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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}
35   \label{introEquation:newtonThirdLaw}
# Line 46 | Line 46 | N \equiv r \times F \label{introEquation:torqueDefinit
46   \end{equation}
47   The torque $\tau$ with respect to the same origin is defined to be
48   \begin{equation}
49 < N \equiv r \times F \label{introEquation:torqueDefinition}
49 > \tau \equiv r \times F \label{introEquation:torqueDefinition}
50   \end{equation}
51   Differentiating Eq.~\ref{introEquation:angularMomentumDefinition},
52   \[
# Line 59 | Line 59 | thus,
59   \]
60   thus,
61   \begin{equation}
62 < \dot L = r \times \dot p = N
62 > \dot L = r \times \dot p = \tau
63   \end{equation}
64   If there are no external torques acting on a body, the angular
65   momentum of it is conserved. The last conservation theorem state
# Line 68 | Line 68 | scheme for rigid body \cite{Dullweber1997}.
68   \end{equation}
69   is conserved. All of these conserved quantities are
70   important factors to determine the quality of numerical integration
71 < scheme for rigid body \cite{Dullweber1997}.
71 > schemes for rigid bodies \cite{Dullweber1997}.
72  
73   \subsection{\label{introSection:lagrangian}Lagrangian Mechanics}
74  
75 < Newtonian Mechanics suffers from two important limitations: it
76 < describes their motion in special cartesian coordinate systems.
77 < Another limitation of Newtonian mechanics becomes obvious when we
78 < try to describe systems with large numbers of particles. It becomes
79 < very difficult to predict the properties of the system by carrying
80 < out calculations involving the each individual interaction between
81 < 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.
75 > Newtonian Mechanics suffers from two important limitations: motions
76 > can only be described in cartesian coordinate systems. Moreover, it
77 > becomes impossible to predict analytically the properties of the
78 > system even if we know all of the details of the interaction. In
79 > order to overcome some of the practical difficulties which arise in
80 > attempts to apply Newton's equation to complex system, approximate
81 > numerical procedures may be developed.
82  
83 < \subsubsection{\label{introSection:halmiltonPrinciple}Hamilton's
84 < Principle}
83 > \subsubsection{\label{introSection:halmiltonPrinciple}\textbf{Hamilton's
84 > Principle}}
85  
86   Hamilton introduced the dynamical principle upon which it is
87 < possible to base all of mechanics and, indeed, most of classical
88 < physics. Hamilton's Principle may be stated as follow,
87 > possible to base all of mechanics and most of classical physics.
88 > Hamilton's Principle may be stated as follows,
89  
90   The actual trajectory, along which a dynamical system may move from
91   one point to another within a specified time, is derived by finding
92   the path which minimizes the time integral of the difference between
93 < the kinetic, $K$, and potential energies, $U$ \cite{Tolman1979}.
93 > the kinetic, $K$, and potential energies, $U$.
94   \begin{equation}
95   \delta \int_{t_1 }^{t_2 } {(K - U)dt = 0} ,
96   \label{introEquation:halmitonianPrinciple1}
97   \end{equation}
98  
99   For simple mechanical systems, where the forces acting on the
100 < different part are derivable from a potential and the velocities are
101 < small compared with that of light, the Lagrangian function $L$ can
102 < be define as the difference between the kinetic energy of the system
106 < and its potential energy,
100 > different parts are derivable from a potential, the Lagrangian
101 > function $L$ can be defined as the difference between the kinetic
102 > energy of the system and its potential energy,
103   \begin{equation}
104   L \equiv K - U = L(q_i ,\dot q_i ) ,
105   \label{introEquation:lagrangianDef}
# Line 114 | Line 110 | then Eq.~\ref{introEquation:halmitonianPrinciple1} bec
110   \label{introEquation:halmitonianPrinciple2}
111   \end{equation}
112  
113 < \subsubsection{\label{introSection:equationOfMotionLagrangian}The
114 < Equations of Motion in Lagrangian Mechanics}
113 > \subsubsection{\label{introSection:equationOfMotionLagrangian}\textbf{The
114 > Equations of Motion in Lagrangian Mechanics}}
115  
116 < For a holonomic system of $f$ degrees of freedom, the equations of
117 < motion in the Lagrangian form is
116 > For a system of $f$ degrees of freedom, the equations of motion in
117 > the Lagrangian form is
118   \begin{equation}
119   \frac{d}{{dt}}\frac{{\partial L}}{{\partial \dot q_i }} -
120   \frac{{\partial L}}{{\partial q_i }} = 0,{\rm{ }}i = 1, \ldots,f
# Line 132 | Line 128 | independent of generalized velocities, the generalized
128   Arising from Lagrangian Mechanics, Hamiltonian Mechanics was
129   introduced by William Rowan Hamilton in 1833 as a re-formulation of
130   classical mechanics. If the potential energy of a system is
131 < independent of generalized velocities, the generalized momenta can
136 < be defined as
131 > independent of velocities, the momenta can be defined as
132   \begin{equation}
133   p_i = \frac{\partial L}{\partial \dot q_i}
134   \label{introEquation:generalizedMomenta}
# Line 172 | Line 167 | find
167   By identifying the coefficients of $dq_k$, $dp_k$ and dt, we can
168   find
169   \begin{equation}
170 < \frac{{\partial H}}{{\partial p_k }} = q_k
170 > \frac{{\partial H}}{{\partial p_k }} = \dot {q_k}
171   \label{introEquation:motionHamiltonianCoordinate}
172   \end{equation}
173   \begin{equation}
174 < \frac{{\partial H}}{{\partial q_k }} =  - p_k
174 > \frac{{\partial H}}{{\partial q_k }} =  - \dot {p_k}
175   \label{introEquation:motionHamiltonianMomentum}
176   \end{equation}
177   and
# Line 193 | Line 188 | function of the generalized velocities $\dot q_i$ and
188  
189   An important difference between Lagrangian approach and the
190   Hamiltonian approach is that the Lagrangian is considered to be a
191 < function of the generalized velocities $\dot q_i$ and the
192 < generalized coordinates $q_i$, while the Hamiltonian is considered
193 < to be a function of the generalized momenta $p_i$ and the conjugate
194 < generalized coordinate $q_i$. Hamiltonian Mechanics is more
195 < appropriate for application to statistical mechanics and quantum
196 < mechanics, since it treats the coordinate and its time derivative as
197 < independent variables and it only works with 1st-order differential
203 < equations\cite{Marion1990}.
191 > function of the generalized velocities $\dot q_i$ and coordinates
192 > $q_i$, while the Hamiltonian is considered to be a function of the
193 > generalized momenta $p_i$ and the conjugate coordinates $q_i$.
194 > Hamiltonian Mechanics is more appropriate for application to
195 > statistical mechanics and quantum mechanics, since it treats the
196 > coordinate and its time derivative as independent variables and it
197 > only works with 1st-order differential equations\cite{Marion1990}.
198  
199   In Newtonian Mechanics, a system described by conservative forces
200   conserves the total energy \ref{introEquation:energyConservation}.
# Line 230 | Line 224 | momentum variables. Consider a dynamic system in a car
224   possible states. Each possible state of the system corresponds to
225   one unique point in the phase space. For mechanical systems, the
226   phase space usually consists of all possible values of position and
227 < momentum variables. Consider a dynamic system in a cartesian space,
228 < where each of the $6f$ coordinates and momenta is assigned to one of
229 < $6f$ mutually orthogonal axes, the phase space of this system is a
230 < $6f$ dimensional space. A point, $x = (q_1 , \ldots ,q_f ,p_1 ,
231 < \ldots ,p_f )$, with a unique set of values of $6f$ coordinates and
232 < momenta is a phase space vector.
227 > momentum variables. Consider a dynamic system of $f$ particles in a
228 > cartesian space, where each of the $6f$ coordinates and momenta is
229 > assigned to one of $6f$ mutually orthogonal axes, the phase space of
230 > this system is a $6f$ dimensional space. A point, $x = (\rightarrow
231 > q_1 , \ldots ,\rightarrow q_f ,\rightarrow p_1 , \ldots ,\rightarrow
232 > p_f )$, with a unique set of values of $6f$ coordinates and momenta
233 > is a phase space vector.
234 > %%%fix me
235  
236 < 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
236 > In statistical mechanics, the condition of an ensemble at any time
237   can be regarded as appropriately specified by the density $\rho$
238   with which representative points are distributed over the phase
239 < space. The density of distribution for an ensemble with $f$ degrees
240 < of freedom is defined as,
239 > space. The density distribution for an ensemble with $f$ degrees of
240 > freedom is defined as,
241   \begin{equation}
242   \rho  = \rho (q_1 , \ldots ,q_f ,p_1 , \ldots ,p_f ,t).
243   \label{introEquation:densityDistribution}
244   \end{equation}
245   Governed by the principles of mechanics, the phase points change
246 < their value which would change the density at any time at phase
247 < space. Hence, the density of distribution is also to be taken as a
246 > their locations which would change the density at any time at phase
247 > space. Hence, the density distribution is also to be taken as a
248   function of the time.
249  
250   The number of systems $\delta N$ at time $t$ can be determined by,
# Line 273 | Line 252 | Assuming a large enough population of systems are expl
252   \delta N = \rho (q,p,t)dq_1  \ldots dq_f dp_1  \ldots dp_f.
253   \label{introEquation:deltaN}
254   \end{equation}
255 < Assuming a large enough population of systems are exploited, we can
256 < sufficiently approximate $\delta N$ without introducing
257 < discontinuity when we go from one region in the phase space to
258 < another. By integrating over the whole phase space,
255 > Assuming a large enough population of systems, we can sufficiently
256 > approximate $\delta N$ without introducing discontinuity when we go
257 > from one region in the phase space to another. By integrating over
258 > the whole phase space,
259   \begin{equation}
260   N = \int { \ldots \int {\rho (q,p,t)dq_1 } ...dq_f dp_1 } ...dp_f
261   \label{introEquation:totalNumberSystem}
# Line 288 | Line 267 | With the help of Equation(\ref{introEquation:unitProba
267   {\rho (q,p,t)dq_1 } ...dq_f dp_1 } ...dp_f }}.
268   \label{introEquation:unitProbability}
269   \end{equation}
270 < With the help of Equation(\ref{introEquation:unitProbability}) and
271 < the knowledge of the system, it is possible to calculate the average
270 > With the help of Eq.~\ref{introEquation:unitProbability} and the
271 > knowledge of the system, it is possible to calculate the average
272   value of any desired quantity which depends on the coordinates and
273   momenta of the system. Even when the dynamics of the real system is
274   complex, or stochastic, or even discontinuous, the average
275 < properties of the ensemble of possibilities as a whole may still
276 < remain well defined. For a classical system in thermal equilibrium
277 < with its environment, the ensemble average of a mechanical quantity,
278 < $\langle A(q , p) \rangle_t$, takes the form of an integral over the
279 < phase space of the system,
275 > properties of the ensemble of possibilities as a whole remaining
276 > well defined. For a classical system in thermal equilibrium with its
277 > environment, the ensemble average of a mechanical quantity, $\langle
278 > A(q , p) \rangle_t$, takes the form of an integral over the phase
279 > space of the system,
280   \begin{equation}
281   \langle  A(q , p) \rangle_t = \frac{{\int { \ldots \int {A(q,p)\rho
282   (q,p,t)dq_1 } ...dq_f dp_1 } ...dp_f }}{{\int { \ldots \int {\rho
# Line 307 | Line 286 | parameters, such as temperature \textit{etc}, partitio
286  
287   There are several different types of ensembles with different
288   statistical characteristics. As a function of macroscopic
289 < parameters, such as temperature \textit{etc}, partition function can
290 < be used to describe the statistical properties of a system in
289 > parameters, such as temperature \textit{etc}, the partition function
290 > can be used to describe the statistical properties of a system in
291   thermodynamic equilibrium.
292  
293   As an ensemble of systems, each of which is known to be thermally
294 < isolated and conserve energy, Microcanonical ensemble(NVE) has a
295 < partition function like,
294 > isolated and conserve energy, the Microcanonical ensemble (NVE) has
295 > a partition function like,
296   \begin{equation}
297   \Omega (N,V,E) = e^{\beta TS} \label{introEquation:NVEPartition}.
