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# Line 3 | Line 3 | Mechanics}
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 | Newton's third law states that
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 | momentum of it is conserved. The last conservation the
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
71 > bodies.\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 < become 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 | where $ \dot q_1  \ldots \dot q_f $ are generalized ve
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}.
181 > known as the canonical equations of motions.\cite{Goldstein2001}
182  
183   An important difference between Lagrangian approach and the
184   Hamiltonian approach is that the Lagrangian is considered to be a
# Line 194 | Line 188 | coordinate and its time derivative as independent vari
188   Hamiltonian Mechanics is more appropriate for application to
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 <
191 > only works with 1st-order differential equations.\cite{Marion1990}
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 215 | Line 208 | The following section will give a brief introduction t
208   The thermodynamic behaviors and properties of Molecular Dynamics
209   simulation are governed by the principle of Statistical Mechanics.
210   The following section will give a brief introduction to some of the
211 < Statistical Mechanics concepts and theorem presented in this
211 > Statistical Mechanics concepts and theorems presented in this
212   dissertation.
213  
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, $x = (q_1 , \ldots
224 < ,q_f ,p_1 , \ldots ,p_f )$, with a unique set of values of $6f$
225 < coordinates and momenta is a phase space vector.
226 <
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 < A microscopic state or microstate of a classical system is
236 < specification of the complete phase space vector of a system at any
237 < instant in time. An ensemble is defined as a collection of systems
238 < sharing one or more macroscopic characteristics but each being in a
239 < unique microstate. The complete ensemble is specified by giving all
240 < systems or microstates consistent with the common macroscopic
241 < characteristics of the ensemble. Although the state of each
242 < individual system in the ensemble could be precisely described at
243 < any instance in time by a suitable phase space vector, when using
244 < ensembles for statistical purposes, there is no need to maintain
245 < distinctions between individual systems, since the numbers of
246 < systems at any time in the different states which correspond to
247 < different regions of the phase space are more interesting. Moreover,
248 < in the point of view of statistical mechanics, one would prefer to
249 < use ensembles containing a large enough population of separate
250 < members so that the numbers of systems in such different states can
251 < be regarded as changing continuously as we traverse different
252 < regions of the phase space. The condition of an ensemble at any time
235 >
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 distribution for an ensemble with $f$ degrees of
# Line 259 | Line 243 | Governed by the principles of mechanics, the phase poi
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 <
266 < 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 276 | Line 259 | N = \int { \ldots \int {\rho (q,p,t)dq_1 } ...dq_f dp_
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 286 | Line 269 | value of any desired quantity which depends on the coo
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  
303 There are several different types of ensembles with different
304 statistical characteristics. As a function of macroscopic
305 parameters, such as temperature \textit{etc}, the partition function
306 can be used to describe the statistical properties of a system in
307 thermodynamic equilibrium.
308
309 As an ensemble of systems, each of which is known to be thermally
310 isolated and conserve energy, the Microcanonical ensemble (NVE) has
311 a partition function like,
312 \begin{equation}
313 \Omega (N,V,E) = e^{\beta TS} \label{introEquation:NVEPartition}.
314 \end{equation}
315 A canonical ensemble (NVT)is an ensemble of systems, each of which
316 can share its energy with a large heat reservoir. The distribution
317 of the total energy amongst the possible dynamical states is given
318 by the partition function,
319 \begin{equation}
320 \Omega (N,V,T) = e^{ - \beta A}
321 \label{introEquation:NVTPartition}
322 \end{equation}
323 Here, $A$ is the Helmholtz free energy which is defined as $ A = U -
324 TS$. Since most experiments are carried out under constant pressure
325 condition, the isothermal-isobaric ensemble (NPT) plays a very
326 important role in molecular simulations. The isothermal-isobaric
327 ensemble allow the system to exchange energy with a heat bath of
328 temperature $T$ and to change the volume as well. Its partition
329 function is given as
330 \begin{equation}
331 \Delta (N,P,T) =  - e^{\beta G}.
332 \label{introEquation:NPTPartition}
333 \end{equation}
334 Here, $G = U - TS + PV$, and $G$ is called Gibbs free energy.
335
286   \subsection{\label{introSection:liouville}Liouville's theorem}
287  
288   Liouville's theorem is the foundation on which statistical mechanics
# Line 374 | Line 324 | simple form,
324   \frac{{\partial \rho }}{{\partial p_i }}\dot p_i } \right)}  = 0 .
325   \label{introEquation:liouvilleTheorem}
326   \end{equation}
377
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 388 | Line 337 | distribution,
337   connected to the Hamiltonian $H$ through Maxwell-Boltzmann
338   distribution,
339   \begin{equation}
340 < \rho  \propto e^{ - \beta H}
340 > \rho  \propto e^{ - \beta H}.
341   \label{introEquation:densityAndHamiltonian}
342   \end{equation}
343  
# Line 400 | Line 349 | inside this region is given by,
349   If this region is small enough, the density $\rho$ can be regarded
350   as uniform over the whole integral. Thus, the number of phase points
351   inside this region is given by,
352 < \begin{equation}
353 < \delta N = \rho \delta v = \rho \int { \ldots \int {dq_1 } ...dq_f
354 < dp_1 } ..dp_f.
406 < \end{equation}
407 <
408 < \begin{equation}
409 < \frac{{d(\delta N)}}{{dt}} = \frac{{d\rho }}{{dt}}\delta v + \rho
352 > \begin{eqnarray}
353 > \delta N &=& \rho \delta v = \rho \int { \ldots \int {dq_1 } ...dq_f dp_1 } ..dp_f,\\
354 > \frac{{d(\delta N)}}{{dt}} &=& \frac{{d\rho }}{{dt}}\delta v + \rho
355   \frac{d}{{dt}}(\delta v) = 0.
356 < \end{equation}
357 < With the help of stationary assumption
358 < (\ref{introEquation:stationary}), we obtain the principle of the
356 > \end{eqnarray}
357 > With the help of the stationary assumption
358 > (Eq.~\ref{introEquation:stationary}), we obtain the principle of
359   \emph{conservation of volume in phase space},
360   \begin{equation}
361   \frac{d}{{dt}}(\delta v) = \frac{d}{{dt}}\int { \ldots \int {dq_1 }
# Line 420 | Line 365 | With the help of stationary assumption
365  
366   \subsubsection{\label{introSection:liouvilleInOtherForms}\textbf{Liouville's Theorem in Other Forms}}
367  
368 < Liouville's theorem can be expresses in a variety of different forms
368 > Liouville's theorem can be expressed in a variety of different forms
369   which are convenient within different contexts. For any two function
370   $F$ and $G$ of the coordinates and momenta of a system, the Poisson
371 < bracket ${F, G}$ is defined as
371 > bracket $\{F,G\}$ is defined as
372   \begin{equation}
373   \left\{ {F,G} \right\} = \sum\limits_i {\left( {\frac{{\partial
374   F}}{{\partial q_i }}\frac{{\partial G}}{{\partial p_i }} -
# Line 431 | Line 376 | q_i }}} \right)}.
376   q_i }}} \right)}.
