{\partial q_i }} = 0,{\rm{ }}i = 1, \ldots,f
# Line 132 | Line 125 | independent of generalized velocities, the generalized
125   Arising from Lagrangian Mechanics, Hamiltonian Mechanics was
126   introduced by William Rowan Hamilton in 1833 as a re-formulation of
127   classical mechanics. If the potential energy of a system is
128 < independent of generalized velocities, the generalized momenta can
136 < be defined as
128 > independent of velocities, the momenta can be defined as
129   \begin{equation}
130   p_i = \frac{\partial L}{\partial \dot q_i}
131   \label{introEquation:generalizedMomenta}
# Line 143 | Line 135 | p_i  = \frac{{\partial L}}{{\partial q_i }}
135   p_i  = \frac{{\partial L}}{{\partial q_i }}
136   \label{introEquation:generalizedMomentaDot}
137   \end{equation}
146
138   With the help of the generalized momenta, we may now define a new
139   quantity $H$ by the equation
140   \begin{equation}
# Line 151 | Line 142 | $L$ is the Lagrangian function for the system.
142   \label{introEquation:hamiltonianDefByLagrangian}
143   \end{equation}
144   where $ \dot q_1  \ldots \dot q_f $ are generalized velocities and
145 < $L$ is the Lagrangian function for the system.
146 <
156 < Differentiating Eq.~\ref{introEquation:hamiltonianDefByLagrangian},
157 < one can obtain
145 > $L$ is the Lagrangian function for the system. Differentiating
146 > Eq.~\ref{introEquation:hamiltonianDefByLagrangian}, one can obtain
147   \begin{equation}
148   dH = \sum\limits_k {\left( {p_k d\dot q_k  + \dot q_k dp_k  -
149   \frac{{\partial L}}{{\partial q_k }}dq_k  - \frac{{\partial
150   L}}{{\partial \dot q_k }}d\dot q_k } \right)}  - \frac{{\partial
151   L}}{{\partial t}}dt \label{introEquation:diffHamiltonian1}
152   \end{equation}
153 < Making use of  Eq.~\ref{introEquation:generalizedMomenta}, the
154 < second and fourth terms in the parentheses cancel. Therefore,
153 > Making use of Eq.~\ref{introEquation:generalizedMomenta}, the second
154 > and fourth terms in the parentheses cancel. Therefore,
155   Eq.~\ref{introEquation:diffHamiltonian1} can be rewritten as
156   \begin{equation}
157   dH = \sum\limits_k {\left( {\dot q_k dp_k  - \dot p_k dq_k }
# Line 172 | Line 161 | find
161   By identifying the coefficients of $dq_k$, $dp_k$ and dt, we can
162   find
163   \begin{equation}
164 < \frac{{\partial H}}{{\partial p_k }} = q_k
164 > \frac{{\partial H}}{{\partial p_k }} = \dot {q_k}
165   \label{introEquation:motionHamiltonianCoordinate}
166   \end{equation}
167   \begin{equation}
168 < \frac{{\partial H}}{{\partial q_k }} =  - p_k
168 > \frac{{\partial H}}{{\partial q_k }} =  - \dot {p_k}
169   \label{introEquation:motionHamiltonianMomentum}
170   \end{equation}
171   and
# Line 185 | Line 174 | t}}
174   t}}
175   \label{introEquation:motionHamiltonianTime}
176   \end{equation}
177 <
189 < Eq.~\ref{introEquation:motionHamiltonianCoordinate} and
177 > where Eq.~\ref{introEquation:motionHamiltonianCoordinate} and
178   Eq.~\ref{introEquation:motionHamiltonianMomentum} are Hamilton's
179   equation of motion. Due to their symmetrical formula, they are also
180 < known as the canonical equations of motions \cite{Goldstein01}.
180 > known as the canonical equations of motions \cite{Goldstein2001}.
181  
182   An important difference between Lagrangian approach and the
183   Hamiltonian approach is that the Lagrangian is considered to be a
184 < function of the generalized velocities $\dot q_i$ and the
185 < generalized coordinates $q_i$, while the Hamiltonian is considered
186 < to be a function of the generalized momenta $p_i$ and the conjugate
187 < generalized coordinate $q_i$. Hamiltonian Mechanics is more
188 < appropriate for application to statistical mechanics and quantum
189 < mechanics, since it treats the coordinate and its time derivative as
190 < independent variables and it only works with 1st-order differential
203 < equations\cite{Marion90}.
204 <
184 > function of the generalized velocities $\dot q_i$ and coordinates
185 > $q_i$, while the Hamiltonian is considered to be a function of the
186 > generalized momenta $p_i$ and the conjugate coordinates $q_i$.
187 > Hamiltonian Mechanics is more appropriate for application to
188 > statistical mechanics and quantum mechanics, since it treats the
189 > coordinate and its time derivative as independent variables and it
190 > only works with 1st-order differential equations\cite{Marion1990}.
191   In Newtonian Mechanics, a system described by conservative forces
192 < conserves the total energy \ref{introEquation:energyConservation}.
193 < It follows that Hamilton's equations of motion conserve the total
194 < Hamiltonian.
192 > conserves the total energy
193 > (Eq.~\ref{introEquation:energyConservation}). It follows that
194 > Hamilton's equations of motion conserve the total Hamiltonian.
195   \begin{equation}
196   \frac{{dH}}{{dt}} = \sum\limits_i {\left( {\frac{{\partial
197   H}}{{\partial q_i }}\dot q_i  + \frac{{\partial H}}{{\partial p_i
# Line 230 | Line 216 | momentum variables. Consider a dynamic system in a car
216   possible states. Each possible state of the system corresponds to
217   one unique point in the phase space. For mechanical systems, the
218   phase space usually consists of all possible values of position and
219 < momentum variables. Consider a dynamic system in a cartesian space,
220 < where each of the $6f$ coordinates and momenta is assigned to one of
221 < $6f$ mutually orthogonal axes, the phase space of this system is a
222 < $6f$ dimensional space. A point, $x = (q_1 , \ldots ,q_f ,p_1 ,
223 < \ldots ,p_f )$, with a unique set of values of $6f$ coordinates and
224 < momenta is a phase space vector.
219 > momentum variables. Consider a dynamic system of $f$ particles in a
220 > cartesian space, where each of the $6f$ coordinates and momenta is
221 > assigned to one of $6f$ mutually orthogonal axes, the phase space of
222 > this system is a $6f$ dimensional space. A point, $x = (\rightarrow
223 > q_1 , \ldots ,\rightarrow q_f ,\rightarrow p_1 , \ldots ,\rightarrow
224 > p_f )$, with a unique set of values of $6f$ coordinates and momenta
225 > is a phase space vector.
226 > %%%fix me
227  
228 < A microscopic state or microstate of a classical system is
241 < specification of the complete phase space vector of a system at any
242 < instant in time. An ensemble is defined as a collection of systems
243 < sharing one or more macroscopic characteristics but each being in a
244 < unique microstate. The complete ensemble is specified by giving all
245 < systems or microstates consistent with the common macroscopic
246 < characteristics of the ensemble. Although the state of each
247 < individual system in the ensemble could be precisely described at
248 < any instance in time by a suitable phase space vector, when using
249 < ensembles for statistical purposes, there is no need to maintain
250 < distinctions between individual systems, since the numbers of
251 < systems at any time in the different states which correspond to
252 < different regions of the phase space are more interesting. Moreover,
253 < in the point of view of statistical mechanics, one would prefer to
254 < use ensembles containing a large enough population of separate
255 < members so that the numbers of systems in such different states can
256 < be regarded as changing continuously as we traverse different
257 < regions of the phase space. The condition of an ensemble at any time
228 > In statistical mechanics, the condition of an ensemble at any time
229   can be regarded as appropriately specified by the density $\rho$
230   with which representative points are distributed over the phase
231 < space. The density of distribution for an ensemble with $f$ degrees
232 < of freedom is defined as,
231 > space. The density distribution for an ensemble with $f$ degrees of
232 > freedom is defined as,
233   \begin{equation}
234   \rho  = \rho (q_1 , \ldots ,q_f ,p_1 , \ldots ,p_f ,t).
235   \label{introEquation:densityDistribution}
236   \end{equation}
237   Governed by the principles of mechanics, the phase points change
238 < their value which would change the density at any time at phase
239 < space. Hence, the density of distribution is also to be taken as a
238 > their locations which would change the density at any time at phase
239 > space. Hence, the density distribution is also to be taken as a
240   function of the time.
241  
242   The number of systems $\delta N$ at time $t$ can be determined by,
# Line 273 | Line 244 | Assuming a large enough population of systems are expl
244   \delta N = \rho (q,p,t)dq_1  \ldots dq_f dp_1  \ldots dp_f.
245   \label{introEquation:deltaN}
246   \end{equation}
247 < Assuming a large enough population of systems are exploited, we can
248 < sufficiently approximate $\delta N$ without introducing
249 < discontinuity when we go from one region in the phase space to
250 < another. By integrating over the whole phase space,
247 > Assuming a large enough population of systems, we can sufficiently
248 > approximate $\delta N$ without introducing discontinuity when we go
249 > from one region in the phase space to another. By integrating over
250 > the whole phase space,
251   \begin{equation}
252   N = \int { \ldots \int {\rho (q,p,t)dq_1 } ...dq_f dp_1 } ...dp_f
253   \label{introEquation:totalNumberSystem}
# Line 288 | Line 259 | With the help of Equation(\ref{introEquation:unitProba
259   {\rho (q,p,t)dq_1 } ...dq_f dp_1 } ...dp_f }}.
260   \label{introEquation:unitProbability}
261   \end{equation}
262 < With the help of Equation(\ref{introEquation:unitProbability}) and
263 < the knowledge of the system, it is possible to calculate the average
262 > With the help of Eq.~\ref{introEquation:unitProbability} and the
263 > knowledge of the system, it is possible to calculate the average
264   value of any desired quantity which depends on the coordinates and
265   momenta of the system. Even when the dynamics of the real system is
266   complex, or stochastic, or even discontinuous, the average
267 < properties of the ensemble of possibilities as a whole may still
268 < remain well defined. For a classical system in thermal equilibrium
269 < with its environment, the ensemble average of a mechanical quantity,
270 < $\langle A(q , p) \rangle_t$, takes the form of an integral over the
271 < phase space of the system,
267 > properties of the ensemble of possibilities as a whole remaining
268 > well defined. For a classical system in thermal equilibrium with its
269 > environment, the ensemble average of a mechanical quantity, $\langle
270 > A(q , p) \rangle_t$, takes the form of an integral over the phase
271 > space of the system,
272   \begin{equation}
273   \langle  A(q , p) \rangle_t = \frac{{\int { \ldots \int {A(q,p)\rho
274   (q,p,t)dq_1 } ...dq_f dp_1 } ...dp_f }}{{\int { \ldots \int {\rho
# Line 307 | Line 278 | parameters, such as temperature \textit{etc}, partitio
278  
279   There are several different types of ensembles with different
280   statistical characteristics. As a function of macroscopic
281 < parameters, such as temperature \textit{etc}, partition function can
282 < be used to describe the statistical properties of a system in
283 < thermodynamic equilibrium.
284 <
285 < As an ensemble of systems, each of which is known to be thermally
315 < isolated and conserve energy, Microcanonical ensemble(NVE) has a
316 < partition function like,
281 > parameters, such as temperature \textit{etc}, the partition function
282 > can be used to describe the statistical properties of a system in
283 > thermodynamic equilibrium. As an ensemble of systems, each of which
284 > is known to be thermally isolated and conserve energy, the
285 > Microcanonical ensemble (NVE) has a partition function like,
286   \begin{equation}
287 < \Omega (N,V,E) = e^{\beta TS} \label{introEquation:NVEPartition}.
287 > \Omega (N,V,E) = e^{\beta TS}. \label{introEquation:NVEPartition}.
288   \end{equation}
289 < A canonical ensemble(NVT)is an ensemble of systems, each of which
289 > A canonical ensemble (NVT)is an ensemble of systems, each of which
290   can share its energy with a large heat reservoir. The distribution
291   of the total energy amongst the possible dynamical states is given
292   by the partition function,
293   \begin{equation}
294 < \Omega (N,V,T) = e^{ - \beta A}
294 > \Omega (N,V,T) = e^{ - \beta A}.
295   \label{introEquation:NVTPartition}
296   \end{equation}
297   Here, $A$ is the Helmholtz free energy which is defined as $ A = U -
298 < TS$. Since most experiment are carried out under constant pressure
299 < condition, isothermal-isobaric ensemble(NPT) play a very important
300 < role in molecular simulation. The isothermal-isobaric ensemble allow
301 < the system to exchange energy with a heat bath of temperature $T$
302 < and to change the volume as well. Its partition function is given as
298 > TS$. Since most experiments are carried out under constant pressure
299 > condition, the isothermal-isobaric ensemble (NPT) plays a very
300 > important role in molecular simulations. The isothermal-isobaric
301 > ensemble allow the system to exchange energy with a heat bath of
302 > temperature $T$ and to change the volume as well. Its partition
303 > function is given as
304   \begin{equation}
305   \Delta (N,P,T) =  - e^{\beta G}.
306   \label{introEquation:NPTPartition}
# Line 339 | Line 309 | The Liouville's theorem is the foundation on which sta
309  
310   \subsection{\label{introSection:liouville}Liouville's theorem}
311  
312 < The Liouville's theorem is the foundation on which statistical
313 < mechanics rests. It describes the time evolution of phase space
312 > Liouville's theorem is the foundation on which statistical mechanics
313 > rests. It describes the time evolution of the phase space
314   distribution function. In order to calculate the rate of change of
315 < $\rho$, we begin from Equation(\ref{introEquation:deltaN}). If we
316 < consider the two faces perpendicular to the $q_1$ axis, which are
317 < located at $q_1$ and $q_1 + \delta q_1$, the number of phase points
318 < leaving the opposite face is given by the expression,
315 > $\rho$, we begin from Eq.~\ref{introEquation:deltaN}. If we consider
316 > the two faces perpendicular to the $q_1$ axis, which are located at
317 > $q_1$ and $q_1 + \delta q_1$, the number of phase points leaving the
318 > opposite face is given by the expression,
319   \begin{equation}
320   \left( {\rho  + \frac{{\partial \rho }}{{\partial q_1 }}\delta q_1 }
321   \right)\left( {\dot q_1  + \frac{{\partial \dot q_1 }}{{\partial q_1
# Line 369 | Line 339 | divining $ \delta q_1  \ldots \delta q_f \delta p_1  \
339   + \frac{{\partial \dot p_i }}{{\partial p_i }}} \right)}  = 0 ,
340   \end{equation}
341   which cancels the first terms of the right hand side. Furthermore,
342 < divining $ \delta q_1  \ldots \delta q_f \delta p_1  \ldots \delta
342 > dividing $ \delta q_1  \ldots \delta q_f \delta p_1  \ldots \delta
343   p_f $ in both sides, we can write out Liouville's theorem in a
344   simple form,
345   \begin{equation}
# Line 378 | Line 348 | simple form,
348   \frac{{\partial \rho }}{{\partial p_i }}\dot p_i } \right)}  = 0 .