298   \end{equation}
299 < A canonical ensemble(NVT)is an ensemble of systems, each of which
299 > A canonical ensemble (NVT)is an ensemble of systems, each of which
300   can share its energy with a large heat reservoir. The distribution
301   of the total energy amongst the possible dynamical states is given
302   by the partition function,
# Line 326 | Line 305 | TS$. Since most experiment are carried out under const
305   \label{introEquation:NVTPartition}
306   \end{equation}
307   Here, $A$ is the Helmholtz free energy which is defined as $ A = U -
308 < TS$. Since most experiment are carried out under constant pressure
309 < condition, isothermal-isobaric ensemble(NPT) play a very important
310 < role in molecular simulation. The isothermal-isobaric ensemble allow
311 < the system to exchange energy with a heat bath of temperature $T$
312 < and to change the volume as well. Its partition function is given as
308 > TS$. Since most experiments are carried out under constant pressure
309 > condition, the isothermal-isobaric ensemble (NPT) plays a very
310 > important role in molecular simulations. The isothermal-isobaric
311 > ensemble allow the system to exchange energy with a heat bath of
312 > temperature $T$ and to change the volume as well. Its partition
313 > function is given as
314   \begin{equation}
315   \Delta (N,P,T) =  - e^{\beta G}.
316   \label{introEquation:NPTPartition}
# Line 339 | Line 319 | The Liouville's theorem is the foundation on which sta
319  
320   \subsection{\label{introSection:liouville}Liouville's theorem}
321  
322 < The Liouville's theorem is the foundation on which statistical
323 < mechanics rests. It describes the time evolution of phase space
322 > Liouville's theorem is the foundation on which statistical mechanics
323 > rests. It describes the time evolution of the phase space
324   distribution function. In order to calculate the rate of change of
325 < $\rho$, we begin from Equation(\ref{introEquation:deltaN}). If we
326 < consider the two faces perpendicular to the $q_1$ axis, which are
327 < located at $q_1$ and $q_1 + \delta q_1$, the number of phase points
328 < leaving the opposite face is given by the expression,
325 > $\rho$, we begin from Eq.~\ref{introEquation:deltaN}. If we consider
326 > the two faces perpendicular to the $q_1$ axis, which are located at
327 > $q_1$ and $q_1 + \delta q_1$, the number of phase points leaving the
328 > opposite face is given by the expression,
329   \begin{equation}
330   \left( {\rho  + \frac{{\partial \rho }}{{\partial q_1 }}\delta q_1 }
331   \right)\left( {\dot q_1  + \frac{{\partial \dot q_1 }}{{\partial q_1
# Line 369 | Line 349 | divining $ \delta q_1  \ldots \delta q_f \delta p_1  \
349   + \frac{{\partial \dot p_i }}{{\partial p_i }}} \right)}  = 0 ,
350   \end{equation}
351   which cancels the first terms of the right hand side. Furthermore,
352 < divining $ \delta q_1  \ldots \delta q_f \delta p_1  \ldots \delta
352 > dividing $ \delta q_1  \ldots \delta q_f \delta p_1  \ldots \delta
353   p_f $ in both sides, we can write out Liouville's theorem in a
354   simple form,
355   \begin{equation}
# Line 381 | Line 361 | statistical mechanics, since the number of particles i
361  
362   Liouville's theorem states that the distribution function is
363   constant along any trajectory in phase space. In classical
364 < statistical mechanics, since the number of particles in the system
365 < is huge, we may be able to believe the system is stationary,
364 > statistical mechanics, since the number of members in an ensemble is
365 > huge and constant, we can assume the local density has no reason
366 > (other than classical mechanics) to change,
367   \begin{equation}
368   \frac{{\partial \rho }}{{\partial t}} = 0.
369   \label{introEquation:stationary}
# Line 395 | Line 376 | distribution,
376   \label{introEquation:densityAndHamiltonian}
377   \end{equation}
378  
379 < \subsubsection{\label{introSection:phaseSpaceConservation}Conservation of Phase Space}
379 > \subsubsection{\label{introSection:phaseSpaceConservation}\textbf{Conservation of Phase Space}}
380   Lets consider a region in the phase space,
381   \begin{equation}
382   \delta v = \int { \ldots \int {dq_1 } ...dq_f dp_1 } ..dp_f .
383   \end{equation}
384   If this region is small enough, the density $\rho$ can be regarded
385 < as uniform over the whole phase space. Thus, the number of phase
386 < points inside this region is given by,
385 > as uniform over the whole integral. Thus, the number of phase points
386 > inside this region is given by,
387   \begin{equation}
388   \delta N = \rho \delta v = \rho \int { \ldots \int {dq_1 } ...dq_f
389   dp_1 } ..dp_f.
# Line 414 | Line 395 | With the help of stationary assumption
395   \end{equation}
396   With the help of stationary assumption
397   (\ref{introEquation:stationary}), we obtain the principle of the
398 < \emph{conservation of extension in phase space},
398 > \emph{conservation of volume in phase space},
399   \begin{equation}
400   \frac{d}{{dt}}(\delta v) = \frac{d}{{dt}}\int { \ldots \int {dq_1 }
401   ...dq_f dp_1 } ..dp_f  = 0.
402   \label{introEquation:volumePreserving}
403   \end{equation}
404  
405 < \subsubsection{\label{introSection:liouvilleInOtherForms}Liouville's Theorem in Other Forms}
405 > \subsubsection{\label{introSection:liouvilleInOtherForms}\textbf{Liouville's Theorem in Other Forms}}
406  
407   Liouville's theorem can be expresses in a variety of different forms
408   which are convenient within different contexts. For any two function
# Line 435 | Line 416 | Substituting equations of motion in Hamiltonian formal
416   \label{introEquation:poissonBracket}
417   \end{equation}
418   Substituting equations of motion in Hamiltonian formalism(
419 < \ref{introEquation:motionHamiltonianCoordinate} ,
420 < \ref{introEquation:motionHamiltonianMomentum} ) into
421 < (\ref{introEquation:liouvilleTheorem}), we can rewrite Liouville's
422 < theorem using Poisson bracket notion,
419 > Eq.~\ref{introEquation:motionHamiltonianCoordinate} ,
420 > Eq.~\ref{introEquation:motionHamiltonianMomentum} ) into
421 > (Eq.~\ref{introEquation:liouvilleTheorem}), we can rewrite
422 > Liouville's theorem using Poisson bracket notion,
423   \begin{equation}
424   \left( {\frac{{\partial \rho }}{{\partial t}}} \right) =  - \left\{
425   {\rho ,H} \right\}.
# Line 463 | Line 444 | simulation and the quality of the underlying model. Ho
444   Various thermodynamic properties can be calculated from Molecular
445   Dynamics simulation. By comparing experimental values with the
446   calculated properties, one can determine the accuracy of the
447 < simulation and the quality of the underlying model. However, both of
448 < experiment and computer simulation are usually performed during a
447 > simulation and the quality of the underlying model. However, both
448 > experiments and computer simulations are usually performed during a
449   certain time interval and the measurements are averaged over a
450   period of them which is different from the average behavior of
451 < many-body system in Statistical Mechanics. Fortunately, Ergodic
452 < Hypothesis is proposed to make a connection between time average and
453 < ensemble average. It states that time average and average over the
451 > many-body system in Statistical Mechanics. Fortunately, the Ergodic
452 > Hypothesis makes a connection between time average and the ensemble
453 > average. It states that the time average and average over the
454   statistical ensemble are identical \cite{Frenkel1996, Leach2001}.
455   \begin{equation}
456   \langle A(q , p) \rangle_t = \mathop {\lim }\limits_{t \to \infty }
# Line 491 | Line 472 | A variety of numerical integrators were proposed to si
472   choice\cite{Frenkel1996}.
473  
474   \section{\label{introSection:geometricIntegratos}Geometric Integrators}
475 < A variety of numerical integrators were proposed to simulate the
476 < motions. They usually begin with an initial conditionals and move
477 < the objects in the direction governed by the differential equations.
478 < However, most of them ignore the hidden physical law contained
479 < within the equations. Since 1990, geometric integrators, which
480 < preserve various phase-flow invariants such as symplectic structure,
481 < volume and time reversal symmetry, are developed to address this
482 < issue\cite{Dullweber1997, McLachlan1998, Leimkuhler1999}. The
483 < velocity verlet method, which happens to be a simple example of
484 < symplectic integrator, continues to gain its popularity in molecular
485 < dynamics community. This fact can be partly explained by its
486 < geometric nature.
475 > A variety of numerical integrators have been proposed to simulate
476 > the motions of atoms in MD simulation. They usually begin with
477 > initial conditionals and move the objects in the direction governed
478 > by the differential equations. However, most of them ignore the
479 > hidden physical laws contained within the equations. Since 1990,
480 > geometric integrators, which preserve various phase-flow invariants
481 > such as symplectic structure, volume and time reversal symmetry, are
482 > developed to address this issue\cite{Dullweber1997, McLachlan1998,
483 > Leimkuhler1999}. The velocity Verlet method, which happens to be a
484 > simple example of symplectic integrator, continues to gain
485 > popularity in the molecular dynamics community. This fact can be
486 > partly explained by its geometric nature.
487  
488 < \subsection{\label{introSection:symplecticManifold}Symplectic Manifold}
489 < A \emph{manifold} is an abstract mathematical space. It locally
490 < looks like Euclidean space, but when viewed globally, it may have
491 < more complicate structure. A good example of manifold is the surface
492 < of Earth. It seems to be flat locally, but it is round if viewed as
493 < a whole. A \emph{differentiable manifold} (also known as
494 < \emph{smooth manifold}) is a manifold with an open cover in which
495 < the covering neighborhoods are all smoothly isomorphic to one
496 < another. In other words,it is possible to apply calculus on
516 < \emph{differentiable manifold}. A \emph{symplectic manifold} is
517 < defined as a pair $(M, \omega)$ which consisting of a
488 > \subsection{\label{introSection:symplecticManifold}Symplectic Manifolds}
489 > A \emph{manifold} is an abstract mathematical space. It looks
490 > locally like Euclidean space, but when viewed globally, it may have
491 > more complicated structure. A good example of manifold is the
492 > surface of Earth. It seems to be flat locally, but it is round if
493 > viewed as a whole. A \emph{differentiable manifold} (also known as
494 > \emph{smooth manifold}) is a manifold on which it is possible to
495 > apply calculus on \emph{differentiable manifold}. A \emph{symplectic
496 > manifold} is defined as a pair $(M, \omega)$ which consists of a
497   \emph{differentiable manifold} $M$ and a close, non-degenerated,
498   bilinear symplectic form, $\omega$. A symplectic form on a vector
499   space $V$ is a function $\omega(x, y)$ which satisfies
500   $\omega(\lambda_1x_1+\lambda_2x_2, y) = \lambda_1\omega(x_1, y)+
501   \lambda_2\omega(x_2, y)$, $\omega(x, y) = - \omega(y, x)$ and
502 < $\omega(x, x) = 0$. Cross product operation in vector field is an
503 < example of symplectic form.
502 > $\omega(x, x) = 0$. The cross product operation in vector field is
503 > an example of symplectic form.
504  
505 < One of the motivations to study \emph{symplectic manifold} in
505 > One of the motivations to study \emph{symplectic manifolds} in
506   Hamiltonian Mechanics is that a symplectic manifold can represent
507   all possible configurations of the system and the phase space of the
508   system can be described by it's cotangent bundle. Every symplectic
509   manifold is even dimensional. For instance, in Hamilton equations,
510   coordinate and momentum always appear in pairs.
511  
533 Let  $(M,\omega)$ and $(N, \eta)$ be symplectic manifolds. A map
534 \[
535 f : M \rightarrow N
536 \]
537 is a \emph{symplectomorphism} if it is a \emph{diffeomorphims} and
538 the \emph{pullback} of $\eta$ under f is equal to $\omega$.
539 Canonical transformation is an example of symplectomorphism in
540 classical mechanics.
541
512   \subsection{\label{introSection:ODE}Ordinary Differential Equations}
513  
514 < For a ordinary differential system defined as
514 > For an ordinary differential system defined as
515   \begin{equation}
516   \dot x = f(x)
517   \end{equation}
518 < where $x = x(q,p)^T$, this system is canonical Hamiltonian, if
518 > where $x = x(q,p)^T$, this system is a canonical Hamiltonian, if
519   \begin{equation}
520   f(r) = J\nabla _x H(r).
521   \end{equation}
# Line 605 | Line 575 | Instead, we use a approximate map, $\psi_\tau$, which
575   \end{equation}
576  
577   In most cases, it is not easy to find the exact flow $\varphi_\tau$.
578 < Instead, we use a approximate map, $\psi_\tau$, which is usually
578 > Instead, we use an approximate map, $\psi_\tau$, which is usually
579   called integrator. The order of an integrator $\psi_\tau$ is $p$, if
580   the Taylor series of $\psi_\tau$ agree to order $p$,
581   \begin{equation}
582 < \psi_tau(x) = x + \tau f(x) + O(\tau^{p+1})
582 > \psi_\tau(x) = x + \tau f(x) + O(\tau^{p+1})
583   \end{equation}
584  
585   \subsection{\label{introSection:geometricProperties}Geometric Properties}
586  
587 < The hidden geometric properties\cite{Budd1999, Marsden1998} of ODE
588 < and its flow play important roles in numerical studies. Many of them
589 < can be found in systems which occur naturally in applications.
