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# Line 3 | Line 3 | Closely related to Classical Mechanics, Molecular Dyna
3   \section{\label{introSection:classicalMechanics}Classical
4   Mechanics}
5  
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
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
13 < specification of this state; Finally, the specification of the state
14 < when further combine with the laws of mechanics will also be
15 < sufficient to predict the future behavior of the system.
6 > Using equations of motion derived from Classical Mechanics,
7 > Molecular Dynamics simulations are carried out by integrating the
8 > equations of motion for a given system of particles. There are three
9 > fundamental ideas behind classical mechanics. Firstly, one can
10 > determine the state of a mechanical system at any time of interest;
11 > Secondly, all the mechanical properties of the system at that time
12 > can be determined by combining the knowledge of the properties of
13 > the system with the specification of this state; Finally, the
14 > specification of the state when further combined with the laws of
15 > mechanics will also be sufficient to predict the future behavior of
16 > the system.
17  
18   \subsection{\label{introSection:newtonian}Newtonian Mechanics}
19   The discovery of Newton's three laws of mechanics which govern the
# Line 31 | Line 32 | F_{ij} = -F_{ji}
32   $F_{ji}$ be the force that particle $j$ exerts on particle $i$.
33   Newton's third law states that
34   \begin{equation}
35 < F_{ij} = -F_{ji}
35 > F_{ij} = -F_{ji}.
36   \label{introEquation:newtonThirdLaw}
37   \end{equation}
37
38   Conservation laws of Newtonian Mechanics play very important roles
39   in solving mechanics problems. The linear momentum of a particle is
40   conserved if it is free or it experiences no force. The second
# Line 63 | Line 63 | that if all forces are conservative, Energy
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
66 < that if all forces are conservative, Energy
67 < \begin{equation}E = T + V \label{introEquation:energyConservation}
66 > that if all forces are conservative, energy is conserved,
67 > \begin{equation}E = T + V. \label{introEquation:energyConservation}
68   \end{equation}
69 < is conserved. All of these conserved quantities are
70 < important factors to determine the quality of numerical integration
71 < schemes for rigid bodies \cite{Dullweber1997}.
69 > All of these conserved quantities are important factors to determine
70 > the quality of numerical integration schemes for rigid bodies
71 > \cite{Dullweber1997}.
72  
73   \subsection{\label{introSection:lagrangian}Lagrangian Mechanics}
74  
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.
75 > Newtonian Mechanics suffers from an important limitation: motion can
76 > only be described in cartesian coordinate systems which make it
77 > impossible to predict analytically the properties of the system even
78 > if we know all of the details of the interaction. In order to
79 > overcome some of the practical difficulties which arise in attempts
80 > to apply Newton's equation to complex systems, approximate numerical
81 > procedures may be developed.
82  
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 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, $U$.
88 > Hamilton's Principle may be stated as follows: the trajectory, along
89 > which a dynamical system may move from one point to another within a
90 > specified time, is derived by finding the path which minimizes the
91 > time integral of the difference between the kinetic $K$, and
92 > potential energies $U$,
93   \begin{equation}
94 < \delta \int_{t_1 }^{t_2 } {(K - U)dt = 0} ,
94 > \delta \int_{t_1 }^{t_2 } {(K - U)dt = 0}.
95   \label{introEquation:halmitonianPrinciple1}
96   \end{equation}
98
97   For simple mechanical systems, where the forces acting on the
98   different parts are derivable from a potential, the Lagrangian
99   function $L$ can be defined as the difference between the kinetic
100   energy of the system and its potential energy,
101   \begin{equation}
102 < L \equiv K - U = L(q_i ,\dot q_i ) ,
102 > L \equiv K - U = L(q_i ,\dot q_i ).
103   \label{introEquation:lagrangianDef}
104   \end{equation}
105 < then Eq.~\ref{introEquation:halmitonianPrinciple1} becomes
105 > Thus, Eq.~\ref{introEquation:halmitonianPrinciple1} becomes
106   \begin{equation}
107 < \delta \int_{t_1 }^{t_2 } {L dt = 0} ,
107 > \delta \int_{t_1 }^{t_2 } {L dt = 0} .
108   \label{introEquation:halmitonianPrinciple2}
109   \end{equation}
110  
# Line 138 | Line 136 | p_i  = \frac{{\partial L}}{{\partial q_i }}
136   p_i  = \frac{{\partial L}}{{\partial q_i }}
137   \label{introEquation:generalizedMomentaDot}
138   \end{equation}
141
139   With the help of the generalized momenta, we may now define a new
140   quantity $H$ by the equation
141   \begin{equation}
# Line 146 | Line 143 | $L$ is the Lagrangian function for the system.
143   \label{introEquation:hamiltonianDefByLagrangian}
144   \end{equation}
145   where $ \dot q_1  \ldots \dot q_f $ are generalized velocities and
146 < $L$ is the Lagrangian function for the system.
147 <
151 < Differentiating Eq.~\ref{introEquation:hamiltonianDefByLagrangian},
152 < one can obtain
146 > $L$ is the Lagrangian function for the system. Differentiating
147 > Eq.~\ref{introEquation:hamiltonianDefByLagrangian}, one can obtain
148   \begin{equation}
149   dH = \sum\limits_k {\left( {p_k d\dot q_k  + \dot q_k dp_k  -
150   \frac{{\partial L}}{{\partial q_k }}dq_k  - \frac{{\partial
151   L}}{{\partial \dot q_k }}d\dot q_k } \right)}  - \frac{{\partial
152 < L}}{{\partial t}}dt \label{introEquation:diffHamiltonian1}
152 > L}}{{\partial t}}dt . \label{introEquation:diffHamiltonian1}
153   \end{equation}
154 < Making use of  Eq.~\ref{introEquation:generalizedMomenta}, the
155 < second and fourth terms in the parentheses cancel. Therefore,
154 > Making use of Eq.~\ref{introEquation:generalizedMomenta}, the second
155 > and fourth terms in the parentheses cancel. Therefore,
156   Eq.~\ref{introEquation:diffHamiltonian1} can be rewritten as
157   \begin{equation}
158   dH = \sum\limits_k {\left( {\dot q_k dp_k  - \dot p_k dq_k }
159 < \right)}  - \frac{{\partial L}}{{\partial t}}dt
159 > \right)}  - \frac{{\partial L}}{{\partial t}}dt .
160   \label{introEquation:diffHamiltonian2}
161   \end{equation}
162   By identifying the coefficients of $dq_k$, $dp_k$ and dt, we can
# Line 180 | Line 175 | t}}
175   t}}
176   \label{introEquation:motionHamiltonianTime}
177   \end{equation}
178 <
184 < Eq.~\ref{introEquation:motionHamiltonianCoordinate} and
178 > where Eq.~\ref{introEquation:motionHamiltonianCoordinate} and
179   Eq.~\ref{introEquation:motionHamiltonianMomentum} are Hamilton's
180   equation of motion. Due to their symmetrical formula, they are also
181   known as the canonical equations of motions \cite{Goldstein2001}.
# Line 195 | Line 189 | only works with 1st-order differential equations\cite{
189   statistical mechanics and quantum mechanics, since it treats the
190   coordinate and its time derivative as independent variables and it
191   only works with 1st-order differential equations\cite{Marion1990}.
198
192   In Newtonian Mechanics, a system described by conservative forces
193 < conserves the total energy \ref{introEquation:energyConservation}.
194 < It follows that Hamilton's equations of motion conserve the total
195 < Hamiltonian.
193 > conserves the total energy
194 > (Eq.~\ref{introEquation:energyConservation}). It follows that
195 > Hamilton's equations of motion conserve the total Hamiltonian
196   \begin{equation}
197   \frac{{dH}}{{dt}} = \sum\limits_i {\left( {\frac{{\partial
198   H}}{{\partial q_i }}\dot q_i  + \frac{{\partial H}}{{\partial p_i
199   }}\dot p_i } \right)}  = \sum\limits_i {\left( {\frac{{\partial
200   H}}{{\partial q_i }}\frac{{\partial H}}{{\partial p_i }} -
201   \frac{{\partial H}}{{\partial p_i }}\frac{{\partial H}}{{\partial
202 < q_i }}} \right) = 0} \label{introEquation:conserveHalmitonian}
202 > q_i }}} \right) = 0}. \label{introEquation:conserveHalmitonian}
203   \end{equation}
204  
205   \section{\label{introSection:statisticalMechanics}Statistical
# Line 221 | Line 214 | possible states. Each possible state of the system cor
214   \subsection{\label{introSection:ensemble}Phase Space and Ensemble}
215  
216   Mathematically, phase space is the space which represents all
217 < possible states. Each possible state of the system corresponds to
218 < one unique point in the phase space. For mechanical systems, the
219 < phase space usually consists of all possible values of position and
220 < momentum variables. Consider a dynamic system of $f$ particles in a
221 < cartesian space, where each of the $6f$ coordinates and momenta is
222 < assigned to one of $6f$ mutually orthogonal axes, the phase space of
223 < this system is a $6f$ dimensional space. A point, $x = (\rightarrow
224 < q_1 , \ldots ,\rightarrow q_f ,\rightarrow p_1 , \ldots ,\rightarrow
225 < p_f )$, with a unique set of values of $6f$ coordinates and momenta
226 < is a phase space vector.
217 > possible states of a system. Each possible state of the system
218 > corresponds to one unique point in the phase space. For mechanical
219 > systems, the phase space usually consists of all possible values of
220 > position and momentum variables. Consider a dynamic system of $f$
221 > particles in a cartesian space, where each of the $6f$ coordinates
222 > and momenta is assigned to one of $6f$ mutually orthogonal axes, the
223 > phase space of this system is a $6f$ dimensional space. A point, $x
224 > =
225 > (\mathord{\buildrel{\lower3pt\hbox{$\scriptscriptstyle\rightharpoonup$}}
226 > \over q} _1 , \ldots
227 > ,\mathord{\buildrel{\lower3pt\hbox{$\scriptscriptstyle\rightharpoonup$}}
228 > \over q} _f
229 > ,\mathord{\buildrel{\lower3pt\hbox{$\scriptscriptstyle\rightharpoonup$}}
230 > \over p} _1  \ldots
231 > ,\mathord{\buildrel{\lower3pt\hbox{$\scriptscriptstyle\rightharpoonup$}}
232 > \over p} _f )$ , with a unique set of values of $6f$ coordinates and
233 > momenta is a phase space vector.
234   %%%fix me
235  
236   In statistical mechanics, the condition of an ensemble at any time
# Line 243 | Line 243 | their locations which would change the density at any
243   \label{introEquation:densityDistribution}
244   \end{equation}
245   Governed by the principles of mechanics, the phase points change
246 < their locations which would change the density at any time at phase
246 > their locations which changes 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,
248 > function of the time. The number of systems $\delta N$ at time $t$
249 > can be determined by,
250   \begin{equation}
251   \delta N = \rho (q,p,t)dq_1  \ldots dq_f dp_1  \ldots dp_f.