377   \label{introEquation:poissonBracket}
378   \end{equation}
379 < Substituting equations of motion in Hamiltonian formalism(
380 < Eq.~\ref{introEquation:motionHamiltonianCoordinate} ,
381 < Eq.~\ref{introEquation:motionHamiltonianMomentum} ) into
379 > Substituting equations of motion in Hamiltonian formalism
380 > (Eq.~\ref{introEquation:motionHamiltonianCoordinate} ,
381 > Eq.~\ref{introEquation:motionHamiltonianMomentum}) into
382   (Eq.~\ref{introEquation:liouvilleTheorem}), we can rewrite
383   Liouville's theorem using Poisson bracket notion,
384   \begin{equation}
# Line 454 | Line 399 | expressed as
399   \left( {\frac{{\partial \rho }}{{\partial t}}} \right) =  - iL\rho
400   \label{introEquation:liouvilleTheoremInOperator}
401   \end{equation}
402 <
402 > which can help define a propagator $\rho (t) = e^{-iLt} \rho (0)$.
403   \subsection{\label{introSection:ergodic}The Ergodic Hypothesis}
404  
405   Various thermodynamic properties can be calculated from Molecular
# Line 463 | Line 408 | certain time interval and the measurements are average
408   simulation and the quality of the underlying model. However, both
409   experiments and computer simulations are usually performed during a
410   certain time interval and the measurements are averaged over a
411 < period of them which is different from the average behavior of
411 > period of time which is different from the average behavior of
412   many-body system in Statistical Mechanics. Fortunately, the Ergodic
413   Hypothesis makes a connection between time average and the ensemble
414   average. It states that the time average and average over the
415 < statistical ensemble are identical \cite{Frenkel1996, Leach2001}.
415 > statistical ensemble are identical:\cite{Frenkel1996, Leach2001}
416   \begin{equation}
417   \langle A(q , p) \rangle_t = \mathop {\lim }\limits_{t \to \infty }
418   \frac{1}{t}\int\limits_0^t {A(q(t),p(t))dt = \int\limits_\Gamma
# Line 476 | Line 421 | distribution function. If an observation is averaged o
421   where $\langle  A(q , p) \rangle_t$ is an equilibrium value of a
422   physical quantity and $\rho (p(t), q(t))$ is the equilibrium
423   distribution function. If an observation is averaged over a
424 < sufficiently long time (longer than relaxation time), all accessible
425 < microstates in phase space are assumed to be equally probed, giving
426 < a properly weighted statistical average. This allows the researcher
427 < freedom of choice when deciding how best to measure a given
428 < observable. In case an ensemble averaged approach sounds most
429 < reasonable, the Monte Carlo techniques\cite{Metropolis1949} can be
424 > sufficiently long time (longer than the relaxation time), all
425 > accessible microstates in phase space are assumed to be equally
426 > probed, giving a properly weighted statistical average. This allows
427 > the researcher freedom of choice when deciding how best to measure a
428 > given observable. In case an ensemble averaged approach sounds most
429 > reasonable, the Monte Carlo methods\cite{Metropolis1949} can be
430   utilized. Or if the system lends itself to a time averaging
431   approach, the Molecular Dynamics techniques in
432   Sec.~\ref{introSection:molecularDynamics} will be the best
433 < choice\cite{Frenkel1996}.
433 > choice.\cite{Frenkel1996}
434  
435   \section{\label{introSection:geometricIntegratos}Geometric Integrators}
436   A variety of numerical integrators have been proposed to simulate
437   the motions of atoms in MD simulation. They usually begin with
438 < initial conditionals and move the objects in the direction governed
439 < by the differential equations. However, most of them ignore the
440 < hidden physical laws contained within the equations. Since 1990,
441 < geometric integrators, which preserve various phase-flow invariants
442 < such as symplectic structure, volume and time reversal symmetry, are
443 < developed to address this issue\cite{Dullweber1997, McLachlan1998,
444 < Leimkuhler1999}. The velocity Verlet method, which happens to be a
438 > initial conditions and move the objects in the direction governed by
439 > the differential equations. However, most of them ignore the hidden
440 > physical laws contained within the equations. Since 1990, geometric
441 > integrators, which preserve various phase-flow invariants such as
442 > symplectic structure, volume and time reversal symmetry, were
443 > developed to address this issue.\cite{Dullweber1997, McLachlan1998,
444 > Leimkuhler1999} The velocity Verlet method, which happens to be a
445   simple example of symplectic integrator, continues to gain
446   popularity in the molecular dynamics community. This fact can be
447   partly explained by its geometric nature.
448  
449 < \subsection{\label{introSection:symplecticManifold}Symplectic Manifolds}
449 > \subsection{\label{introSection:symplecticManifold}Manifolds and Bundles}
450   A \emph{manifold} is an abstract mathematical space. It looks
451   locally like Euclidean space, but when viewed globally, it may have
452   more complicated structure. A good example of manifold is the
453   surface of Earth. It seems to be flat locally, but it is round if
454   viewed as a whole. A \emph{differentiable manifold} (also known as
455   \emph{smooth manifold}) is a manifold on which it is possible to
456 < apply calculus on \emph{differentiable manifold}. A \emph{symplectic
457 < manifold} is defined as a pair $(M, \omega)$ which consists of a
458 < \emph{differentiable manifold} $M$ and a close, non-degenerated,
456 > apply calculus.\cite{Hirsch1997} A \emph{symplectic manifold} is
457 > defined as a pair $(M, \omega)$ which consists of a
458 > \emph{differentiable manifold} $M$ and a close, non-degenerate,
459   bilinear symplectic form, $\omega$. A symplectic form on a vector
460   space $V$ is a function $\omega(x, y)$ which satisfies
461   $\omega(\lambda_1x_1+\lambda_2x_2, y) = \lambda_1\omega(x_1, y)+
462   \lambda_2\omega(x_2, y)$, $\omega(x, y) = - \omega(y, x)$ and
463 < $\omega(x, x) = 0$. The cross product operation in vector field is
464 < an example of symplectic form.
465 <
466 < One of the motivations to study \emph{symplectic manifolds} in
467 < Hamiltonian Mechanics is that a symplectic manifold can represent
468 < all possible configurations of the system and the phase space of the
469 < system can be described by it's cotangent bundle. Every symplectic
470 < manifold is even dimensional. For instance, in Hamilton equations,
471 < coordinate and momentum always appear in pairs.