587 > The hidden geometric properties\cite{Budd1999, Marsden1998} of an
588 > ODE and its flow play important roles in numerical studies. Many of
589 > them can be found in systems which occur naturally in applications.
590  
591   Let $\varphi$ be the flow of Hamiltonian vector field, $\varphi$ is
592   a \emph{symplectic} flow if it satisfies,
# Line 631 | Line 601 | is the property must be preserved by the integrator.
601   \begin{equation}
602   {\varphi '}^T J \varphi ' = J \circ \varphi
603   \end{equation}
604 < is the property must be preserved by the integrator.
604 > is the property that must be preserved by the integrator.
605  
606   It is possible to construct a \emph{volume-preserving} flow for a
607 < source free($ \nabla \cdot f = 0 $) ODE, if the flow satisfies $
607 > source free ODE ($ \nabla \cdot f = 0 $), if the flow satisfies $
608   \det d\varphi  = 1$. One can show easily that a symplectic flow will
609   be volume-preserving.
610  
611 < Changing the variables $y = h(x)$ in a ODE\ref{introEquation:ODE}
612 < will result in a new system,
611 > Changing the variables $y = h(x)$ in an ODE
612 > (Eq.~\ref{introEquation:ODE}) will result in a new system,
613   \[
614   \dot y = \tilde f(y) = ((dh \cdot f)h^{ - 1} )(y).
615   \]
# Line 689 | Line 659 | constructed. The most famous example is leapfrog metho
659   A lot of well established and very effective numerical methods have
660   been successful precisely because of their symplecticities even
661   though this fact was not recognized when they were first
662 < constructed. The most famous example is leapfrog methods in
663 < molecular dynamics. In general, symplectic integrators can be
662 > constructed. The most famous example is the Verlet-leapfrog method
663 > in molecular dynamics. In general, symplectic integrators can be
664   constructed using one of four different methods.
665   \begin{enumerate}
666   \item Generating functions
# Line 708 | Line 678 | implementing the Runge-Kutta methods, they do not attr
678   high-order explicit Runge-Kutta methods
679   \cite{Owren1992,Chen2003}have been developed to overcome this
680   instability. However, due to computational penalty involved in
681 < implementing the Runge-Kutta methods, they do not attract too much
682 < attention from Molecular Dynamics community. Instead, splitting have
683 < been widely accepted since they exploit natural decompositions of
684 < the system\cite{Tuckerman1992, McLachlan1998}.
681 > implementing the Runge-Kutta methods, they have not attracted much
682 > attention from the Molecular Dynamics community. Instead, splitting
683 > methods have been widely accepted since they exploit natural
684 > decompositions of the system\cite{Tuckerman1992, McLachlan1998}.
685  
686 < \subsubsection{\label{introSection:splittingMethod}Splitting Method}
686 > \subsubsection{\label{introSection:splittingMethod}\textbf{Splitting Methods}}
687  
688   The main idea behind splitting methods is to decompose the discrete
689   $\varphi_h$ as a composition of simpler flows,
# Line 734 | Line 704 | order is then given by the Lie-Trotter formula
704   energy respectively, which is a natural decomposition of the
705   problem. If $H_1$ and $H_2$ can be integrated using exact flows
706   $\varphi_1(t)$ and $\varphi_2(t)$, respectively, a simple first
707 < order is then given by the Lie-Trotter formula
707 > order expression is then given by the Lie-Trotter formula
708   \begin{equation}
709   \varphi _h  = \varphi _{1,h}  \circ \varphi _{2,h},
710   \label{introEquation:firstOrderSplitting}
# Line 760 | Line 730 | which has a local error proportional to $h^3$. Sprang
730   \varphi _h  = \varphi _{1,h/2}  \circ \varphi _{2,h}  \circ \varphi
731   _{1,h/2} , \label{introEquation:secondOrderSplitting}
732   \end{equation}
733 < which has a local error proportional to $h^3$. Sprang splitting's
734 < popularity in molecular simulation community attribute to its
735 < symmetric property,
733 > which has a local error proportional to $h^3$. The Sprang
734 > splitting's popularity in molecular simulation community attribute
735 > to its symmetric property,
736   \begin{equation}
737   \varphi _h^{ - 1} = \varphi _{ - h}.
738   \label{introEquation:timeReversible}
739   \end{equation}
740  
741 < \subsubsection{\label{introSection:exampleSplittingMethod}Example of Splitting Method}
741 > \subsubsection{\label{introSection:exampleSplittingMethod}\textbf{Examples of the Splitting Method}}
742   The classical equation for a system consisting of interacting
743   particles can be written in Hamiltonian form,
744   \[
745   H = T + V
746   \]
747   where $T$ is the kinetic energy and $V$ is the potential energy.
748 < Setting $H_1 = T, H_2 = V$ and applying Strang splitting, one
748 > Setting $H_1 = T, H_2 = V$ and applying the Strang splitting, one
749   obtains the following:
750   \begin{align}
751   q(\Delta t) &= q(0) + \dot{q}(0)\Delta t +
# Line 802 | Line 772 | q(\Delta t) &= q(0) + \Delta t\, \dot{q}\biggl (\frac{
772      \label{introEquation:Lp9b}\\%
773   %
774   \dot{q}(\Delta t) &= \dot{q}\biggl (\frac{\Delta t}{2}\biggr ) +
775 <    \frac{\Delta t}{2m}\, F[q(0)]. \label{introEquation:Lp9c}
775 >    \frac{\Delta t}{2m}\, F[q(t)]. \label{introEquation:Lp9c}
776   \end{align}
777   From the preceding splitting, one can see that the integration of
778   the equations of motion would follow:
# Line 811 | Line 781 | the equations of motion would follow:
781  
782   \item Use the half step velocities to move positions one whole step, $\Delta t$.
783  
784 < \item Evaluate the forces at the new positions, $\mathbf{r}(\Delta t)$, and use the new forces to complete the velocity move.
784 > \item Evaluate the forces at the new positions, $\mathbf{q}(\Delta t)$, and use the new forces to complete the velocity move.
785  
786   \item Repeat from step 1 with the new position, velocities, and forces assuming the roles of the initial values.
787   \end{enumerate}
788  
789 < Simply switching the order of splitting and composing, a new
790 < integrator, the \emph{position verlet} integrator, can be generated,
789 > By simply switching the order of the propagators in the splitting
790 > and composing a new integrator, the \emph{position verlet}
791 > integrator, can be generated,
792   \begin{align}
793   \dot q(\Delta t) &= \dot q(0) + \Delta tF(q(0))\left[ {q(0) +
794   \frac{{\Delta t}}{{2m}}\dot q(0)} \right], %
# Line 828 | Line 799 | q(\Delta t)} \right]. %
799   \label{introEquation:positionVerlet2}
800   \end{align}
801  
802 < \subsubsection{\label{introSection:errorAnalysis}Error Analysis and Higher Order Methods}
802 > \subsubsection{\label{introSection:errorAnalysis}\textbf{Error Analysis and Higher Order Methods}}
803  
804 < Baker-Campbell-Hausdorff formula can be used to determine the local
805 < error of splitting method in terms of commutator of the
804 > The Baker-Campbell-Hausdorff formula can be used to determine the
805 > local error of splitting method in terms of the commutator of the
806   operators(\ref{introEquation:exponentialOperator}) associated with
807 < the sub-flow. For operators $hX$ and $hY$ which are associate to
807 > the sub-flow. For operators $hX$ and $hY$ which are associated with
808   $\varphi_1(t)$ and $\varphi_2(t)$ respectively , we have
809   \begin{equation}
810   \exp (hX + hY) = \exp (hZ)
# Line 847 | Line 818 | Applying Baker-Campbell-Hausdorff formula\cite{Varadar
818   \[
819   [X,Y] = XY - YX .
820   \]
821 < Applying Baker-Campbell-Hausdorff formula\cite{Varadarajan1974} to
822 < Sprang splitting, we can obtain
821 > Applying the Baker-Campbell-Hausdorff formula\cite{Varadarajan1974}
822 > to the Sprang splitting, we can obtain
823   \begin{eqnarray*}
824   \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 \\
825                                     &   & \mbox{} + h^2 [X,X]/8 + h^2 [Y,Y]/8 \\
826                                     &   & \mbox{} + h^3 [Y,[Y,X]]/12 - h^3[X,[X,Y]]/24 + \ldots )
827   \end{eqnarray*}
828 < Since \[ [X,Y] + [Y,X] = 0\] and \[ [X,X] = 0\], the dominant local
828 > Since \[ [X,Y] + [Y,X] = 0\] and \[ [X,X] = 0,\] the dominant local
829   error of Spring splitting is proportional to $h^3$. The same
830 < procedure can be applied to general splitting,  of the form
830 > procedure can be applied to a general splitting,  of the form
831   \begin{equation}
832   \varphi _{b_m h}^2  \circ \varphi _{a_m h}^1  \circ \varphi _{b_{m -
833   1} h}^2  \circ  \ldots  \circ \varphi _{a_1 h}^1 .
834   \end{equation}
835 < Careful choice of coefficient $a_1 \ldot b_m$ will lead to higher
836 < order method. Yoshida proposed an elegant way to compose higher
835 > A careful choice of coefficient $a_1 \ldots b_m$ will lead to higher
836 > order methods. Yoshida proposed an elegant way to compose higher
837   order methods based on symmetric splitting\cite{Yoshida1990}. Given
838   a symmetric second order base method $ \varphi _h^{(2)} $, a
839   fourth-order symmetric method can be constructed by composing,
# Line 875 | Line 846 | _{\beta h}^{(2n)}  \circ \varphi _{\alpha h}^{(2n)}
846   integrator $ \varphi _h^{(2n + 2)}$ can be composed by
847   \begin{equation}
848   \varphi _h^{(2n + 2)}  = \varphi _{\alpha h}^{(2n)}  \circ \varphi
849 < _{\beta h}^{(2n)}  \circ \varphi _{\alpha h}^{(2n)}
849 > _{\beta h}^{(2n)}  \circ \varphi _{\alpha h}^{(2n)},
850   \end{equation}
851 < , if the weights are chosen as
851 > if the weights are chosen as
852   \[
853   \alpha  =  - \frac{{2^{1/(2n + 1)} }}{{2 - 2^{1/(2n + 1)} }},\beta =
854   \frac{{2^{1/(2n + 1)} }}{{2 - 2^{1/(2n + 1)} }} .
# Line 914 | Line 885 | initialization of a simulation. Sec.~\ref{introSec:pro
885   \end{enumerate}
886   These three individual steps will be covered in the following
887   sections. Sec.~\ref{introSec:initialSystemSettings} deals with the
888 < initialization of a simulation. Sec.~\ref{introSec:production} will
889 < discusses issues in production run. Sec.~\ref{introSection:Analysis}
890 < provides the theoretical tools for trajectory analysis.
888 > initialization of a simulation. Sec.~\ref{introSection:production}
889 > will discusse issues in production run.
890 > Sec.~\ref{introSection:Analysis} provides the theoretical tools for
891 > trajectory analysis.
892  
893   \subsection{\label{introSec:initialSystemSettings}Initialization}
894  
895 < \subsubsection{Preliminary preparation}
895 > \subsubsection{\textbf{Preliminary preparation}}
896  
897   When selecting the starting structure of a molecule for molecular
898   simulation, one may retrieve its Cartesian coordinates from public
899   databases, such as RCSB Protein Data Bank \textit{etc}. Although
900   thousands of crystal structures of molecules are discovered every
901   year, many more remain unknown due to the difficulties of
902 < purification and crystallization. Even for the molecule with known
903 < structure, some important information is missing. For example, the
902 > purification and crystallization. Even for molecules with known
903 > structure, some important information is missing. For example, a
904   missing hydrogen atom which acts as donor in hydrogen bonding must
905   be added. Moreover, in order to include electrostatic interaction,
906   one may need to specify the partial charges for individual atoms.
907   Under some circumstances, we may even need to prepare the system in
908 < a special setup. For instance, when studying transport phenomenon in
909 < membrane system, we may prepare the lipids in bilayer structure
910 < instead of placing lipids randomly in solvent, since we are not
911 < interested in self-aggregation and it takes a long time to happen.