252   \label{introEquation:deltaN}
253   \end{equation}
254 < Assuming a large enough population of systems, we can sufficiently
254 > Assuming enough copies of the systems, we can sufficiently
255   approximate $\delta N$ without introducing discontinuity when we go
256   from one region in the phase space to another. By integrating over
257   the whole phase space,
# Line 260 | Line 259 | gives us an expression for the total number of the sys
259   N = \int { \ldots \int {\rho (q,p,t)dq_1 } ...dq_f dp_1 } ...dp_f
260   \label{introEquation:totalNumberSystem}
261   \end{equation}
262 < gives us an expression for the total number of the systems. Hence,
263 < the probability per unit in the phase space can be obtained by,
262 > gives us an expression for the total number of copies. Hence, the
263 > probability per unit volume in the phase space can be obtained by,
264   \begin{equation}
265   \frac{{\rho (q,p,t)}}{N} = \frac{{\rho (q,p,t)}}{{\int { \ldots \int
266   {\rho (q,p,t)dq_1 } ...dq_f dp_1 } ...dp_f }}.
# Line 270 | Line 269 | momenta of the system. Even when the dynamics of the r
269   With the help of Eq.~\ref{introEquation:unitProbability} and the
270   knowledge of the system, it is possible to calculate the average
271   value of any desired quantity which depends on the coordinates and
272 < momenta of the system. Even when the dynamics of the real system is
272 > momenta of the system. Even when the dynamics of the real system are
273   complex, or stochastic, or even discontinuous, the average
274 < properties of the ensemble of possibilities as a whole remaining
275 < well defined. For a classical system in thermal equilibrium with its
274 > properties of the ensemble of possibilities as a whole remain well
275 > defined. For a classical system in thermal equilibrium with its
276   environment, the ensemble average of a mechanical quantity, $\langle
277   A(q , p) \rangle_t$, takes the form of an integral over the phase
278   space of the system,
279   \begin{equation}
280   \langle  A(q , p) \rangle_t = \frac{{\int { \ldots \int {A(q,p)\rho
281   (q,p,t)dq_1 } ...dq_f dp_1 } ...dp_f }}{{\int { \ldots \int {\rho
282 < (q,p,t)dq_1 } ...dq_f dp_1 } ...dp_f }}
282 > (q,p,t)dq_1 } ...dq_f dp_1 } ...dp_f }}.
283   \label{introEquation:ensembelAverage}
284   \end{equation}
285  
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}, 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, 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
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,
303 \begin{equation}
304 \Omega (N,V,T) = e^{ - \beta A}
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 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}
317 \end{equation}
318 Here, $G = U - TS + PV$, and $G$ is called Gibbs free energy.
319
286   \subsection{\label{introSection:liouville}Liouville's theorem}
287  
288   Liouville's theorem is the foundation on which statistical mechanics
# Line 358 | Line 324 | simple form,
324   \frac{{\partial \rho }}{{\partial p_i }}\dot p_i } \right)}  = 0 .
325   \label{introEquation:liouvilleTheorem}
326   \end{equation}
361
327   Liouville's theorem states that the distribution function is
328   constant along any trajectory in phase space. In classical
329 < statistical mechanics, since the number of members in an ensemble is
330 < huge and constant, we can assume the local density has no reason
331 < (other than classical mechanics) to change,
329 > statistical mechanics, since the number of system copies in an
330 > ensemble is huge and constant, we can assume the local density has
331 > no reason (other than classical mechanics) to change,
332   \begin{equation}
333   \frac{{\partial \rho }}{{\partial t}} = 0.
334   \label{introEquation:stationary}
# Line 393 | Line 358 | With the help of stationary assumption
358   \frac{{d(\delta N)}}{{dt}} = \frac{{d\rho }}{{dt}}\delta v + \rho
359   \frac{d}{{dt}}(\delta v) = 0.
360   \end{equation}
361 < With the help of stationary assumption
362 < (\ref{introEquation:stationary}), we obtain the principle of the
361 > With the help of the stationary assumption
362 > (Eq.~\ref{introEquation:stationary}), we obtain the principle of
363   \emph{conservation of volume in phase space},
364   \begin{equation}
365   \frac{d}{{dt}}(\delta v) = \frac{d}{{dt}}\int { \ldots \int {dq_1 }
# Line 404 | Line 369 | Liouville's theorem can be expresses in a variety of d
369  
370   \subsubsection{\label{introSection:liouvilleInOtherForms}\textbf{Liouville's Theorem in Other Forms}}
371  
372 < Liouville's theorem can be expresses in a variety of different forms
372 > Liouville's theorem can be expressed in a variety of different forms
373   which are convenient within different contexts. For any two function
374   $F$ and $G$ of the coordinates and momenta of a system, the Poisson
375   bracket ${F, G}$ is defined as
# Line 415 | Line 380 | Substituting equations of motion in Hamiltonian formal
380   q_i }}} \right)}.
381   \label{introEquation:poissonBracket}
382   \end{equation}
383 < Substituting equations of motion in Hamiltonian formalism(
384 < Eq.~\ref{introEquation:motionHamiltonianCoordinate} ,
385 < Eq.~\ref{introEquation:motionHamiltonianMomentum} ) into
383 > Substituting equations of motion in Hamiltonian formalism
384 > (Eq.~\ref{introEquation:motionHamiltonianCoordinate} ,
385 > Eq.~\ref{introEquation:motionHamiltonianMomentum}) into
386   (Eq.~\ref{introEquation:liouvilleTheorem}), we can rewrite
387   Liouville's theorem using Poisson bracket notion,
388   \begin{equation}
# Line 438 | Line 403 | expressed as
403   \left( {\frac{{\partial \rho }}{{\partial t}}} \right) =  - iL\rho
404   \label{introEquation:liouvilleTheoremInOperator}
405   \end{equation}
406 <
406 > which can help define a propagator $\rho (t) = e^{-iLt} \rho (0)$.
407   \subsection{\label{introSection:ergodic}The Ergodic Hypothesis}
408  
409   Various thermodynamic properties can be calculated from Molecular
# Line 447 | Line 412 | period of them which is different from the average beh
412   simulation and the quality of the underlying model. However, both
413   experiments and computer simulations are usually performed during a
414   certain time interval and the measurements are averaged over a
415 < period of them which is different from the average behavior of
415 > period of time which is different from the average behavior of
416   many-body system in Statistical Mechanics. Fortunately, the Ergodic
417   Hypothesis makes a connection between time average and the ensemble
418   average. It states that the time average and average over the
419 < statistical ensemble are identical \cite{Frenkel1996, Leach2001}.
419 > statistical ensemble are identical \cite{Frenkel1996, Leach2001}:
420   \begin{equation}
421   \langle A(q , p) \rangle_t = \mathop {\lim }\limits_{t \to \infty }
422   \frac{1}{t}\int\limits_0^t {A(q(t),p(t))dt = \int\limits_\Gamma
# Line 460 | Line 425 | sufficiently long time (longer than relaxation time),
425   where $\langle  A(q , p) \rangle_t$ is an equilibrium value of a
426   physical quantity and $\rho (p(t), q(t))$ is the equilibrium
427   distribution function. If an observation is averaged over a
428 < sufficiently long time (longer than relaxation time), all accessible
429 < microstates in phase space are assumed to be equally probed, giving
430 < a properly weighted statistical average. This allows the researcher
431 < freedom of choice when deciding how best to measure a given
432 < observable. In case an ensemble averaged approach sounds most
433 < reasonable, the Monte Carlo techniques\cite{Metropolis1949} can be
428 > sufficiently long time (longer than the relaxation time), all
429 > accessible microstates in phase space are assumed to be equally
430 > probed, giving a properly weighted statistical average. This allows
431 > the researcher freedom of choice when deciding how best to measure a
432 > given observable. In case an ensemble averaged approach sounds most
433 > reasonable, the Monte Carlo methods\cite{Metropolis1949} can be
434   utilized. Or if the system lends itself to a time averaging
435   approach, the Molecular Dynamics techniques in
436   Sec.~\ref{introSection:molecularDynamics} will be the best
# Line 478 | Line 443 | such as symplectic structure, volume and time reversal
443   by the differential equations. However, most of them ignore the
444   hidden physical laws contained within the equations. Since 1990,
445   geometric integrators, which preserve various phase-flow invariants
446 < such as symplectic structure, volume and time reversal symmetry, are
447 < developed to address this issue\cite{Dullweber1997, McLachlan1998,
448 < Leimkuhler1999}. The velocity Verlet method, which happens to be a
449 < simple example of symplectic integrator, continues to gain
450 < popularity in the molecular dynamics community. This fact can be
451 < partly explained by its geometric nature.
446 > such as symplectic structure, volume and time reversal symmetry,
447 > were developed to address this issue\cite{Dullweber1997,
448 > McLachlan1998, Leimkuhler1999}. The velocity Verlet method, which
449 > happens to be a simple example of symplectic integrator, continues
450 > to gain popularity in the molecular dynamics community. This fact
451 > can be partly explained by its geometric nature.
452  
453   \subsection{\label{introSection:symplecticManifold}Symplectic Manifolds}
454   A \emph{manifold} is an abstract mathematical space. It looks
# Line 492 | Line 457 | apply calculus on \emph{differentiable manifold}. A \e
457   surface of Earth. It seems to be flat locally, but it is round if
458   viewed as a whole. A \emph{differentiable manifold} (also known as
459   \emph{smooth manifold}) is a manifold on which it is possible to
460 < apply calculus on \emph{differentiable manifold}. A \emph{symplectic
461 < manifold} is defined as a pair $(M, \omega)$ which consists of a
460 > apply calculus\cite{Hirsch1997}. A \emph{symplectic manifold} is
461 > defined as a pair $(M, \omega)$ which consists of a
462   \emph{differentiable manifold} $M$ and a close, non-degenerated,
463   bilinear symplectic form, $\omega$. A symplectic form on a vector
464   space $V$ is a function $\omega(x, y)$ which satisfies
465   $\omega(\lambda_1x_1+\lambda_2x_2, y) = \lambda_1\omega(x_1, y)+
466   \lambda_2\omega(x_2, y)$, $\omega(x, y) = - \omega(y, x)$ and
467 < $\omega(x, x) = 0$. The cross product operation in vector field is
468 < an example of symplectic form.
467 > $\omega(x, x) = 0$\cite{McDuff1998}. The cross product operation in
468 > vector field is an example of symplectic form. One of the
469 > motivations to study \emph{symplectic manifolds} in Hamiltonian
470 > Mechanics is that a symplectic manifold can represent all possible
471 > configurations of the system and the phase space of the system can
472 > be described by it's cotangent bundle\cite{Jost2002}. Every
473 > symplectic manifold is even dimensional. For instance, in Hamilton
474 > equations, coordinate and momentum always appear in pairs.
475  
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
476   \subsection{\label{introSection:ODE}Ordinary Differential Equations}
477  
478   For an ordinary differential system defined as
# Line 516 | Line 480 | where $x = x(q,p)^T$, this system is a canonical Hamil
480   \dot x = f(x)
481   \end{equation}
482   where $x = x(q,p)^T$, this system is a canonical Hamiltonian, if
483 + $f(x) = J\nabla _x H(x)$. Here, $H = H (q, p)$ is Hamiltonian
484 + function and $J$ is the skew-symmetric matrix
485   \begin{equation}
520 f(r) = J\nabla _x H(r).