463 > $\omega(x, x) = 0$.\cite{McDuff1998} The cross product operation in
464 > vector field is an example of symplectic form.
465 > Given vector spaces $V$ and $W$ over same field $F$, $f: V \to W$ is a linear transformation if
466 > \begin{eqnarray*}
467 > f(x+y) & = & f(x) + f(y) \\
468 > f(ax) & = & af(x)
469 > \end{eqnarray*}
470 > are always satisfied for any two vectors $x$ and $y$ in $V$ and any scalar $a$ in $F$. One can define the dual vector space $V^*$ of $V$ if any two built-in linear transformations $\phi$ and $\psi$ in $V^*$ satisfy the following definition of addition and scalar multiplication:
471 > \begin{eqnarray*}
472 > (\phi+\psi)(x) & = & \phi(x)+\psi(x) \\
473 > (a\phi)(x) & = & a \phi(x)
474 > \end{eqnarray*}
475 > for all $a$ in $F$ and $x$ in $V$. For a manifold $M$, one can define a tangent vector of a tangent space $TM_q$ at every point $q$
476 > \begin{equation}
477 > \dot q = \mathop {\lim }\limits_{t \to 0} \frac{{\phi (t) - \phi (0)}}{t}
478 > \end{equation}
479 > where $\phi(0)=q$ and $\phi(t) \in M$. One may also define a cotangent space $T^*M_q$ as the dual space of the tangent space $TM_q$. The tangent space and the cotangent space are isomorphic to each other, since they are both real vector spaces with same dimension.
480 > The union of tangent spaces at every point of $M$ is called the tangent bundle of $M$ and is denoted by $TM$, while cotangent bundle $T^*M$ is defined as the union of the cotangent spaces to $M$.\cite{Jost2002} For a Hamiltonian system with configuration manifold $V$, the $(q,\dot q)$ phase space is the tangent bundle of the configuration manifold $V$, while the cotangent bundle is represented by $(q,p)$.
481  
482   \subsection{\label{introSection:ODE}Ordinary Differential Equations}
483  
# Line 531 | Line 485 | For an ordinary differential system defined as
485   \begin{equation}
486   \dot x = f(x)
487   \end{equation}
488 < where $x = x(q,p)^T$, this system is a canonical Hamiltonian, if
488 > where $x = x(q,p)$, this system is a canonical Hamiltonian, if
489 > $f(x) = J\nabla _x H(x)$. Here, $H = H (q, p)$ is Hamiltonian
490 > function and $J$ is the skew-symmetric matrix
491   \begin{equation}
536 f(r) = J\nabla _x H(r).
537 \end{equation}
538 $H = H (q, p)$ is Hamiltonian function and $J$ is the skew-symmetric
539 matrix
540 \begin{equation}
492   J = \left( {\begin{array}{*{20}c}
493     0 & I  \\
494     { - I} & 0  \\
# Line 547 | Line 498 | system can be rewritten as,
498   where $I$ is an identity matrix. Using this notation, Hamiltonian
499   system can be rewritten as,
500   \begin{equation}
501 < \frac{d}{{dt}}x = J\nabla _x H(x)
501 > \frac{d}{{dt}}x = J\nabla _x H(x).
502   \label{introEquation:compactHamiltonian}
503   \end{equation}In this case, $f$ is
504 < called a \emph{Hamiltonian vector field}.
505 <
555 < Another generalization of Hamiltonian dynamics is Poisson
556 < Dynamics\cite{Olver1986},
504 > called a \emph{Hamiltonian vector field}. Another generalization of
505 > Hamiltonian dynamics is Poisson Dynamics,\cite{Olver1986}
506   \begin{equation}
507   \dot x = J(x)\nabla _x H \label{introEquation:poissonHamiltonian}
508   \end{equation}
509 < The most obvious change being that matrix $J$ now depends on $x$.
509 > where the most obvious change being that matrix $J$ now depends on
510 > $x$.
511  
512 < \subsection{\label{introSection:exactFlow}Exact Flow}
512 > \subsection{\label{introSection:exactFlow}Exact Propagator}
513  
514 < Let $x(t)$ be the exact solution of the ODE system,
514 > Let $x(t)$ be the exact solution of the ODE
515 > system,
516   \begin{equation}
517 < \frac{{dx}}{{dt}} = f(x) \label{introEquation:ODE}
518 < \end{equation}
519 < The exact flow(solution) $\varphi_\tau$ is defined by
520 < \[
521 < x(t+\tau) =\varphi_\tau(x(t))
517 > \frac{{dx}}{{dt}} = f(x), \label{introEquation:ODE}
518 > \end{equation} we can
519 > define its exact propagator $\varphi_\tau$:
520 > \[ x(t+\tau)
521 > =\varphi_\tau(x(t))
522   \]
523   where $\tau$ is a fixed time step and $\varphi$ is a map from phase
524 < space to itself. The flow has the continuous group property,
524 > space to itself. The propagator has the continuous group property,
525   \begin{equation}
526   \varphi _{\tau _1 }  \circ \varphi _{\tau _2 }  = \varphi _{\tau _1
527   + \tau _2 } .
# Line 579 | Line 530 | In particular,
530   \begin{equation}
531   \varphi _\tau   \circ \varphi _{ - \tau }  = I
532   \end{equation}
533 < Therefore, the exact flow is self-adjoint,
533 > Therefore, the exact propagator is self-adjoint,
534   \begin{equation}
535   \varphi _\tau   = \varphi _{ - \tau }^{ - 1}.
536   \end{equation}
537 < The exact flow can also be written in terms of the of an operator,
537 > In most cases, it is not easy to find the exact propagator
538 > $\varphi_\tau$. Instead, we use an approximate map, $\psi_\tau$,
539 > which is usually called an integrator. The order of an integrator
540 > $\psi_\tau$ is $p$, if the Taylor series of $\psi_\tau$ agree to
541 > order $p$,
542   \begin{equation}
588 \varphi _\tau  (x) = e^{\tau \sum\limits_i {f_i (x)\frac{\partial
589 }{{\partial x_i }}} } (x) \equiv \exp (\tau f)(x).
590 \label{introEquation:exponentialOperator}
591 \end{equation}
592
593 In most cases, it is not easy to find the exact flow $\varphi_\tau$.
594 Instead, we use an approximate map, $\psi_\tau$, which is usually
595 called integrator. The order of an integrator $\psi_\tau$ is $p$, if
596 the Taylor series of $\psi_\tau$ agree to order $p$,
597 \begin{equation}
543   \psi_\tau(x) = x + \tau f(x) + O(\tau^{p+1})
544   \end{equation}
545  
546   \subsection{\label{introSection:geometricProperties}Geometric Properties}
547  
548   The hidden geometric properties\cite{Budd1999, Marsden1998} of an
549 < ODE and its flow play important roles in numerical studies. Many of
550 < them can be found in systems which occur naturally in applications.