908 > a special configuration. For instance, when studying transport
909 > phenomenon in membrane systems, we may prepare the lipids in a
910 > bilayer structure instead of placing lipids randomly in solvent,
911 > since we are not interested in the slow self-aggregation process.
912  
913 < \subsubsection{Minimization}
913 > \subsubsection{\textbf{Minimization}}
914  
915   It is quite possible that some of molecules in the system from
916 < preliminary preparation may be overlapped with each other. This
917 < close proximity leads to high potential energy which consequently
918 < jeopardizes any molecular dynamics simulations. To remove these
919 < steric overlaps, one typically performs energy minimization to find
920 < a more reasonable conformation. Several energy minimization methods
921 < have been developed to exploit the energy surface and to locate the
922 < local minimum. While converging slowly near the minimum, steepest
923 < descent method is extremely robust when systems are far from
924 < harmonic. Thus, it is often used to refine structure from
925 < crystallographic data. Relied on the gradient or hessian, advanced
926 < methods like conjugate gradient and Newton-Raphson converge rapidly
927 < to a local minimum, while become unstable if the energy surface is
928 < far from quadratic. Another factor must be taken into account, when
916 > preliminary preparation may be overlapping with each other. This
917 > close proximity leads to high initial potential energy which
918 > consequently jeopardizes any molecular dynamics simulations. To
919 > remove these steric overlaps, one typically performs energy
920 > minimization to find a more reasonable conformation. Several energy
921 > minimization methods have been developed to exploit the energy
922 > surface and to locate the local minimum. While converging slowly
923 > near the minimum, steepest descent method is extremely robust when
924 > systems are strongly anharmonic. Thus, it is often used to refine
925 > structure from crystallographic data. Relied on the gradient or
926 > hessian, advanced methods like Newton-Raphson converge rapidly to a
927 > local minimum, but become unstable if the energy surface is far from
928 > quadratic. Another factor that must be taken into account, when
929   choosing energy minimization method, is the size of the system.
930   Steepest descent and conjugate gradient can deal with models of any
931 < size. Because of the limit of computation power to calculate hessian
932 < matrix and insufficient storage capacity to store them, most
933 < Newton-Raphson methods can not be used with very large models.
931 > size. Because of the limits on computer memory to store the hessian
932 > matrix and the computing power needed to diagonalized these
933 > matrices, most Newton-Raphson methods can not be used with very
934 > large systems.
935  
936 < \subsubsection{Heating}
936 > \subsubsection{\textbf{Heating}}
937  
938   Typically, Heating is performed by assigning random velocities
939 < according to a Gaussian distribution for a temperature. Beginning at
940 < a lower temperature and gradually increasing the temperature by
941 < assigning greater random velocities, we end up with setting the
942 < temperature of the system to a final temperature at which the
943 < simulation will be conducted. In heating phase, we should also keep
944 < the system from drifting or rotating as a whole. Equivalently, the
945 < net linear momentum and angular momentum of the system should be
946 < shifted to zero.
939 > according to a Maxwell-Boltzman distribution for a desired
940 > temperature. Beginning at a lower temperature and gradually
941 > increasing the temperature by assigning larger random velocities, we
942 > end up with setting the temperature of the system to a final
943 > temperature at which the simulation will be conducted. In heating
944 > phase, we should also keep the system from drifting or rotating as a
945 > whole. To do this, the net linear momentum and angular momentum of
946 > the system is shifted to zero after each resampling from the Maxwell
947 > -Boltzman distribution.
948  
949 < \subsubsection{Equilibration}
949 > \subsubsection{\textbf{Equilibration}}
950  
951   The purpose of equilibration is to allow the system to evolve
952   spontaneously for a period of time and reach equilibrium. The
# Line 986 | Line 960 | Production run is the most important step of the simul
960  
961   \subsection{\label{introSection:production}Production}
962  
963 < Production run is the most important step of the simulation, in
963 > The production run is the most important step of the simulation, in
964   which the equilibrated structure is used as a starting point and the
965   motions of the molecules are collected for later analysis. In order
966   to capture the macroscopic properties of the system, the molecular
967 < dynamics simulation must be performed in correct and efficient way.
967 > dynamics simulation must be performed by sampling correctly and
968 > efficiently from the relevant thermodynamic ensemble.
969  
970   The most expensive part of a molecular dynamics simulation is the
971   calculation of non-bonded forces, such as van der Waals force and
972   Coulombic forces \textit{etc}. For a system of $N$ particles, the
973   complexity of the algorithm for pair-wise interactions is $O(N^2 )$,
974   which making large simulations prohibitive in the absence of any
975 < computation saving techniques.
975 > algorithmic tricks.
976  
977 < A natural approach to avoid system size issue is to represent the
977 > A natural approach to avoid system size issues is to represent the
978   bulk behavior by a finite number of the particles. However, this
979 < approach will suffer from the surface effect. To offset this,
980 < \textit{Periodic boundary condition} (see Fig.~\ref{introFig:pbc})
981 < is developed to simulate bulk properties with a relatively small
982 < number of particles. In this method, the simulation box is
983 < replicated throughout space to form an infinite lattice. During the
984 < simulation, when a particle moves in the primary cell, its image in
985 < other cells move in exactly the same direction with exactly the same
986 < orientation. Thus, as a particle leaves the primary cell, one of its
987 < images will enter through the opposite face.
979 > approach will suffer from the surface effect at the edges of the
980 > simulation. To offset this, \textit{Periodic boundary conditions}
981 > (see Fig.~\ref{introFig:pbc}) is developed to simulate bulk
982 > properties with a relatively small number of particles. In this
983 > method, the simulation box is replicated throughout space to form an
984 > infinite lattice. During the simulation, when a particle moves in
985 > the primary cell, its image in other cells move in exactly the same
986 > direction with exactly the same orientation. Thus, as a particle
987 > leaves the primary cell, one of its images will enter through the
988 > opposite face.
989   \begin{figure}
990   \centering
991   \includegraphics[width=\linewidth]{pbc.eps}
# Line 1021 | Line 997 | evaluation is to apply cutoff where particles farther
997  
998   %cutoff and minimum image convention
999   Another important technique to improve the efficiency of force
1000 < evaluation is to apply cutoff where particles farther than a
1001 < predetermined distance, are not included in the calculation
1000 > evaluation is to apply spherical cutoff where particles farther than
1001 > a predetermined distance are not included in the calculation
1002   \cite{Frenkel1996}. The use of a cutoff radius will cause a
1003   discontinuity in the potential energy curve. Fortunately, one can
1004 < shift the potential to ensure the potential curve go smoothly to
1005 < zero at the cutoff radius. Cutoff strategy works pretty well for
1006 < Lennard-Jones interaction because of its short range nature.
1007 < However, simply truncating the electrostatic interaction with the
1008 < use of cutoff has been shown to lead to severe artifacts in
1009 < simulations. Ewald summation, in which the slowly conditionally
1010 < convergent Coulomb potential is transformed into direct and
1011 < reciprocal sums with rapid and absolute convergence, has proved to
1012 < minimize the periodicity artifacts in liquid simulations. Taking the
1013 < advantages of the fast Fourier transform (FFT) for calculating
1014 < discrete Fourier transforms, the particle mesh-based
1004 > shift simple radial potential to ensure the potential curve go
1005 > smoothly to zero at the cutoff radius. The cutoff strategy works
1006 > well for Lennard-Jones interaction because of its short range
1007 > nature. However, simply truncating the electrostatic interaction
1008 > with the use of cutoffs has been shown to lead to severe artifacts
1009 > in simulations. The Ewald summation, in which the slowly decaying
1010 > Coulomb potential is transformed into direct and reciprocal sums
1011 > with rapid and absolute convergence, has proved to minimize the
1012 > periodicity artifacts in liquid simulations. Taking the advantages
1013 > of the fast Fourier transform (FFT) for calculating discrete Fourier
1014 > transforms, the particle mesh-based
1015   methods\cite{Hockney1981,Shimada1993, Luty1994} are accelerated from
1016 < $O(N^{3/2})$ to $O(N logN)$. An alternative approach is \emph{fast
1017 < multipole method}\cite{Greengard1987, Greengard1994}, which treats
1018 < Coulombic interaction exactly at short range, and approximate the
1019 < potential at long range through multipolar expansion. In spite of
1020 < their wide acceptances at the molecular simulation community, these
1021 < two methods are hard to be implemented correctly and efficiently.
1022 < Instead, we use a damped and charge-neutralized Coulomb potential
1023 < method developed by Wolf and his coworkers\cite{Wolf1999}. The
1024 < shifted Coulomb potential for particle $i$ and particle $j$ at
1025 < distance $r_{rj}$ is given by:
1016 > $O(N^{3/2})$ to $O(N logN)$. An alternative approach is the
1017 > \emph{fast multipole method}\cite{Greengard1987, Greengard1994},
1018 > which treats Coulombic interactions exactly at short range, and
1019 > approximate the potential at long range through multipolar
1020 > expansion. In spite of their wide acceptance at the molecular
1021 > simulation community, these two methods are difficult to implement
1022 > correctly and efficiently. Instead, we use a damped and
1023 > charge-neutralized Coulomb potential method developed by Wolf and
1024 > his coworkers\cite{Wolf1999}. The shifted Coulomb potential for
1025 > particle $i$ and particle $j$ at distance $r_{rj}$ is given by:
1026   \begin{equation}
1027   V(r_{ij})= \frac{q_i q_j \textrm{erfc}(\alpha
1028   r_{ij})}{r_{ij}}-\lim_{r_{ij}\rightarrow
# Line 1068 | Line 1044 | Recently, advanced visualization technique are widely
1044  
1045   \subsection{\label{introSection:Analysis} Analysis}
1046  
1047 < Recently, advanced visualization technique are widely applied to
1047 > Recently, advanced visualization technique have become applied to
1048   monitor the motions of molecules. Although the dynamics of the
1049   system can be described qualitatively from animation, quantitative
1050 < trajectory analysis are more appreciable. According to the
1051 < principles of Statistical Mechanics,
1052 < Sec.~\ref{introSection:statisticalMechanics}, one can compute
1053 < thermodynamics properties, analyze fluctuations of structural
1054 < parameters, and investigate time-dependent processes of the molecule
1079 < from the trajectories.
1050 > trajectory analysis are more useful. According to the principles of
1051 > Statistical Mechanics, Sec.~\ref{introSection:statisticalMechanics},
1052 > one can compute thermodynamic properties, analyze fluctuations of
1053 > structural parameters, and investigate time-dependent processes of
1054 > the molecule from the trajectories.
1055  
1056 < \subsubsection{\label{introSection:thermodynamicsProperties}Thermodynamics Properties}
1056 > \subsubsection{\label{introSection:thermodynamicsProperties}\textbf{Thermodynamic Properties}}
1057  
1058 < Thermodynamics properties, which can be expressed in terms of some
1058 > Thermodynamic properties, which can be expressed in terms of some
1059   function of the coordinates and momenta of all particles in the
1060   system, can be directly computed from molecular dynamics. The usual
1061   way to measure the pressure is based on virial theorem of Clausius
# Line 1100 | Line 1075 | P = \frac{{Nk_B T}}{V} - \frac{1}{{3V}}\left\langle {\
1075   < j} {r{}_{ij} \cdot f_{ij} } } \right\rangle
1076   \end{equation}
1077  
1078 < \subsubsection{\label{introSection:structuralProperties}Structural Properties}
1078 > \subsubsection{\label{introSection:structuralProperties}\textbf{Structural Properties}}
1079  
1080   Structural Properties of a simple fluid can be described by a set of
1081 < distribution functions. Among these functions,\emph{pair
1081 > distribution functions. Among these functions,the \emph{pair
1082   distribution function}, also known as \emph{radial distribution
1083 < function}, is of most fundamental importance to liquid-state theory.
1084 < Pair distribution function can be gathered by Fourier transforming
1085 < raw data from a series of neutron diffraction experiments and
1086 < integrating over the surface factor \cite{Powles1973}. The
1087 < experiment result can serve as a criterion to justify the
1088 < correctness of the theory. Moreover, various equilibrium
1089 < thermodynamic and structural properties can also be expressed in
1090 < terms of radial distribution function \cite{Allen1987}.
1083 > function}, is of most fundamental importance to liquid theory.
1084 > Experimentally, pair distribution function can be gathered by
1085 > Fourier transforming raw data from a series of neutron diffraction
1086 > experiments and integrating over the surface factor
1087 > \cite{Powles1973}. The experimental results can serve as a criterion
1088 > to justify the correctness of a liquid model. Moreover, various
1089 > equilibrium thermodynamic and structural properties can also be
1090 > expressed in terms of radial distribution function \cite{Allen1987}.