349   \label{introEquation:liouvilleTheorem}
350   \end{equation}
381
351   Liouville's theorem states that the distribution function is
352   constant along any trajectory in phase space. In classical
353 < statistical mechanics, since the number of particles in the system
354 < is huge, we may be able to believe the system is stationary,
353 > statistical mechanics, since the number of members in an ensemble is
354 > huge and constant, we can assume the local density has no reason
355 > (other than classical mechanics) to change,
356   \begin{equation}
357   \frac{{\partial \rho }}{{\partial t}} = 0.
358   \label{introEquation:stationary}
# Line 395 | Line 365 | distribution,
365   \label{introEquation:densityAndHamiltonian}
366   \end{equation}
367  
368 < \subsubsection{\label{introSection:phaseSpaceConservation}Conservation of Phase Space}
368 > \subsubsection{\label{introSection:phaseSpaceConservation}\textbf{Conservation of Phase Space}}
369   Lets consider a region in the phase space,
370   \begin{equation}
371   \delta v = \int { \ldots \int {dq_1 } ...dq_f dp_1 } ..dp_f .
372   \end{equation}
373   If this region is small enough, the density $\rho$ can be regarded
374 < as uniform over the whole phase space. Thus, the number of phase
375 < points inside this region is given by,
374 > as uniform over the whole integral. Thus, the number of phase points
375 > inside this region is given by,
376   \begin{equation}
377   \delta N = \rho \delta v = \rho \int { \ldots \int {dq_1 } ...dq_f
378   dp_1 } ..dp_f.
# Line 414 | Line 384 | With the help of stationary assumption
384   \end{equation}
385   With the help of stationary assumption
386   (\ref{introEquation:stationary}), we obtain the principle of the
387 < \emph{conservation of extension in phase space},
387 > \emph{conservation of volume in phase space},
388   \begin{equation}
389   \frac{d}{{dt}}(\delta v) = \frac{d}{{dt}}\int { \ldots \int {dq_1 }
390   ...dq_f dp_1 } ..dp_f  = 0.
391   \label{introEquation:volumePreserving}
392   \end{equation}
393  
394 < \subsubsection{\label{introSection:liouvilleInOtherForms}Liouville's Theorem in Other Forms}
394 > \subsubsection{\label{introSection:liouvilleInOtherForms}\textbf{Liouville's Theorem in Other Forms}}
395  
396   Liouville's theorem can be expresses in a variety of different forms
397   which are convenient within different contexts. For any two function
# Line 435 | Line 405 | Substituting equations of motion in Hamiltonian formal
405   \label{introEquation:poissonBracket}
406   \end{equation}
407   Substituting equations of motion in Hamiltonian formalism(
408 < \ref{introEquation:motionHamiltonianCoordinate} ,
409 < \ref{introEquation:motionHamiltonianMomentum} ) into
410 < (\ref{introEquation:liouvilleTheorem}), we can rewrite Liouville's
411 < theorem using Poisson bracket notion,
408 > Eq.~\ref{introEquation:motionHamiltonianCoordinate} ,
409 > Eq.~\ref{introEquation:motionHamiltonianMomentum} ) into
410 > (Eq.~\ref{introEquation:liouvilleTheorem}), we can rewrite
411 > Liouville's theorem using Poisson bracket notion,
412   \begin{equation}
413   \left( {\frac{{\partial \rho }}{{\partial t}}} \right) =  - \left\{
414   {\rho ,H} \right\}.
# Line 463 | Line 433 | simulation and the quality of the underlying model. Ho
433   Various thermodynamic properties can be calculated from Molecular
434   Dynamics simulation. By comparing experimental values with the
435   calculated properties, one can determine the accuracy of the
436 < simulation and the quality of the underlying model. However, both of
437 < experiment and computer simulation are usually performed during a
436 > simulation and the quality of the underlying model. However, both
437 > experiments and computer simulations are usually performed during a
438   certain time interval and the measurements are averaged over a
439   period of them which is different from the average behavior of
440 < many-body system in Statistical Mechanics. Fortunately, Ergodic
441 < Hypothesis is proposed to make a connection between time average and
442 < ensemble average. It states that time average and average over the
443 < statistical ensemble are identical \cite{Frenkel1996, leach01:mm}.
440 > many-body system in Statistical Mechanics. Fortunately, the Ergodic
441 > Hypothesis makes a connection between time average and the ensemble
442 > average. It states that the time average and average over the
443 > statistical ensemble are identical \cite{Frenkel1996, Leach2001}.
444   \begin{equation}
445   \langle A(q , p) \rangle_t = \mathop {\lim }\limits_{t \to \infty }
446   \frac{1}{t}\int\limits_0^t {A(q(t),p(t))dt = \int\limits_\Gamma
# Line 484 | Line 454 | reasonable, the Monte Carlo techniques\cite{metropolis
454   a properly weighted statistical average. This allows the researcher
455   freedom of choice when deciding how best to measure a given
456   observable. In case an ensemble averaged approach sounds most
457 < reasonable, the Monte Carlo techniques\cite{metropolis:1949} can be
457 > reasonable, the Monte Carlo techniques\cite{Metropolis1949} can be
458   utilized. Or if the system lends itself to a time averaging
459   approach, the Molecular Dynamics techniques in
460   Sec.~\ref{introSection:molecularDynamics} will be the best
461   choice\cite{Frenkel1996}.
462  
463   \section{\label{introSection:geometricIntegratos}Geometric Integrators}
464 < A variety of numerical integrators were proposed to simulate the
465 < motions. They usually begin with an initial conditionals and move
466 < the objects in the direction governed by the differential equations.
467 < However, most of them ignore the hidden physical law contained
468 < within the equations. Since 1990, geometric integrators, which
469 < preserve various phase-flow invariants such as symplectic structure,
470 < volume and time reversal symmetry, are developed to address this
471 < issue. The velocity verlet method, which happens to be a simple
472 < example of symplectic integrator, continues to gain its popularity
473 < in molecular dynamics community. This fact can be partly explained
474 < by its geometric nature.
464 > A variety of numerical integrators have been proposed to simulate
465 > the motions of atoms in MD simulation. They usually begin with
466 > initial conditionals and move the objects in the direction governed
467 > by the differential equations. However, most of them ignore the
468 > hidden physical laws contained within the equations. Since 1990,
469 > geometric integrators, which preserve various phase-flow invariants
470 > such as symplectic structure, volume and time reversal symmetry, are
471 > developed to address this issue\cite{Dullweber1997, McLachlan1998,
472 > Leimkuhler1999}. The velocity Verlet method, which happens to be a
473 > simple example of symplectic integrator, continues to gain
474 > popularity in the molecular dynamics community. This fact can be
475 > partly explained by its geometric nature.
476  
477 < \subsection{\label{introSection:symplecticManifold}Symplectic Manifold}
478 < A \emph{manifold} is an abstract mathematical space. It locally
479 < looks like Euclidean space, but when viewed globally, it may have
480 < more complicate structure. A good example of manifold is the surface
481 < of Earth. It seems to be flat locally, but it is round if viewed as
482 < a whole. A \emph{differentiable manifold} (also known as
483 < \emph{smooth manifold}) is a manifold with an open cover in which
484 < the covering neighborhoods are all smoothly isomorphic to one
485 < another. In other words,it is possible to apply calculus on
515 < \emph{differentiable manifold}. A \emph{symplectic manifold} is
516 < defined as a pair $(M, \omega)$ which consisting of a
477 > \subsection{\label{introSection:symplecticManifold}Symplectic Manifolds}
478 > A \emph{manifold} is an abstract mathematical space. It looks
479 > locally like Euclidean space, but when viewed globally, it may have
480 > more complicated structure. A good example of manifold is the
481 > surface of Earth. It seems to be flat locally, but it is round if
482 > viewed as a whole. A \emph{differentiable manifold} (also known as
483 > \emph{smooth manifold}) is a manifold on which it is possible to
484 > apply calculus on \emph{differentiable manifold}. A \emph{symplectic
485 > manifold} is defined as a pair $(M, \omega)$ which consists of a
486   \emph{differentiable manifold} $M$ and a close, non-degenerated,
487   bilinear symplectic form, $\omega$. A symplectic form on a vector
488   space $V$ is a function $\omega(x, y)$ which satisfies
489   $\omega(\lambda_1x_1+\lambda_2x_2, y) = \lambda_1\omega(x_1, y)+
490   \lambda_2\omega(x_2, y)$, $\omega(x, y) = - \omega(y, x)$ and
491 < $\omega(x, x) = 0$. Cross product operation in vector field is an
492 < example of symplectic form.
491 > $\omega(x, x) = 0$. The cross product operation in vector field is
492 > an example of symplectic form. One of the motivations to study
493 > \emph{symplectic manifolds} in Hamiltonian Mechanics is that a
494 > symplectic manifold can represent all possible configurations of the
495 > system and the phase space of the system can be described by it's
496 > cotangent bundle. Every symplectic manifold is even dimensional. For
497 > instance, in Hamilton equations, coordinate and momentum always
498 > appear in pairs.
499  
525 One of the motivations to study \emph{symplectic manifold} in
526 Hamiltonian Mechanics is that a symplectic manifold can represent
527 all possible configurations of the system and the phase space of the
528 system can be described by it's cotangent bundle. Every symplectic
529 manifold is even dimensional. For instance, in Hamilton equations,
530 coordinate and momentum always appear in pairs.
531
532 Let  $(M,\omega)$ and $(N, \eta)$ be symplectic manifolds. A map
533 \[
534 f : M \rightarrow N
535 \]
536 is a \emph{symplectomorphism} if it is a \emph{diffeomorphims} and
537 the \emph{pullback} of $\eta$ under f is equal to $\omega$.
538 Canonical transformation is an example of symplectomorphism in
539 classical mechanics.
540
500   \subsection{\label{introSection:ODE}Ordinary Differential Equations}
501  
502 < For a ordinary differential system defined as
502 > For an ordinary differential system defined as
503   \begin{equation}
504   \dot x = f(x)
505   \end{equation}
506 < where $x = x(q,p)^T$, this system is canonical Hamiltonian, if
506 > where $x = x(q,p)^T$, this system is a canonical Hamiltonian, if
507   \begin{equation}
508   f(r) = J\nabla _x H(r).
509   \end{equation}
# Line 563 | Line 522 | called a \emph{Hamiltonian vector field}.
522   \frac{d}{{dt}}x = J\nabla _x H(x)
523   \label{introEquation:compactHamiltonian}
524   \end{equation}In this case, $f$ is
525 < called a \emph{Hamiltonian vector field}.
526 <
568 < Another generalization of Hamiltonian dynamics is Poisson Dynamics,
525 > called a \emph{Hamiltonian vector field}. Another generalization of
526 > Hamiltonian dynamics is Poisson Dynamics\cite{Olver1986},
527   \begin{equation}
528   \dot x = J(x)\nabla _x H \label{introEquation:poissonHamiltonian}
529   \end{equation}
# Line 603 | Line 561 | Instead, we use a approximate map, $\psi_\tau$, which
561   \end{equation}
562  
563   In most cases, it is not easy to find the exact flow $\varphi_\tau$.
564 < Instead, we use a approximate map, $\psi_\tau$, which is usually
564 > Instead, we use an approximate map, $\psi_\tau$, which is usually
565   called integrator. The order of an integrator $\psi_\tau$ is $p$, if
566   the Taylor series of $\psi_\tau$ agree to order $p$,
567   \begin{equation}
568 < \psi_tau(x) = x + \tau f(x) + O(\tau^{p+1})
568 > \psi_\tau(x) = x + \tau f(x) + O(\tau^{p+1})
569   \end{equation}
570  
571   \subsection{\label{introSection:geometricProperties}Geometric Properties}
572  
573 < The hidden geometric properties of ODE and its flow play important
574 < roles in numerical studies. Many of them can be found in systems
575 < which occur naturally in applications.
618 <
573 > The hidden geometric properties\cite{Budd1999, Marsden1998} of an
574 > ODE and its flow play important roles in numerical studies. Many of
575 > them can be found in systems which occur naturally in applications.
576   Let $\varphi$ be the flow of Hamiltonian vector field, $\varphi$ is
577   a \emph{symplectic} flow if it satisfies,
578   \begin{equation}
# Line 629 | Line 586 | is the property must be preserved by the integrator.
586   \begin{equation}
587   {\varphi '}^T J \varphi ' = J \circ \varphi
588   \end{equation}
589 < is the property must be preserved by the integrator.
590 <
591 < It is possible to construct a \emph{volume-preserving} flow for a
592 < source free($ \nabla \cdot f = 0 $) ODE, if the flow satisfies $
593 < \det d\varphi  = 1$. One can show easily that a symplectic flow will
594 < be volume-preserving.
638 <
639 < Changing the variables $y = h(x)$ in a ODE\ref{introEquation:ODE}
640 < will result in a new system,
589 > is the property that must be preserved by the integrator. It is
590 > possible to construct a \emph{volume-preserving} flow for a source
591 > free ODE ($ \nabla \cdot f = 0 $), if the flow satisfies $ \det
592 > d\varphi  = 1$. One can show easily that a symplectic flow will be
593 > volume-preserving. Changing the variables $y = h(x)$ in an ODE
594 > (Eq.~\ref{introEquation:ODE}) will result in a new system,
595   \[
596   \dot y = \tilde f(y) = ((dh \cdot f)h^{ - 1} )(y).
597   \]
598   The vector filed $f$ has reversing symmetry $h$ if $f = - \tilde f$.
599   In other words, the flow of this vector field is reversible if and
600 < only if $ h \circ \varphi ^{ - 1}  = \varphi  \circ h $.
601 <
648 < A \emph{first integral}, or conserved quantity of a general
600 > only if $ h \circ \varphi ^{ - 1}  = \varphi  \circ h $. A
601 > \emph{first integral}, or conserved quantity of a general
602   differential function is a function $ G:R^{2d}  \to R^d $ which is
603   constant for all solutions of the ODE $\frac{{dx}}{{dt}} = f(x)$ ,
604   \[
# Line 658 | Line 611 | smooth function $G$ is given by,
611   which is the condition for conserving \emph{first integral}. For a
612   canonical Hamiltonian system, the time evolution of an arbitrary
613   smooth function $G$ is given by,
614 < \begin{equation}
615 < \begin{array}{c}
616 < \frac{{dG(x(t))}}{{dt}} = [\nabla _x G(x(t))]^T \dot x(t) \\
664 <  = [\nabla _x G(x(t))]^T J\nabla _x H(x(t)). \\
665 < \end{array}
614 > \begin{eqnarray}
615 > \frac{{dG(x(t))}}{{dt}} & = & [\nabla _x G(x(t))]^T \dot x(t) \\
616 >                        & = & [\nabla _x G(x(t))]^T J\nabla _x H(x(t)). \\
617   \label{introEquation:firstIntegral1}
618 < \end{equation}
618 > \end{eqnarray}
619   Using poisson bracket notion, Equation
620   \ref{introEquation:firstIntegral1} can be rewritten as
621   \[
# Line 677 | Line 628 | is a \emph{first integral}, which is due to the fact $
628   \]
629   As well known, the Hamiltonian (or energy) H of a Hamiltonian system
630   is a \emph{first integral}, which is due to the fact $\{ H,H\}  =
631 < 0$.