521 \end{equation}
522 $H = H (q, p)$ is Hamiltonian function and $J$ is the skew-symmetric
523 matrix
524 \begin{equation}
486   J = \left( {\begin{array}{*{20}c}
487     0 & I  \\
488     { - I} & 0  \\
# Line 531 | Line 492 | system can be rewritten as,
492   where $I$ is an identity matrix. Using this notation, Hamiltonian
493   system can be rewritten as,
494   \begin{equation}
495 < \frac{d}{{dt}}x = J\nabla _x H(x)
495 > \frac{d}{{dt}}x = J\nabla _x H(x).
496   \label{introEquation:compactHamiltonian}
497   \end{equation}In this case, $f$ is
498 < called a \emph{Hamiltonian vector field}.
499 <
539 < Another generalization of Hamiltonian dynamics is Poisson
540 < Dynamics\cite{Olver1986},
498 > called a \emph{Hamiltonian vector field}. Another generalization of
499 > Hamiltonian dynamics is Poisson Dynamics\cite{Olver1986},
500   \begin{equation}
501   \dot x = J(x)\nabla _x H \label{introEquation:poissonHamiltonian}
502   \end{equation}
503   The most obvious change being that matrix $J$ now depends on $x$.
504  
505 < \subsection{\label{introSection:exactFlow}Exact Flow}
505 > \subsection{\label{introSection:exactFlow}Exact Propagator}
506  
507 < Let $x(t)$ be the exact solution of the ODE system,
508 < \begin{equation}
509 < \frac{{dx}}{{dt}} = f(x) \label{introEquation:ODE}
510 < \end{equation}
511 < The exact flow(solution) $\varphi_\tau$ is defined by
553 < \[
554 < x(t+\tau) =\varphi_\tau(x(t))
507 > Let $x(t)$ be the exact solution of the ODE
508 > system,$\frac{{dx}}{{dt}} = f(x) \label{introEquation:ODE}$, we can
509 > define its exact propagator(solution) $\varphi_\tau$
510 > \[ x(t+\tau)
511 > =\varphi_\tau(x(t))
512   \]
513   where $\tau$ is a fixed time step and $\varphi$ is a map from phase
514 < space to itself. The flow has the continuous group property,
514 > space to itself. The propagator has the continuous group property,
515   \begin{equation}
516   \varphi _{\tau _1 }  \circ \varphi _{\tau _2 }  = \varphi _{\tau _1
517   + \tau _2 } .
# Line 563 | Line 520 | Therefore, the exact flow is self-adjoint,
520   \begin{equation}
521   \varphi _\tau   \circ \varphi _{ - \tau }  = I
522   \end{equation}
523 < Therefore, the exact flow is self-adjoint,
523 > Therefore, the exact propagator is self-adjoint,
524   \begin{equation}
525   \varphi _\tau   = \varphi _{ - \tau }^{ - 1}.
526   \end{equation}
527 < The exact flow can also be written in terms of the of an operator,
527 > The exact propagator can also be written in terms of operator,
528   \begin{equation}
529   \varphi _\tau  (x) = e^{\tau \sum\limits_i {f_i (x)\frac{\partial
530   }{{\partial x_i }}} } (x) \equiv \exp (\tau f)(x).
531   \label{introEquation:exponentialOperator}
532   \end{equation}
533 <
534 < In most cases, it is not easy to find the exact flow $\varphi_\tau$.
535 < Instead, we use an approximate map, $\psi_\tau$, which is usually
536 < called integrator. The order of an integrator $\psi_\tau$ is $p$, if
537 < the Taylor series of $\psi_\tau$ agree to order $p$,
533 > In most cases, it is not easy to find the exact propagator
534 > $\varphi_\tau$. Instead, we use an approximate map, $\psi_\tau$,
535 > which is usually called an integrator. The order of an integrator
536 > $\psi_\tau$ is $p$, if the Taylor series of $\psi_\tau$ agree to
537 > order $p$,
538   \begin{equation}
539   \psi_\tau(x) = x + \tau f(x) + O(\tau^{p+1})
540   \end{equation}
# Line 585 | Line 542 | ODE and its flow play important roles in numerical stu
542   \subsection{\label{introSection:geometricProperties}Geometric Properties}
543  
544   The hidden geometric properties\cite{Budd1999, Marsden1998} of an
545 < ODE and its flow play important roles in numerical studies. Many of
546 < them can be found in systems which occur naturally in applications.
547 <
548 < Let $\varphi$ be the flow of Hamiltonian vector field, $\varphi$ is
592 < a \emph{symplectic} flow if it satisfies,
545 > ODE and its propagator play important roles in numerical studies.
546 > Many of them can be found in systems which occur naturally in
547 > applications. Let $\varphi$ be the propagator of Hamiltonian vector
548 > field, $\varphi$ is a \emph{symplectic} propagator if it satisfies,
549   \begin{equation}
550   {\varphi '}^T J \varphi ' = J.
551   \end{equation}
552   According to Liouville's theorem, the symplectic volume is invariant
553 < under a Hamiltonian flow, which is the basis for classical
554 < statistical mechanics. Furthermore, the flow of a Hamiltonian vector
555 < field on a symplectic manifold can be shown to be a
553 > under a Hamiltonian propagator, which is the basis for classical
554 > statistical mechanics. Furthermore, the propagator of a Hamiltonian
555 > vector field on a symplectic manifold can be shown to be a
556   symplectomorphism. As to the Poisson system,
557   \begin{equation}
558   {\varphi '}^T J \varphi ' = J \circ \varphi
559   \end{equation}
560 < is the property that must be preserved by the integrator.
561 <
562 < It is possible to construct a \emph{volume-preserving} flow for a
563 < source free ODE ($ \nabla \cdot f = 0 $), if the flow satisfies $
564 < \det d\varphi  = 1$. One can show easily that a symplectic flow will
565 < be volume-preserving.
566 <
611 < Changing the variables $y = h(x)$ in an ODE
612 < (Eq.~\ref{introEquation:ODE}) will result in a new system,
560 > is the property that must be preserved by the integrator. It is
561 > possible to construct a \emph{volume-preserving} propagator for a
562 > source free ODE ($ \nabla \cdot f = 0 $), if the propagator
563 > satisfies $ \det d\varphi  = 1$. One can show easily that a
564 > symplectic propagator will be volume-preserving. Changing the
565 > variables $y = h(x)$ in an ODE (Eq.~\ref{introEquation:ODE}) will
566 > result in a new system,
567   \[
568   \dot y = \tilde f(y) = ((dh \cdot f)h^{ - 1} )(y).
569   \]
570   The vector filed $f$ has reversing symmetry $h$ if $f = - \tilde f$.
571 < In other words, the flow of this vector field is reversible if and
572 < only if $ h \circ \varphi ^{ - 1}  = \varphi  \circ h $.
573 <
574 < A \emph{first integral}, or conserved quantity of a general
575 < differential function is a function $ G:R^{2d}  \to R^d $ which is
622 < constant for all solutions of the ODE $\frac{{dx}}{{dt}} = f(x)$ ,
571 > In other words, the propagator of this vector field is reversible if
572 > and only if $ h \circ \varphi ^{ - 1}  = \varphi  \circ h $. A
573 > conserved quantity of a general differential function is a function
574 > $ G:R^{2d}  \to R^d $ which is constant for all solutions of the ODE
575 > $\frac{{dx}}{{dt}} = f(x)$ ,
576   \[
577   \frac{{dG(x(t))}}{{dt}} = 0.
578   \]
579 < Using chain rule, one may obtain,
579 > Using the chain rule, one may obtain,
580   \[
581 < \sum\limits_i {\frac{{dG}}{{dx_i }}} f_i (x) = f \bullet \nabla G,
581 > \sum\limits_i {\frac{{dG}}{{dx_i }}} f_i (x) = f \dot \nabla G,
582   \]
583 < which is the condition for conserving \emph{first integral}. For a
584 < canonical Hamiltonian system, the time evolution of an arbitrary
585 < smooth function $G$ is given by,
633 <
583 > which is the condition for conserved quantities. For a canonical
584 > Hamiltonian system, the time evolution of an arbitrary smooth
585 > function $G$ is given by,
586   \begin{eqnarray}
587 < \frac{{dG(x(t))}}{{dt}} & = & [\nabla _x G(x(t))]^T \dot x(t) \\
588 <                        & = & [\nabla _x G(x(t))]^T J\nabla _x H(x(t)). \\
587 > \frac{{dG(x(t))}}{{dt}} & = & [\nabla _x G(x(t))]^T \dot x(t) \notag\\
588 >                        & = & [\nabla _x G(x(t))]^T J\nabla _x H(x(t)).
589   \label{introEquation:firstIntegral1}
590   \end{eqnarray}
591 <
592 <
641 < Using poisson bracket notion, Equation
642 < \ref{introEquation:firstIntegral1} can be rewritten as
591 > Using poisson bracket notion, Eq.~\ref{introEquation:firstIntegral1}
592 > can be rewritten as
593   \[
594   \frac{d}{{dt}}G(x(t)) = \left\{ {G,H} \right\}(x(t)).
595   \]
596 < Therefore, the sufficient condition for $G$ to be the \emph{first
597 < integral} of a Hamiltonian system is
598 < \[
599 < \left\{ {G,H} \right\} = 0.
650 < \]
651 < As well known, the Hamiltonian (or energy) H of a Hamiltonian system
652 < is a \emph{first integral}, which is due to the fact $\{ H,H\}  =
653 < 0$.
654 <
596 > Therefore, the sufficient condition for $G$ to be a conserved
597 > quantity of a Hamiltonian system is $\left\{ {G,H} \right\} = 0.$ As
598 > is well known, the Hamiltonian (or energy) H of a Hamiltonian system
599 > is a conserved quantity, which is due to the fact $\{ H,H\}  = 0$.
600   When designing any numerical methods, one should always try to
601 < preserve the structural properties of the original ODE and its flow.
601 > preserve the structural properties of the original ODE and its
602 > propagator.
603  
604   \subsection{\label{introSection:constructionSymplectic}Construction of Symplectic Methods}
605   A lot of well established and very effective numerical methods have
606 < been successful precisely because of their symplecticities even
606 > been successful precisely because of their symplectic nature even
607   though this fact was not recognized when they were first
608   constructed. The most famous example is the Verlet-leapfrog method
609   in molecular dynamics. In general, symplectic integrators can be
# Line 668 | Line 614 | constructed using one of four different methods.
614   \item Runge-Kutta methods
615   \item Splitting methods
616   \end{enumerate}
617 <
672 < Generating function\cite{Channell1990} tends to lead to methods
617 > Generating functions\cite{Channell1990} tend to lead to methods
618   which are cumbersome and difficult to use. In dissipative systems,
619   variational methods can capture the decay of energy
620 < accurately\cite{Kane2000}. Since their geometrically unstable nature
620 > accurately\cite{Kane2000}. Since they are geometrically unstable
621   against non-Hamiltonian perturbations, ordinary implicit Runge-Kutta
622   methods are not suitable for Hamiltonian system. Recently, various
623 < high-order explicit Runge-Kutta methods
624 < \cite{Owren1992,Chen2003}have been developed to overcome this
625 < instability. However, due to computational penalty involved in
626 < implementing the Runge-Kutta methods, they have not attracted much
627 < attention from the Molecular Dynamics community. Instead, splitting
628 < methods have been widely accepted since they exploit natural
629 < decompositions of the system\cite{Tuckerman1992, McLachlan1998}.