1091  
1092 < A pair distribution functions $g(r)$ gives the probability that a
1092 > The pair distribution functions $g(r)$ gives the probability that a
1093   particle $i$ will be located at a distance $r$ from a another
1094   particle $j$ in the system
1095   \[
1096   g(r) = \frac{V}{{N^2 }}\left\langle {\sum\limits_i {\sum\limits_{j
1097 < \ne i} {\delta (r - r_{ij} )} } } \right\rangle.
1097 > \ne i} {\delta (r - r_{ij} )} } } \right\rangle = \frac{\rho
1098 > (r)}{\rho}.
1099   \]
1100   Note that the delta function can be replaced by a histogram in
1101 < computer simulation. Figure
1102 < \ref{introFigure:pairDistributionFunction} shows a typical pair
1103 < distribution function for the liquid argon system. The occurrence of
1128 < several peaks in the plot of $g(r)$ suggests that it is more likely
1129 < to find particles at certain radial values than at others. This is a
1130 < result of the attractive interaction at such distances. Because of
1131 < the strong repulsive forces at short distance, the probability of
1132 < locating particles at distances less than about 2.5{\AA} from each
1133 < other is essentially zero.
1101 > computer simulation. Peaks in $g(r)$ represent solvent shells, and
1102 > the height of these peaks gradually decreases to 1 as the liquid of
1103 > large distance approaches the bulk density.
1104  
1135 %\begin{figure}
1136 %\centering
1137 %\includegraphics[width=\linewidth]{pdf.eps}
1138 %\caption[Pair distribution function for the liquid argon
1139 %]{Pair distribution function for the liquid argon}
1140 %\label{introFigure:pairDistributionFunction}
1141 %\end{figure}
1105  
1106 < \subsubsection{\label{introSection:timeDependentProperties}Time-dependent
1107 < Properties}
1106 > \subsubsection{\label{introSection:timeDependentProperties}\textbf{Time-dependent
1107 > Properties}}
1108  
1109   Time-dependent properties are usually calculated using \emph{time
1110 < correlation function}, which correlates random variables $A$ and $B$
1111 < at two different time
1110 > correlation functions}, which correlate random variables $A$ and $B$
1111 > at two different times,
1112   \begin{equation}
1113   C_{AB} (t) = \left\langle {A(t)B(0)} \right\rangle.
1114   \label{introEquation:timeCorrelationFunction}
1115   \end{equation}
1116   If $A$ and $B$ refer to same variable, this kind of correlation
1117 < function is called \emph{auto correlation function}. One example of
1118 < auto correlation function is velocity auto-correlation function
1119 < which is directly related to transport properties of molecular
1120 < liquids:
1117 > function is called an \emph{autocorrelation function}. One example
1118 > of an auto correlation function is the velocity auto-correlation
1119 > function which is directly related to transport properties of
1120 > molecular liquids:
1121   \[
1122   D = \frac{1}{3}\int\limits_0^\infty  {\left\langle {v(t) \cdot v(0)}
1123   \right\rangle } dt
1124   \]
1125 < where $D$ is diffusion constant. Unlike velocity autocorrelation
1126 < function which is averaging over time origins and over all the
1127 < atoms, dipole autocorrelation are calculated for the entire system.
1128 < The dipole autocorrelation function is given by:
1125 > where $D$ is diffusion constant. Unlike the velocity autocorrelation
1126 > function, which is averaging over time origins and over all the
1127 > atoms, the dipole autocorrelation functions are calculated for the
1128 > entire system. The dipole autocorrelation function is given by:
1129   \[
1130   c_{dipole}  = \left\langle {u_{tot} (t) \cdot u_{tot} (t)}
1131   \right\rangle
# Line 1188 | Line 1151 | simulator is governed by the rigid body dynamics. In m
1151   areas, from engineering, physics, to chemistry. For example,
1152   missiles and vehicle are usually modeled by rigid bodies.  The
1153   movement of the objects in 3D gaming engine or other physics
1154 < simulator is governed by the rigid body dynamics. In molecular
1155 < simulation, rigid body is used to simplify the model in
1156 < protein-protein docking study\cite{Gray2003}.
1154 > simulator is governed by rigid body dynamics. In molecular
1155 > simulations, rigid bodies are used to simplify protein-protein
1156 > docking studies\cite{Gray2003}.
1157  
1158   It is very important to develop stable and efficient methods to
1159 < integrate the equations of motion of orientational degrees of
1160 < freedom. Euler angles are the nature choice to describe the
1161 < rotational degrees of freedom. However, due to its singularity, the
1162 < numerical integration of corresponding equations of motion is very
1163 < inefficient and inaccurate. Although an alternative integrator using
1164 < different sets of Euler angles can overcome this
1165 < difficulty\cite{Barojas1973}, the computational penalty and the lost
1166 < of angular momentum conservation still remain. A singularity free
1167 < representation utilizing quaternions was developed by Evans in
1168 < 1977\cite{Evans1977}. Unfortunately, this approach suffer from the
1169 < nonseparable Hamiltonian resulted from quaternion representation,
1170 < which prevents the symplectic algorithm to be utilized. Another
1171 < different approach is to apply holonomic constraints to the atoms
1172 < belonging to the rigid body. Each atom moves independently under the
1173 < normal forces deriving from potential energy and constraint forces
1174 < which are used to guarantee the rigidness. However, due to their
1175 < iterative nature, SHAKE and Rattle algorithm converge very slowly
1176 < when the number of constraint increases\cite{Ryckaert1977,
1177 < Andersen1983}.
1159 > integrate the equations of motion for orientational degrees of
1160 > freedom. Euler angles are the natural choice to describe the
1161 > rotational degrees of freedom. However, due to $\frac {1}{sin
1162 > \theta}$ singularities, the numerical integration of corresponding
1163 > equations of motion is very inefficient and inaccurate. Although an
1164 > alternative integrator using multiple sets of Euler angles can
1165 > overcome this difficulty\cite{Barojas1973}, the computational
1166 > penalty and the loss of angular momentum conservation still remain.
1167 > A singularity-free representation utilizing quaternions was
1168 > developed by Evans in 1977\cite{Evans1977}. Unfortunately, this
1169 > approach uses a nonseparable Hamiltonian resulting from the
1170 > quaternion representation, which prevents the symplectic algorithm
1171 > to be utilized. Another different approach is to apply holonomic
1172 > constraints to the atoms belonging to the rigid body. Each atom
1173 > moves independently under the normal forces deriving from potential
1174 > energy and constraint forces which are used to guarantee the
1175 > rigidness. However, due to their iterative nature, the SHAKE and
1176 > Rattle algorithms also converge very slowly when the number of
1177 > constraints increases\cite{Ryckaert1977, Andersen1983}.
1178  
1179 < The break through in geometric literature suggests that, in order to
1179 > A break-through in geometric literature suggests that, in order to
1180   develop a long-term integration scheme, one should preserve the
1181 < symplectic structure of the flow. Introducing conjugate momentum to
1182 < rotation matrix $Q$ and re-formulating Hamiltonian's equation, a
1183 < symplectic integrator, RSHAKE\cite{Kol1997}, was proposed to evolve
1184 < the Hamiltonian system in a constraint manifold by iteratively
1185 < satisfying the orthogonality constraint $Q_T Q = 1$. An alternative
1186 < method using quaternion representation was developed by
1187 < Omelyan\cite{Omelyan1998}. However, both of these methods are
1188 < iterative and inefficient. In this section, we will present a
1181 > symplectic structure of the flow. By introducing a conjugate
1182 > momentum to the rotation matrix $Q$ and re-formulating Hamiltonian's
1183 > equation, a symplectic integrator, RSHAKE\cite{Kol1997}, was
1184 > proposed to evolve the Hamiltonian system in a constraint manifold
1185 > by iteratively satisfying the orthogonality constraint $Q^T Q = 1$.
1186 > An alternative method using the quaternion representation was
1187 > developed by Omelyan\cite{Omelyan1998}. However, both of these
1188 > methods are iterative and inefficient. In this section, we descibe a
1189   symplectic Lie-Poisson integrator for rigid body developed by
1190   Dullweber and his coworkers\cite{Dullweber1997} in depth.
1191  
1192 < \subsection{\label{introSection:constrainedHamiltonianRB}Constrained Hamiltonian for Rigid Body}
1193 < The motion of the rigid body is Hamiltonian with the Hamiltonian
1192 > \subsection{\label{introSection:constrainedHamiltonianRB}Constrained Hamiltonian for Rigid Bodies}
1193 > The motion of a rigid body is Hamiltonian with the Hamiltonian
1194   function
1195   \begin{equation}
1196   H = \frac{1}{2}(p^T m^{ - 1} p) + \frac{1}{2}tr(PJ^{ - 1} P) +
# Line 1241 | Line 1204 | constrained Hamiltonian equation subjects to a holonom
1204   I_{ii}^{ - 1}  = \frac{1}{2}\sum\limits_{i \ne j} {J_{jj}^{ - 1} }
1205   \]
1206   where $I_{ii}$ is the diagonal element of the inertia tensor. This
1207 < constrained Hamiltonian equation subjects to a holonomic constraint,
1207 > constrained Hamiltonian equation is subjected to a holonomic
1208 > constraint,
1209   \begin{equation}
1210   Q^T Q = 1, \label{introEquation:orthogonalConstraint}
1211   \end{equation}
1212 < which is used to ensure rotation matrix's orthogonality.
1213 < Differentiating \ref{introEquation:orthogonalConstraint} and using
1214 < Equation \ref{introEquation:RBMotionMomentum}, one may obtain,
1212 > which is used to ensure rotation matrix's unitarity. Differentiating
1213 > \ref{introEquation:orthogonalConstraint} and using Equation
1214 > \ref{introEquation:RBMotionMomentum}, one may obtain,
1215   \begin{equation}
1216   Q^T PJ^{ - 1}  + J^{ - 1} P^T Q = 0 . \\
1217   \label{introEquation:RBFirstOrderConstraint}
# Line 1256 | Line 1220 | the equations of motion,
1220   Using Equation (\ref{introEquation:motionHamiltonianCoordinate},
1221   \ref{introEquation:motionHamiltonianMomentum}), one can write down
1222   the equations of motion,
1259 \[
1260 \begin{array}{c}
1261 \frac{{dq}}{{dt}} = \frac{p}{m} \label{introEquation:RBMotionPosition}\\
1262 \frac{{dp}}{{dt}} =  - \nabla _q V(q,Q) \label{introEquation:RBMotionMomentum}\\
1263 \frac{{dQ}}{{dt}} = PJ^{ - 1}  \label{introEquation:RBMotionRotation}\\
1264 \frac{{dP}}{{dt}} =  - \nabla _Q V(q,Q) - 2Q\Lambda . \label{introEquation:RBMotionP}\\
1265 \end{array}
1266 \]
1223  
1224 + \begin{eqnarray}
1225 + \frac{{dq}}{{dt}} & = & \frac{p}{m} \label{introEquation:RBMotionPosition}\\
1226 + \frac{{dp}}{{dt}} & = & - \nabla _q V(q,Q) \label{introEquation:RBMotionMomentum}\\
1227 + \frac{{dQ}}{{dt}} & = & PJ^{ - 1}  \label{introEquation:RBMotionRotation}\\
1228 + \frac{{dP}}{{dt}} & = & - \nabla _Q V(q,Q) - 2Q\Lambda . \label{introEquation:RBMotionP}
1229 + \end{eqnarray}
1230 +
1231   In general, there are two ways to satisfy the holonomic constraints.
1232 < We can use constraint force provided by lagrange multiplier on the
1233 < normal manifold to keep the motion on constraint space. Or we can
1234 < simply evolve the system in constraint manifold. These two methods
1235 < are proved to be equivalent. The holonomic constraint and equations
1236 < of motions define a constraint manifold for rigid body
1232 > We can use a constraint force provided by a Lagrange multiplier on
1233 > the normal manifold to keep the motion on constraint space. Or we
1234 > can simply evolve the system on the constraint manifold. These two
1235 > methods have been proved to be equivalent. The holonomic constraint
1236 > and equations of motions define a constraint manifold for rigid
1237 > bodies
1238   \[
1239   M = \left\{ {(Q,P):Q^T Q = 1,Q^T PJ^{ - 1}  + J^{ - 1} P^T Q = 0}
1240   \right\}.