551 <
552 < Let $\varphi$ be the flow of Hamiltonian vector field, $\varphi$ is
608 < a \emph{symplectic} flow if it satisfies,
549 > ODE and its propagator play important roles in numerical studies.
550 > Many of them can be found in systems which occur naturally in
551 > applications. Let $\varphi$ be the propagator of Hamiltonian vector
552 > field, $\varphi$ is a \emph{symplectic} propagator if it satisfies,
553   \begin{equation}
554   {\varphi '}^T J \varphi ' = J.
555   \end{equation}
556   According to Liouville's theorem, the symplectic volume is invariant
557 < under a Hamiltonian flow, which is the basis for classical
558 < statistical mechanics. Furthermore, the flow of a Hamiltonian vector
559 < field on a symplectic manifold can be shown to be a
557 > under a Hamiltonian propagator, which is the basis for classical
558 > statistical mechanics. Furthermore, the propagator of a Hamiltonian
559 > vector field on a symplectic manifold can be shown to be a
560   symplectomorphism. As to the Poisson system,
561   \begin{equation}
562   {\varphi '}^T J \varphi ' = J \circ \varphi
563   \end{equation}
564 < is the property that must be preserved by the integrator.
565 <
566 < It is possible to construct a \emph{volume-preserving} flow for a
567 < source free ODE ($ \nabla \cdot f = 0 $), if the flow satisfies $
568 < \det d\varphi  = 1$. One can show easily that a symplectic flow will
569 < be volume-preserving.
570 <
627 < Changing the variables $y = h(x)$ in an ODE
628 < (Eq.~\ref{introEquation:ODE}) will result in a new system,
564 > is the property that must be preserved by the integrator. It is
565 > possible to construct a \emph{volume-preserving} propagator for a
566 > source free ODE ($ \nabla \cdot f = 0 $), if the propagator
567 > satisfies $ \det d\varphi  = 1$. One can show easily that a
568 > symplectic propagator will be volume-preserving. Changing the
569 > variables $y = h(x)$ in an ODE (Eq.~\ref{introEquation:ODE}) will
570 > result in a new system,
571   \[
572   \dot y = \tilde f(y) = ((dh \cdot f)h^{ - 1} )(y).
573   \]
574   The vector filed $f$ has reversing symmetry $h$ if $f = - \tilde f$.
575 < In other words, the flow of this vector field is reversible if and
576 < only if $ h \circ \varphi ^{ - 1}  = \varphi  \circ h $.
577 <
578 < A \emph{first integral}, or conserved quantity of a general
579 < differential function is a function $ G:R^{2d}  \to R^d $ which is
638 < constant for all solutions of the ODE $\frac{{dx}}{{dt}} = f(x)$ ,
575 > In other words, the propagator of this vector field is reversible if
576 > and only if $ h \circ \varphi ^{ - 1}  = \varphi  \circ h $. A
577 > conserved quantity of a general differential function is a function
578 > $ G:R^{2d}  \to R^d $ which is constant for all solutions of the ODE
579 > $\frac{{dx}}{{dt}} = f(x)$ ,
580   \[
581   \frac{{dG(x(t))}}{{dt}} = 0.
582   \]
583 < Using chain rule, one may obtain,
583 > Using the chain rule, one may obtain,
584   \[
585 < \sum\limits_i {\frac{{dG}}{{dx_i }}} f_i (x) = f \bullet \nabla G,
585 > \sum\limits_i {\frac{{dG}}{{dx_i }}} f_i (x) = f \cdot \nabla G,
586   \]
587 < which is the condition for conserving \emph{first integral}. For a
588 < canonical Hamiltonian system, the time evolution of an arbitrary
589 < smooth function $G$ is given by,
649 <
587 > which is the condition for conserved quantities. For a canonical
588 > Hamiltonian system, the time evolution of an arbitrary smooth
589 > function $G$ is given by,
590   \begin{eqnarray}
591 < \frac{{dG(x(t))}}{{dt}} & = & [\nabla _x G(x(t))]^T \dot x(t) \\
592 <                        & = & [\nabla _x G(x(t))]^T J\nabla _x H(x(t)). \\
591 > \frac{{dG(x(t))}}{{dt}} & = & [\nabla _x G(x(t))]^T \dot x(t) \notag\\
592 >                        & = & [\nabla _x G(x(t))]^T J\nabla _x H(x(t)).
593   \label{introEquation:firstIntegral1}
594   \end{eqnarray}
595 <
596 <
657 < Using poisson bracket notion, Equation
658 < \ref{introEquation:firstIntegral1} can be rewritten as
595 > Using poisson bracket notion, Eq.~\ref{introEquation:firstIntegral1}
596 > can be rewritten as
597   \[
598   \frac{d}{{dt}}G(x(t)) = \left\{ {G,H} \right\}(x(t)).
599   \]
600 < Therefore, the sufficient condition for $G$ to be the \emph{first
601 < integral} of a Hamiltonian system is
602 < \[
603 < \left\{ {G,H} \right\} = 0.
666 < \]
667 < As well known, the Hamiltonian (or energy) H of a Hamiltonian system
668 < is a \emph{first integral}, which is due to the fact $\{ H,H\}  =
669 < 0$.
670 <
600 > Therefore, the sufficient condition for $G$ to be a conserved
601 > quantity of a Hamiltonian system is $\left\{ {G,H} \right\} = 0.$ As
602 > is well known, the Hamiltonian (or energy) H of a Hamiltonian system
603 > is a conserved quantity, which is due to the fact $\{ H,H\}  = 0$.
604   When designing any numerical methods, one should always try to
605 < preserve the structural properties of the original ODE and its flow.
605 > preserve the structural properties of the original ODE and its
606 > propagator.