623 > high-order explicit Runge-Kutta methods \cite{Owren1992,Chen2003}
624 > have been developed to overcome this instability. However, due to
625 > computational penalty involved in implementing the Runge-Kutta
626 > methods, they have not attracted much attention from the Molecular
627 > Dynamics community. Instead, splitting methods have been widely
628 > accepted since they exploit natural decompositions of the
629 > system\cite{Tuckerman1992, McLachlan1998}.
630  
631   \subsubsection{\label{introSection:splittingMethod}\textbf{Splitting Methods}}
632  
633   The main idea behind splitting methods is to decompose the discrete
634 < $\varphi_h$ as a composition of simpler flows,
634 > $\varphi_h$ as a composition of simpler propagators,
635   \begin{equation}
636   \varphi _h  = \varphi _{h_1 }  \circ \varphi _{h_2 }  \ldots  \circ
637   \varphi _{h_n }
638   \label{introEquation:FlowDecomposition}
639   \end{equation}
640 < where each of the sub-flow is chosen such that each represent a
641 < simpler integration of the system.
642 <
698 < Suppose that a Hamiltonian system takes the form,
640 > where each of the sub-propagator is chosen such that each represent
641 > a simpler integration of the system. Suppose that a Hamiltonian
642 > system takes the form,
643   \[
644   H = H_1 + H_2.
645   \]
646   Here, $H_1$ and $H_2$ may represent different physical processes of
647   the system. For instance, they may relate to kinetic and potential
648   energy respectively, which is a natural decomposition of the
649 < problem. If $H_1$ and $H_2$ can be integrated using exact flows
650 < $\varphi_1(t)$ and $\varphi_2(t)$, respectively, a simple first
651 < order expression is then given by the Lie-Trotter formula
649 > problem. If $H_1$ and $H_2$ can be integrated using exact
650 > propagators $\varphi_1(t)$ and $\varphi_2(t)$, respectively, a
651 > simple first order expression is then given by the Lie-Trotter
652 > formula
653   \begin{equation}
654   \varphi _h  = \varphi _{1,h}  \circ \varphi _{2,h},
655   \label{introEquation:firstOrderSplitting}
# Line 713 | Line 658 | It is easy to show that any composition of symplectic
658   continuous $\varphi _i$ over a time $h$. By definition, as
659   $\varphi_i(t)$ is the exact solution of a Hamiltonian system, it
660   must follow that each operator $\varphi_i(t)$ is a symplectic map.
661 < It is easy to show that any composition of symplectic flows yields a
662 < symplectic map,
661 > It is easy to show that any composition of symplectic propagators
662 > yields a symplectic map,
663   \begin{equation}
664   (\varphi '\phi ')^T J\varphi '\phi ' = \phi '^T \varphi '^T J\varphi
665   '\phi ' = \phi '^T J\phi ' = J,
# Line 722 | Line 667 | splitting in this context automatically generates a sy
667   \end{equation}
668   where $\phi$ and $\psi$ both are symplectic maps. Thus operator
669   splitting in this context automatically generates a symplectic map.
670 <
671 < The Lie-Trotter splitting(\ref{introEquation:firstOrderSplitting})
672 < introduces local errors proportional to $h^2$, while Strang
673 < splitting gives a second-order decomposition,
670 > The Lie-Trotter
671 > splitting(Eq.~\ref{introEquation:firstOrderSplitting}) introduces
672 > local errors proportional to $h^2$, while the Strang splitting gives
673 > a second-order decomposition,
674   \begin{equation}
675   \varphi _h  = \varphi _{1,h/2}  \circ \varphi _{2,h}  \circ \varphi
676   _{1,h/2} , \label{introEquation:secondOrderSplitting}
677   \end{equation}
678 < which has a local error proportional to $h^3$. The Sprang
678 > which has a local error proportional to $h^3$. The Strang
679   splitting's popularity in molecular simulation community attribute
680   to its symmetric property,
681   \begin{equation}
# Line 785 | Line 730 | the equations of motion would follow:
730  
731   \item Repeat from step 1 with the new position, velocities, and forces assuming the roles of the initial values.
732   \end{enumerate}
788
733   By simply switching the order of the propagators in the splitting
734   and composing a new integrator, the \emph{position verlet}
735   integrator, can be generated,
# Line 802 | Line 746 | local error of splitting method in terms of the commut
746   \subsubsection{\label{introSection:errorAnalysis}\textbf{Error Analysis and Higher Order Methods}}
747  
748   The Baker-Campbell-Hausdorff formula can be used to determine the
749 < local error of splitting method in terms of the commutator of the
749 > local error of a splitting method in terms of the commutator of the
750   operators(\ref{introEquation:exponentialOperator}) associated with
751 < the sub-flow. For operators $hX$ and $hY$ which are associated with
752 < $\varphi_1(t)$ and $\varphi_2(t)$ respectively , we have
751 > the sub-propagator. For operators $hX$ and $hY$ which are associated
752 > with $\varphi_1(t)$ and $\varphi_2(t)$ respectively , we have
753   \begin{equation}
754   \exp (hX + hY) = \exp (hZ)
755   \end{equation}
# Line 814 | Line 758 | Here, $[X,Y]$ is the commutators of operator $X$ and $
758   hZ = hX + hY + \frac{{h^2 }}{2}[X,Y] + \frac{{h^3 }}{2}\left(
759   {[X,[X,Y]] + [Y,[Y,X]]} \right) +  \ldots .
760   \end{equation}
761 < Here, $[X,Y]$ is the commutators of operator $X$ and $Y$ given by
761 > Here, $[X,Y]$ is the commutator of operator $X$ and $Y$ given by
762   \[
763   [X,Y] = XY - YX .
764   \]
765   Applying the Baker-Campbell-Hausdorff formula\cite{Varadarajan1974}
766 < to the Sprang splitting, we can obtain
766 > to the Strang splitting, we can obtain
767   \begin{eqnarray*}
768   \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 \\
769                                     &   & \mbox{} + h^2 [X,X]/8 + h^2 [Y,Y]/8 \\
770 <                                   &   & \mbox{} + h^3 [Y,[Y,X]]/12 - h^3[X,[X,Y]]/24 + \ldots )
770 >                                   &   & \mbox{} + h^3 [Y,[Y,X]]/12 - h^3[X,[X,Y]]/24 + \ldots
771 >                                   ).
772   \end{eqnarray*}
773 < Since \[ [X,Y] + [Y,X] = 0\] and \[ [X,X] = 0,\] the dominant local
774 < error of Spring splitting is proportional to $h^3$. The same
775 < procedure can be applied to a general splitting,  of the form
773 > Since $ [X,Y] + [Y,X] = 0$ and $ [X,X] = 0$, the dominant local
774 > error of Strang splitting is proportional to $h^3$. The same
775 > procedure can be applied to a general splitting of the form
776   \begin{equation}
777   \varphi _{b_m h}^2  \circ \varphi _{a_m h}^1  \circ \varphi _{b_{m -
778   1} h}^2  \circ  \ldots  \circ \varphi _{a_1 h}^1 .
# Line 862 | Line 807 | simulations. For instance, instantaneous temperature o
807   dynamical information. The basic idea of molecular dynamics is that
808   macroscopic properties are related to microscopic behavior and
809   microscopic behavior can be calculated from the trajectories in
810 < simulations. For instance, instantaneous temperature of an
811 < Hamiltonian system of $N$ particle can be measured by
810 > simulations. For instance, instantaneous temperature of a
811 > Hamiltonian system of $N$ particles can be measured by
812   \[
813   T = \sum\limits_{i = 1}^N {\frac{{m_i v_i^2 }}{{fk_B }}}
814   \]
815   where $m_i$ and $v_i$ are the mass and velocity of $i$th particle
816   respectively, $f$ is the number of degrees of freedom, and $k_B$ is
817 < the boltzman constant.
817 > the Boltzman constant.
818  
819   A typical molecular dynamics run consists of three essential steps:
820   \begin{enumerate}
# Line 886 | Line 831 | will discusse issues in production run.
831   These three individual steps will be covered in the following
832   sections. Sec.~\ref{introSec:initialSystemSettings} deals with the
833   initialization of a simulation. Sec.~\ref{introSection:production}
834 < will discusse issues in production run.
834 > will discuss issues of production runs.
835   Sec.~\ref{introSection:Analysis} provides the theoretical tools for
836 < trajectory analysis.
836 > analysis of trajectories.
837  
838   \subsection{\label{introSec:initialSystemSettings}Initialization}
839  
# Line 900 | Line 845 | structure, some important information is missing. For
845   thousands of crystal structures of molecules are discovered every
846   year, many more remain unknown due to the difficulties of
847   purification and crystallization. Even for molecules with known
848 < structure, some important information is missing. For example, a
848 > structures, some important information is missing. For example, a
849   missing hydrogen atom which acts as donor in hydrogen bonding must
850 < be added. Moreover, in order to include electrostatic interaction,
850 > be added. Moreover, in order to include electrostatic interactions,
851   one may need to specify the partial charges for individual atoms.
852   Under some circumstances, we may even need to prepare the system in
853   a special configuration. For instance, when studying transport
# Line 922 | Line 867 | structure from crystallographic data. Relied on the gr
867   surface and to locate the local minimum. While converging slowly
868   near the minimum, steepest descent method is extremely robust when
869   systems are strongly anharmonic. Thus, it is often used to refine
870 < structure from crystallographic data. Relied on the gradient or
871 < hessian, advanced methods like Newton-Raphson converge rapidly to a
872 < local minimum, but become unstable if the energy surface is far from
870 > structures from crystallographic data. Relying on the Hessian,
871 > advanced methods like Newton-Raphson converge rapidly to a local
872 > minimum, but become unstable if the energy surface is far from
873   quadratic. Another factor that must be taken into account, when
874   choosing energy minimization method, is the size of the system.
875   Steepest descent and conjugate gradient can deal with models of any
876   size. Because of the limits on computer memory to store the hessian
877 < matrix and the computing power needed to diagonalized these
878 < matrices, most Newton-Raphson methods can not be used with very
934 < large systems.
877 > matrix and the computing power needed to diagonalize these matrices,
878 > most Newton-Raphson methods can not be used with very large systems.
879  
880   \subsubsection{\textbf{Heating}}
881  
882 < Typically, Heating is performed by assigning random velocities
882 > Typically, heating is performed by assigning random velocities
883   according to a Maxwell-Boltzman distribution for a desired
884   temperature. Beginning at a lower temperature and gradually
885   increasing the temperature by assigning larger random velocities, we
886 < end up with setting the temperature of the system to a final
887 < temperature at which the simulation will be conducted. In heating
888 < phase, we should also keep the system from drifting or rotating as a
889 < whole. To do this, the net linear momentum and angular momentum of
890 < the system is shifted to zero after each resampling from the Maxwell
891 < -Boltzman distribution.