1241   \]
1242  
1243   Unfortunately, this constraint manifold is not the cotangent bundle
1244 < $T_{\star}SO(3)$. However, it turns out that under symplectic
1244 > $T^* SO(3)$ which can be consider as a symplectic manifold on Lie
1245 > rotation group $SO(3)$. However, it turns out that under symplectic
1246   transformation, the cotangent space and the phase space are
1247 < diffeomorphic. Introducing
1247 > diffeomorphic. By introducing
1248   \[
1249   \tilde Q = Q,\tilde P = \frac{1}{2}\left( {P - QP^T Q} \right),
1250   \]
# Line 1311 | Line 1276 | body, angular momentum on body frame $\Pi  = Q^t P$ is
1276   respectively.
1277  
1278   As a common choice to describe the rotation dynamics of the rigid
1279 < body, angular momentum on body frame $\Pi  = Q^t P$ is introduced to
1280 < rewrite the equations of motion,
1279 > body, the angular momentum on the body fixed frame $\Pi  = Q^t P$ is
1280 > introduced to rewrite the equations of motion,
1281   \begin{equation}
1282   \begin{array}{l}
1283 < \mathop \Pi \limits^ \bullet   = J^{ - 1} \Pi ^T \Pi  + Q^T \sum\limits_i {F_i (q,Q)X_i^T }  - \Lambda  \\
1284 < \mathop Q\limits^{{\rm{   }} \bullet }  = Q\Pi {\rm{ }}J^{ - 1}  \\
1283 > \dot \Pi  = J^{ - 1} \Pi ^T \Pi  + Q^T \sum\limits_i {F_i (q,Q)X_i^T }  - \Lambda  \\
1284 > \dot Q  = Q\Pi {\rm{ }}J^{ - 1}  \\
1285   \end{array}
1286   \label{introEqaution:RBMotionPI}
1287   \end{equation}
# Line 1344 | Line 1309 | operations
1309   \[
1310   \hat vu = v \times u
1311   \]
1347
1312   Using \ref{introEqaution:RBMotionPI}, one can construct a skew
1313   matrix,
1314 < \begin{equation}
1315 < (\mathop \Pi \limits^ \bullet   - \mathop \Pi \limits^ \bullet  ^T
1316 < ){\rm{ }} = {\rm{ }}(\Pi  - \Pi ^T ){\rm{ }}(J^{ - 1} \Pi  + \Pi J^{
1317 < - 1} ) + \sum\limits_i {[Q^T F_i (r,Q)X_i^T  - X_i F_i (r,Q)^T Q]} -
1318 < (\Lambda  - \Lambda ^T ) . \label{introEquation:skewMatrixPI}
1319 < \end{equation}
1314 >
1315 > \begin{eqnarray*}
1316 > (\dot \Pi  - \dot \Pi ^T ){\rm{ }} = {\rm{ }}(\Pi  - \Pi ^T ){\rm{
1317 > }}(J^{ - 1} \Pi  + \Pi J^{ - 1} ) + \sum\limits_i {[Q^T F_i
1318 > (r,Q)X_i^T  - X_i F_i (r,Q)^T Q]}  - (\Lambda  - \Lambda ^T ).
1319 > \label{introEquation:skewMatrixPI}
1320 > \end{eqnarray*}
1321 >
1322   Since $\Lambda$ is symmetric, the last term of Equation
1323   \ref{introEquation:skewMatrixPI} is zero, which implies the Lagrange
1324   multiplier $\Lambda$ is absent from the equations of motion. This
1325 < unique property eliminate the requirement of iterations which can
1325 > unique property eliminates the requirement of iterations which can
1326   not be avoided in other methods\cite{Kol1997, Omelyan1998}.
1327  
1328 < Applying hat-map isomorphism, we obtain the equation of motion for
1329 < angular momentum on body frame
1328 > Applying the hat-map isomorphism, we obtain the equation of motion
1329 > for angular momentum on body frame
1330   \begin{equation}
1331   \dot \pi  = \pi  \times I^{ - 1} \pi  + \sum\limits_i {\left( {Q^T
1332   F_i (r,Q)} \right) \times X_i }.
# Line 1375 | Line 1341 | If there is not external forces exerted on the rigid b
1341   \subsection{\label{introSection:SymplecticFreeRB}Symplectic
1342   Lie-Poisson Integrator for Free Rigid Body}
1343  
1344 < If there is not external forces exerted on the rigid body, the only
1345 < contribution to the rotational is from the kinetic potential (the
1346 < first term of \ref{ introEquation:bodyAngularMotion}). The free
1347 < rigid body is an example of Lie-Poisson system with Hamiltonian
1344 > If there are no external forces exerted on the rigid body, the only
1345 > contribution to the rotational motion is from the kinetic energy
1346 > (the first term of \ref{introEquation:bodyAngularMotion}). The free
1347 > rigid body is an example of a Lie-Poisson system with Hamiltonian
1348   function
1349   \begin{equation}
1350   T^r (\pi ) = T_1 ^r (\pi _1 ) + T_2^r (\pi _2 ) + T_3^r (\pi _3 )
# Line 1426 | Line 1392 | tR_1 }$, we can use Cayley transformation,
1392   \end{array}} \right),\theta _1  = \frac{{\pi _1 }}{{I_1 }}\Delta t.
1393   \]
1394   To reduce the cost of computing expensive functions in $e^{\Delta
1395 < tR_1 }$, we can use Cayley transformation,
1395 > tR_1 }$, we can use Cayley transformation to obtain a single-aixs
1396 > propagator,
1397   \[
1398   e^{\Delta tR_1 }  \approx (1 - \Delta tR_1 )^{ - 1} (1 + \Delta tR_1
1399   )
1400   \]
1401   The flow maps for $T_2^r$ and $T_3^r$ can be found in the same
1402 < manner.
1403 <
1437 < In order to construct a second-order symplectic method, we split the
1438 < angular kinetic Hamiltonian function can into five terms
1402 > manner. In order to construct a second-order symplectic method, we
1403 > split the angular kinetic Hamiltonian function can into five terms
1404   \[
1405   T^r (\pi ) = \frac{1}{2}T_1 ^r (\pi _1 ) + \frac{1}{2}T_2^r (\pi _2
1406   ) + T_3^r (\pi _3 ) + \frac{1}{2}T_2^r (\pi _2 ) + \frac{1}{2}T_1 ^r
1407 < (\pi _1 )
1408 < \].
1409 < Concatenating flows corresponding to these five terms, we can obtain
1410 < an symplectic integrator,
1407 > (\pi _1 ).
1408 > \]
1409 > By concatenating the propagators corresponding to these five terms,
1410 > we can obtain an symplectic integrator,
1411   \[
1412   \varphi _{\Delta t,T^r }  = \varphi _{\Delta t/2,\pi _1 }  \circ
1413   \varphi _{\Delta t/2,\pi _2 }  \circ \varphi _{\Delta t,\pi _3 }
# Line 1469 | Line 1434 | Lie-Poisson integrator is found to be extremely effici
1434   \]
1435   Thus $ [\nabla _\pi  F(\pi )]^T J(\pi ) =  - S'(\frac{{\parallel \pi
1436   \parallel ^2 }}{2})\pi  \times \pi  = 0 $. This explicit
1437 < Lie-Poisson integrator is found to be extremely efficient and stable
1438 < which can be explained by the fact the small angle approximation is
1439 < used and the norm of the angular momentum is conserved.
1437 > Lie-Poisson integrator is found to be both extremely efficient and
1438 > stable. These properties can be explained by the fact the small
1439 > angle approximation is used and the norm of the angular momentum is
1440 > conserved.
1441  
1442   \subsection{\label{introSection:RBHamiltonianSplitting} Hamiltonian
1443   Splitting for Rigid Body}
# Line 1484 | Line 1450 | kinetic energy are listed in the below table,
1450   The equations of motion corresponding to potential energy and
1451   kinetic energy are listed in the below table,
1452   \begin{table}
1453 < \caption{Equations of motion due to Potential and Kinetic Energies}
1453 > \caption{EQUATIONS OF MOTION DUE TO POTENTIAL AND KINETIC ENERGIES}
1454   \begin{center}
1455   \begin{tabular}{|l|l|}
1456    \hline
# Line 1498 | Line 1464 | A second-order symplectic method is now obtained by th
1464   \end{tabular}
1465   \end{center}
1466   \end{table}
1467 < A second-order symplectic method is now obtained by the
1468 < composition of the flow maps,
1467 > A second-order symplectic method is now obtained by the composition
1468 > of the position and velocity propagators,
1469   \[
1470   \varphi _{\Delta t}  = \varphi _{\Delta t/2,V}  \circ \varphi
1471   _{\Delta t,T}  \circ \varphi _{\Delta t/2,V}.
1472   \]
1473   Moreover, $\varphi _{\Delta t/2,V}$ can be divided into two
1474 < sub-flows which corresponding to force and torque respectively,
1474 > sub-propagators which corresponding to force and torque
1475 > respectively,
1476   \[
1477   \varphi _{\Delta t/2,V}  = \varphi _{\Delta t/2,F}  \circ \varphi
1478   _{\Delta t/2,\tau }.
1479   \]
1480   Since the associated operators of $\varphi _{\Delta t/2,F} $ and
1481 < $\circ \varphi _{\Delta t/2,\tau }$ are commuted, the composition
1482 < order inside $\varphi _{\Delta t/2,V}$ does not matter.
1483 <
1484 < Furthermore, kinetic potential can be separated to translational
1518 < kinetic term, $T^t (p)$, and rotational kinetic term, $T^r (\pi )$,
1481 > $\circ \varphi _{\Delta t/2,\tau }$ commute, the composition order
1482 > inside $\varphi _{\Delta t/2,V}$ does not matter. Furthermore, the
1483 > kinetic energy can be separated to translational kinetic term, $T^t
1484 > (p)$, and rotational kinetic term, $T^r (\pi )$,
1485   \begin{equation}
1486   T(p,\pi ) =T^t (p) + T^r (\pi ).
1487   \end{equation}
1488   where $ T^t (p) = \frac{1}{2}p^T m^{ - 1} p $ and $T^r (\pi )$ is
1489   defined by \ref{introEquation:rotationalKineticRB}. Therefore, the
1490 < corresponding flow maps are given by
1490 > corresponding propagators are given by
1491   \[
1492   \varphi _{\Delta t,T}  = \varphi _{\Delta t,T^t }  \circ \varphi
1493   _{\Delta t,T^r }.
1494   \]
1495 < Finally, we obtain the overall symplectic flow maps for free moving
1496 < rigid body
1495 > Finally, we obtain the overall symplectic propagators for freely
1496 > moving rigid bodies
1497   \begin{equation}
1498   \begin{array}{c}
1499   \varphi _{\Delta t}  = \varphi _{\Delta t/2,F}  \circ \varphi _{\Delta t/2,\tau }  \\
# Line 1541 | Line 1507 | the theory of Langevin dynamics simulation. A brief de
1507   As an alternative to newtonian dynamics, Langevin dynamics, which
1508   mimics a simple heat bath with stochastic and dissipative forces,
1509   has been applied in a variety of studies. This section will review
1510 < the theory of Langevin dynamics simulation. A brief derivation of
1511 < generalized Langevin equation will be given first. Follow that, we
1512 < will discuss the physical meaning of the terms appearing in the
1513 < equation as well as the calculation of friction tensor from
1514 < hydrodynamics theory.
1510 > the theory of Langevin dynamics. A brief derivation of generalized
1511 > Langevin equation will be given first. Following that, we will
1512 > discuss the physical meaning of the terms appearing in the equation
1513 > as well as the calculation of friction tensor from hydrodynamics
1514 > theory.
1515  
1516   \subsection{\label{introSection:generalizedLangevinDynamics}Derivation of Generalized Langevin Equation}
1517  
1518 < Harmonic bath model, in which an effective set of harmonic
1518 > A harmonic bath model, in which an effective set of harmonic
1519   oscillators are used to mimic the effect of a linearly responding
1520   environment, has been widely used in quantum chemistry and
1521   statistical mechanics. One of the successful applications of
1522 < Harmonic bath model is the derivation of Deriving Generalized
1523 < Langevin Dynamics. Lets consider a system, in which the degree of
1522 > Harmonic bath model is the derivation of the Generalized Langevin
1523 > Dynamics (GLE). Lets consider a system, in which the degree of
1524   freedom $x$ is assumed to couple to the bath linearly, giving a
1525   Hamiltonian of the form
1526   \begin{equation}
1527   H = \frac{{p^2 }}{{2m}} + U(x) + H_B  + \Delta U(x,x_1 , \ldots x_N)
1528   \label{introEquation:bathGLE}.