607  
608   \subsection{\label{introSection:constructionSymplectic}Construction of Symplectic Methods}
609   A lot of well established and very effective numerical methods have
610 < been successful precisely because of their symplecticities even
610 > been successful precisely because of their symplectic nature even
611   though this fact was not recognized when they were first
612   constructed. The most famous example is the Verlet-leapfrog method
613   in molecular dynamics. In general, symplectic integrators can be
# Line 684 | Line 618 | constructed using one of four different methods.
618   \item Runge-Kutta methods
619   \item Splitting methods
620   \end{enumerate}
621 <
688 < Generating function\cite{Channell1990} tends to lead to methods
621 > Generating functions\cite{Channell1990} tend to lead to methods
622   which are cumbersome and difficult to use. In dissipative systems,
623   variational methods can capture the decay of energy
624 < accurately\cite{Kane2000}. Since their geometrically unstable nature
624 > accurately.\cite{Kane2000} Since they are geometrically unstable
625   against non-Hamiltonian perturbations, ordinary implicit Runge-Kutta
626 < methods are not suitable for Hamiltonian system. Recently, various
627 < high-order explicit Runge-Kutta methods
628 < \cite{Owren1992,Chen2003}have been developed to overcome this
629 < instability. However, due to computational penalty involved in
630 < implementing the Runge-Kutta methods, they have not attracted much
631 < attention from the Molecular Dynamics community. Instead, splitting
632 < methods have been widely accepted since they exploit natural
633 < decompositions of the system\cite{Tuckerman1992, McLachlan1998}.
626 > methods are not suitable for Hamiltonian
627 > system.\cite{Cartwright1992} Recently, various high-order explicit
628 > Runge-Kutta methods \cite{Owren1992,Chen2003} have been developed to
629 > overcome this instability. However, due to computational penalty
630 > involved in implementing the Runge-Kutta methods, they have not
631 > attracted much attention from the Molecular Dynamics community.
632 > Instead, splitting methods have been widely accepted since they
633 > exploit natural decompositions of the system.\cite{McLachlan1998,
634 > Tuckerman1992}
635  
636   \subsubsection{\label{introSection:splittingMethod}\textbf{Splitting Methods}}
637  
638   The main idea behind splitting methods is to decompose the discrete
639 < $\varphi_h$ as a composition of simpler flows,
639 > $\varphi_h$ as a composition of simpler propagators,
640   \begin{equation}
641   \varphi _h  = \varphi _{h_1 }  \circ \varphi _{h_2 }  \ldots  \circ
642   \varphi _{h_n }
643   \label{introEquation:FlowDecomposition}
644   \end{equation}
645 < where each of the sub-flow is chosen such that each represent a
646 < simpler integration of the system.
647 <
714 < Suppose that a Hamiltonian system takes the form,
645 > where each of the sub-propagator is chosen such that each represent
646 > a simpler integration of the system. Suppose that a Hamiltonian
647 > system takes the form,
648   \[
649   H = H_1 + H_2.
650   \]
651   Here, $H_1$ and $H_2$ may represent different physical processes of
652   the system. For instance, they may relate to kinetic and potential
653   energy respectively, which is a natural decomposition of the
654 < problem. If $H_1$ and $H_2$ can be integrated using exact flows
655 < $\varphi_1(t)$ and $\varphi_2(t)$, respectively, a simple first
656 < order expression is then given by the Lie-Trotter formula
654 > problem. If $H_1$ and $H_2$ can be integrated using exact
655 > propagators $\varphi_1(t)$ and $\varphi_2(t)$, respectively, a
656 > simple first order expression is then given by the Lie-Trotter
657 > formula\cite{Trotter1959}
658   \begin{equation}
659   \varphi _h  = \varphi _{1,h}  \circ \varphi _{2,h},
660   \label{introEquation:firstOrderSplitting}
# Line 729 | Line 663 | must follow that each operator $\varphi_i(t)$ is a sym
663   continuous $\varphi _i$ over a time $h$. By definition, as
664   $\varphi_i(t)$ is the exact solution of a Hamiltonian system, it
665   must follow that each operator $\varphi_i(t)$ is a symplectic map.
666 < It is easy to show that any composition of symplectic flows yields a
667 < symplectic map,
666 > It is easy to show that any composition of symplectic propagators
667 > yields a symplectic map,
668   \begin{equation}
669   (\varphi '\phi ')^T J\varphi '\phi ' = \phi '^T \varphi '^T J\varphi
670   '\phi ' = \phi '^T J\phi ' = J,
# Line 738 | Line 672 | splitting in this context automatically generates a sy
672   \end{equation}
673   where $\phi$ and $\psi$ both are symplectic maps. Thus operator
674   splitting in this context automatically generates a symplectic map.
675 <
676 < The Lie-Trotter splitting(\ref{introEquation:firstOrderSplitting})
677 < introduces local errors proportional to $h^2$, while Strang
678 < splitting gives a second-order decomposition,
675 > The Lie-Trotter
676 > splitting(Eq.~\ref{introEquation:firstOrderSplitting}) introduces
677 > local errors proportional to $h^2$, while the Strang splitting gives
678 > a second-order decomposition,\cite{Strang1968}
679   \begin{equation}
680   \varphi _h  = \varphi _{1,h/2}  \circ \varphi _{2,h}  \circ \varphi
681   _{1,h/2} , \label{introEquation:secondOrderSplitting}
682   \end{equation}
683 < which has a local error proportional to $h^3$. The Sprang
683 > which has a local error proportional to $h^3$. The Strang
684   splitting's popularity in molecular simulation community attribute
685   to its symmetric property,
686   \begin{equation}
687   \varphi _h^{ - 1} = \varphi _{ - h}.
688   \label{introEquation:timeReversible}
689 < \end{equation},appendixFig:architecture
689 > \end{equation}
690  
691   \subsubsection{\label{introSection:exampleSplittingMethod}\textbf{Examples of the Splitting Method}}
692   The classical equation for a system consisting of interacting
# Line 774 | Line 708 | known as \emph{velocity verlet} which is
708   \end{align}
709   where $F(t)$ is the force at time $t$. This integration scheme is
710   known as \emph{velocity verlet} which is
711 < symplectic(\ref{introEquation:SymplecticFlowComposition}),
712 < time-reversible(\ref{introEquation:timeReversible}) and
713 < volume-preserving (\ref{introEquation:volumePreserving}). These
711 > symplectic(Eq.~\ref{introEquation:SymplecticFlowComposition}),
712 > time-reversible(Eq.~\ref{introEquation:timeReversible}) and
713 > volume-preserving (Eq.~\ref{introEquation:volumePreserving}). These
714   geometric properties attribute to its long-time stability and its
715   popularity in the community. However, the most commonly used
716   velocity verlet integration scheme is written as below,
# Line 797 | Line 731 | the equations of motion would follow:
731  
732   \item Use the half step velocities to move positions one whole step, $\Delta t$.
733  
734 < \item Evaluate the forces at the new positions, $\mathbf{q}(\Delta t)$, and use the new forces to complete the velocity move.
734 > \item Evaluate the forces at the new positions, $q(\Delta t)$, and use the new forces to complete the velocity move.
735  
736   \item Repeat from step 1 with the new position, velocities, and forces assuming the roles of the initial values.