886 > end up setting the temperature of the system to a final temperature
887 > at which the simulation will be conducted. In heating phase, we
888 > should also keep the system from drifting or rotating as a whole. To
889 > do this, the net linear momentum and angular momentum of the system
890 > is shifted to zero after each resampling from the Maxwell -Boltzman
891 > distribution.
892  
893   \subsubsection{\textbf{Equilibration}}
894  
# Line 971 | Line 915 | which making large simulations prohibitive in the abse
915   calculation of non-bonded forces, such as van der Waals force and
916   Coulombic forces \textit{etc}. For a system of $N$ particles, the
917   complexity of the algorithm for pair-wise interactions is $O(N^2 )$,
918 < which making large simulations prohibitive in the absence of any
919 < algorithmic tricks.
920 <
921 < A natural approach to avoid system size issues is to represent the
922 < bulk behavior by a finite number of the particles. However, this
923 < approach will suffer from the surface effect at the edges of the
924 < simulation. To offset this, \textit{Periodic boundary conditions}
925 < (see Fig.~\ref{introFig:pbc}) is developed to simulate bulk
926 < properties with a relatively small number of particles. In this
927 < method, the simulation box is replicated throughout space to form an
928 < infinite lattice. During the simulation, when a particle moves in
929 < the primary cell, its image in other cells move in exactly the same
930 < 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.
918 > which makes large simulations prohibitive in the absence of any
919 > algorithmic tricks. A natural approach to avoid system size issues
920 > is to represent the bulk behavior by a finite number of the
921 > particles. However, this approach will suffer from surface effects
922 > at the edges of the simulation. To offset this, \textit{Periodic
923 > boundary conditions} (see Fig.~\ref{introFig:pbc}) were developed to
924 > simulate bulk properties with a relatively small number of
925 > particles. In this method, the simulation box is replicated
926 > throughout space to form an infinite lattice. During the simulation,
927 > when a particle moves in the primary cell, its image in other cells
928 > move in exactly the same direction with exactly the same
929 > orientation. Thus, as a particle leaves the primary cell, one of its
930 > images will enter through the opposite face.
931   \begin{figure}
932   \centering
933   \includegraphics[width=\linewidth]{pbc.eps}
# Line 997 | Line 939 | evaluation is to apply spherical cutoff where particle
939  
940   %cutoff and minimum image convention
941   Another important technique to improve the efficiency of force
942 < evaluation is to apply spherical cutoff where particles farther than
943 < a predetermined distance are not included in the calculation
942 > evaluation is to apply spherical cutoffs where particles farther
943 > than a predetermined distance are not included in the calculation
944   \cite{Frenkel1996}. The use of a cutoff radius will cause a
945   discontinuity in the potential energy curve. Fortunately, one can
946 < shift simple radial potential to ensure the potential curve go
946 > shift a simple radial potential to ensure the potential curve go
947   smoothly to zero at the cutoff radius. The cutoff strategy works
948   well for Lennard-Jones interaction because of its short range
949   nature. However, simply truncating the electrostatic interaction
# Line 1047 | Line 989 | trajectory analysis are more useful. According to the
989   Recently, advanced visualization technique have become applied to
990   monitor the motions of molecules. Although the dynamics of the
991   system can be described qualitatively from animation, quantitative
992 < trajectory analysis are more useful. According to the principles of
993 < Statistical Mechanics, Sec.~\ref{introSection:statisticalMechanics},
994 < one can compute thermodynamic properties, analyze fluctuations of
995 < structural parameters, and investigate time-dependent processes of
996 < the molecule from the trajectories.
992 > trajectory analysis is more useful. According to the principles of
993 > Statistical Mechanics in
994 > Sec.~\ref{introSection:statisticalMechanics}, one can compute
995 > thermodynamic properties, analyze fluctuations of structural
996 > parameters, and investigate time-dependent processes of the molecule
997 > from the trajectories.
998  
999   \subsubsection{\label{introSection:thermodynamicsProperties}\textbf{Thermodynamic Properties}}
1000  
# Line 1081 | Line 1024 | Experimentally, pair distribution function can be gath
1024   distribution functions. Among these functions,the \emph{pair
1025   distribution function}, also known as \emph{radial distribution
1026   function}, is of most fundamental importance to liquid theory.
1027 < Experimentally, pair distribution function can be gathered by
1027 > Experimentally, pair distribution functions can be gathered by
1028   Fourier transforming raw data from a series of neutron diffraction
1029   experiments and integrating over the surface factor
1030   \cite{Powles1973}. The experimental results can serve as a criterion
1031   to justify the correctness of a liquid model. Moreover, various
1032   equilibrium thermodynamic and structural properties can also be
1033 < expressed in terms of radial distribution function \cite{Allen1987}.
1034 <
1035 < The pair distribution functions $g(r)$ gives the probability that a
1036 < particle $i$ will be located at a distance $r$ from a another
1037 < particle $j$ in the system
1095 < \[
1033 > expressed in terms of the radial distribution function
1034 > \cite{Allen1987}. The pair distribution functions $g(r)$ gives the
1035 > probability that a particle $i$ will be located at a distance $r$
1036 > from a another particle $j$ in the system
1037 > \begin{equation}
1038   g(r) = \frac{V}{{N^2 }}\left\langle {\sum\limits_i {\sum\limits_{j
1039   \ne i} {\delta (r - r_{ij} )} } } \right\rangle = \frac{\rho
1040   (r)}{\rho}.
1041 < \]
1041 > \end{equation}
1042   Note that the delta function can be replaced by a histogram in
1043   computer simulation. Peaks in $g(r)$ represent solvent shells, and
1044   the height of these peaks gradually decreases to 1 as the liquid of
# Line 1123 | Line 1065 | function, which is averaging over time origins and ove
1065   \right\rangle } dt
1066   \]
1067   where $D$ is diffusion constant. Unlike the velocity autocorrelation
1068 < function, which is averaging over time origins and over all the
1069 < atoms, the dipole autocorrelation functions are calculated for the
1068 > function, which is averaged over time origins and over all the
1069 > atoms, the dipole autocorrelation functions is calculated for the
1070   entire system. The dipole autocorrelation function is given by:
1071   \[
1072   c_{dipole}  = \left\langle {u_{tot} (t) \cdot u_{tot} (t)}
# Line 1133 | Line 1075 | u_{tot} (t) = \sum\limits_i {u_i (t)}
1075   Here $u_{tot}$ is the net dipole of the entire system and is given
1076   by
1077   \[
1078 < u_{tot} (t) = \sum\limits_i {u_i (t)}
1078 > u_{tot} (t) = \sum\limits_i {u_i (t)}.
1079   \]
1080 < In principle, many time correlation functions can be related with
1080 > In principle, many time correlation functions can be related to
1081   Fourier transforms of the infrared, Raman, and inelastic neutron
1082   scattering spectra of molecular liquids. In practice, one can
1083 < extract the IR spectrum from the intensity of dipole fluctuation at
1084 < each frequency using the following relationship:
1083 > extract the IR spectrum from the intensity of the molecular dipole
1084 > fluctuation at each frequency using the following relationship:
1085   \[
1086   \hat c_{dipole} (v) = \int_{ - \infty }^\infty  {c_{dipole} (t)e^{ -
1087 < i2\pi vt} dt}
1087 > i2\pi vt} dt}.
1088   \]
1089  
1090   \section{\label{introSection:rigidBody}Dynamics of Rigid Bodies}
1091  
1092   Rigid bodies are frequently involved in the modeling of different
1093   areas, from engineering, physics, to chemistry. For example,
1094 < missiles and vehicle are usually modeled by rigid bodies.  The
1095 < movement of the objects in 3D gaming engine or other physics
1096 < simulator is governed by rigid body dynamics. In molecular
1094 > missiles and vehicles are usually modeled by rigid bodies.  The
1095 > movement of the objects in 3D gaming engines or other physics
1096 > simulators is governed by rigid body dynamics. In molecular
1097   simulations, rigid bodies are used to simplify protein-protein
1098   docking studies\cite{Gray2003}.
1099  
# Line 1160 | Line 1102 | equations of motion is very inefficient and inaccurate
1102   freedom. Euler angles are the natural choice to describe the
1103   rotational degrees of freedom. However, due to $\frac {1}{sin
1104   \theta}$ singularities, the numerical integration of corresponding
1105 < equations of motion is very inefficient and inaccurate. Although an
1106 < alternative integrator using multiple sets of Euler angles can
1107 < overcome this difficulty\cite{Barojas1973}, the computational
1108 < penalty and the loss of angular momentum conservation still remain.
1109 < A singularity-free representation utilizing quaternions was
1110 < developed by Evans in 1977\cite{Evans1977}. Unfortunately, this
1111 < approach uses a nonseparable Hamiltonian resulting from the
1112 < quaternion representation, which prevents the symplectic algorithm
1113 < to be utilized. Another different approach is to apply holonomic
1114 < constraints to the atoms belonging to the rigid body. Each atom
1115 < moves independently under the normal forces deriving from potential
1116 < energy and constraint forces which are used to guarantee the
1117 < rigidness. However, due to their iterative nature, the SHAKE and
1118 < Rattle algorithms also converge very slowly when the number of
1119 < constraints increases\cite{Ryckaert1977, Andersen1983}.
1105 > equations of these motion is very inefficient and inaccurate.
1106 > Although an alternative integrator using multiple sets of Euler
1107 > angles can overcome this difficulty\cite{Barojas1973}, the
1108 > computational penalty and the loss of angular momentum conservation
1109 > still remain. A singularity-free representation utilizing
1110 > quaternions was developed by Evans in 1977\cite{Evans1977}.
1111 > Unfortunately, this approach uses a nonseparable Hamiltonian
1112 > resulting from the quaternion representation, which prevents the
1113 > symplectic algorithm from being utilized. Another different approach
1114 > is to apply holonomic constraints to the atoms belonging to the
1115 > rigid body. Each atom moves independently under the normal forces
1116 > deriving from potential energy and constraint forces which are used
1117 > to guarantee the rigidness. However, due to their iterative nature,
1118 > the SHAKE and Rattle algorithms also converge very slowly when the
1119 > number of constraints increases\cite{Ryckaert1977, Andersen1983}.