1529   \end{equation}
1530 < Here $p$ is a momentum conjugate to $q$, $m$ is the mass associated
1531 < with this degree of freedom, $H_B$ is harmonic bath Hamiltonian,
1530 > Here $p$ is a momentum conjugate to $x$, $m$ is the mass associated
1531 > with this degree of freedom, $H_B$ is a harmonic bath Hamiltonian,
1532   \[
1533   H_B  = \sum\limits_{\alpha  = 1}^N {\left\{ {\frac{{p_\alpha ^2
1534   }}{{2m_\alpha  }} + \frac{1}{2}m_\alpha  \omega _\alpha ^2 }
# Line 1570 | Line 1536 | the harmonic bath masses, and $\Delta U$ is bilinear s
1536   \]
1537   where the index $\alpha$ runs over all the bath degrees of freedom,
1538   $\omega _\alpha$ are the harmonic bath frequencies, $m_\alpha$ are
1539 < the harmonic bath masses, and $\Delta U$ is bilinear system-bath
1539 > the harmonic bath masses, and $\Delta U$ is a bilinear system-bath
1540   coupling,
1541   \[
1542   \Delta U =  - \sum\limits_{\alpha  = 1}^N {g_\alpha  x_\alpha  x}
1543   \]
1544 < where $g_\alpha$ are the coupling constants between the bath and the
1545 < coordinate $x$. Introducing
1544 > where $g_\alpha$ are the coupling constants between the bath
1545 > coordinates ($x_ \alpha$) and the system coordinate ($x$).
1546 > Introducing
1547   \[
1548   W(x) = U(x) - \sum\limits_{\alpha  = 1}^N {\frac{{g_\alpha ^2
1549   }}{{2m_\alpha  w_\alpha ^2 }}} x^2
# Line 1591 | Line 1558 | Generalized Langevin Dynamics by Hamilton's equations
1558   \]
1559   Since the first two terms of the new Hamiltonian depend only on the
1560   system coordinates, we can get the equations of motion for
1561 < Generalized Langevin Dynamics by Hamilton's equations
1595 < \ref{introEquation:motionHamiltonianCoordinate,
1596 < introEquation:motionHamiltonianMomentum},
1561 > Generalized Langevin Dynamics by Hamilton's equations,
1562   \begin{equation}
1563   m\ddot x =  - \frac{{\partial W(x)}}{{\partial x}} -
1564   \sum\limits_{\alpha  = 1}^N {g_\alpha  \left( {x_\alpha   -
# Line 1610 | Line 1575 | differential equations, Laplace transform is the appro
1575   In order to derive an equation for $x$, the dynamics of the bath
1576   variables $x_\alpha$ must be solved exactly first. As an integral
1577   transform which is particularly useful in solving linear ordinary
1578 < differential equations, Laplace transform is the appropriate tool to
1579 < solve this problem. The basic idea is to transform the difficult
1578 > differential equations,the Laplace transform is the appropriate tool
1579 > to solve this problem. The basic idea is to transform the difficult
1580   differential equations into simple algebra problems which can be
1581 < solved easily. Then applying inverse Laplace transform, also known
1582 < as the Bromwich integral, we can retrieve the solutions of the
1581 > solved easily. Then, by applying the inverse Laplace transform, also
1582 > known as the Bromwich integral, we can retrieve the solutions of the
1583   original problems.
1584  
1585   Let $f(t)$ be a function defined on $ [0,\infty ) $. The Laplace
# Line 1634 | Line 1599 | Applying Laplace transform to the bath coordinates, we
1599   \end{eqnarray*}
1600  
1601  
1602 < Applying Laplace transform to the bath coordinates, we obtain
1602 > Applying the Laplace transform to the bath coordinates, we obtain
1603   \begin{eqnarray*}
1604   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) \\
1605   L(x_\alpha  ) & = & \frac{{\frac{{g_\alpha  }}{{\omega _\alpha  }}L(x) + px_\alpha  (0) + \dot x_\alpha  (0)}}{{p^2  + \omega _\alpha ^2 }} \\
# Line 1657 | Line 1622 | m\ddot x & = & - \frac{{\partial W(x)}}{{\partial x}}
1622   \]
1623   , we obtain
1624   \begin{eqnarray*}
1625 < m\ddot x & = & - \frac{{\partial W(x)}}{{\partial x}} -
1625 > m\ddot x & =  & - \frac{{\partial W(x)}}{{\partial x}} -
1626   \sum\limits_{\alpha  = 1}^N {\left\{ {\left( { - \frac{{g_\alpha ^2
1627   }}{{m_\alpha  \omega _\alpha ^2 }}} \right)\int_0^t {\cos (\omega
1628 < _\alpha  t)\dot x(t - \tau )d\tau  \\
1629 < & &\mbox{} - \left[ {g_\alpha  x_\alpha (0) - \frac{{g_\alpha
1630 < }}{{m_\alpha \omega _\alpha  }}} \right]\cos (\omega _\alpha  t) -
1631 < \frac{{g_\alpha  \dot x_\alpha  (0)}}{{\omega
1632 < _\alpha  }}\sin (\omega _\alpha  t)} } \right\}} \\
1633 < %
1634 < & = & - \frac{{\partial W(x)}}{{\partial x}} - \int_0^t
1628 > _\alpha  t)\dot x(t - \tau )d\tau } } \right\}}  \\
1629 > & & + \sum\limits_{\alpha  = 1}^N {\left\{ {\left[ {g_\alpha
1630 > x_\alpha (0) - \frac{{g_\alpha  }}{{m_\alpha  \omega _\alpha  }}}
1631 > \right]\cos (\omega _\alpha  t) + \frac{{g_\alpha  \dot x_\alpha
1632 > (0)}}{{\omega _\alpha  }}\sin (\omega _\alpha  t)} \right\}}
1633 > \end{eqnarray*}
1634 > \begin{eqnarray*}
1635 > m\ddot x & = & - \frac{{\partial W(x)}}{{\partial x}} - \int_0^t
1636   {\sum\limits_{\alpha  = 1}^N {\left( { - \frac{{g_\alpha ^2
1637   }}{{m_\alpha  \omega _\alpha ^2 }}} \right)\cos (\omega _\alpha
1638 < t)\dot x(t - \tau )d} \tau }  + \sum\limits_{\alpha  = 1}^N {\left\{
1639 < {\left[ {g_\alpha  x_\alpha  (0) \\
1640 < & & \mbox{} - \frac{{g_\alpha  }}{{m_\alpha \omega _\alpha  }}}
1638 > t)\dot x(t - \tau )d} \tau }  \\
1639 > & & + \sum\limits_{\alpha  = 1}^N {\left\{ {\left[ {g_\alpha
1640 > x_\alpha (0) - \frac{{g_\alpha }}{{m_\alpha \omega _\alpha  }}}
1641   \right]\cos (\omega _\alpha  t) + \frac{{g_\alpha  \dot x_\alpha
1642   (0)}}{{\omega _\alpha  }}\sin (\omega _\alpha  t)} \right\}}
1643   \end{eqnarray*}
# Line 1697 | Line 1663 | which is known as the \emph{generalized Langevin equat
1663   \end{equation}
1664   which is known as the \emph{generalized Langevin equation}.
1665  
1666 < \subsubsection{\label{introSection:randomForceDynamicFrictionKernel}Random Force and Dynamic Friction Kernel}
1666 > \subsubsection{\label{introSection:randomForceDynamicFrictionKernel}\textbf{Random Force and Dynamic Friction Kernel}}
1667  
1668   One may notice that $R(t)$ depends only on initial conditions, which
1669   implies it is completely deterministic within the context of a
# Line 1710 | Line 1676 | as the model, which is gaussian distribution in genera
1676   \end{array}
1677   \]
1678   This property is what we expect from a truly random process. As long
1679 < as the model, which is gaussian distribution in general, chosen for
1680 < $R(t)$ is a truly random process, the stochastic nature of the GLE
1715 < still remains.
1679 > as the model chosen for $R(t)$ was a gaussian distribution in
1680 > general, the stochastic nature of the GLE still remains.
1681  
1682   %dynamic friction kernel
1683   The convolution integral
# Line 1733 | Line 1698 | which can be used to describe dynamic caging effect. T
1698   m\ddot x =  - \frac{\partial }{{\partial x}}\left( {W(x) +
1699   \frac{1}{2}\xi _0 (x - x_0 )^2 } \right) + R(t),
1700   \]
1701 < which can be used to describe dynamic caging effect. The other
1702 < extreme is the bath that responds infinitely quickly to motions in
1703 < the system. Thus, $\xi (t)$ can be taken as a $delta$ function in
1704 < time:
1701 > which can be used to describe the effect of dynamic caging in
1702 > viscous solvents. The other extreme is the bath that responds
1703 > infinitely quickly to motions in the system. Thus, $\xi (t)$ can be
1704 > taken as a $delta$ function in time:
1705   \[
1706   \xi (t) = 2\xi _0 \delta (t)
1707   \]
# Line 1752 | Line 1717 | or be determined by Stokes' law for regular shaped par
1717   \end{equation}
1718   which is known as the Langevin equation. The static friction
1719   coefficient $\xi _0$ can either be calculated from spectral density
1720 < or be determined by Stokes' law for regular shaped particles.A
1720 > or be determined by Stokes' law for regular shaped particles. A
1721   briefly review on calculating friction tensor for arbitrary shaped
1722   particles is given in Sec.~\ref{introSection:frictionTensor}.
1723  
1724 < \subsubsection{\label{introSection:secondFluctuationDissipation}The Second Fluctuation Dissipation Theorem}
1724 > \subsubsection{\label{introSection:secondFluctuationDissipation}\textbf{The Second Fluctuation Dissipation Theorem}}
1725  
1726   Defining a new set of coordinates,
1727   \[
# Line 1785 | Line 1750 | can model the random force and friction kernel.
1750   \end{equation}
1751   In effect, it acts as a constraint on the possible ways in which one
1752   can model the random force and friction kernel.
1788
1789 \subsection{\label{introSection:frictionTensor} Friction Tensor}
1790 Theoretically, the friction kernel can be determined using velocity
1791 autocorrelation function. However, this approach become impractical
1792 when the system become more and more complicate. Instead, various
1793 approaches based on hydrodynamics have been developed to calculate
1794 the friction coefficients. The friction effect is isotropic in
1795 Equation, $\zeta$ can be taken as a scalar. In general, friction
1796 tensor $\Xi$ is a $6\times 6$ matrix given by
1797 \[
1798 \Xi  = \left( {\begin{array}{*{20}c}
1799   {\Xi _{}^{tt} } & {\Xi _{}^{rt} }  \\
1800   {\Xi _{}^{tr} } & {\Xi _{}^{rr} }  \\
1801 \end{array}} \right).
1802 \]
1803 Here, $ {\Xi^{tt} }$ and $ {\Xi^{rr} }$ are translational friction
1804 tensor and rotational resistance (friction) tensor respectively,
1805 while ${\Xi^{tr} }$ is translation-rotation coupling tensor and $
1806 {\Xi^{rt} }$ is rotation-translation coupling tensor. When a
1807 particle moves in a fluid, it may experience friction force or
1808 torque along the opposite direction of the velocity or angular
1809 velocity,
1810 \[
1811 \left( \begin{array}{l}
1812 F_R  \\
1813 \tau _R  \\
1814 \end{array} \right) =  - \left( {\begin{array}{*{20}c}
1815   {\Xi ^{tt} } & {\Xi ^{rt} }  \\
1816   {\Xi ^{tr} } & {\Xi ^{rr} }  \\
1817 \end{array}} \right)\left( \begin{array}{l}
1818 v \\
1819 w \\
1820 \end{array} \right)
1821 \]
1822 where $F_r$ is the friction force and $\tau _R$ is the friction
1823 toque.
1824
1825 \subsubsection{\label{introSection:resistanceTensorRegular}The Resistance Tensor for Regular Shape}
1826
1827 For a spherical particle, the translational and rotational friction
1828 constant can be calculated from Stoke's law,
1829 \[
1830 \Xi ^{tt}  = \left( {\begin{array}{*{20}c}
1831   {6\pi \eta R} & 0 & 0  \\
1832   0 & {6\pi \eta R} & 0  \\
1833   0 & 0 & {6\pi \eta R}  \\
1834 \end{array}} \right)
1835 \]
1836 and
1837 \[
1838 \Xi ^{rr}  = \left( {\begin{array}{*{20}c}
1839   {8\pi \eta R^3 } & 0 & 0  \\
1840   0 & {8\pi \eta R^3 } & 0  \\
1841   0 & 0 & {8\pi \eta R^3 }  \\
1842 \end{array}} \right)
1843 \]
1844 where $\eta$ is the viscosity of the solvent and $R$ is the
1845 hydrodynamics radius.