737   \end{enumerate}
804
738   By simply switching the order of the propagators in the splitting
739   and composing a new integrator, the \emph{position verlet}
740   integrator, can be generated,
# Line 817 | Line 750 | q(\Delta t)} \right]. %
750  
751   \subsubsection{\label{introSection:errorAnalysis}\textbf{Error Analysis and Higher Order Methods}}
752  
753 < The Baker-Campbell-Hausdorff formula can be used to determine the
754 < local error of splitting method in terms of the commutator of the
755 < operators(\ref{introEquation:exponentialOperator}) associated with
756 < the sub-flow. For operators $hX$ and $hY$ which are associated with
757 < $\varphi_1(t)$ and $\varphi_2(t)$ respectively , we have
753 > The Baker-Campbell-Hausdorff formula\cite{Gilmore1974} can be used
754 > to determine the local error of a splitting method in terms of the
755 > commutator of the
756 > operators associated
757 > with the sub-propagator. For operators $hX$ and $hY$ which are
758 > associated with $\varphi_1(t)$ and $\varphi_2(t)$ respectively , we
759 > have
760   \begin{equation}
761   \exp (hX + hY) = \exp (hZ)
762   \end{equation}
# Line 830 | Line 765 | hZ = hX + hY + \frac{{h^2 }}{2}[X,Y] + \frac{{h^3 }}{2
765   hZ = hX + hY + \frac{{h^2 }}{2}[X,Y] + \frac{{h^3 }}{2}\left(
766   {[X,[X,Y]] + [Y,[Y,X]]} \right) +  \ldots .
767   \end{equation}
768 < Here, $[X,Y]$ is the commutators of operator $X$ and $Y$ given by
768 > Here, $[X,Y]$ is the commutator of operator $X$ and $Y$ given by
769   \[
770   [X,Y] = XY - YX .
771   \]
772   Applying the Baker-Campbell-Hausdorff formula\cite{Varadarajan1974}
773 < to the Sprang splitting, we can obtain
773 > to the Strang splitting, we can obtain
774   \begin{eqnarray*}
775   \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 \\
776                                     &   & \mbox{} + h^2 [X,X]/8 + h^2 [Y,Y]/8 \\
777 <                                   &   & \mbox{} + h^3 [Y,[Y,X]]/12 - h^3[X,[X,Y]]/24 + \ldots )
777 >                                   &   & \mbox{} + h^3 [Y,[Y,X]]/12 - h^3[X,[X,Y]]/24 + \ldots
778 >                                   ).
779   \end{eqnarray*}
780 < Since \[ [X,Y] + [Y,X] = 0\] and \[ [X,X] = 0,\] the dominant local
781 < error of Spring splitting is proportional to $h^3$. The same
782 < procedure can be applied to a general splitting,  of the form
780 > Since $ [X,Y] + [Y,X] = 0$ and $ [X,X] = 0$, the dominant local
781 > error of Strang splitting is proportional to $h^3$. The same
782 > procedure can be applied to a general splitting of the form
783   \begin{equation}
784   \varphi _{b_m h}^2  \circ \varphi _{a_m h}^1  \circ \varphi _{b_{m -
785   1} h}^2  \circ  \ldots  \circ \varphi _{a_1 h}^1 .
786   \end{equation}
787   A careful choice of coefficient $a_1 \ldots b_m$ will lead to higher
788   order methods. Yoshida proposed an elegant way to compose higher
789 < order methods based on symmetric splitting\cite{Yoshida1990}. Given
789 > order methods based on symmetric splitting.\cite{Yoshida1990} Given
790   a symmetric second order base method $ \varphi _h^{(2)} $, a
791   fourth-order symmetric method can be constructed by composing,
792   \[
# Line 878 | Line 814 | microscopic behavior can be calculated from the trajec
814   dynamical information. The basic idea of molecular dynamics is that
815   macroscopic properties are related to microscopic behavior and
816   microscopic behavior can be calculated from the trajectories in
817 < simulations. For instance, instantaneous temperature of an
818 < Hamiltonian system of $N$ particle can be measured by
817 > simulations. For instance, instantaneous temperature of a
818 > Hamiltonian system of $N$ particles can be measured by
819   \[
820   T = \sum\limits_{i = 1}^N {\frac{{m_i v_i^2 }}{{fk_B }}}
821   \]
822   where $m_i$ and $v_i$ are the mass and velocity of $i$th particle
823   respectively, $f$ is the number of degrees of freedom, and $k_B$ is
824 < the boltzman constant.
824 > the Boltzman constant.
825  
826   A typical molecular dynamics run consists of three essential steps:
827   \begin{enumerate}
# Line 902 | Line 838 | initialization of a simulation. Sec.~\ref{introSection
838   These three individual steps will be covered in the following
839   sections. Sec.~\ref{introSec:initialSystemSettings} deals with the
840   initialization of a simulation. Sec.~\ref{introSection:production}
841 < will discusse issues in production run.
841 > discusses issues of production runs.
842   Sec.~\ref{introSection:Analysis} provides the theoretical tools for
843 < trajectory analysis.
843 > analysis of trajectories.
844  
845   \subsection{\label{introSec:initialSystemSettings}Initialization}
846  
# Line 916 | Line 852 | purification and crystallization. Even for molecules w
852   thousands of crystal structures of molecules are discovered every
853   year, many more remain unknown due to the difficulties of
854   purification and crystallization. Even for molecules with known
855 < structure, some important information is missing. For example, a
855 > structures, some important information is missing. For example, a
856   missing hydrogen atom which acts as donor in hydrogen bonding must
857 < be added. Moreover, in order to include electrostatic interaction,
857 > be added. Moreover, in order to include electrostatic interactions,
858   one may need to specify the partial charges for individual atoms.
859   Under some circumstances, we may even need to prepare the system in
860   a special configuration. For instance, when studying transport
# Line 936 | Line 872 | surface and to locate the local minimum. While converg
872   minimization to find a more reasonable conformation. Several energy
873   minimization methods have been developed to exploit the energy
874   surface and to locate the local minimum. While converging slowly
875 < near the minimum, steepest descent method is extremely robust when
875 > near the minimum, the steepest descent method is extremely robust when
876   systems are strongly anharmonic. Thus, it is often used to refine
877 < structure from crystallographic data. Relied on the gradient or
878 < hessian, advanced methods like Newton-Raphson converge rapidly to a
879 < local minimum, but become unstable if the energy surface is far from
877 > structures from crystallographic data. Relying on the Hessian,
878 > advanced methods like Newton-Raphson converge rapidly to a local
879 > minimum, but become unstable if the energy surface is far from
880   quadratic. Another factor that must be taken into account, when
881   choosing energy minimization method, is the size of the system.