681 <
682 <
683 < When designing any numerical methods, one should always try to
631 > 0$. When designing any numerical methods, one should always try to
632   preserve the structural properties of the original ODE and its flow.
633  
634   \subsection{\label{introSection:constructionSymplectic}Construction of Symplectic Methods}
635   A lot of well established and very effective numerical methods have
636   been successful precisely because of their symplecticities even
637   though this fact was not recognized when they were first
638 < constructed. The most famous example is leapfrog methods in
639 < molecular dynamics. In general, symplectic integrators can be
638 > constructed. The most famous example is the Verlet-leapfrog method
639 > in molecular dynamics. In general, symplectic integrators can be
640   constructed using one of four different methods.
641   \begin{enumerate}
642   \item Generating functions
# Line 697 | Line 645 | Generating function tends to lead to methods which are
645   \item Splitting methods
646   \end{enumerate}
647  
648 < Generating function tends to lead to methods which are cumbersome
649 < and difficult to use. In dissipative systems, variational methods
650 < can capture the decay of energy accurately. Since their
651 < geometrically unstable nature against non-Hamiltonian perturbations,
652 < ordinary implicit Runge-Kutta methods are not suitable for
653 < Hamiltonian system. Recently, various high-order explicit
654 < Runge--Kutta methods have been developed to overcome this
648 > Generating function\cite{Channell1990} tends to lead to methods
649 > which are cumbersome and difficult to use. In dissipative systems,
650 > variational methods can capture the decay of energy
651 > accurately\cite{Kane2000}. Since their geometrically unstable nature
652 > against non-Hamiltonian perturbations, ordinary implicit Runge-Kutta
653 > methods are not suitable for Hamiltonian system. Recently, various
654 > high-order explicit Runge-Kutta methods
655 > \cite{Owren1992,Chen2003}have been developed to overcome this
656   instability. However, due to computational penalty involved in
657 < implementing the Runge-Kutta methods, they do not attract too much
658 < attention from Molecular Dynamics community. Instead, splitting have
659 < been widely accepted since they exploit natural decompositions of
660 < the system\cite{Tuckerman92}.
657 > implementing the Runge-Kutta methods, they have not attracted much
658 > attention from the Molecular Dynamics community. Instead, splitting
659 > methods have been widely accepted since they exploit natural
660 > decompositions of the system\cite{Tuckerman1992, McLachlan1998}.
661  
662 < \subsubsection{\label{introSection:splittingMethod}Splitting Method}
662 > \subsubsection{\label{introSection:splittingMethod}\textbf{Splitting Methods}}
663  
664   The main idea behind splitting methods is to decompose the discrete
665   $\varphi_h$ as a composition of simpler flows,
# Line 720 | Line 669 | simpler integration of the system.
669   \label{introEquation:FlowDecomposition}
670   \end{equation}
671   where each of the sub-flow is chosen such that each represent a
672 < simpler integration of the system.
673 <
725 < Suppose that a Hamiltonian system takes the form,
672 > simpler integration of the system. Suppose that a Hamiltonian system
673 > takes the form,
674   \[
675   H = H_1 + H_2.
676   \]
# Line 731 | Line 679 | order is then given by the Lie-Trotter formula
679   energy respectively, which is a natural decomposition of the
680   problem. If $H_1$ and $H_2$ can be integrated using exact flows
681   $\varphi_1(t)$ and $\varphi_2(t)$, respectively, a simple first
682 < order is then given by the Lie-Trotter formula
682 > order expression is then given by the Lie-Trotter formula
683   \begin{equation}
684   \varphi _h  = \varphi _{1,h}  \circ \varphi _{2,h},
685   \label{introEquation:firstOrderSplitting}
# Line 757 | Line 705 | which has a local error proportional to $h^3$. Sprang
705   \varphi _h  = \varphi _{1,h/2}  \circ \varphi _{2,h}  \circ \varphi
706   _{1,h/2} , \label{introEquation:secondOrderSplitting}
707   \end{equation}
708 < which has a local error proportional to $h^3$. Sprang splitting's
709 < popularity in molecular simulation community attribute to its
710 < symmetric property,
708 > which has a local error proportional to $h^3$. The Sprang
709 > splitting's popularity in molecular simulation community attribute
710 > to its symmetric property,
711   \begin{equation}
712   \varphi _h^{ - 1} = \varphi _{ - h}.
713   \label{introEquation:timeReversible}
714   \end{equation}
715  
716 < \subsubsection{\label{introSection:exampleSplittingMethod}Example of Splitting Method}
716 > \subsubsection{\label{introSection:exampleSplittingMethod}\textbf{Examples of the Splitting Method}}
717   The classical equation for a system consisting of interacting
718   particles can be written in Hamiltonian form,
719   \[
720   H = T + V
721   \]
722   where $T$ is the kinetic energy and $V$ is the potential energy.
723 < Setting $H_1 = T, H_2 = V$ and applying Strang splitting, one
723 > Setting $H_1 = T, H_2 = V$ and applying the Strang splitting, one
724   obtains the following:
725   \begin{align}
726   q(\Delta t) &= q(0) + \dot{q}(0)\Delta t +
# Line 799 | Line 747 | q(\Delta t) &= q(0) + \Delta t\, \dot{q}\biggl (\frac{
747      \label{introEquation:Lp9b}\\%
748   %
749   \dot{q}(\Delta t) &= \dot{q}\biggl (\frac{\Delta t}{2}\biggr ) +
750 <    \frac{\Delta t}{2m}\, F[q(0)]. \label{introEquation:Lp9c}
750 >    \frac{\Delta t}{2m}\, F[q(t)]. \label{introEquation:Lp9c}
751   \end{align}
752   From the preceding splitting, one can see that the integration of
753   the equations of motion would follow:
# Line 808 | Line 756 | the equations of motion would follow:
756  
757   \item Use the half step velocities to move positions one whole step, $\Delta t$.
758  
759 < \item Evaluate the forces at the new positions, $\mathbf{r}(\Delta t)$, and use the new forces to complete the velocity move.
759 > \item Evaluate the forces at the new positions, $\mathbf{q}(\Delta t)$, and use the new forces to complete the velocity move.
760  
761   \item Repeat from step 1 with the new position, velocities, and forces assuming the roles of the initial values.
762   \end{enumerate}
763 <
764 < Simply switching the order of splitting and composing, a new
765 < integrator, the \emph{position verlet} integrator, can be generated,
763 > By simply switching the order of the propagators in the splitting
764 > and composing a new integrator, the \emph{position verlet}
765 > integrator, can be generated,
766   \begin{align}
767   \dot q(\Delta t) &= \dot q(0) + \Delta tF(q(0))\left[ {q(0) +
768   \frac{{\Delta t}}{{2m}}\dot q(0)} \right], %
# Line 825 | Line 773 | q(\Delta t)} \right]. %
773   \label{introEquation:positionVerlet2}
774   \end{align}
775  
776 < \subsubsection{\label{introSection:errorAnalysis}Error Analysis and Higher Order Methods}
776 > \subsubsection{\label{introSection:errorAnalysis}\textbf{Error Analysis and Higher Order Methods}}
777  
778 < Baker-Campbell-Hausdorff formula can be used to determine the local
779 < error of splitting method in terms of commutator of the
778 > The Baker-Campbell-Hausdorff formula can be used to determine the
779 > local error of splitting method in terms of the commutator of the
780   operators(\ref{introEquation:exponentialOperator}) associated with
781 < the sub-flow. For operators $hX$ and $hY$ which are associate to
782 < $\varphi_1(t)$ and $\varphi_2(t$ respectively , we have
781 > the sub-flow. For operators $hX$ and $hY$ which are associated with
782 > $\varphi_1(t)$ and $\varphi_2(t)$ respectively , we have
783   \begin{equation}
784   \exp (hX + hY) = \exp (hZ)
785   \end{equation}
# Line 844 | Line 792 | Applying Baker-Campbell-Hausdorff formula to Sprang sp
792   \[
793   [X,Y] = XY - YX .
794   \]
795 < Applying Baker-Campbell-Hausdorff formula to Sprang splitting, we
796 < can obtain
795 > Applying the Baker-Campbell-Hausdorff formula\cite{Varadarajan1974}
796 > to the Sprang splitting, we can obtain
797   \begin{eqnarray*}
798 < \exp (h X/2)\exp (h Y)\exp (h X/2) & = & \exp (h X + h Y + h^2
799 < [X,Y]/4 + h^2 [Y,X]/4 \\ & & \mbox{} + h^2 [X,X]/8 + h^2 [Y,Y]/8 \\
800 < & & \mbox{} + h^3 [Y,[Y,X]]/12 - h^3 [X,[X,Y]]/24 & & \mbox{} +
853 < \ldots )
798 > \exp (h X/2)\exp (h Y)\exp (h X/2) & = & \exp (h X + h Y + h^2 [X,Y]/4 + h^2 [Y,X]/4 \\
799 >                                   &   & \mbox{} + h^2 [X,X]/8 + h^2 [Y,Y]/8 \\
800 >                                   &   & \mbox{} + h^3 [Y,[Y,X]]/12 - h^3[X,[X,Y]]/24 + \ldots )
801   \end{eqnarray*}
802 < Since \[ [X,Y] + [Y,X] = 0\] and \[ [X,X] = 0\], the dominant local
802 > Since \[ [X,Y] + [Y,X] = 0\] and \[ [X,X] = 0,\] the dominant local
803   error of Spring splitting is proportional to $h^3$. The same
804 < procedure can be applied to general splitting,  of the form
804 > procedure can be applied to a general splitting,  of the form
805   \begin{equation}
806   \varphi _{b_m h}^2  \circ \varphi _{a_m h}^1  \circ \varphi _{b_{m -
807   1} h}^2  \circ  \ldots  \circ \varphi _{a_1 h}^1 .
808   \end{equation}
809 < Careful choice of coefficient $a_1 ,\ldot , b_m$ will lead to higher
810 < order method. Yoshida proposed an elegant way to compose higher
811 < order methods based on symmetric splitting. Given a symmetric second
812 < order base method $ \varphi _h^{(2)} $, a fourth-order symmetric
813 < method can be constructed by composing,
809 > A careful choice of coefficient $a_1 \ldots b_m$ will lead to higher
810 > order methods. Yoshida proposed an elegant way to compose higher
811 > order methods based on symmetric splitting\cite{Yoshida1990}. Given
812 > a symmetric second order base method $ \varphi _h^{(2)} $, a
813 > fourth-order symmetric method can be constructed by composing,
814   \[
815   \varphi _h^{(4)}  = \varphi _{\alpha h}^{(2)}  \circ \varphi _{\beta
816   h}^{(2)}  \circ \varphi _{\alpha h}^{(2)}
# Line 873 | Line 820 | _{\beta h}^{(2n)}  \circ \varphi _{\alpha h}^{(2n)}
820   integrator $ \varphi _h^{(2n + 2)}$ can be composed by
821   \begin{equation}
822   \varphi _h^{(2n + 2)}  = \varphi _{\alpha h}^{(2n)}  \circ \varphi
823 < _{\beta h}^{(2n)}  \circ \varphi _{\alpha h}^{(2n)}
823 > _{\beta h}^{(2n)}  \circ \varphi _{\alpha h}^{(2n)},
824   \end{equation}
825 < , if the weights are chosen as
825 > if the weights are chosen as
826   \[
827   \alpha  =  - \frac{{2^{1/(2n + 1)} }}{{2 - 2^{1/(2n + 1)} }},\beta =
828   \frac{{2^{1/(2n + 1)} }}{{2 - 2^{1/(2n + 1)} }} .
# Line 912 | Line 859 | initialization of a simulation. Sec.~\ref{introSec:pro
859   \end{enumerate}
860   These three individual steps will be covered in the following
861   sections. Sec.~\ref{introSec:initialSystemSettings} deals with the
862 < initialization of a simulation. Sec.~\ref{introSec:production} will
863 < discusses issues in production run. Sec.~\ref{introSection:Analysis}
864 < provides the theoretical tools for trajectory analysis.
862 > initialization of a simulation. Sec.~\ref{introSection:production}
863 > will discusse issues in production run.
864 > Sec.~\ref{introSection:Analysis} provides the theoretical tools for
865 > trajectory analysis.
866  
867   \subsection{\label{introSec:initialSystemSettings}Initialization}
868  
869 < \subsubsection{Preliminary preparation}
869 > \subsubsection{\textbf{Preliminary preparation}}
870  
871   When selecting the starting structure of a molecule for molecular
872   simulation, one may retrieve its Cartesian coordinates from public
873   databases, such as RCSB Protein Data Bank \textit{etc}. Although
874   thousands of crystal structures of molecules are discovered every
875   year, many more remain unknown due to the difficulties of
876 < purification and crystallization. Even for the molecule with known
877 < structure, some important information is missing. For example, the
876 > purification and crystallization. Even for molecules with known
877 > structure, some important information is missing. For example, a
878   missing hydrogen atom which acts as donor in hydrogen bonding must
879   be added. Moreover, in order to include electrostatic interaction,
880   one may need to specify the partial charges for individual atoms.
881   Under some circumstances, we may even need to prepare the system in
882 < a special setup. For instance, when studying transport phenomenon in
883 < membrane system, we may prepare the lipids in bilayer structure
884 < instead of placing lipids randomly in solvent, since we are not
885 < interested in self-aggregation and it takes a long time to happen.
882 > a special configuration. For instance, when studying transport
883 > phenomenon in membrane systems, we may prepare the lipids in a
884 > bilayer structure instead of placing lipids randomly in solvent,
885 > since we are not interested in the slow self-aggregation process.
886  
887 < \subsubsection{Minimization}
887 > \subsubsection{\textbf{Minimization}}
888  
889   It is quite possible that some of molecules in the system from
890 < preliminary preparation may be overlapped with each other. This
891 < close proximity leads to high potential energy which consequently
892 < jeopardizes any molecular dynamics simulations. To remove these
893 < steric overlaps, one typically performs energy minimization to find
894 < a more reasonable conformation. Several energy minimization methods
895 < have been developed to exploit the energy surface and to locate the
896 < local minimum. While converging slowly near the minimum, steepest
897 < descent method is extremely robust when systems are far from
898 < harmonic. Thus, it is often used to refine structure from
899 < crystallographic data. Relied on the gradient or hessian, advanced
900 < methods like conjugate gradient and Newton-Raphson converge rapidly
901 < to a local minimum, while become unstable if the energy surface is
902 < far from quadratic. Another factor must be taken into account, when
890 > preliminary preparation may be overlapping with each other. This
891 > close proximity leads to high initial potential energy which
892 > consequently jeopardizes any molecular dynamics simulations. To
893 > remove these steric overlaps, one typically performs energy
894 > minimization to find a more reasonable conformation. Several energy
895 > minimization methods have been developed to exploit the energy
896 > surface and to locate the local minimum. While converging slowly
897 > near the minimum, steepest descent method is extremely robust when
898 > systems are strongly anharmonic. Thus, it is often used to refine
899 > structure from crystallographic data. Relied on the gradient or
900 > hessian, advanced methods like Newton-Raphson converge rapidly to a
901 > local minimum, but become unstable if the energy surface is far from
902 > quadratic. Another factor that must be taken into account, when
903   choosing energy minimization method, is the size of the system.