1846
1847 Other non-spherical shape, such as cylinder and ellipsoid
1848 \textit{etc}, are widely used as reference for developing new
1849 hydrodynamics theory, because their properties can be calculated
1850 exactly. In 1936, Perrin extended Stokes's law to general ellipsoid,
1851 also called a triaxial ellipsoid, which is given in Cartesian
1852 coordinates by\cite{Perrin1934, Perrin1936}
1853 \[
1854 \frac{{x^2 }}{{a^2 }} + \frac{{y^2 }}{{b^2 }} + \frac{{z^2 }}{{c^2
1855 }} = 1
1856 \]
1857 where the semi-axes are of lengths $a$, $b$, and $c$. Unfortunately,
1858 due to the complexity of the elliptic integral, only the ellipsoid
1859 with the restriction of two axes having to be equal, \textit{i.e.}
1860 prolate($ a \ge b = c$) and oblate ($ a < b = c $), can be solved
1861 exactly. Introducing an elliptic integral parameter $S$ for prolate,
1862 \[
1863 S = \frac{2}{{\sqrt {a^2  - b^2 } }}\ln \frac{{a + \sqrt {a^2  - b^2
1864 } }}{b},
1865 \]
1866 and oblate,
1867 \[
1868 S = \frac{2}{{\sqrt {b^2  - a^2 } }}arctg\frac{{\sqrt {b^2  - a^2 }
1869 }}{a}
1870 \],
1871 one can write down the translational and rotational resistance
1872 tensors
1873 \[
1874 \begin{array}{l}
1875 \Xi _a^{tt}  = 16\pi \eta \frac{{a^2  - b^2 }}{{(2a^2  - b^2 )S - 2a}} \\
1876 \Xi _b^{tt}  = \Xi _c^{tt}  = 32\pi \eta \frac{{a^2  - b^2 }}{{(2a^2  - 3b^2 )S + 2a}} \\
1877 \end{array},
1878 \]
1879 and
1880 \[
1881 \begin{array}{l}
1882 \Xi _a^{rr}  = \frac{{32\pi }}{3}\eta \frac{{(a^2  - b^2 )b^2 }}{{2a - b^2 S}} \\
1883 \Xi _b^{rr}  = \Xi _c^{rr}  = \frac{{32\pi }}{3}\eta \frac{{(a^4  - b^4 )}}{{(2a^2  - b^2 )S - 2a}} \\
1884 \end{array}.
1885 \]
1886
1887 \subsubsection{\label{introSection:resistanceTensorRegularArbitrary}The Resistance Tensor for Arbitrary Shape}
1888
1889 Unlike spherical and other regular shaped molecules, there is not
1890 analytical solution for friction tensor of any arbitrary shaped
1891 rigid molecules. The ellipsoid of revolution model and general
1892 triaxial ellipsoid model have been used to approximate the
1893 hydrodynamic properties of rigid bodies. However, since the mapping
1894 from all possible ellipsoidal space, $r$-space, to all possible
1895 combination of rotational diffusion coefficients, $D$-space is not
1896 unique\cite{Wegener1979} as well as the intrinsic coupling between
1897 translational and rotational motion of rigid body, general ellipsoid
1898 is not always suitable for modeling arbitrarily shaped rigid
1899 molecule. A number of studies have been devoted to determine the
1900 friction tensor for irregularly shaped rigid bodies using more
1901 advanced method where the molecule of interest was modeled by
1902 combinations of spheres(beads)\cite{Carrasco1999} and the
1903 hydrodynamics properties of the molecule can be calculated using the
1904 hydrodynamic interaction tensor. Let us consider a rigid assembly of
1905 $N$ beads immersed in a continuous medium. Due to hydrodynamics
1906 interaction, the ``net'' velocity of $i$th bead, $v'_i$ is different
1907 than its unperturbed velocity $v_i$,
1908 \[
1909 v'_i  = v_i  - \sum\limits_{j \ne i} {T_{ij} F_j }
1910 \]
1911 where $F_i$ is the frictional force, and $T_{ij}$ is the
1912 hydrodynamic interaction tensor. The friction force of $i$th bead is
1913 proportional to its ``net'' velocity
1914 \begin{equation}
1915 F_i  = \zeta _i v_i  - \zeta _i \sum\limits_{j \ne i} {T_{ij} F_j }.
1916 \label{introEquation:tensorExpression}
1917 \end{equation}
1918 This equation is the basis for deriving the hydrodynamic tensor. In
1919 1930, Oseen and Burgers gave a simple solution to Equation
1920 \ref{introEquation:tensorExpression}
1921 \begin{equation}
1922 T_{ij}  = \frac{1}{{8\pi \eta r_{ij} }}\left( {I + \frac{{R_{ij}
1923 R_{ij}^T }}{{R_{ij}^2 }}} \right).
1924 \label{introEquation:oseenTensor}
1925 \end{equation}
1926 Here $R_{ij}$ is the distance vector between bead $i$ and bead $j$.
1927 A second order expression for element of different size was
1928 introduced by Rotne and Prager\cite{Rotne1969} and improved by
1929 Garc\'{i}a de la Torre and Bloomfield\cite{Torre1977},
1930 \begin{equation}
1931 T_{ij}  = \frac{1}{{8\pi \eta R_{ij} }}\left[ {\left( {I +
1932 \frac{{R_{ij} R_{ij}^T }}{{R_{ij}^2 }}} \right) + R\frac{{\sigma
1933 _i^2  + \sigma _j^2 }}{{r_{ij}^2 }}\left( {\frac{I}{3} -
1934 \frac{{R_{ij} R_{ij}^T }}{{R_{ij}^2 }}} \right)} \right].
1935 \label{introEquation:RPTensorNonOverlapped}
1936 \end{equation}
1937 Both of the Equation \ref{introEquation:oseenTensor} and Equation
1938 \ref{introEquation:RPTensorNonOverlapped} have an assumption $R_{ij}
1939 \ge \sigma _i  + \sigma _j$. An alternative expression for
1940 overlapping beads with the same radius, $\sigma$, is given by
1941 \begin{equation}
1942 T_{ij}  = \frac{1}{{6\pi \eta R_{ij} }}\left[ {\left( {1 -
1943 \frac{2}{{32}}\frac{{R_{ij} }}{\sigma }} \right)I +
1944 \frac{2}{{32}}\frac{{R_{ij} R_{ij}^T }}{{R_{ij} \sigma }}} \right]
1945 \label{introEquation:RPTensorOverlapped}
1946 \end{equation}
1947
1948 To calculate the resistance tensor at an arbitrary origin $O$, we
1949 construct a $3N \times 3N$ matrix consisting of $N \times N$
1950 $B_{ij}$ blocks
1951 \begin{equation}
1952 B = \left( {\begin{array}{*{20}c}
1953   {B_{11} } &  \ldots  & {B_{1N} }  \\
1954    \vdots  &  \ddots  &  \vdots   \\
1955   {B_{N1} } &  \cdots  & {B_{NN} }  \\
1956 \end{array}} \right),
1957 \end{equation}
1958 where $B_{ij}$ is given by
1959 \[
1960 B_{ij}  = \delta _{ij} \frac{I}{{6\pi \eta R}} + (1 - \delta _{ij}
1961 )T_{ij}
1962 \]
1963 where $\delta _{ij}$ is Kronecker delta function. Inverting matrix
1964 $B$, we obtain
1965
1966 \[
1967 C = B^{ - 1}  = \left( {\begin{array}{*{20}c}
1968   {C_{11} } &  \ldots  & {C_{1N} }  \\
1969    \vdots  &  \ddots  &  \vdots   \\
1970   {C_{N1} } &  \cdots  & {C_{NN} }  \\
1971 \end{array}} \right)
1972 \]
1973 , which can be partitioned into $N \times N$ $3 \times 3$ block
1974 $C_{ij}$. With the help of $C_{ij}$ and skew matrix $U_i$
1975 \[
1976 U_i  = \left( {\begin{array}{*{20}c}
1977   0 & { - z_i } & {y_i }  \\
1978   {z_i } & 0 & { - x_i }  \\
1979   { - y_i } & {x_i } & 0  \\
1980 \end{array}} \right)
1981 \]
1982 where $x_i$, $y_i$, $z_i$ are the components of the vector joining
1983 bead $i$ and origin $O$. Hence, the elements of resistance tensor at
1984 arbitrary origin $O$ can be written as
1985 \begin{equation}
1986 \begin{array}{l}
1987 \Xi _{}^{tt}  = \sum\limits_i {\sum\limits_j {C_{ij} } } , \\
1988 \Xi _{}^{tr}  = \Xi _{}^{rt}  = \sum\limits_i {\sum\limits_j {U_i C_{ij} } } , \\
1989 \Xi _{}^{rr}  =  - \sum\limits_i {\sum\limits_j {U_i C_{ij} } } U_j  \\
1990 \end{array}
1991 \label{introEquation:ResistanceTensorArbitraryOrigin}
1992 \end{equation}
1993
1994 The resistance tensor depends on the origin to which they refer. The
1995 proper location for applying friction force is the center of
1996 resistance (reaction), at which the trace of rotational resistance
1997 tensor, $ \Xi ^{rr}$ reaches minimum. Mathematically, the center of
1998 resistance is defined as an unique point of the rigid body at which
1999 the translation-rotation coupling tensor are symmetric,
2000 \begin{equation}
2001 \Xi^{tr}  = \left( {\Xi^{tr} } \right)^T
2002 \label{introEquation:definitionCR}
2003 \end{equation}
2004 Form Equation \ref{introEquation:ResistanceTensorArbitraryOrigin},
2005 we can easily find out that the translational resistance tensor is
2006 origin independent, while the rotational resistance tensor and
2007 translation-rotation coupling resistance tensor depend on the
2008 origin. Given resistance tensor at an arbitrary origin $O$, and a
2009 vector ,$r_{OP}(x_{OP}, y_{OP}, z_{OP})$, from $O$ to $P$, we can
2010 obtain the resistance tensor at $P$ by
2011 \begin{equation}
2012 \begin{array}{l}
2013 \Xi _P^{tt}  = \Xi _O^{tt}  \\
2014 \Xi _P^{tr}  = \Xi _P^{rt}  = \Xi _O^{tr}  - U_{OP} \Xi _O^{tt}  \\
2015 \Xi _P^{rr}  = \Xi _O^{rr}  - U_{OP} \Xi _O^{tt} U_{OP}  + \Xi _O^{tr} U_{OP}  - U_{OP} \Xi _O^{tr} ^{^T }  \\
2016 \end{array}
2017 \label{introEquation:resistanceTensorTransformation}
2018 \end{equation}
2019 where
2020 \[
2021 U_{OP}  = \left( {\begin{array}{*{20}c}
2022   0 & { - z_{OP} } & {y_{OP} }  \\
2023   {z_i } & 0 & { - x_{OP} }  \\
2024   { - y_{OP} } & {x_{OP} } & 0  \\
2025 \end{array}} \right)
2026 \]
2027 Using Equations \ref{introEquation:definitionCR} and
2028 \ref{introEquation:resistanceTensorTransformation}, one can locate
2029 the position of center of resistance,
2030 \begin{eqnarray*}
2031 \left( \begin{array}{l}
2032 x_{OR}  \\
2033 y_{OR}  \\
2034 z_{OR}  \\
2035 \end{array} \right) & = &\left( {\begin{array}{*{20}c}
2036   {(\Xi _O^{rr} )_{yy}  + (\Xi _O^{rr} )_{zz} } & { - (\Xi _O^{rr} )_{xy} } & { - (\Xi _O^{rr} )_{xz} }  \\
2037   { - (\Xi _O^{rr} )_{xy} } & {(\Xi _O^{rr} )_{zz}  + (\Xi _O^{rr} )_{xx} } & { - (\Xi _O^{rr} )_{yz} }  \\
2038   { - (\Xi _O^{rr} )_{xz} } & { - (\Xi _O^{rr} )_{yz} } & {(\Xi _O^{rr} )_{xx}  + (\Xi _O^{rr} )_{yy} }  \\
2039 \end{array}} \right)^{ - 1}  \\
2040  & & \left( \begin{array}{l}
2041 (\Xi _O^{tr} )_{yz}  - (\Xi _O^{tr} )_{zy}  \\
2042 (\Xi _O^{tr} )_{zx}  - (\Xi _O^{tr} )_{xz}  \\
2043 (\Xi _O^{tr} )_{xy}  - (\Xi _O^{tr} )_{yx}  \\
2044 \end{array} \right) \\
2045 \end{eqnarray*}
2046
2047
2048
2049 where $x_OR$, $y_OR$, $z_OR$ are the components of the vector
2050 joining center of resistance $R$ and origin $O$.

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