882   Steepest descent and conjugate gradient can deal with models of any
883   size. Because of the limits on computer memory to store the hessian
884 < matrix and the computing power needed to diagonalized these
885 < matrices, most Newton-Raphson methods can not be used with very
950 < large systems.
884 > matrix and the computing power needed to diagonalize these matrices,
885 > most Newton-Raphson methods can not be used with very large systems.
886  
887   \subsubsection{\textbf{Heating}}
888  
889 < Typically, Heating is performed by assigning random velocities
889 > Typically, heating is performed by assigning random velocities
890   according to a Maxwell-Boltzman distribution for a desired
891   temperature. Beginning at a lower temperature and gradually
892   increasing the temperature by assigning larger random velocities, we
893 < end up with setting the temperature of the system to a final
894 < temperature at which the simulation will be conducted. In heating
895 < phase, we should also keep the system from drifting or rotating as a
896 < whole. To do this, the net linear momentum and angular momentum of
897 < the system is shifted to zero after each resampling from the Maxwell
898 < -Boltzman distribution.
893 > end up setting the temperature of the system to a final temperature
894 > at which the simulation will be conducted. In the heating phase, we
895 > should also keep the system from drifting or rotating as a whole. To
896 > do this, the net linear momentum and angular momentum of the system
897 > is shifted to zero after each resampling from the Maxwell -Boltzman
898 > distribution.
899  
900   \subsubsection{\textbf{Equilibration}}
901  
# Line 971 | Line 906 | equilibration process is long enough. However, these s
906   properties \textit{etc}, become independent of time. Strictly
907   speaking, minimization and heating are not necessary, provided the
908   equilibration process is long enough. However, these steps can serve
909 < as a means to arrive at an equilibrated structure in an effective
909 > as a mean to arrive at an equilibrated structure in an effective
910   way.
911  
912   \subsection{\label{introSection:production}Production}
# Line 987 | Line 922 | complexity of the algorithm for pair-wise interactions
922   calculation of non-bonded forces, such as van der Waals force and
923   Coulombic forces \textit{etc}. For a system of $N$ particles, the
924   complexity of the algorithm for pair-wise interactions is $O(N^2 )$,
925 < which making large simulations prohibitive in the absence of any
926 < algorithmic tricks.
927 <
928 < A natural approach to avoid system size issues is to represent the
929 < bulk behavior by a finite number of the particles. However, this
930 < approach will suffer from the surface effect at the edges of the
931 < simulation. To offset this, \textit{Periodic boundary conditions}
932 < (see Fig.~\ref{introFig:pbc}) is developed to simulate bulk
933 < properties with a relatively small number of particles. In this
934 < method, the simulation box is replicated throughout space to form an
935 < infinite lattice. During the simulation, when a particle moves in
936 < the primary cell, its image in other cells move in exactly the same
937 < direction with exactly the same orientation. Thus, as a particle
1003 < leaves the primary cell, one of its images will enter through the
1004 < opposite face.
925 > which makes large simulations prohibitive in the absence of any
926 > algorithmic tricks. A natural approach to avoid system size issues
927 > is to represent the bulk behavior by a finite number of the
928 > particles. However, this approach will suffer from surface effects
929 > at the edges of the simulation. To offset this, \textit{Periodic
930 > boundary conditions} (see Fig.~\ref{introFig:pbc}) were developed to
931 > simulate bulk properties with a relatively small number of
932 > particles. In this method, the simulation box is replicated
933 > throughout space to form an infinite lattice. During the simulation,
934 > when a particle moves in the primary cell, its image in other cells
935 > move in exactly the same direction with exactly the same
936 > orientation. Thus, as a particle leaves the primary cell, one of its
937 > images will enter through the opposite face.
938   \begin{figure}
939   \centering
940   \includegraphics[width=\linewidth]{pbc.eps}
# Line 1013 | Line 946 | Another important technique to improve the efficiency
946  
947   %cutoff and minimum image convention
948   Another important technique to improve the efficiency of force
949 < evaluation is to apply spherical cutoff where particles farther than
950 < a predetermined distance are not included in the calculation
951 < \cite{Frenkel1996}. The use of a cutoff radius will cause a
952 < discontinuity in the potential energy curve. Fortunately, one can
953 < shift simple radial potential to ensure the potential curve go
949 > evaluation is to apply spherical cutoffs where particles farther
950 > than a predetermined distance are not included in the
951 > calculation.\cite{Frenkel1996} The use of a cutoff radius will cause
952 > a discontinuity in the potential energy curve. Fortunately, one can
953 > shift a simple radial potential to ensure the potential curve go
954   smoothly to zero at the cutoff radius. The cutoff strategy works
955   well for Lennard-Jones interaction because of its short range
956   nature. However, simply truncating the electrostatic interaction
# Line 1025 | Line 958 | with rapid and absolute convergence, has proved to min
958   in simulations. The Ewald summation, in which the slowly decaying
959   Coulomb potential is transformed into direct and reciprocal sums
960   with rapid and absolute convergence, has proved to minimize the
961 < periodicity artifacts in liquid simulations. Taking the advantages
962 < of the fast Fourier transform (FFT) for calculating discrete Fourier
963 < transforms, the particle mesh-based
961 > periodicity artifacts in liquid simulations. Taking advantage of
962 > fast Fourier transform (FFT) techniques for calculating discrete
963 > Fourier transforms, the particle mesh-based
964   methods\cite{Hockney1981,Shimada1993, Luty1994} are accelerated from
965   $O(N^{3/2})$ to $O(N logN)$. An alternative approach is the
966   \emph{fast multipole method}\cite{Greengard1987, Greengard1994},
# Line 1037 | Line 970 | charge-neutralized Coulomb potential method developed
970   simulation community, these two methods are difficult to implement
971   correctly and efficiently. Instead, we use a damped and
972   charge-neutralized Coulomb potential method developed by Wolf and
973 < his coworkers\cite{Wolf1999}. The shifted Coulomb potential for
973 > his coworkers.\cite{Wolf1999} The shifted Coulomb potential for
974   particle $i$ and particle $j$ at distance $r_{rj}$ is given by:
975   \begin{equation}
976   V(r_{ij})= \frac{q_i q_j \textrm{erfc}(\alpha
977   r_{ij})}{r_{ij}}-\lim_{r_{ij}\rightarrow
978   R_\textrm{c}}\left\{\frac{q_iq_j \textrm{erfc}(\alpha
979 < r_{ij})}{r_{ij}}\right\}. \label{introEquation:shiftedCoulomb}
979 > r_{ij})}{r_{ij}}\right\}, \label{introEquation:shiftedCoulomb}
980   \end{equation}
981   where $\alpha$ is the convergence parameter. Due to the lack of
982   inherent periodicity and rapid convergence,this method is extremely
# Line 1056 | Line 989 | illustration of shifted Coulomb potential.}
989   \label{introFigure:shiftedCoulomb}
990   \end{figure}
991  
1059 %multiple time step
1060
992   \subsection{\label{introSection:Analysis} Analysis}
993  
994 < Recently, advanced visualization technique have become applied to
995 < monitor the motions of molecules. Although the dynamics of the
996 < system can be described qualitatively from animation, quantitative
997 < trajectory analysis are more useful. According to the principles of
998 < Statistical Mechanics, Sec.~\ref{introSection:statisticalMechanics},
999 < one can compute thermodynamic properties, analyze fluctuations of
1069 < structural parameters, and investigate time-dependent processes of
1070 < the molecule from the trajectories.