904   Steepest descent and conjugate gradient can deal with models of any
905 < size. Because of the limit of computation power to calculate hessian
906 < matrix and insufficient storage capacity to store them, most
907 < Newton-Raphson methods can not be used with very large models.
905 > size. Because of the limits on computer memory to store the hessian
906 > matrix and the computing power needed to diagonalized these
907 > matrices, most Newton-Raphson methods can not be used with very
908 > large systems.
909  
910 < \subsubsection{Heating}
910 > \subsubsection{\textbf{Heating}}
911  
912   Typically, Heating is performed by assigning random velocities
913 < according to a Gaussian distribution for a temperature. Beginning at
914 < a lower temperature and gradually increasing the temperature by
915 < assigning greater random velocities, we end up with setting the
916 < temperature of the system to a final temperature at which the
917 < simulation will be conducted. In heating phase, we should also keep
918 < the system from drifting or rotating as a whole. Equivalently, the
919 < net linear momentum and angular momentum of the system should be
920 < shifted to zero.
913 > according to a Maxwell-Boltzman distribution for a desired
914 > temperature. Beginning at a lower temperature and gradually
915 > increasing the temperature by assigning larger random velocities, we
916 > end up with setting the temperature of the system to a final
917 > temperature at which the simulation will be conducted. In heating
918 > phase, we should also keep the system from drifting or rotating as a
919 > whole. To do this, the net linear momentum and angular momentum of
920 > the system is shifted to zero after each resampling from the Maxwell
921 > -Boltzman distribution.
922  
923 < \subsubsection{Equilibration}
923 > \subsubsection{\textbf{Equilibration}}
924  
925   The purpose of equilibration is to allow the system to evolve
926   spontaneously for a period of time and reach equilibrium. The
# Line 984 | Line 934 | Production run is the most important steps of the simu
934  
935   \subsection{\label{introSection:production}Production}
936  
937 < Production run is the most important steps of the simulation, in
937 > The production run is the most important step of the simulation, in
938   which the equilibrated structure is used as a starting point and the
939   motions of the molecules are collected for later analysis. In order
940   to capture the macroscopic properties of the system, the molecular
941 < dynamics simulation must be performed in correct and efficient way.
941 > dynamics simulation must be performed by sampling correctly and
942 > efficiently from the relevant thermodynamic ensemble.
943  
944   The most expensive part of a molecular dynamics simulation is the
945   calculation of non-bonded forces, such as van der Waals force and
946   Coulombic forces \textit{etc}. For a system of $N$ particles, the
947   complexity of the algorithm for pair-wise interactions is $O(N^2 )$,
948   which making large simulations prohibitive in the absence of any
949 < computation saving techniques.
949 > algorithmic tricks.
950  
951 < A natural approach to avoid system size issue is to represent the
951 > A natural approach to avoid system size issues is to represent the
952   bulk behavior by a finite number of the particles. However, this
953 < approach will suffer from the surface effect. To offset this,
954 < \textit{Periodic boundary condition} is developed to simulate bulk
953 > approach will suffer from the surface effect at the edges of the
954 > simulation. To offset this, \textit{Periodic boundary conditions}
955 > (see Fig.~\ref{introFig:pbc}) is developed to simulate bulk
956   properties with a relatively small number of particles. In this
957   method, the simulation box is replicated throughout space to form an
958   infinite lattice. During the simulation, when a particle moves in
# Line 1008 | Line 960 | opposite face.
960   direction with exactly the same orientation. Thus, as a particle
961   leaves the primary cell, one of its images will enter through the
962   opposite face.
963 < %\begin{figure}
964 < %\centering
965 < %\includegraphics[width=\linewidth]{pbcFig.eps}
966 < %\caption[An illustration of periodic boundary conditions]{A 2-D
967 < %illustration of periodic boundary conditions. As one particle leaves
968 < %the right of the simulation box, an image of it enters the left.}
969 < %\label{introFig:pbc}
970 < %\end{figure}
963 > \begin{figure}
964 > \centering
965 > \includegraphics[width=\linewidth]{pbc.eps}
966 > \caption[An illustration of periodic boundary conditions]{A 2-D
967 > illustration of periodic boundary conditions. As one particle leaves
968 > the left of the simulation box, an image of it enters the right.}
969 > \label{introFig:pbc}
970 > \end{figure}
971  
972   %cutoff and minimum image convention
973   Another important technique to improve the efficiency of force
974 < evaluation is to apply cutoff where particles farther than a
975 < predetermined distance, are not included in the calculation
974 > evaluation is to apply spherical cutoff where particles farther than
975 > a predetermined distance are not included in the calculation
976   \cite{Frenkel1996}. The use of a cutoff radius will cause a
977 < discontinuity in the potential energy curve
978 < (Fig.~\ref{introFig:shiftPot}). Fortunately, one can shift the
979 < potential to ensure the potential curve go smoothly to zero at the
980 < cutoff radius. Cutoff strategy works pretty well for Lennard-Jones
981 < interaction because of its short range nature. However, simply
982 < truncating the electrostatic interaction with the use of cutoff has
983 < been shown to lead to severe artifacts in simulations. Ewald
984 < summation, in which the slowly conditionally convergent Coulomb
985 < potential is transformed into direct and reciprocal sums with rapid
986 < and absolute convergence, has proved to minimize the periodicity
987 < artifacts in liquid simulations. Taking the advantages of the fast
988 < Fourier transform (FFT) for calculating discrete Fourier transforms,
989 < the particle mesh-based methods are accelerated from $O(N^{3/2})$ to
990 < $O(N logN)$. An alternative approach is \emph{fast multipole
991 < method}, which treats Coulombic interaction exactly at short range,
992 < and approximate the potential at long range through multipolar
993 < expansion. In spite of their wide acceptances at the molecular
994 < simulation community, these two methods are hard to be implemented
977 > discontinuity in the potential energy curve. Fortunately, one can
978 > shift simple radial potential to ensure the potential curve go
979 > smoothly to zero at the cutoff radius. The cutoff strategy works
980 > well for Lennard-Jones interaction because of its short range
981 > nature. However, simply truncating the electrostatic interaction
982 > with the use of cutoffs has been shown to lead to severe artifacts
983 > in simulations. The Ewald summation, in which the slowly decaying
984 > Coulomb potential is transformed into direct and reciprocal sums
985 > with rapid and absolute convergence, has proved to minimize the
986 > periodicity artifacts in liquid simulations. Taking the advantages
987 > of the fast Fourier transform (FFT) for calculating discrete Fourier
988 > transforms, the particle mesh-based
989 > methods\cite{Hockney1981,Shimada1993, Luty1994} are accelerated from
990 > $O(N^{3/2})$ to $O(N logN)$. An alternative approach is the
991 > \emph{fast multipole method}\cite{Greengard1987, Greengard1994},
992 > which treats Coulombic interactions exactly at short range, and
993 > approximate the potential at long range through multipolar
994 > expansion. In spite of their wide acceptance at the molecular
995 > simulation community, these two methods are difficult to implement
996   correctly and efficiently. Instead, we use a damped and
997   charge-neutralized Coulomb potential method developed by Wolf and
998 < his coworkers. The shifted Coulomb potential for particle $i$ and
999 < particle $j$ at distance $r_{rj}$ is given by:
998 > his coworkers\cite{Wolf1999}. The shifted Coulomb potential for
999 > particle $i$ and particle $j$ at distance $r_{rj}$ is given by:
1000   \begin{equation}
1001   V(r_{ij})= \frac{q_i q_j \textrm{erfc}(\alpha
1002   r_{ij})}{r_{ij}}-\lim_{r_{ij}\rightarrow
# Line 1053 | Line 1006 | efficient and easy to implement.
1006   where $\alpha$ is the convergence parameter. Due to the lack of
1007   inherent periodicity and rapid convergence,this method is extremely
1008   efficient and easy to implement.
1009 < %\begin{figure}
1010 < %\centering
1011 < %\includegraphics[width=\linewidth]{pbcFig.eps}
1012 < %\caption[An illustration of shifted Coulomb potential]{An illustration of shifted Coulomb potential.}
1013 < %\label{introFigure:shiftedCoulomb}
1014 < %\end{figure}
1009 > \begin{figure}
1010 > \centering
1011 > \includegraphics[width=\linewidth]{shifted_coulomb.eps}
1012 > \caption[An illustration of shifted Coulomb potential]{An
1013 > illustration of shifted Coulomb potential.}
1014 > \label{introFigure:shiftedCoulomb}
1015 > \end{figure}
1016  
1017   %multiple time step
1018  
1019   \subsection{\label{introSection:Analysis} Analysis}
1020  
1021 < Recently, advanced visualization technique are widely applied to
1021 > Recently, advanced visualization technique have become applied to
1022   monitor the motions of molecules. Although the dynamics of the
1023   system can be described qualitatively from animation, quantitative
1024 < trajectory analysis are more appreciable. According to the
1025 < principles of Statistical Mechanics,
1026 < Sec.~\ref{introSection:statisticalMechanics}, one can compute
1027 < thermodynamics properties, analyze fluctuations of structural
1028 < parameters, and investigate time-dependent processes of the molecule
1075 < from the trajectories.
1024 > trajectory analysis are more useful. According to the principles of
1025 > Statistical Mechanics, Sec.~\ref{introSection:statisticalMechanics},
1026 > one can compute thermodynamic properties, analyze fluctuations of
1027 > structural parameters, and investigate time-dependent processes of
1028 > the molecule from the trajectories.
1029  
1030 < \subsubsection{\label{introSection:thermodynamicsProperties}Thermodynamics Properties}
1030 > \subsubsection{\label{introSection:thermodynamicsProperties}\textbf{Thermodynamic Properties}}
1031  
1032 < Thermodynamics properties, which can be expressed in terms of some
1032 > Thermodynamic properties, which can be expressed in terms of some
1033   function of the coordinates and momenta of all particles in the
1034   system, can be directly computed from molecular dynamics. The usual
1035   way to measure the pressure is based on virial theorem of Clausius
# Line 1096 | Line 1049 | P = \frac{{Nk_B T}}{V} - \frac{1}{{3V}}\left\langle {\
1049   < j} {r{}_{ij} \cdot f_{ij} } } \right\rangle
1050   \end{equation}
1051  
1052 < \subsubsection{\label{introSection:structuralProperties}Structural Properties}
1052 > \subsubsection{\label{introSection:structuralProperties}\textbf{Structural Properties}}
1053  
1054   Structural Properties of a simple fluid can be described by a set of
1055 < distribution functions. Among these functions,\emph{pair
1055 > distribution functions. Among these functions,the \emph{pair
1056   distribution function}, also known as \emph{radial distribution
1057 < function}, is of most fundamental importance to liquid-state theory.
1058 < Pair distribution function can be gathered by Fourier transforming
1059 < raw data from a series of neutron diffraction experiments and
1060 < integrating over the surface factor \cite{Powles73}. The experiment
1061 < result can serve as a criterion to justify the correctness of the
1062 < theory. Moreover, various equilibrium thermodynamic and structural
1063 < properties can also be expressed in terms of radial distribution
1064 < function \cite{allen87:csl}.
1065 <
1113 < A pair distribution functions $g(r)$ gives the probability that a
1057 > function}, is of most fundamental importance to liquid theory.
1058 > Experimentally, pair distribution function can be gathered by
1059 > Fourier transforming raw data from a series of neutron diffraction
1060 > experiments and integrating over the surface factor
1061 > \cite{Powles1973}. The experimental results can serve as a criterion
1062 > to justify the correctness of a liquid model. Moreover, various
1063 > equilibrium thermodynamic and structural properties can also be
1064 > expressed in terms of radial distribution function \cite{Allen1987}.
1065 > The pair distribution functions $g(r)$ gives the probability that a
1066   particle $i$ will be located at a distance $r$ from a another
1067   particle $j$ in the system
1068   \[
1069   g(r) = \frac{V}{{N^2 }}\left\langle {\sum\limits_i {\sum\limits_{j
1070 < \ne i} {\delta (r - r_{ij} )} } } \right\rangle.
1070 > \ne i} {\delta (r - r_{ij} )} } } \right\rangle = \frac{\rho
1071 > (r)}{\rho}.
1072   \]
1073   Note that the delta function can be replaced by a histogram in
1074 < computer simulation. Figure
1075 < \ref{introFigure:pairDistributionFunction} shows a typical pair
1076 < distribution function for the liquid argon system. The occurrence of
1124 < several peaks in the plot of $g(r)$ suggests that it is more likely
1125 < to find particles at certain radial values than at others. This is a
1126 < result of the attractive interaction at such distances. Because of
1127 < the strong repulsive forces at short distance, the probability of
1128 < locating particles at distances less than about 2.5{\AA} from each
1129 < other is essentially zero.
1074 > computer simulation. Peaks in $g(r)$ represent solvent shells, and
1075 > the height of these peaks gradually decreases to 1 as the liquid of
1076 > large distance approaches the bulk density.
1077  
1131 %\begin{figure}
1132 %\centering
1133 %\includegraphics[width=\linewidth]{pdf.eps}
1134 %\caption[Pair distribution function for the liquid argon
1135 %]{Pair distribution function for the liquid argon}
1136 %\label{introFigure:pairDistributionFunction}
1137 %\end{figure}
1078  
1079 < \subsubsection{\label{introSection:timeDependentProperties}Time-dependent
1080 < Properties}
1079 > \subsubsection{\label{introSection:timeDependentProperties}\textbf{Time-dependent
1080 > Properties}}
1081  
1082   Time-dependent properties are usually calculated using \emph{time
1083 < correlation function}, which correlates random variables $A$ and $B$
1084 < at two different time
1083 > correlation functions}, which correlate random variables $A$ and $B$
1084 > at two different times,
1085   \begin{equation}
1086   C_{AB} (t) = \left\langle {A(t)B(0)} \right\rangle.
1087   \label{introEquation:timeCorrelationFunction}
1088   \end{equation}
1089   If $A$ and $B$ refer to same variable, this kind of correlation
1090 < function is called \emph{auto correlation function}. One example of
1091 < auto correlation function is velocity auto-correlation function
1092 < which is directly related to transport properties of molecular
1093 < liquids:
1090 > function is called an \emph{autocorrelation function}. One example
1091 > of an auto correlation function is the velocity auto-correlation
1092 > function which is directly related to transport properties of
1093 > molecular liquids:
1094   \[
1095   D = \frac{1}{3}\int\limits_0^\infty  {\left\langle {v(t) \cdot v(0)}
1096   \right\rangle } dt
1097   \]
1098 < where $D$ is diffusion constant. Unlike velocity autocorrelation
1099 < function which is averaging over time origins and over all the
1100 < atoms, dipole autocorrelation are calculated for the entire system.