1120  
1121   A break-through in geometric literature suggests that, in order to
1122   develop a long-term integration scheme, one should preserve the
1123 < symplectic structure of the flow. By introducing a conjugate
1123 > symplectic structure of the propagator. By introducing a conjugate
1124   momentum to the rotation matrix $Q$ and re-formulating Hamiltonian's
1125   equation, a symplectic integrator, RSHAKE\cite{Kol1997}, was
1126   proposed to evolve the Hamiltonian system in a constraint manifold
# Line 1186 | Line 1128 | symplectic Lie-Poisson integrator for rigid body devel
1128   An alternative method using the quaternion representation was
1129   developed by Omelyan\cite{Omelyan1998}. However, both of these
1130   methods are iterative and inefficient. In this section, we descibe a
1131 < symplectic Lie-Poisson integrator for rigid body developed by
1131 > symplectic Lie-Poisson integrator for rigid bodies developed by
1132   Dullweber and his coworkers\cite{Dullweber1997} in depth.
1133  
1134   \subsection{\label{introSection:constrainedHamiltonianRB}Constrained Hamiltonian for Rigid Bodies}
# Line 1197 | Line 1139 | Here, $q$ and $Q$  are the position and rotation matri
1139   V(q,Q) + \frac{1}{2}tr[(QQ^T  - 1)\Lambda ].
1140   \label{introEquation:RBHamiltonian}
1141   \end{equation}
1142 < Here, $q$ and $Q$  are the position and rotation matrix for the
1143 < rigid-body, $p$ and $P$  are conjugate momenta to $q$  and $Q$ , and
1144 < $J$, a diagonal matrix, is defined by
1142 > Here, $q$ and $Q$  are the position vector and rotation matrix for
1143 > the rigid-body, $p$ and $P$  are conjugate momenta to $q$  and $Q$ ,
1144 > and $J$, a diagonal matrix, is defined by
1145   \[
1146   I_{ii}^{ - 1}  = \frac{1}{2}\sum\limits_{i \ne j} {J_{jj}^{ - 1} }
1147   \]
# Line 1209 | Line 1151 | which is used to ensure rotation matrix's unitarity. D
1151   \begin{equation}
1152   Q^T Q = 1, \label{introEquation:orthogonalConstraint}
1153   \end{equation}
1154 < which is used to ensure rotation matrix's unitarity. Differentiating
1155 < \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}
1218 < \end{equation}
1219 <
1220 < Using Equation (\ref{introEquation:motionHamiltonianCoordinate},
1154 > which is used to ensure the rotation matrix's unitarity. Using
1155 > Equation (\ref{introEquation:motionHamiltonianCoordinate},
1156   \ref{introEquation:motionHamiltonianMomentum}), one can write down
1157   the equations of motion,
1223
1158   \begin{eqnarray}
1159 < \frac{{dq}}{{dt}} & = & \frac{p}{m} \label{introEquation:RBMotionPosition}\\
1160 < \frac{{dp}}{{dt}} & = & - \nabla _q V(q,Q) \label{introEquation:RBMotionMomentum}\\
1161 < \frac{{dQ}}{{dt}} & = & PJ^{ - 1}  \label{introEquation:RBMotionRotation}\\
1159 > \frac{{dq}}{{dt}} & = & \frac{p}{m}, \label{introEquation:RBMotionPosition}\\
1160 > \frac{{dp}}{{dt}} & = & - \nabla _q V(q,Q), \label{introEquation:RBMotionMomentum}\\
1161 > \frac{{dQ}}{{dt}} & = & PJ^{ - 1},  \label{introEquation:RBMotionRotation}\\
1162   \frac{{dP}}{{dt}} & = & - \nabla _Q V(q,Q) - 2Q\Lambda . \label{introEquation:RBMotionP}
1163   \end{eqnarray}
1164 <
1164 > Differentiating Eq.~\ref{introEquation:orthogonalConstraint} and
1165 > using Eq.~\ref{introEquation:RBMotionMomentum}, one may obtain,
1166 > \begin{equation}
1167 > Q^T PJ^{ - 1}  + J^{ - 1} P^T Q = 0 . \\
1168 > \label{introEquation:RBFirstOrderConstraint}
1169 > \end{equation}
1170   In general, there are two ways to satisfy the holonomic constraints.
1171   We can use a constraint force provided by a Lagrange multiplier on
1172 < the normal manifold to keep the motion on constraint space. Or we
1173 < can simply evolve the system on the constraint manifold. These two
1174 < methods have been proved to be equivalent. The holonomic constraint
1175 < and equations of motions define a constraint manifold for rigid
1176 < bodies
1172 > the normal manifold to keep the motion on the constraint space. Or
1173 > we can simply evolve the system on the constraint manifold. These
1174 > two methods have been proved to be equivalent. The holonomic
1175 > constraint and equations of motions define a constraint manifold for
1176 > rigid bodies
1177   \[
1178   M = \left\{ {(Q,P):Q^T Q = 1,Q^T PJ^{ - 1}  + J^{ - 1} P^T Q = 0}
1179   \right\}.
1180   \]
1181 <
1182 < Unfortunately, this constraint manifold is not the cotangent bundle
1183 < $T^* SO(3)$ which can be consider as a symplectic manifold on Lie
1184 < rotation group $SO(3)$. However, it turns out that under symplectic
1246 < transformation, the cotangent space and the phase space are
1247 < diffeomorphic. By introducing
1181 > Unfortunately, this constraint manifold is not $T^* SO(3)$ which is
1182 > a symplectic manifold on Lie rotation group $SO(3)$. However, it
1183 > turns out that under symplectic transformation, the cotangent space
1184 > and the phase space are diffeomorphic. By introducing
1185   \[
1186   \tilde Q = Q,\tilde P = \frac{1}{2}\left( {P - QP^T Q} \right),
1187   \]
# Line 1254 | Line 1191 | T^* SO(3) = \left\{ {(\tilde Q,\tilde P):\tilde Q^T \t
1191   T^* SO(3) = \left\{ {(\tilde Q,\tilde P):\tilde Q^T \tilde Q =
1192   1,\tilde Q^T \tilde PJ^{ - 1}  + J^{ - 1} P^T \tilde Q = 0} \right\}
1193   \]
1257
1194   For a body fixed vector $X_i$ with respect to the center of mass of
1195   the rigid body, its corresponding lab fixed vector $X_0^{lab}$  is
1196   given as
# Line 1273 | Line 1209 | respectively.
1209   \[
1210   \nabla _Q V(q,Q) = F(q,Q)X_i^t
1211   \]
1212 < respectively.
1213 <
1214 < As a common choice to describe the rotation dynamics of the rigid
1279 < body, the angular momentum on the body fixed frame $\Pi  = Q^t P$ is
1280 < introduced to rewrite the equations of motion,
1212 > respectively. As a common choice to describe the rotation dynamics
1213 > of the rigid body, the angular momentum on the body fixed frame $\Pi
1214 > = Q^t P$ is introduced to rewrite the equations of motion,
1215   \begin{equation}
1216   \begin{array}{l}
1217 < \dot \Pi  = J^{ - 1} \Pi ^T \Pi  + Q^T \sum\limits_i {F_i (q,Q)X_i^T }  - \Lambda  \\
1218 < \dot Q  = Q\Pi {\rm{ }}J^{ - 1}  \\
1217 > \dot \Pi  = J^{ - 1} \Pi ^T \Pi  + Q^T \sum\limits_i {F_i (q,Q)X_i^T }  - \Lambda,  \\
1218 > \dot Q  = Q\Pi {\rm{ }}J^{ - 1},  \\
1219   \end{array}
1220   \label{introEqaution:RBMotionPI}
1221   \end{equation}
1222 < , as well as holonomic constraints,
1223 < \[
1224 < \begin{array}{l}
1291 < \Pi J^{ - 1}  + J^{ - 1} \Pi ^t  = 0 \\
1292 < Q^T Q = 1 \\
1293 < \end{array}
1294 < \]
1295 <
1296 < For a vector $v(v_1 ,v_2 ,v_3 ) \in R^3$ and a matrix $\hat v \in
1297 < so(3)^ \star$, the hat-map isomorphism,
1222 > as well as holonomic constraints $\Pi J^{ - 1}  + J^{ - 1} \Pi ^t  =
1223 > 0$ and $Q^T Q = 1$. For a vector $v(v_1 ,v_2 ,v_3 ) \in R^3$ and a
1224 > matrix $\hat v \in so(3)^ \star$, the hat-map isomorphism,
1225   \begin{equation}
1226   v(v_1 ,v_2 ,v_3 ) \Leftrightarrow \hat v = \left(
1227   {\begin{array}{*{20}c}
# Line 1307 | Line 1234 | operations
1234   will let us associate the matrix products with traditional vector
1235   operations
1236   \[
1237 < \hat vu = v \times u
1237 > \hat vu = v \times u.
1238   \]
1239 < Using \ref{introEqaution:RBMotionPI}, one can construct a skew
1239 > Using Eq.~\ref{introEqaution:RBMotionPI}, one can construct a skew
1240   matrix,
1241 <
1242 < \begin{eqnarray*}
1243 < (\dot \Pi  - \dot \Pi ^T ){\rm{ }} = {\rm{ }}(\Pi  - \Pi ^T ){\rm{
1244 < }}(J^{ - 1} \Pi  + \Pi J^{ - 1} ) + \sum\limits_i {[Q^T F_i
1245 < (r,Q)X_i^T  - X_i F_i (r,Q)^T Q]}  - (\Lambda  - \Lambda ^T ).
1246 < \label{introEquation:skewMatrixPI}
1247 < \end{eqnarray*}
1248 <
1249 < Since $\Lambda$ is symmetric, the last term of Equation
1250 < \ref{introEquation:skewMatrixPI} is zero, which implies the Lagrange
1251 < multiplier $\Lambda$ is absent from the equations of motion. This
1252 < unique property eliminates the requirement of iterations which can
1326 < not be avoided in other methods\cite{Kol1997, Omelyan1998}.
1327 <
1328 < Applying the hat-map isomorphism, we obtain the equation of motion
1329 < for angular momentum on body frame
1241 > \begin{eqnarray}
1242 > (\dot \Pi  - \dot \Pi ^T )&= &(\Pi  - \Pi ^T )(J^{ - 1} \Pi  + \Pi J^{ - 1} ) \notag \\
1243 > & & + \sum\limits_i {[Q^T F_i (r,Q)X_i^T  - X_i F_i (r,Q)^T Q]}  -
1244 > (\Lambda  - \Lambda ^T ). \label{introEquation:skewMatrixPI}
1245 > \end{eqnarray}
1246 > Since $\Lambda$ is symmetric, the last term of
1247 > Eq.~\ref{introEquation:skewMatrixPI} is zero, which implies the
1248 > Lagrange multiplier $\Lambda$ is absent from the equations of
1249 > motion. This unique property eliminates the requirement of
1250 > iterations which can not be avoided in other methods\cite{Kol1997,
1251 > Omelyan1998}. Applying the hat-map isomorphism, we obtain the
1252 > equation of motion for angular momentum in the body frame
1253   \begin{equation}
1254   \dot \pi  = \pi  \times I^{ - 1} \pi  + \sum\limits_i {\left( {Q^T
1255   F_i (r,Q)} \right) \times X_i }.
# Line 1335 | Line 1258 | given by
1258   In the same manner, the equation of motion for rotation matrix is
1259   given by
1260   \[
1261 < \dot Q = Qskew(I^{ - 1} \pi )
1261 > \dot Q = Qskew(I^{ - 1} \pi ).
1262   \]
1263  
1264   \subsection{\label{introSection:SymplecticFreeRB}Symplectic
1265 < Lie-Poisson Integrator for Free Rigid Body}
1265 > Lie-Poisson Integrator for Free Rigid Bodies}
1266  
1267   If there are no external forces exerted on the rigid body, the only
1268   contribution to the rotational motion is from the kinetic energy
# Line 1357 | Line 1280 | J(\pi ) = \left( {\begin{array}{*{20}c}
1280     0 & {\pi _3 } & { - \pi _2 }  \\
1281     { - \pi _3 } & 0 & {\pi _1 }  \\
1282     {\pi _2 } & { - \pi _1 } & 0  \\
1283 < \end{array}} \right)
1283 > \end{array}} \right).
1284   \end{equation}
1285   Thus, the dynamics of free rigid body is governed by
1286   \begin{equation}
1287 < \frac{d}{{dt}}\pi  = J(\pi )\nabla _\pi  T^r (\pi )
1287 > \frac{d}{{dt}}\pi  = J(\pi )\nabla _\pi  T^r (\pi ).
1288   \end{equation}
1289 <
1290 < One may notice that each $T_i^r$ in Equation
1291 < \ref{introEquation:rotationalKineticRB} can be solved exactly. For
1369 < instance, the equations of motion due to $T_1^r$ are given by
1289 > One may notice that each $T_i^r$ in
1290 > Eq.~\ref{introEquation:rotationalKineticRB} can be solved exactly.
1291 > For instance, the equations of motion due to $T_1^r$ are given by
1292   \begin{equation}
1293   \frac{d}{{dt}}\pi  = R_1 \pi ,\frac{d}{{dt}}Q = QR_1
1294   \label{introEqaution:RBMotionSingleTerm}
1295   \end{equation}
1296 < where
1296 > with
1297   \[ R_1  = \left( {\begin{array}{*{20}c}
1298     0 & 0 & 0  \\
1299     0 & 0 & {\pi _1 }  \\
1300     0 & { - \pi _1 } & 0  \\
1301   \end{array}} \right).
1302   \]
1303 < The solutions of Equation \ref{introEqaution:RBMotionSingleTerm} is
1303 > The solutions of Eq.~\ref{introEqaution:RBMotionSingleTerm} is
1304   \[
1305   \pi (\Delta t) = e^{\Delta tR_1 } \pi (0),Q(\Delta t) =
1306   Q(0)e^{\Delta tR_1 }
# Line 1392 | Line 1314 | tR_1 }$, we can use Cayley transformation to obtain a
1314   \end{array}} \right),\theta _1  = \frac{{\pi _1 }}{{I_1 }}\Delta t.
1315   \]
1316   To reduce the cost of computing expensive functions in $e^{\Delta
1317 < tR_1 }$, we can use Cayley transformation to obtain a single-aixs
1318 < propagator,
1319 < \[
1320 < e^{\Delta tR_1 }  \approx (1 - \Delta tR_1 )^{ - 1} (1 + \Delta tR_1
1321 < )
1322 < \]
1323 < The flow maps for $T_2^r$ and $T_3^r$ can be found in the same
1317 > tR_1 }$, we can use the Cayley transformation to obtain a
1318 > single-aixs propagator,
1319 > \begin{eqnarray*}
1320 > e^{\Delta tR_1 }  & \approx & (1 - \Delta tR_1 )^{ - 1} (1 + \Delta
1321 > tR_1 ) \\
1322 > %
1323 > & \approx & \left( \begin{array}{ccc}
1324 > 1 & 0 & 0 \\
1325 > 0 & \frac{1-\theta^2 / 4}{1 + \theta^2 / 4}  & -\frac{\theta}{1+
1326 > \theta^2 / 4} \\
1327 > 0 & \frac{\theta}{1+ \theta^2 / 4} & \frac{1-\theta^2 / 4}{1 +
1328 > \theta^2 / 4}
1329 > \end{array}
1330 > \right).
1331 > \end{eqnarray*}
1332 > The propagators for $T_2^r$ and $T_3^r$ can be found in the same
1333   manner. In order to construct a second-order symplectic method, we
1334 < split the angular kinetic Hamiltonian function can into five terms
1334 > split the angular kinetic Hamiltonian function into five terms
1335   \[
1336   T^r (\pi ) = \frac{1}{2}T_1 ^r (\pi _1 ) + \frac{1}{2}T_2^r (\pi _2
1337   ) + T_3^r (\pi _3 ) + \frac{1}{2}T_2^r (\pi _2 ) + \frac{1}{2}T_1 ^r
# Line 1414 | Line 1345 | _1 }.
1345   \circ \varphi _{\Delta t/2,\pi _2 }  \circ \varphi _{\Delta t/2,\pi
1346   _1 }.
1347   \]
1417
1348   The non-canonical Lie-Poisson bracket ${F, G}$ of two function
1349   $F(\pi )$ and $G(\pi )$ is defined by
1350   \[
1351   \{ F,G\} (\pi ) = [\nabla _\pi  F(\pi )]^T J(\pi )\nabla _\pi  G(\pi
1352 < )
1352 > ).
1353   \]
1354   If the Poisson bracket of a function $F$ with an arbitrary smooth
1355   function $G$ is zero, $F$ is a \emph{Casimir}, which is the
1356   conserved quantity in Poisson system. We can easily verify that the
1357   norm of the angular momentum, $\parallel \pi
1358 < \parallel$, is a \emph{Casimir}. Let$ F(\pi ) = S(\frac{{\parallel
1358 > \parallel$, is a \emph{Casimir}\cite{McLachlan1993}. Let$ F(\pi ) = S(\frac{{\parallel
1359   \pi \parallel ^2 }}{2})$ for an arbitrary function $ S:R \to R$ ,
1360   then by the chain rule
1361   \[
1362   \nabla _\pi  F(\pi ) = S'(\frac{{\parallel \pi \parallel ^2
1363 < }}{2})\pi
1363 > }}{2})\pi.
1364   \]
1365 < Thus $ [\nabla _\pi  F(\pi )]^T J(\pi ) =  - S'(\frac{{\parallel \pi
1365 > Thus, $ [\nabla _\pi  F(\pi )]^T J(\pi ) =  - S'(\frac{{\parallel
1366 > \pi
1367   \parallel ^2 }}{2})\pi  \times \pi  = 0 $. This explicit
1368   Lie-Poisson integrator is found to be both extremely efficient and
1369   stable. These properties can be explained by the fact the small
# Line 1443 | Line 1374 | energy and potential energy,
1374   Splitting for Rigid Body}
1375  
1376   The Hamiltonian of rigid body can be separated in terms of kinetic
1377 < energy and potential energy,
1378 < \[
1379 < H = T(p,\pi ) + V(q,Q)
1449 < \]
1450 < The equations of motion corresponding to potential energy and
1451 < kinetic energy are listed in the below table,
1377 > energy and potential energy,$H = T(p,\pi ) + V(q,Q)$. The equations
1378 > of motion corresponding to potential energy and kinetic energy are
1379 > listed in the below table,
1380   \begin{table}
1381   \caption{EQUATIONS OF MOTION DUE TO POTENTIAL AND KINETIC ENERGIES}
1382   \begin{center}
# Line 1486 | Line 1414 | defined by \ref{introEquation:rotationalKineticRB}. Th
1414   T(p,\pi ) =T^t (p) + T^r (\pi ).
1415   \end{equation}
1416   where $ T^t (p) = \frac{1}{2}p^T m^{ - 1} p $ and $T^r (\pi )$ is
1417 < defined by \ref{introEquation:rotationalKineticRB}. Therefore, the
1418 < corresponding propagators are given by
1417 > defined by Eq.~\ref{introEquation:rotationalKineticRB}. Therefore,
1418 > the corresponding propagators are given by
1419   \[
1420   \varphi _{\Delta t,T}  = \varphi _{\Delta t,T^t }  \circ \varphi
1421   _{\Delta t,T^r }.
1422   \]
1423   Finally, we obtain the overall symplectic propagators for freely
1424   moving rigid bodies
1425 < \begin{equation}
1426 < \begin{array}{c}
1427 < \varphi _{\Delta t}  = \varphi _{\Delta t/2,F}  \circ \varphi _{\Delta t/2,\tau }  \\
1428 <  \circ \varphi _{\Delta t,T^t }  \circ \varphi _{\Delta t/2,\pi _1 }  \circ \varphi _{\Delta t/2,\pi _2 }  \circ \varphi _{\Delta t,\pi _3 }  \circ \varphi _{\Delta t/2,\pi _2 }  \circ \varphi _{\Delta t/2,\pi _1 }  \\
1501 <  \circ \varphi _{\Delta t/2,\tau }  \circ \varphi _{\Delta t/2,F}  .\\
1502 < \end{array}
1425 > \begin{eqnarray}
1426 > \varphi _{\Delta t}  &=& \varphi _{\Delta t/2,F}  \circ \varphi _{\Delta t/2,\tau }  \notag\\
1427 >  & & \circ \varphi _{\Delta t,T^t }  \circ \varphi _{\Delta t/2,\pi _1 }  \circ \varphi _{\Delta t/2,\pi _2 }  \circ \varphi _{\Delta t,\pi _3 }  \circ \varphi _{\Delta t/2,\pi _2 }  \circ \varphi _{\Delta t/2,\pi _1 }  \notag\\
1428 >  & & \circ \varphi _{\Delta t/2,\tau }  \circ \varphi _{\Delta t/2,F}  .
1429   \label{introEquation:overallRBFlowMaps}
1430 < \end{equation}
1430 > \end{eqnarray}
1431  
1432   \section{\label{introSection:langevinDynamics}Langevin Dynamics}
1433   As an alternative to newtonian dynamics, Langevin dynamics, which
# Line 1547 | Line 1473 | W(x) = U(x) - \sum\limits_{\alpha  = 1}^N {\frac{{g_\a
1473   \[
1474   W(x) = U(x) - \sum\limits_{\alpha  = 1}^N {\frac{{g_\alpha ^2
1475   }}{{2m_\alpha  w_\alpha ^2 }}} x^2
1476 < \] and combining the last two terms in Equation
1477 < \ref{introEquation:bathGLE}, we may rewrite the Harmonic bath
1552 < Hamiltonian as
1476 > \]
1477 > and combining the last two terms in Eq.~\ref{introEquation:bathGLE}, we may rewrite the Harmonic bath Hamiltonian as
1478   \[
1479   H = \frac{{p^2 }}{{2m}} + W(x) + \sum\limits_{\alpha  = 1}^N
1480   {\left\{ {\frac{{p_\alpha ^2 }}{{2m_\alpha  }} + \frac{1}{2}m_\alpha
1481   w_\alpha ^2 \left( {x_\alpha   - \frac{{g_\alpha  }}{{m_\alpha
1482 < w_\alpha ^2 }}x} \right)^2 } \right\}}
1482 > w_\alpha ^2 }}x} \right)^2 } \right\}}.
1483   \]
1484   Since the first two terms of the new Hamiltonian depend only on the
1485   system coordinates, we can get the equations of motion for
# Line 1571 | Line 1496 | m\ddot x_\alpha   =  - m_\alpha  w_\alpha ^2 \left( {x
1496   \frac{{g_\alpha  }}{{m_\alpha  w_\alpha ^2 }}x} \right).
1497   \label{introEquation:bathMotionGLE}
1498   \end{equation}
1574
1499   In order to derive an equation for $x$, the dynamics of the bath
1500   variables $x_\alpha$ must be solved exactly first. As an integral
1501   transform which is particularly useful in solving linear ordinary
1502   differential equations,the Laplace transform is the appropriate tool
1503   to solve this problem. The basic idea is to transform the difficult
1504   differential equations into simple algebra problems which can be
1505 < solved easily. Then, by applying the inverse Laplace transform, also
1506 < known as the Bromwich integral, we can retrieve the solutions of the
1507 < original problems.