1101 < The dipole autocorrelation function is given by:
1098 > where $D$ is diffusion constant. Unlike the velocity autocorrelation
1099 > function, which is averaging over time origins and over all the
1100 > atoms, the dipole autocorrelation functions are calculated for the
1101 > entire system. The dipole autocorrelation function is given by:
1102   \[
1103   c_{dipole}  = \left\langle {u_{tot} (t) \cdot u_{tot} (t)}
1104   \right\rangle
# Line 1184 | Line 1124 | simulator is governed by the rigid body dynamics. In m
1124   areas, from engineering, physics, to chemistry. For example,
1125   missiles and vehicle are usually modeled by rigid bodies.  The
1126   movement of the objects in 3D gaming engine or other physics
1127 < simulator is governed by the rigid body dynamics. In molecular
1128 < simulation, rigid body is used to simplify the model in
1129 < protein-protein docking study{\cite{Gray03}}.
1127 > simulator is governed by rigid body dynamics. In molecular
1128 > simulations, rigid bodies are used to simplify protein-protein
1129 > docking studies\cite{Gray2003}.
1130  
1131   It is very important to develop stable and efficient methods to
1132 < integrate the equations of motion of orientational degrees of
1133 < freedom. Euler angles are the nature choice to describe the
1134 < rotational degrees of freedom. However, due to its singularity, the
1135 < numerical integration of corresponding equations of motion is very
1136 < inefficient and inaccurate. Although an alternative integrator using
1137 < different sets of Euler angles can overcome this difficulty\cite{},
1138 < the computational penalty and the lost of angular momentum
1139 < conservation still remain. A singularity free representation
1140 < utilizing quaternions was developed by Evans in 1977. Unfortunately,
1141 < this approach suffer from the nonseparable Hamiltonian resulted from
1132 > integrate the equations of motion for orientational degrees of
1133 > freedom. Euler angles are the natural choice to describe the
1134 > rotational degrees of freedom. However, due to $\frac {1}{sin
1135 > \theta}$ singularities, the numerical integration of corresponding
1136 > equations of motion is very inefficient and inaccurate. Although an
1137 > alternative integrator using multiple sets of Euler angles can
1138 > overcome this difficulty\cite{Barojas1973}, the computational
1139 > penalty and the loss of angular momentum conservation still remain.
1140 > A singularity-free representation utilizing quaternions was
1141 > developed by Evans in 1977\cite{Evans1977}. Unfortunately, this
1142 > approach uses a nonseparable Hamiltonian resulting from the
1143   quaternion representation, which prevents the symplectic algorithm
1144   to be utilized. Another different approach is to apply holonomic
1145   constraints to the atoms belonging to the rigid body. Each atom
1146   moves independently under the normal forces deriving from potential
1147   energy and constraint forces which are used to guarantee the
1148 < rigidness. However, due to their iterative nature, SHAKE and Rattle
1149 < algorithm converge very slowly when the number of constraint
1150 < increases.
1148 > rigidness. However, due to their iterative nature, the SHAKE and
1149 > Rattle algorithms also converge very slowly when the number of
1150 > constraints increases\cite{Ryckaert1977, Andersen1983}.
1151  
1152 < The break through in geometric literature suggests that, in order to
1152 > A break-through in geometric literature suggests that, in order to
1153   develop a long-term integration scheme, one should preserve the
1154 < symplectic structure of the flow. Introducing conjugate momentum to
1155 < rotation matrix $Q$ and re-formulating Hamiltonian's equation, a
1156 < symplectic integrator, RSHAKE, was proposed to evolve the
1157 < Hamiltonian system in a constraint manifold by iteratively
1158 < satisfying the orthogonality constraint $Q_T Q = 1$. An alternative
1159 < method using quaternion representation was developed by Omelyan.
1160 < However, both of these methods are iterative and inefficient. In
1161 < this section, we will present a symplectic Lie-Poisson integrator
1162 < for rigid body developed by Dullweber and his
1163 < coworkers\cite{Dullweber1997} in depth.
1154 > symplectic structure of the flow. By introducing a conjugate
1155 > momentum to the rotation matrix $Q$ and re-formulating Hamiltonian's
1156 > equation, a symplectic integrator, RSHAKE\cite{Kol1997}, was
1157 > proposed to evolve the Hamiltonian system in a constraint manifold
1158 > by iteratively satisfying the orthogonality constraint $Q^T Q = 1$.
1159 > An alternative method using the quaternion representation was
1160 > developed by Omelyan\cite{Omelyan1998}. However, both of these
1161 > methods are iterative and inefficient. In this section, we descibe a
1162 > symplectic Lie-Poisson integrator for rigid body developed by
1163 > Dullweber and his coworkers\cite{Dullweber1997} in depth.
1164  
1165 < \subsection{\label{introSection:constrainedHamiltonianRB}Constrained Hamiltonian for Rigid Body}
1166 < The motion of the rigid body is Hamiltonian with the Hamiltonian
1165 > \subsection{\label{introSection:constrainedHamiltonianRB}Constrained Hamiltonian for Rigid Bodies}
1166 > The motion of a rigid body is Hamiltonian with the Hamiltonian
1167   function
1168   \begin{equation}
1169   H = \frac{1}{2}(p^T m^{ - 1} p) + \frac{1}{2}tr(PJ^{ - 1} P) +
# Line 1236 | Line 1177 | constrained Hamiltonian equation subjects to a holonom
1177   I_{ii}^{ - 1}  = \frac{1}{2}\sum\limits_{i \ne j} {J_{jj}^{ - 1} }
1178   \]
1179   where $I_{ii}$ is the diagonal element of the inertia tensor. This
1180 < constrained Hamiltonian equation subjects to a holonomic constraint,
1180 > constrained Hamiltonian equation is subjected to a holonomic
1181 > constraint,
1182   \begin{equation}
1183 < Q^T Q = 1$, \label{introEquation:orthogonalConstraint}
1183 > Q^T Q = 1, \label{introEquation:orthogonalConstraint}
1184   \end{equation}
1185 < which is used to ensure rotation matrix's orthogonality.
1186 < Differentiating \ref{introEquation:orthogonalConstraint} and using
1187 < Equation \ref{introEquation:RBMotionMomentum}, one may obtain,
1185 > which is used to ensure rotation matrix's unitarity. Differentiating
1186 > \ref{introEquation:orthogonalConstraint} and using Equation
1187 > \ref{introEquation:RBMotionMomentum}, one may obtain,
1188   \begin{equation}
1189   Q^T PJ^{ - 1}  + J^{ - 1} P^T Q = 0 . \\
1190   \label{introEquation:RBFirstOrderConstraint}
1191   \end{equation}
1250
1192   Using Equation (\ref{introEquation:motionHamiltonianCoordinate},
1193   \ref{introEquation:motionHamiltonianMomentum}), one can write down
1194   the equations of motion,
1195 < \[
1196 < \begin{array}{c}
1197 < \frac{{dq}}{{dt}} = \frac{p}{m} \label{introEquation:RBMotionPosition}\\
1198 < \frac{{dp}}{{dt}} =  - \nabla _q V(q,Q) \label{introEquation:RBMotionMomentum}\\
1199 < \frac{{dQ}}{{dt}} = PJ^{ - 1}  \label{introEquation:RBMotionRotation}\\
1200 < \frac{{dP}}{{dt}} =  - \nabla _Q V(q,Q) - 2Q\Lambda . \label{introEquation:RBMotionP}\\
1260 < \end{array}
1261 < \]
1262 <
1195 > \begin{eqnarray}
1196 > \frac{{dq}}{{dt}} & = & \frac{p}{m} \label{introEquation:RBMotionPosition}\\
1197 > \frac{{dp}}{{dt}} & = & - \nabla _q V(q,Q) \label{introEquation:RBMotionMomentum}\\
1198 > \frac{{dQ}}{{dt}} & = & PJ^{ - 1}  \label{introEquation:RBMotionRotation}\\
1199 > \frac{{dP}}{{dt}} & = & - \nabla _Q V(q,Q) - 2Q\Lambda . \label{introEquation:RBMotionP}
1200 > \end{eqnarray}
1201   In general, there are two ways to satisfy the holonomic constraints.
1202 < We can use constraint force provided by lagrange multiplier on the
1203 < normal manifold to keep the motion on constraint space. Or we can
1204 < simply evolve the system in constraint manifold. The two method are
1205 < proved to be equivalent. The holonomic constraint and equations of
1206 < motions define a constraint manifold for rigid body
1202 > We can use a constraint force provided by a Lagrange multiplier on
1203 > the normal manifold to keep the motion on constraint space. Or we
1204 > can simply evolve the system on the constraint manifold. These two
1205 > methods have been proved to be equivalent. The holonomic constraint
1206 > and equations of motions define a constraint manifold for rigid
1207 > bodies
1208   \[
1209   M = \left\{ {(Q,P):Q^T Q = 1,Q^T PJ^{ - 1}  + J^{ - 1} P^T Q = 0}
1210   \right\}.
1211   \]
1273
1212   Unfortunately, this constraint manifold is not the cotangent bundle
1213 < $T_{\star}SO(3)$. However, it turns out that under symplectic
1213 > $T^* SO(3)$ which can be consider as a symplectic manifold on Lie
1214 > rotation group $SO(3)$. However, it turns out that under symplectic
1215   transformation, the cotangent space and the phase space are
1216 < diffeomorphic. Introducing
1216 > diffeomorphic. By introducing
1217   \[
1218   \tilde Q = Q,\tilde P = \frac{1}{2}\left( {P - QP^T Q} \right),
1219   \]
# Line 1284 | Line 1223 | T^* SO(3) = \left\{ {(\tilde Q,\tilde P):\tilde Q^T \t
1223   T^* SO(3) = \left\{ {(\tilde Q,\tilde P):\tilde Q^T \tilde Q =
1224   1,\tilde Q^T \tilde PJ^{ - 1}  + J^{ - 1} P^T \tilde Q = 0} \right\}
1225   \]
1287
1226   For a body fixed vector $X_i$ with respect to the center of mass of
1227   the rigid body, its corresponding lab fixed vector $X_0^{lab}$  is
1228   given as
# Line 1303 | Line 1241 | respectively.
1241   \[
1242   \nabla _Q V(q,Q) = F(q,Q)X_i^t
1243   \]
1244 < respectively.
1245 <
1246 < As a common choice to describe the rotation dynamics of the rigid
1309 < body, angular momentum on body frame $\Pi  = Q^t P$ is introduced to
1310 < rewrite the equations of motion,
1244 > respectively. As a common choice to describe the rotation dynamics
1245 > of the rigid body, the angular momentum on the body fixed frame $\Pi
1246 > = Q^t P$ is introduced to rewrite the equations of motion,
1247   \begin{equation}
1248   \begin{array}{l}
1249 < \mathop \Pi \limits^ \bullet   = J^{ - 1} \Pi ^T \Pi  + Q^T \sum\limits_i {F_i (q,Q)X_i^T }  - \Lambda  \\
1250 < \mathop Q\limits^{{\rm{   }} \bullet }  = Q\Pi {\rm{ }}J^{ - 1}  \\
1249 > \dot \Pi  = J^{ - 1} \Pi ^T \Pi  + Q^T \sum\limits_i {F_i (q,Q)X_i^T }  - \Lambda,  \\
1250 > \dot Q  = Q\Pi {\rm{ }}J^{ - 1},  \\
1251   \end{array}
1252   \label{introEqaution:RBMotionPI}
1253   \end{equation}
1254 < , as well as holonomic constraints,
1254 > as well as holonomic constraints,
1255   \[
1256   \begin{array}{l}
1257 < \Pi J^{ - 1}  + J^{ - 1} \Pi ^t  = 0 \\
1258 < Q^T Q = 1 \\
1257 > \Pi J^{ - 1}  + J^{ - 1} \Pi ^t  = 0, \\
1258 > Q^T Q = 1 .\\
1259   \end{array}
1260   \]
1325
1261   For a vector $v(v_1 ,v_2 ,v_3 ) \in R^3$ and a matrix $\hat v \in
1262   so(3)^ \star$, the hat-map isomorphism,
1263   \begin{equation}
# Line 1337 | Line 1272 | operations
1272   will let us associate the matrix products with traditional vector
1273   operations
1274   \[
1275 < \hat vu = v \times u
1275 > \hat vu = v \times u.
1276   \]
1277 <
1343 < Using \ref{introEqaution:RBMotionPI}, one can construct a skew
1277 > Using Eq.~\ref{introEqaution:RBMotionPI}, one can construct a skew
1278   matrix,
1279 + \begin{eqnarray}
1280 + (\dot \Pi  - \dot \Pi ^T ){\rm{ }} &= &{\rm{ }}(\Pi  - \Pi ^T ){\rm{
1281 + }}(J^{ - 1} \Pi  + \Pi J^{ - 1} ) \notag \\
1282 + + \sum\limits_i {[Q^T F_i
1283 + (r,Q)X_i^T  - X_i F_i (r,Q)^T Q]}  - (\Lambda  - \Lambda ^T ).
1284 + \label{introEquation:skewMatrixPI}
1285 + \end{eqnarray}
1286 + Since $\Lambda$ is symmetric, the last term of
1287 + Eq.~\ref{introEquation:skewMatrixPI} is zero, which implies the
1288 + Lagrange multiplier $\Lambda$ is absent from the equations of
1289 + motion. This unique property eliminates the requirement of
1290 + iterations which can not be avoided in other methods\cite{Kol1997,
1291 + Omelyan1998}. Applying the hat-map isomorphism, we obtain the
1292 + equation of motion for angular momentum on body frame
1293   \begin{equation}
1346 (\mathop \Pi \limits^ \bullet   - \mathop \Pi \limits^ \bullet  ^T
1347 ){\rm{ }} = {\rm{ }}(\Pi  - \Pi ^T ){\rm{ }}(J^{ - 1} \Pi  + \Pi J^{
1348 - 1} ) + \sum\limits_i {[Q^T F_i (r,Q)X_i^T  - X_i F_i (r,Q)^T Q]} -
1349 (\Lambda  - \Lambda ^T ) . \label{introEquation:skewMatrixPI}
1350 \end{equation}
1351 Since $\Lambda$ is symmetric, the last term of Equation
1352 \ref{introEquation:skewMatrixPI} is zero, which implies the Lagrange
1353 multiplier $\Lambda$ is absent from the equations of motion. This
1354 unique property eliminate the requirement of iterations which can
1355 not be avoided in other methods\cite{}.
1356
1357 Applying hat-map isomorphism, we obtain the equation of motion for
1358 angular momentum on body frame
1359 \begin{equation}
1294   \dot \pi  = \pi  \times I^{ - 1} \pi  + \sum\limits_i {\left( {Q^T
1295   F_i (r,Q)} \right) \times X_i }.
1296   \label{introEquation:bodyAngularMotion}
# Line 1364 | Line 1298 | given by
1298   In the same manner, the equation of motion for rotation matrix is
1299   given by
1300   \[
1301 < \dot Q = Qskew(I^{ - 1} \pi )
1301 > \dot Q = Qskew(I^{ - 1} \pi ).
1302   \]
1303  
1304   \subsection{\label{introSection:SymplecticFreeRB}Symplectic
1305   Lie-Poisson Integrator for Free Rigid Body}
1306  
1307 < If there is not external forces exerted on the rigid body, the only
1308 < contribution to the rotational is from the kinetic potential (the
1309 < first term of \ref{ introEquation:bodyAngularMotion}). The free
1310 < rigid body is an example of Lie-Poisson system with Hamiltonian
1307 > If there are no external forces exerted on the rigid body, the only
1308 > contribution to the rotational motion is from the kinetic energy
1309 > (the first term of \ref{introEquation:bodyAngularMotion}). The free
1310 > rigid body is an example of a Lie-Poisson system with Hamiltonian
1311   function
1312   \begin{equation}
1313   T^r (\pi ) = T_1 ^r (\pi _1 ) + T_2^r (\pi _2 ) + T_3^r (\pi _3 )
# Line 1386 | Line 1320 | J(\pi ) = \left( {\begin{array}{*{20}c}
1320     0 & {\pi _3 } & { - \pi _2 }  \\
1321     { - \pi _3 } & 0 & {\pi _1 }  \\
1322     {\pi _2 } & { - \pi _1 } & 0  \\
1323 < \end{array}} \right)
1323 > \end{array}} \right).
1324   \end{equation}
1325   Thus, the dynamics of free rigid body is governed by
1326   \begin{equation}
1327 < \frac{d}{{dt}}\pi  = J(\pi )\nabla _\pi  T^r (\pi )
1327 > \frac{d}{{dt}}\pi  = J(\pi )\nabla _\pi  T^r (\pi ).
1328   \end{equation}
1395
1329   One may notice that each $T_i^r$ in Equation
1330   \ref{introEquation:rotationalKineticRB} can be solved exactly. For
1331   instance, the equations of motion due to $T_1^r$ are given by
# Line 1421 | Line 1354 | tR_1 }$, we can use Cayley transformation,
1354   \end{array}} \right),\theta _1  = \frac{{\pi _1 }}{{I_1 }}\Delta t.
1355   \]
1356   To reduce the cost of computing expensive functions in $e^{\Delta
1357 < tR_1 }$, we can use Cayley transformation,
1357 > tR_1 }$, we can use Cayley transformation to obtain a single-aixs
1358 > propagator,
1359   \[
1360   e^{\Delta tR_1 }  \approx (1 - \Delta tR_1 )^{ - 1} (1 + \Delta tR_1
1361 < )
1361 > ).
1362   \]
1363   The flow maps for $T_2^r$ and $T_3^r$ can be found in the same
1364 < manner.
1365 <
1432 < In order to construct a second-order symplectic method, we split the
1433 < angular kinetic Hamiltonian function can into five terms
1364 > manner. In order to construct a second-order symplectic method, we
1365 > split the angular kinetic Hamiltonian function can into five terms
1366   \[
1367   T^r (\pi ) = \frac{1}{2}T_1 ^r (\pi _1 ) + \frac{1}{2}T_2^r (\pi _2
1368   ) + T_3^r (\pi _3 ) + \frac{1}{2}T_2^r (\pi _2 ) + \frac{1}{2}T_1 ^r
1369 < (\pi _1 )
1370 < \].
1371 < Concatenating flows corresponding to these five terms, we can obtain
1372 < an symplectic integrator,
1369 > (\pi _1 ).
1370 > \]
1371 > By concatenating the propagators corresponding to these five terms,
1372 > we can obtain an symplectic integrator,
1373   \[
1374   \varphi _{\Delta t,T^r }  = \varphi _{\Delta t/2,\pi _1 }  \circ
1375   \varphi _{\Delta t/2,\pi _2 }  \circ \varphi _{\Delta t,\pi _3 }
1376   \circ \varphi _{\Delta t/2,\pi _2 }  \circ \varphi _{\Delta t/2,\pi
1377   _1 }.
1378   \]
1447
1379   The non-canonical Lie-Poisson bracket ${F, G}$ of two function
1380   $F(\pi )$ and $G(\pi )$ is defined by
1381   \[
1382   \{ F,G\} (\pi ) = [\nabla _\pi  F(\pi )]^T J(\pi )\nabla _\pi  G(\pi
1383 < )
1383 > ).
1384   \]
1385   If the Poisson bracket of a function $F$ with an arbitrary smooth
1386   function $G$ is zero, $F$ is a \emph{Casimir}, which is the
# Line 1460 | Line 1391 | then by the chain rule
1391   then by the chain rule
1392   \[
1393   \nabla _\pi  F(\pi ) = S'(\frac{{\parallel \pi \parallel ^2
1394 < }}{2})\pi
1394 > }}{2})\pi.
1395   \]
1396 < Thus $ [\nabla _\pi  F(\pi )]^T J(\pi ) =  - S'(\frac{{\parallel \pi
1396 > Thus, $ [\nabla _\pi  F(\pi )]^T J(\pi ) =  - S'(\frac{{\parallel
1397 > \pi
1398   \parallel ^2 }}{2})\pi  \times \pi  = 0 $. This explicit
1399 < Lie-Poisson integrator is found to be extremely efficient and stable
1400 < which can be explained by the fact the small angle approximation is
1401 < used and the norm of the angular momentum is conserved.
1399 > Lie-Poisson integrator is found to be both extremely efficient and
1400 > stable. These properties can be explained by the fact the small
1401 > angle approximation is used and the norm of the angular momentum is
1402 > conserved.
1403  
1404   \subsection{\label{introSection:RBHamiltonianSplitting} Hamiltonian
1405   Splitting for Rigid Body}
# Line 1474 | Line 1407 | H = T(p,\pi ) + V(q,Q)
1407   The Hamiltonian of rigid body can be separated in terms of kinetic
1408   energy and potential energy,
1409   \[
1410 < H = T(p,\pi ) + V(q,Q)
1410 > H = T(p,\pi ) + V(q,Q).
1411   \]
1412   The equations of motion corresponding to potential energy and
1413   kinetic energy are listed in the below table,
1414 + \begin{table}
1415 + \caption{EQUATIONS OF MOTION DUE TO POTENTIAL AND KINETIC ENERGIES}
1416   \begin{center}
1417   \begin{tabular}{|l|l|}
1418    \hline
# Line 1490 | Line 1425 | A second-order symplectic method is now obtained by th
1425    \hline
1426   \end{tabular}
1427   \end{center}
1428 + \end{table}
1429   A second-order symplectic method is now obtained by the composition
1430 < of the flow maps,
1430 > of the position and velocity propagators,
1431   \[
1432   \varphi _{\Delta t}  = \varphi _{\Delta t/2,V}  \circ \varphi
1433   _{\Delta t,T}  \circ \varphi _{\Delta t/2,V}.
1434   \]
1435   Moreover, $\varphi _{\Delta t/2,V}$ can be divided into two
1436 < sub-flows which corresponding to force and torque respectively,
1436 > sub-propagators which corresponding to force and torque
1437 > respectively,
1438   \[
1439   \varphi _{\Delta t/2,V}  = \varphi _{\Delta t/2,F}  \circ \varphi
1440   _{\Delta t/2,\tau }.
1441   \]
1442   Since the associated operators of $\varphi _{\Delta t/2,F} $ and
1443 < $\circ \varphi _{\Delta t/2,\tau }$ are commuted, the composition
1444 < order inside $\varphi _{\Delta t/2,V}$ does not matter.
1445 <
1446 < Furthermore, kinetic potential can be separated to translational
1510 < kinetic term, $T^t (p)$, and rotational kinetic term, $T^r (\pi )$,
1443 > $\circ \varphi _{\Delta t/2,\tau }$ commute, the composition order
1444 > inside $\varphi _{\Delta t/2,V}$ does not matter. Furthermore, the
1445 > kinetic energy can be separated to translational kinetic term, $T^t
1446 > (p)$, and rotational kinetic term, $T^r (\pi )$,
1447   \begin{equation}
1448   T(p,\pi ) =T^t (p) + T^r (\pi ).
1449   \end{equation}
1450   where $ T^t (p) = \frac{1}{2}p^T m^{ - 1} p $ and $T^r (\pi )$ is
1451   defined by \ref{introEquation:rotationalKineticRB}. Therefore, the
1452 < corresponding flow maps are given by
1452 > corresponding propagators are given by
1453   \[
1454   \varphi _{\Delta t,T}  = \varphi _{\Delta t,T^t }  \circ \varphi
1455   _{\Delta t,T^r }.
1456   \]
1457 < Finally, we obtain the overall symplectic flow maps for free moving
1458 < rigid body
1459 < \begin{equation}
1460 < \begin{array}{c}
1461 < \varphi _{\Delta t}  = \varphi _{\Delta t/2,F}  \circ \varphi _{\Delta t/2,\tau }  \\
1462 <  \circ \varphi _{\Delta t,T^t }  \circ \varphi _{\Delta t/2,\pi _1 }  \circ \varphi _{\Delta t/2,\pi _2 }  \circ \varphi _{\Delta t,\pi _3 }  \circ \varphi _{\Delta t/2,\pi _2 }  \circ \varphi _{\Delta t/2,\pi _1 }  \\
1527 <  \circ \varphi _{\Delta t/2,\tau }  \circ \varphi _{\Delta t/2,F}  .\\
1528 < \end{array}
1457 > Finally, we obtain the overall symplectic propagators for freely
1458 > moving rigid bodies
1459 > \begin{eqnarray*}
1460 > \varphi _{\Delta t}  &=& \varphi _{\Delta t/2,F}  \circ \varphi _{\Delta t/2,\tau }  \\
1461 >  & & \circ \varphi _{\Delta t,T^t }  \circ \varphi _{\Delta t/2,\pi _1 }  \circ \varphi _{\Delta t/2,\pi _2 }  \circ \varphi _{\Delta t,\pi _3 }  \circ \varphi _{\Delta t/2,\pi _2 }  \circ \varphi _{\Delta t/2,\pi _1 }  \\
1462 >  & & \circ \varphi _{\Delta t/2,\tau }  \circ \varphi _{\Delta t/2,F}  .\\
1463   \label{introEquation:overallRBFlowMaps}
1464 < \end{equation}
1464 > \end{eqnarray*}
1465  
1466   \section{\label{introSection:langevinDynamics}Langevin Dynamics}
1467   As an alternative to newtonian dynamics, Langevin dynamics, which
1468   mimics a simple heat bath with stochastic and dissipative forces,
1469   has been applied in a variety of studies. This section will review
1470 < the theory of Langevin dynamics simulation. A brief derivation of
1471 < generalized Langevin equation will be given first. Follow that, we
1472 < will discuss the physical meaning of the terms appearing in the
1473 < equation as well as the calculation of friction tensor from
1474 < hydrodynamics theory.
1470 > the theory of Langevin dynamics. A brief derivation of generalized
1471 > Langevin equation will be given first. Following that, we will
1472 > discuss the physical meaning of the terms appearing in the equation
1473 > as well as the calculation of friction tensor from hydrodynamics
1474 > theory.
1475  
1476   \subsection{\label{introSection:generalizedLangevinDynamics}Derivation of Generalized Langevin Equation}
1477  
1478 < Harmonic bath model, in which an effective set of harmonic
1478 > A harmonic bath model, in which an effective set of harmonic
1479   oscillators are used to mimic the effect of a linearly responding
1480   environment, has been widely used in quantum chemistry and
1481   statistical mechanics. One of the successful applications of
1482 < Harmonic bath model is the derivation of Deriving Generalized
1483 < Langevin Dynamics. Lets consider a system, in which the degree of
1482 > Harmonic bath model is the derivation of the Generalized Langevin
1483 > Dynamics (GLE). Lets consider a system, in which the degree of
1484   freedom $x$ is assumed to couple to the bath linearly, giving a
1485   Hamiltonian of the form
1486   \begin{equation}
1487   H = \frac{{p^2 }}{{2m}} + U(x) + H_B  + \Delta U(x,x_1 , \ldots x_N)
1488   \label{introEquation:bathGLE}.
1489   \end{equation}
1490 < Here $p$ is a momentum conjugate to $q$, $m$ is the mass associated
1491 < with this degree of freedom, $H_B$ is harmonic bath Hamiltonian,
1490 > Here $p$ is a momentum conjugate to $x$, $m$ is the mass associated
1491 > with this degree of freedom, $H_B$ is a harmonic bath Hamiltonian,
1492   \[
1493   H_B  = \sum\limits_{\alpha  = 1}^N {\left\{ {\frac{{p_\alpha ^2
1494   }}{{2m_\alpha  }} + \frac{1}{2}m_\alpha  \omega _\alpha ^2 }
# Line 1562 | Line 1496 | the harmonic bath masses, and $\Delta U$ is bilinear s
1496   \]
1497   where the index $\alpha$ runs over all the bath degrees of freedom,
1498   $\omega _\alpha$ are the harmonic bath frequencies, $m_\alpha$ are
1499 < the harmonic bath masses, and $\Delta U$ is bilinear system-bath
1499 > the harmonic bath masses, and $\Delta U$ is a bilinear system-bath
1500   coupling,
1501   \[
1502   \Delta U =  - \sum\limits_{\alpha  = 1}^N {g_\alpha  x_\alpha  x}
1503   \]
1504 < where $g_\alpha$ are the coupling constants between the bath and the
1505 < coordinate $x$. Introducing
1504 > where $g_\alpha$ are the coupling constants between the bath
1505 > coordinates ($x_ \alpha$) and the system coordinate ($x$).
1506 > Introducing
1507   \[
1508   W(x) = U(x) - \sum\limits_{\alpha  = 1}^N {\frac{{g_\alpha ^2
1509   }}{{2m_\alpha  w_\alpha ^2 }}} x^2
1510 < \] and combining the last two terms in Equation
1511 < \ref{introEquation:bathGLE}, we may rewrite the Harmonic bath
1577 < Hamiltonian as
1510 > \]
1511 > and combining the last two terms in Eq.~\ref{introEquation:bathGLE}, we may rewrite the Harmonic bath Hamiltonian as
1512   \[
1513   H = \frac{{p^2 }}{{2m}} + W(x) + \sum\limits_{\alpha  = 1}^N
1514   {\left\{ {\frac{{p_\alpha ^2 }}{{2m_\alpha  }} + \frac{1}{2}m_\alpha
1515   w_\alpha ^2 \left( {x_\alpha   - \frac{{g_\alpha  }}{{m_\alpha
1516 < w_\alpha ^2 }}x} \right)^2 } \right\}}
1516 > w_\alpha ^2 }}x} \right)^2 } \right\}}.
1517   \]
1518   Since the first two terms of the new Hamiltonian depend only on the
1519   system coordinates, we can get the equations of motion for
1520 < Generalized Langevin Dynamics by Hamilton's equations
1587 < \ref{introEquation:motionHamiltonianCoordinate,
1588 < introEquation:motionHamiltonianMomentum},
1520 > Generalized Langevin Dynamics by Hamilton's equations,
1521   \begin{equation}
1522   m\ddot x =  - \frac{{\partial W(x)}}{{\partial x}} -
1523   \sum\limits_{\alpha  = 1}^N {g_\alpha  \left( {x_\alpha   -
# Line 1598 | Line 1530 | m\ddot x_\alpha   =  - m_\alpha  w_\alpha ^2 \left( {x
1530   \frac{{g_\alpha  }}{{m_\alpha  w_\alpha ^2 }}x} \right).