1508 <
1585 < Let $f(t)$ be a function defined on $ [0,\infty ) $. The Laplace
1586 < transform of f(t) is a new function defined as
1505 > solved easily. Then, by applying the inverse Laplace transform, we
1506 > can retrieve the solutions of the original problems. Let $f(t)$ be a
1507 > function defined on $ [0,\infty ) $, the Laplace transform of $f(t)$
1508 > is a new function defined as
1509   \[
1510   L(f(t)) \equiv F(p) = \int_0^\infty  {f(t)e^{ - pt} dt}
1511   \]
1512   where  $p$ is real and  $L$ is called the Laplace Transform
1513   Operator. Below are some important properties of Laplace transform
1592
1514   \begin{eqnarray*}
1515   L(x + y)  & = & L(x) + L(y) \\
1516   L(ax)     & = & aL(x) \\
# Line 1597 | Line 1518 | Operator. Below are some important properties of Lapla
1518   L(\ddot x)& = & p^2 L(x) - px(0) - \dot x(0) \\
1519   L\left( {\int_0^t {g(t - \tau )h(\tau )d\tau } } \right)& = & G(p)H(p) \\
1520   \end{eqnarray*}
1600
1601
1521   Applying the Laplace transform to the bath coordinates, we obtain
1522   \begin{eqnarray*}
1523 < 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) \\
1524 < L(x_\alpha  ) & = & \frac{{\frac{{g_\alpha  }}{{\omega _\alpha  }}L(x) + px_\alpha  (0) + \dot x_\alpha  (0)}}{{p^2  + \omega _\alpha ^2 }} \\
1523 > 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), \\
1524 > L(x_\alpha  ) & = & \frac{{\frac{{g_\alpha  }}{{\omega _\alpha  }}L(x) + px_\alpha  (0) + \dot x_\alpha  (0)}}{{p^2  + \omega _\alpha ^2 }}. \\
1525   \end{eqnarray*}
1526 <
1608 < By the same way, the system coordinates become
1526 > In the same way, the system coordinates become
1527   \begin{eqnarray*}
1528 < mL(\ddot x) & = & - \frac{1}{p}\frac{{\partial W(x)}}{{\partial x}} \\
1529 <  & & \mbox{} - \sum\limits_{\alpha  = 1}^N {\left\{ { - \frac{{g_\alpha ^2 }}{{m_\alpha  \omega _\alpha ^2 }}\frac{p}{{p^2  + \omega _\alpha ^2 }}pL(x) - \frac{p}{{p^2  + \omega _\alpha ^2 }}g_\alpha  x_\alpha  (0) - \frac{1}{{p^2  + \omega _\alpha ^2 }}g_\alpha  \dot x_\alpha  (0)} \right\}}  \\
1528 > mL(\ddot x) & = &
1529 >  - \sum\limits_{\alpha  = 1}^N {\left\{ { - \frac{{g_\alpha ^2 }}{{m_\alpha  \omega _\alpha ^2 }}\frac{p}{{p^2  + \omega _\alpha ^2 }}pL(x) - \frac{p}{{p^2  + \omega _\alpha ^2 }}g_\alpha  x_\alpha  (0) - \frac{1}{{p^2  + \omega _\alpha ^2 }}g_\alpha  \dot x_\alpha  (0)} \right\}}  \\
1530 >  & & - \frac{1}{p}\frac{{\partial W(x)}}{{\partial x}}.
1531   \end{eqnarray*}
1613
1532   With the help of some relatively important inverse Laplace
1533   transformations:
1534   \[
# Line 1620 | Line 1538 | transformations:
1538   L(1) = \frac{1}{p} \\
1539   \end{array}
1540   \]
1541 < , we obtain
1541 > we obtain
1542   \begin{eqnarray*}
1543   m\ddot x & =  & - \frac{{\partial W(x)}}{{\partial x}} -
1544   \sum\limits_{\alpha  = 1}^N {\left\{ {\left( { - \frac{{g_\alpha ^2
# Line 1629 | Line 1547 | x_\alpha (0) - \frac{{g_\alpha  }}{{m_\alpha  \omega _
1547   & & + \sum\limits_{\alpha  = 1}^N {\left\{ {\left[ {g_\alpha
1548   x_\alpha (0) - \frac{{g_\alpha  }}{{m_\alpha  \omega _\alpha  }}}
1549   \right]\cos (\omega _\alpha  t) + \frac{{g_\alpha  \dot x_\alpha
1550 < (0)}}{{\omega _\alpha  }}\sin (\omega _\alpha  t)} \right\}}
1551 < \end{eqnarray*}
1552 < \begin{eqnarray*}
1553 < m\ddot x & = & - \frac{{\partial W(x)}}{{\partial x}} - \int_0^t
1554 < {\sum\limits_{\alpha  = 1}^N {\left( { - \frac{{g_\alpha ^2
1555 < }}{{m_\alpha  \omega _\alpha ^2 }}} \right)\cos (\omega _\alpha
1550 > (0)}}{{\omega _\alpha  }}\sin (\omega _\alpha  t)} \right\}}\\
1551 > %
1552 > & = & -
1553 > \frac{{\partial W(x)}}{{\partial x}} - \int_0^t {\sum\limits_{\alpha
1554 > = 1}^N {\left( { - \frac{{g_\alpha ^2 }}{{m_\alpha  \omega _\alpha
1555 > ^2 }}} \right)\cos (\omega _\alpha
1556   t)\dot x(t - \tau )d} \tau }  \\
1557   & & + \sum\limits_{\alpha  = 1}^N {\left\{ {\left[ {g_\alpha
1558   x_\alpha (0) - \frac{{g_\alpha }}{{m_\alpha \omega _\alpha  }}}
# Line 1668 | Line 1586 | uncorrelated to $x$ and $\dot x$,
1586   One may notice that $R(t)$ depends only on initial conditions, which
1587   implies it is completely deterministic within the context of a
1588   harmonic bath. However, it is easy to verify that $R(t)$ is totally
1589 < uncorrelated to $x$ and $\dot x$,
1590 < \[
1591 < \begin{array}{l}
1592 < \left\langle {x(t)R(t)} \right\rangle  = 0, \\
1675 < \left\langle {\dot x(t)R(t)} \right\rangle  = 0. \\
1676 < \end{array}
1677 < \]
1678 < This property is what we expect from a truly random process. As long
1679 < as the model chosen for $R(t)$ was a gaussian distribution in
1589 > uncorrelated to $x$ and $\dot x$,$\left\langle {x(t)R(t)}
1590 > \right\rangle  = 0, \left\langle {\dot x(t)R(t)} \right\rangle  =
1591 > 0.$ This property is what we expect from a truly random process. As
1592 > long as the model chosen for $R(t)$ was a gaussian distribution in
1593   general, the stochastic nature of the GLE still remains.
1681
1594   %dynamic friction kernel
1595   The convolution integral
1596   \[
# Line 1693 | Line 1605 | and Equation \ref{introEuqation:GeneralizedLangevinDyn
1605   \[
1606   \int_0^t {\xi (t)\dot x(t - \tau )d\tau }  = \xi _0 (x(t) - x(0))
1607   \]
1608 < and Equation \ref{introEuqation:GeneralizedLangevinDynamics} becomes
1608 > and Eq.~\ref{introEuqation:GeneralizedLangevinDynamics} becomes
1609   \[
1610   m\ddot x =  - \frac{\partial }{{\partial x}}\left( {W(x) +
1611   \frac{1}{2}\xi _0 (x - x_0 )^2 } \right) + R(t),
# Line 1710 | Line 1622 | and Equation \ref{introEuqation:GeneralizedLangevinDyn
1622   \int_0^t {\xi (t)\dot x(t - \tau )d\tau }  = 2\xi _0 \int_0^t
1623   {\delta (t)\dot x(t - \tau )d\tau }  = \xi _0 \dot x(t),
1624   \]
1625 < and Equation \ref{introEuqation:GeneralizedLangevinDynamics} becomes
1625 > and Eq.~\ref{introEuqation:GeneralizedLangevinDynamics} becomes
1626   \begin{equation}
1627   m\ddot x =  - \frac{{\partial W(x)}}{{\partial x}} - \xi _0 \dot
1628   x(t) + R(t) \label{introEquation:LangevinEquation}
# Line 1718 | Line 1630 | briefly review on calculating friction tensor for arbi
1630   which is known as the Langevin equation. The static friction
1631   coefficient $\xi _0$ can either be calculated from spectral density
1632   or be determined by Stokes' law for regular shaped particles. A
1633 < briefly review on calculating friction tensor for arbitrary shaped
1633 > brief review on calculating friction tensors for arbitrary shaped
1634   particles is given in Sec.~\ref{introSection:frictionTensor}.
1635  
1636   \subsubsection{\label{introSection:secondFluctuationDissipation}\textbf{The Second Fluctuation Dissipation Theorem}}
1637  
1638 < Defining a new set of coordinates,
1638 > Defining a new set of coordinates
1639   \[
1640   q_\alpha  (t) = x_\alpha  (t) - \frac{1}{{m_\alpha  \omega _\alpha
1641 < ^2 }}x(0)
1642 < \],
1641 > ^2 }}x(0),
1642 > \]
1643   we can rewrite $R(T)$ as
1644   \[
1645   R(t) = \sum\limits_{\alpha  = 1}^N {g_\alpha  q_\alpha  (t)}.
1646   \]
1647   And since the $q$ coordinates are harmonic oscillators,
1736
1648   \begin{eqnarray*}
1649   \left\langle {q_\alpha ^2 } \right\rangle  & = & \frac{{kT}}{{m_\alpha  \omega _\alpha ^2 }} \\
1650   \left\langle {q_\alpha  (t)q_\alpha  (0)} \right\rangle & = & \left\langle {q_\alpha ^2 (0)} \right\rangle \cos (\omega _\alpha  t) \\
1651   \left\langle {q_\alpha  (t)q_\beta  (0)} \right\rangle & = &\delta _{\alpha \beta } \left\langle {q_\alpha  (t)q_\alpha  (0)} \right\rangle  \\
1652   \left\langle {R(t)R(0)} \right\rangle & = & \sum\limits_\alpha  {\sum\limits_\beta  {g_\alpha  g_\beta  \left\langle {q_\alpha  (t)q_\beta  (0)} \right\rangle } }  \\
1653    & = &\sum\limits_\alpha  {g_\alpha ^2 \left\langle {q_\alpha ^2 (0)} \right\rangle \cos (\omega _\alpha  t)}  \\
1654 <  & = &kT\xi (t) \\
1654 >  & = &kT\xi (t)
1655   \end{eqnarray*}
1745
1656   Thus, we recover the \emph{second fluctuation dissipation theorem}
1657   \begin{equation}
1658   \xi (t) = \left\langle {R(t)R(0)} \right\rangle
1659 < \label{introEquation:secondFluctuationDissipation}.
1659 > \label{introEquation:secondFluctuationDissipation},
1660   \end{equation}
1661 < In effect, it acts as a constraint on the possible ways in which one
1662 < can model the random force and friction kernel.
1661 > which acts as a constraint on the possible ways in which one can
1662 > model the random force and friction kernel.

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