1531   \label{introEquation:bathMotionGLE}
1532   \end{equation}
1601
1533   In order to derive an equation for $x$, the dynamics of the bath
1534   variables $x_\alpha$ must be solved exactly first. As an integral
1535   transform which is particularly useful in solving linear ordinary
1536 < differential equations, Laplace transform is the appropriate tool to
1537 < solve this problem. The basic idea is to transform the difficult
1536 > differential equations,the Laplace transform is the appropriate tool
1537 > to solve this problem. The basic idea is to transform the difficult
1538   differential equations into simple algebra problems which can be
1539 < solved easily. Then applying inverse Laplace transform, also known
1540 < as the Bromwich integral, we can retrieve the solutions of the
1541 < original problems.
1542 <
1612 < Let $f(t)$ be a function defined on $ [0,\infty ) $. The Laplace
1613 < transform of f(t) is a new function defined as
1539 > solved easily. Then, by applying the inverse Laplace transform, also
1540 > known as the Bromwich integral, we can retrieve the solutions of the
1541 > original problems. Let $f(t)$ be a function defined on $ [0,\infty )
1542 > $. The Laplace transform of f(t) is a new function defined as
1543   \[
1544   L(f(t)) \equiv F(p) = \int_0^\infty  {f(t)e^{ - pt} dt}
1545   \]
1546   where  $p$ is real and  $L$ is called the Laplace Transform
1547   Operator. Below are some important properties of Laplace transform
1548 < \begin{equation}
1549 < \begin{array}{c}
1550 < L(x + y) = L(x) + L(y) \\
1551 < L(ax) = aL(x) \\
1552 < L(\dot x) = pL(x) - px(0) \\
1553 < L(\ddot x) = p^2 L(x) - px(0) - \dot x(0) \\
1554 < L\left( {\int_0^t {g(t - \tau )h(\tau )d\tau } } \right) = G(p)H(p) \\
1555 < \end{array}
1556 < \end{equation}
1557 <
1558 < Applying Laplace transform to the bath coordinates, we obtain
1559 < \[
1560 < \begin{array}{c}
1561 < p^2 L(x_\alpha  ) - px_\alpha  (0) - \dot x_\alpha  (0) =  - \omega _\alpha ^2 L(x_\alpha  ) + \frac{{g_\alpha  }}{{\omega _\alpha  }}L(x) \\
1562 < L(x_\alpha  ) = \frac{{\frac{{g_\alpha  }}{{\omega _\alpha  }}L(x) + px_\alpha  (0) + \dot x_\alpha  (0)}}{{p^2  + \omega _\alpha ^2 }} \\
1634 < \end{array}
1635 < \]
1636 < By the same way, the system coordinates become
1637 < \[
1638 < \begin{array}{c}
1639 < mL(\ddot x) =  - \frac{1}{p}\frac{{\partial W(x)}}{{\partial x}} \\
1548 > \begin{eqnarray*}
1549 > L(x + y)  & = & L(x) + L(y) \\
1550 > L(ax)     & = & aL(x) \\
1551 > L(\dot x) & = & pL(x) - px(0) \\
1552 > L(\ddot x)& = & p^2 L(x) - px(0) - \dot x(0) \\
1553 > L\left( {\int_0^t {g(t - \tau )h(\tau )d\tau } } \right)& = & G(p)H(p) \\
1554 > \end{eqnarray*}
1555 > Applying the Laplace transform to the bath coordinates, we obtain
1556 > \begin{eqnarray*}
1557 > p^2 L(x_\alpha  ) - px_\alpha  (0) - \dot x_\alpha  (0) & = & - \omega _\alpha ^2 L(x_\alpha  ) + \frac{{g_\alpha  }}{{\omega _\alpha  }}L(x) \\
1558 > L(x_\alpha  ) & = & \frac{{\frac{{g_\alpha  }}{{\omega _\alpha  }}L(x) + px_\alpha  (0) + \dot x_\alpha  (0)}}{{p^2  + \omega _\alpha ^2 }} \\
1559 > \end{eqnarray*}
1560 > By the same way, the system coordinates become
1561 > \begin{eqnarray*}
1562 > mL(\ddot x) & = &
1563    - \sum\limits_{\alpha  = 1}^N {\left\{ { - \frac{{g_\alpha ^2 }}{{m_\alpha  \omega _\alpha ^2 }}\frac{p}{{p^2  + \omega _\alpha ^2 }}pL(x) - \frac{p}{{p^2  + \omega _\alpha ^2 }}g_\alpha  x_\alpha  (0) - \frac{1}{{p^2  + \omega _\alpha ^2 }}g_\alpha  \dot x_\alpha  (0)} \right\}}  \\
1564 < \end{array}
1565 < \]
1643 <
1564 >  & & - \frac{1}{p}\frac{{\partial W(x)}}{{\partial x}}
1565 > \end{eqnarray*}
1566   With the help of some relatively important inverse Laplace
1567   transformations:
1568   \[
# Line 1650 | Line 1572 | transformations:
1572   L(1) = \frac{1}{p} \\
1573   \end{array}
1574   \]
1575 < , we obtain
1576 < \begin{align}
1577 < m\ddot x &=  - \frac{{\partial W(x)}}{{\partial x}} -
1575 > we obtain
1576 > \begin{eqnarray*}
1577 > m\ddot x & =  & - \frac{{\partial W(x)}}{{\partial x}} -
1578   \sum\limits_{\alpha  = 1}^N {\left\{ {\left( { - \frac{{g_\alpha ^2
1579   }}{{m_\alpha  \omega _\alpha ^2 }}} \right)\int_0^t {\cos (\omega
1580 < _\alpha  t)\dot x(t - \tau )d\tau  - \left[ {g_\alpha  x_\alpha  (0)
1581 < - \frac{{g_\alpha  }}{{m_\alpha  \omega _\alpha  }}} \right]\cos
1582 < (\omega _\alpha  t) - \frac{{g_\alpha  \dot x_\alpha  (0)}}{{\omega
1583 < _\alpha  }}\sin (\omega _\alpha  t)} } \right\}}
1584 < %
1585 < &= - \frac{{\partial W(x)}}{{\partial x}} - \int_0^t
1580 > _\alpha  t)\dot x(t - \tau )d\tau } } \right\}}  \\
1581 > & & + \sum\limits_{\alpha  = 1}^N {\left\{ {\left[ {g_\alpha
1582 > x_\alpha (0) - \frac{{g_\alpha  }}{{m_\alpha  \omega _\alpha  }}}
1583 > \right]\cos (\omega _\alpha  t) + \frac{{g_\alpha  \dot x_\alpha
1584 > (0)}}{{\omega _\alpha  }}\sin (\omega _\alpha  t)} \right\}}
1585 > \end{eqnarray*}
1586 > \begin{eqnarray*}
1587 > m\ddot x & = & - \frac{{\partial W(x)}}{{\partial x}} - \int_0^t
1588   {\sum\limits_{\alpha  = 1}^N {\left( { - \frac{{g_\alpha ^2
1589   }}{{m_\alpha  \omega _\alpha ^2 }}} \right)\cos (\omega _\alpha
1590 < t)\dot x(t - \tau )d} \tau }  + \sum\limits_{\alpha  = 1}^N {\left\{
1591 < {\left[ {g_\alpha  x_\alpha  (0) - \frac{{g_\alpha  }}{{m_\alpha
1592 < \omega _\alpha  }}} \right]\cos (\omega _\alpha  t) +
1593 < \frac{{g_\alpha  \dot x_\alpha  (0)}}{{\omega _\alpha  }}\sin
1594 < (\omega _\alpha  t)} \right\}}
1595 < \end{align}
1672 <
1590 > t)\dot x(t - \tau )d} \tau }  \\
1591 > & & + \sum\limits_{\alpha  = 1}^N {\left\{ {\left[ {g_\alpha
1592 > x_\alpha (0) - \frac{{g_\alpha }}{{m_\alpha \omega _\alpha  }}}
1593 > \right]\cos (\omega _\alpha  t) + \frac{{g_\alpha  \dot x_\alpha
1594 > (0)}}{{\omega _\alpha  }}\sin (\omega _\alpha  t)} \right\}}
1595 > \end{eqnarray*}
1596   Introducing a \emph{dynamic friction kernel}
1597   \begin{equation}
1598   \xi (t) = \sum\limits_{\alpha  = 1}^N {\left( { - \frac{{g_\alpha ^2
# Line 1692 | Line 1615 | which is known as the \emph{generalized Langevin equat
1615   \end{equation}
1616   which is known as the \emph{generalized Langevin equation}.
1617  
1618 < \subsubsection{\label{introSection:randomForceDynamicFrictionKernel}Random Force and Dynamic Friction Kernel}
1618 > \subsubsection{\label{introSection:randomForceDynamicFrictionKernel}\textbf{Random Force and Dynamic Friction Kernel}}
1619  
1620   One may notice that $R(t)$ depends only on initial conditions, which
1621   implies it is completely deterministic within the context of a
# Line 1705 | Line 1628 | as the model, which is gaussian distribution in genera
1628   \end{array}
1629   \]
1630   This property is what we expect from a truly random process. As long
1631 < as the model, which is gaussian distribution in general, chosen for
1632 < $R(t)$ is a truly random process, the stochastic nature of the GLE
1710 < still remains.
1631 > as the model chosen for $R(t)$ was a gaussian distribution in
1632 > general, the stochastic nature of the GLE still remains.
1633  
1634   %dynamic friction kernel
1635   The convolution integral
# Line 1723 | Line 1645 | and Equation \ref{introEuqation:GeneralizedLangevinDyn
1645   \[
1646   \int_0^t {\xi (t)\dot x(t - \tau )d\tau }  = \xi _0 (x(t) - x(0))
1647   \]
1648 < and Equation \ref{introEuqation:GeneralizedLangevinDynamics} becomes
1648 > and Eq.~\ref{introEuqation:GeneralizedLangevinDynamics} becomes
1649   \[
1650   m\ddot x =  - \frac{\partial }{{\partial x}}\left( {W(x) +
1651   \frac{1}{2}\xi _0 (x - x_0 )^2 } \right) + R(t),
1652   \]
1653 < which can be used to describe dynamic caging effect. The other
1654 < extreme is the bath that responds infinitely quickly to motions in
1655 < the system. Thus, $\xi (t)$ can be taken as a $delta$ function in
1656 < time:
1653 > which can be used to describe the effect of dynamic caging in
1654 > viscous solvents. The other extreme is the bath that responds
1655 > infinitely quickly to motions in the system. Thus, $\xi (t)$ can be
1656 > taken as a $delta$ function in time:
1657   \[
1658   \xi (t) = 2\xi _0 \delta (t)
1659   \]
# Line 1740 | Line 1662 | and Equation \ref{introEuqation:GeneralizedLangevinDyn
1662   \int_0^t {\xi (t)\dot x(t - \tau )d\tau }  = 2\xi _0 \int_0^t
1663   {\delta (t)\dot x(t - \tau )d\tau }  = \xi _0 \dot x(t),
1664   \]
1665 < and Equation \ref{introEuqation:GeneralizedLangevinDynamics} becomes
1665 > and Eq.~\ref{introEuqation:GeneralizedLangevinDynamics} becomes
1666   \begin{equation}
1667   m\ddot x =  - \frac{{\partial W(x)}}{{\partial x}} - \xi _0 \dot
1668   x(t) + R(t) \label{introEquation:LangevinEquation}
1669   \end{equation}
1670   which is known as the Langevin equation. The static friction
1671   coefficient $\xi _0$ can either be calculated from spectral density
1672 < or be determined by Stokes' law for regular shaped particles.A
1672 > or be determined by Stokes' law for regular shaped particles. A
1673   briefly review on calculating friction tensor for arbitrary shaped
1674   particles is given in Sec.~\ref{introSection:frictionTensor}.
1675  
1676 < \subsubsection{\label{introSection:secondFluctuationDissipation}The Second Fluctuation Dissipation Theorem}
1676 > \subsubsection{\label{introSection:secondFluctuationDissipation}\textbf{The Second Fluctuation Dissipation Theorem}}
1677  
1678   Defining a new set of coordinates,
1679   \[
# Line 1763 | Line 1685 | And since the $q$ coordinates are harmonic oscillators
1685   R(t) = \sum\limits_{\alpha  = 1}^N {g_\alpha  q_\alpha  (t)}.
1686   \]
1687   And since the $q$ coordinates are harmonic oscillators,
1688 < \[
1689 < \begin{array}{c}
1690 < \left\langle {q_\alpha ^2 } \right\rangle  = \frac{{kT}}{{m_\alpha  \omega _\alpha ^2 }} \\
1691 < \left\langle {q_\alpha  (t)q_\alpha  (0)} \right\rangle  = \left\langle {q_\alpha ^2 (0)} \right\rangle \cos (\omega _\alpha  t) \\
1692 < \left\langle {q_\alpha  (t)q_\beta  (0)} \right\rangle  = \delta _{\alpha \beta } \left\langle {q_\alpha  (t)q_\alpha  (0)} \right\rangle  \\
1693 < \left\langle {R(t)R(0)} \right\rangle  = \sum\limits_\alpha  {\sum\limits_\beta  {g_\alpha  g_\beta  \left\langle {q_\alpha  (t)q_\beta  (0)} \right\rangle } }  \\
1694 <  = \sum\limits_\alpha  {g_\alpha ^2 \left\langle {q_\alpha ^2 (0)} \right\rangle \cos (\omega _\alpha  t)}  \\
1695 <  = kT\xi (t) \\
1774 < \end{array}
1775 < \]
1688 > \begin{eqnarray*}
1689 > \left\langle {q_\alpha ^2 } \right\rangle  & = & \frac{{kT}}{{m_\alpha  \omega _\alpha ^2 }} \\
1690 > \left\langle {q_\alpha  (t)q_\alpha  (0)} \right\rangle & = & \left\langle {q_\alpha ^2 (0)} \right\rangle \cos (\omega _\alpha  t) \\
1691 > \left\langle {q_\alpha  (t)q_\beta  (0)} \right\rangle & = &\delta _{\alpha \beta } \left\langle {q_\alpha  (t)q_\alpha  (0)} \right\rangle  \\
1692 > \left\langle {R(t)R(0)} \right\rangle & = & \sum\limits_\alpha  {\sum\limits_\beta  {g_\alpha  g_\beta  \left\langle {q_\alpha  (t)q_\beta  (0)} \right\rangle } }  \\
1693 >  & = &\sum\limits_\alpha  {g_\alpha ^2 \left\langle {q_\alpha ^2 (0)} \right\rangle \cos (\omega _\alpha  t)}  \\
1694 >  & = &kT\xi (t) \\
1695 > \end{eqnarray*}
1696   Thus, we recover the \emph{second fluctuation dissipation theorem}
1697   \begin{equation}
1698   \xi (t) = \left\langle {R(t)R(0)} \right\rangle
# Line 1780 | Line 1700 | can model the random force and friction kernel.
1700   \end{equation}
1701   In effect, it acts as a constraint on the possible ways in which one
1702   can model the random force and friction kernel.
1783
1784 \subsection{\label{introSection:frictionTensor} Friction Tensor}
1785 Theoretically, the friction kernel can be determined using velocity
1786 autocorrelation function. However, this approach become impractical
1787 when the system become more and more complicate. Instead, various
1788 approaches based on hydrodynamics have been developed to calculate
1789 the friction coefficients. The friction effect is isotropic in
1790 Equation, \zeta can be taken as a scalar. In general, friction
1791 tensor \Xi is a $6\times 6$ matrix given by
1792 \[
1793 \Xi  = \left( {\begin{array}{*{20}c}
1794   {\Xi _{}^{tt} } & {\Xi _{}^{rt} }  \\
1795   {\Xi _{}^{tr} } & {\Xi _{}^{rr} }  \\
1796 \end{array}} \right).
1797 \]
1798 Here, $ {\Xi^{tt} }$ and $ {\Xi^{rr} }$ are translational friction
1799 tensor and rotational resistance (friction) tensor respectively,
1800 while ${\Xi^{tr} }$ is translation-rotation coupling tensor and $
1801 {\Xi^{rt} }$ is rotation-translation coupling tensor. When a
1802 particle moves in a fluid, it may experience friction force or
1803 torque along the opposite direction of the velocity or angular
1804 velocity,
1805 \[
1806 \left( \begin{array}{l}
1807 F_R  \\
1808 \tau _R  \\
1809 \end{array} \right) =  - \left( {\begin{array}{*{20}c}
1810   {\Xi ^{tt} } & {\Xi ^{rt} }  \\
1811   {\Xi ^{tr} } & {\Xi ^{rr} }  \\
1812 \end{array}} \right)\left( \begin{array}{l}
1813 v \\
1814 w \\
1815 \end{array} \right)
1816 \]
1817 where $F_r$ is the friction force and $\tau _R$ is the friction
1818 toque.
1819
1820 \subsubsection{\label{introSection:resistanceTensorRegular}The Resistance Tensor for Regular Shape}
1821
1822 For a spherical particle, the translational and rotational friction
1823 constant can be calculated from Stoke's law,
1824 \[
1825 \Xi ^{tt}  = \left( {\begin{array}{*{20}c}
1826   {6\pi \eta R} & 0 & 0  \\
1827   0 & {6\pi \eta R} & 0  \\
1828   0 & 0 & {6\pi \eta R}  \\
1829 \end{array}} \right)
1830 \]
1831 and
1832 \[
1833 \Xi ^{rr}  = \left( {\begin{array}{*{20}c}
1834   {8\pi \eta R^3 } & 0 & 0  \\
1835   0 & {8\pi \eta R^3 } & 0  \\
1836   0 & 0 & {8\pi \eta R^3 }  \\
1837 \end{array}} \right)
1838 \]
1839 where $\eta$ is the viscosity of the solvent and $R$ is the
1840 hydrodynamics radius.
1841
1842 Other non-spherical shape, such as cylinder and ellipsoid
1843 \textit{etc}, are widely used as reference for developing new
1844 hydrodynamics theory, because their properties can be calculated
1845 exactly. In 1936, Perrin extended Stokes's law to general ellipsoid,
1846 also called a triaxial ellipsoid, which is given in Cartesian
1847 coordinates by
1848 \[
1849 \frac{{x^2 }}{{a^2 }} + \frac{{y^2 }}{{b^2 }} + \frac{{z^2 }}{{c^2
1850 }} = 1
1851 \]
1852 where the semi-axes are of lengths $a$, $b$, and $c$. Unfortunately,
1853 due to the complexity of the elliptic integral, only the ellipsoid
1854 with the restriction of two axes having to be equal, \textit{i.e.}
1855 prolate($ a \ge b = c$) and oblate ($ a < b = c $), can be solved
1856 exactly. Introducing an elliptic integral parameter $S$ for prolate,
1857 \[
1858 S = \frac{2}{{\sqrt {a^2  - b^2 } }}\ln \frac{{a + \sqrt {a^2  - b^2
1859 } }}{b},
1860 \]
1861 and oblate,
1862 \[
1863 S = \frac{2}{{\sqrt {b^2  - a^2 } }}arctg\frac{{\sqrt {b^2  - a^2 }
1864 }}{a}
1865 \],
1866 one can write down the translational and rotational resistance
1867 tensors
1868 \[
1869 \begin{array}{l}
1870 \Xi _a^{tt}  = 16\pi \eta \frac{{a^2  - b^2 }}{{(2a^2  - b^2 )S - 2a}} \\
1871 \Xi _b^{tt}  = \Xi _c^{tt}  = 32\pi \eta \frac{{a^2  - b^2 }}{{(2a^2  - 3b^2 )S + 2a}} \\
1872 \end{array},
1873 \]
1874 and
1875 \[
1876 \begin{array}{l}
1877 \Xi _a^{rr}  = \frac{{32\pi }}{3}\eta \frac{{(a^2  - b^2 )b^2 }}{{2a - b^2 S}} \\
1878 \Xi _b^{rr}  = \Xi _c^{rr}  = \frac{{32\pi }}{3}\eta \frac{{(a^4  - b^4 )}}{{(2a^2  - b^2 )S - 2a}} \\
1879 \end{array}.
1880 \]
1881
1882 \subsubsection{\label{introSection:resistanceTensorRegularArbitrary}The Resistance Tensor for Arbitrary Shape}
1883
1884 Unlike spherical and other regular shaped molecules, there is not
1885 analytical solution for friction tensor of any arbitrary shaped
1886 rigid molecules. The ellipsoid of revolution model and general
1887 triaxial ellipsoid model have been used to approximate the
1888 hydrodynamic properties of rigid bodies. However, since the mapping
1889 from all possible ellipsoidal space, $r$-space, to all possible
1890 combination of rotational diffusion coefficients, $D$-space is not
1891 unique\cite{Wegener79} as well as the intrinsic coupling between
1892 translational and rotational motion of rigid body\cite{}, general
1893 ellipsoid is not always suitable for modeling arbitrarily shaped
1894 rigid molecule. A number of studies have been devoted to determine
1895 the friction tensor for irregularly shaped rigid bodies using more
1896 advanced method\cite{} where the molecule of interest was modeled by
1897 combinations of spheres(beads)\cite{} and the hydrodynamics
1898 properties of the molecule can be calculated using the hydrodynamic
1899 interaction tensor. Let us consider a rigid assembly of $N$ beads
1900 immersed in a continuous medium. Due to hydrodynamics interaction,
1901 the ``net'' velocity of $i$th bead, $v'_i$ is different than its
1902 unperturbed velocity $v_i$,
1903 \[
1904 v'_i  = v_i  - \sum\limits_{j \ne i} {T_{ij} F_j }
1905 \]
1906 where $F_i$ is the frictional force, and $T_{ij}$ is the
1907 hydrodynamic interaction tensor. The friction force of $i$th bead is
1908 proportional to its ``net'' velocity
1909 \begin{equation}
1910 F_i  = \zeta _i v_i  - \zeta _i \sum\limits_{j \ne i} {T_{ij} F_j }.
1911 \label{introEquation:tensorExpression}
1912 \end{equation}
1913 This equation is the basis for deriving the hydrodynamic tensor. In
1914 1930, Oseen and Burgers gave a simple solution to Equation
1915 \ref{introEquation:tensorExpression}
1916 \begin{equation}
1917 T_{ij}  = \frac{1}{{8\pi \eta r_{ij} }}\left( {I + \frac{{R_{ij}
1918 R_{ij}^T }}{{R_{ij}^2 }}} \right).
1919 \label{introEquation:oseenTensor}
1920 \end{equation}
1921 Here $R_{ij}$ is the distance vector between bead $i$ and bead $j$.
1922 A second order expression for element of different size was
1923 introduced by Rotne and Prager\cite{} and improved by Garc\'{i}a de
1924 la Torre and Bloomfield,
1925 \begin{equation}
1926 T_{ij}  = \frac{1}{{8\pi \eta R_{ij} }}\left[ {\left( {I +
1927 \frac{{R_{ij} R_{ij}^T }}{{R_{ij}^2 }}} \right) + R\frac{{\sigma
1928 _i^2  + \sigma _j^2 }}{{r_{ij}^2 }}\left( {\frac{I}{3} -
1929 \frac{{R_{ij} R_{ij}^T }}{{R_{ij}^2 }}} \right)} \right].
1930 \label{introEquation:RPTensorNonOverlapped}
1931 \end{equation}
1932 Both of the Equation \ref{introEquation:oseenTensor} and Equation
1933 \ref{introEquation:RPTensorNonOverlapped} have an assumption $R_{ij}
1934 \ge \sigma _i  + \sigma _j$. An alternative expression for
1935 overlapping beads with the same radius, $\sigma$, is given by
1936 \begin{equation}
1937 T_{ij}  = \frac{1}{{6\pi \eta R_{ij} }}\left[ {\left( {1 -
1938 \frac{2}{{32}}\frac{{R_{ij} }}{\sigma }} \right)I +
1939 \frac{2}{{32}}\frac{{R_{ij} R_{ij}^T }}{{R_{ij} \sigma }}} \right]
1940 \label{introEquation:RPTensorOverlapped}
1941 \end{equation}
1942
1943 To calculate the resistance tensor at an arbitrary origin $O$, we
1944 construct a $3N \times 3N$ matrix consisting of $N \times N$
1945 $B_{ij}$ blocks
1946 \begin{equation}
1947 B = \left( {\begin{array}{*{20}c}
1948   {B_{11} } &  \ldots  & {B_{1N} }  \\
1949    \vdots  &  \ddots  &  \vdots   \\
1950   {B_{N1} } &  \cdots  & {B_{NN} }  \\
1951 \end{array}} \right),
1952 \end{equation}
1953 where $B_{ij}$ is given by
1954 \[
1955 B_{ij}  = \delta _{ij} \frac{I}{{6\pi \eta R}} + (1 - \delta _{ij}
1956 )T_{ij}
1957 \]
1958 where $\delta _{ij}$ is Kronecker delta function. Inverting matrix
1959 $B$, we obtain
1960
1961 \[
1962 C = B^{ - 1}  = \left( {\begin{array}{*{20}c}
1963   {C_{11} } &  \ldots  & {C_{1N} }  \\
1964    \vdots  &  \ddots  &  \vdots   \\
1965   {C_{N1} } &  \cdots  & {C_{NN} }  \\
1966 \end{array}} \right)
1967 \]
1968 , which can be partitioned into $N \times N$ $3 \times 3$ block
1969 $C_{ij}$. With the help of $C_{ij}$ and skew matrix $U_i$
1970 \[
1971 U_i  = \left( {\begin{array}{*{20}c}
1972   0 & { - z_i } & {y_i }  \\
1973   {z_i } & 0 & { - x_i }  \\
1974   { - y_i } & {x_i } & 0  \\
1975 \end{array}} \right)
1976 \]
1977 where $x_i$, $y_i$, $z_i$ are the components of the vector joining
1978 bead $i$ and origin $O$. Hence, the elements of resistance tensor at
1979 arbitrary origin $O$ can be written as
1980 \begin{equation}
1981 \begin{array}{l}
1982 \Xi _{}^{tt}  = \sum\limits_i {\sum\limits_j {C_{ij} } } , \\
1983 \Xi _{}^{tr}  = \Xi _{}^{rt}  = \sum\limits_i {\sum\limits_j {U_i C_{ij} } } , \\
1984 \Xi _{}^{rr}  =  - \sum\limits_i {\sum\limits_j {U_i C_{ij} } } U_j  \\
1985 \end{array}
1986 \label{introEquation:ResistanceTensorArbitraryOrigin}
1987 \end{equation}
1988
1989 The resistance tensor depends on the origin to which they refer. The
1990 proper location for applying friction force is the center of
1991 resistance (reaction), at which the trace of rotational resistance
1992 tensor, $ \Xi ^{rr}$ reaches minimum. Mathematically, the center of
1993 resistance is defined as an unique point of the rigid body at which
1994 the translation-rotation coupling tensor are symmetric,
1995 \begin{equation}
1996 \Xi^{tr}  = \left( {\Xi^{tr} } \right)^T
1997 \label{introEquation:definitionCR}
1998 \end{equation}
1999 Form Equation \ref{introEquation:ResistanceTensorArbitraryOrigin},
2000 we can easily find out that the translational resistance tensor is
2001 origin independent, while the rotational resistance tensor and
2002 translation-rotation coupling resistance tensor depend on the
2003 origin. Given resistance tensor at an arbitrary origin $O$, and a
2004 vector ,$r_{OP}(x_{OP}, y_{OP}, z_{OP})$, from $O$ to $P$, we can
2005 obtain the resistance tensor at $P$ by
2006 \begin{equation}
2007 \begin{array}{l}
2008 \Xi _P^{tt}  = \Xi _O^{tt}  \\
2009 \Xi _P^{tr}  = \Xi _P^{rt}  = \Xi _O^{tr}  - U_{OP} \Xi _O^{tt}  \\
2010 \Xi _P^{rr}  = \Xi _O^{rr}  - U_{OP} \Xi _O^{tt} U_{OP}  + \Xi _O^{tr} U_{OP}  - U_{OP} \Xi _O^{tr} ^{^T }  \\
2011 \end{array}
2012 \label{introEquation:resistanceTensorTransformation}
2013 \end{equation}
2014 where
2015 \[
2016 U_{OP}  = \left( {\begin{array}{*{20}c}
2017   0 & { - z_{OP} } & {y_{OP} }  \\
2018   {z_i } & 0 & { - x_{OP} }  \\
2019   { - y_{OP} } & {x_{OP} } & 0  \\
2020 \end{array}} \right)
2021 \]
2022 Using Equations \ref{introEquation:definitionCR} and
2023 \ref{introEquation:resistanceTensorTransformation}, one can locate
2024 the position of center of resistance,
2025 \[
2026 \left( \begin{array}{l}
2027 x_{OR}  \\
2028 y_{OR}  \\
2029 z_{OR}  \\
2030 \end{array} \right) = \left( {\begin{array}{*{20}c}
2031   {(\Xi _O^{rr} )_{yy}  + (\Xi _O^{rr} )_{zz} } & { - (\Xi _O^{rr} )_{xy} } & { - (\Xi _O^{rr} )_{xz} }  \\
2032   { - (\Xi _O^{rr} )_{xy} } & {(\Xi _O^{rr} )_{zz}  + (\Xi _O^{rr} )_{xx} } & { - (\Xi _O^{rr} )_{yz} }  \\
2033   { - (\Xi _O^{rr} )_{xz} } & { - (\Xi _O^{rr} )_{yz} } & {(\Xi _O^{rr} )_{xx}  + (\Xi _O^{rr} )_{yy} }  \\
2034 \end{array}} \right)^{ - 1} \left( \begin{array}{l}
2035 (\Xi _O^{tr} )_{yz}  - (\Xi _O^{tr} )_{zy}  \\
2036 (\Xi _O^{tr} )_{zx}  - (\Xi _O^{tr} )_{xz}  \\
2037 (\Xi _O^{tr} )_{xy}  - (\Xi _O^{tr} )_{yx}  \\
2038 \end{array} \right).
2039 \]
2040 where $x_OR$, $y_OR$, $z_OR$ are the components of the vector
2041 joining center of resistance $R$ and origin $O$.

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