994 > According to the principles of
995 > Statistical Mechanics in
996 > Sec.~\ref{introSection:statisticalMechanics}, one can compute
997 > thermodynamic properties, analyze fluctuations of structural
998 > parameters, and investigate time-dependent processes of the molecule
999 > from the trajectories.
1000  
1001   \subsubsection{\label{introSection:thermodynamicsProperties}\textbf{Thermodynamic Properties}}
1002  
# Line 1097 | Line 1026 | function}, is of most fundamental importance to liquid
1026   distribution functions. Among these functions,the \emph{pair
1027   distribution function}, also known as \emph{radial distribution
1028   function}, is of most fundamental importance to liquid theory.
1029 < Experimentally, pair distribution function can be gathered by
1029 > Experimentally, pair distribution functions can be gathered by
1030   Fourier transforming raw data from a series of neutron diffraction
1031 < experiments and integrating over the surface factor
1032 < \cite{Powles1973}. The experimental results can serve as a criterion
1033 < to justify the correctness of a liquid model. Moreover, various
1034 < equilibrium thermodynamic and structural properties can also be
1035 < expressed in terms of radial distribution function \cite{Allen1987}.
1036 <
1037 < The pair distribution functions $g(r)$ gives the probability that a
1038 < particle $i$ will be located at a distance $r$ from a another
1039 < particle $j$ in the system
1111 < \[
1031 > experiments and integrating over the surface
1032 > factor.\cite{Powles1973} The experimental results can serve as a
1033 > criterion to justify the correctness of a liquid model. Moreover,
1034 > various equilibrium thermodynamic and structural properties can also
1035 > be expressed in terms of the radial distribution
1036 > function.\cite{Allen1987} The pair distribution functions $g(r)$
1037 > gives the probability that a particle $i$ will be located at a
1038 > distance $r$ from a another particle $j$ in the system
1039 > \begin{equation}
1040   g(r) = \frac{V}{{N^2 }}\left\langle {\sum\limits_i {\sum\limits_{j
1041   \ne i} {\delta (r - r_{ij} )} } } \right\rangle = \frac{\rho
1042   (r)}{\rho}.
1043 < \]
1043 > \end{equation}
1044   Note that the delta function can be replaced by a histogram in
1045   computer simulation. Peaks in $g(r)$ represent solvent shells, and
1046   the height of these peaks gradually decreases to 1 as the liquid of
# Line 1130 | Line 1058 | If $A$ and $B$ refer to same variable, this kind of co
1058   \label{introEquation:timeCorrelationFunction}
1059   \end{equation}
1060   If $A$ and $B$ refer to same variable, this kind of correlation
1061 < function is called an \emph{autocorrelation function}. One example
1134 < of an auto correlation function is the velocity auto-correlation
1061 > functions are called \emph{autocorrelation functions}. One typical example is the velocity autocorrelation
1062   function which is directly related to transport properties of
1063   molecular liquids:
1064 < \[
1064 > \begin{equation}
1065   D = \frac{1}{3}\int\limits_0^\infty  {\left\langle {v(t) \cdot v(0)}
1066   \right\rangle } dt
1067 < \]
1067 > \end{equation}
1068   where $D$ is diffusion constant. Unlike the velocity autocorrelation
1069 < function, which is averaging over time origins and over all the
1070 < atoms, the dipole autocorrelation functions are calculated for the
1069 > function, which is averaged over time origins and over all the
1070 > atoms, the dipole autocorrelation functions is calculated for the
1071   entire system. The dipole autocorrelation function is given by:
1072 < \[
1072 > \begin{equation}
1073   c_{dipole}  = \left\langle {u_{tot} (t) \cdot u_{tot} (t)}
1074   \right\rangle
1075 < \]
1075 > \end{equation}
1076   Here $u_{tot}$ is the net dipole of the entire system and is given
1077   by
1078 < \[
1079 < u_{tot} (t) = \sum\limits_i {u_i (t)}
1080 < \]
1081 < In principle, many time correlation functions can be related with
1078 > \begin{equation}
1079 > u_{tot} (t) = \sum\limits_i {u_i (t)}.
1080 > \end{equation}
1081 > In principle, many time correlation functions can be related to
1082   Fourier transforms of the infrared, Raman, and inelastic neutron
1083   scattering spectra of molecular liquids. In practice, one can
1084 < extract the IR spectrum from the intensity of dipole fluctuation at
1085 < each frequency using the following relationship:
1086 < \[
1084 > extract the IR spectrum from the intensity of the molecular dipole
1085 > fluctuation at each frequency using the following relationship:
1086 > \begin{equation}
1087   \hat c_{dipole} (v) = \int_{ - \infty }^\infty  {c_{dipole} (t)e^{ -
1088 < i2\pi vt} dt}
1089 < \]
1088 > i2\pi vt} dt}.
1089 > \end{equation}
1090  
1091   \section{\label{introSection:rigidBody}Dynamics of Rigid Bodies}
1092  
1093   Rigid bodies are frequently involved in the modeling of different
1094 < areas, from engineering, physics, to chemistry. For example,
1095 < missiles and vehicle are usually modeled by rigid bodies.  The
1096 < movement of the objects in 3D gaming engine or other physics
1097 < simulator is governed by rigid body dynamics. In molecular
1094 > areas, including engineering, physics and chemistry. For example,
1095 > missiles and vehicles are usually modeled by rigid bodies.  The
1096 > movement of the objects in 3D gaming engines or other physics
1097 > simulators is governed by rigid body dynamics. In molecular
1098   simulations, rigid bodies are used to simplify protein-protein
1099 < docking studies\cite{Gray2003}.
1099 > docking studies.\cite{Gray2003}
1100  
1101   It is very important to develop stable and efficient methods to
1102   integrate the equations of motion for orientational degrees of
1103   freedom. Euler angles are the natural choice to describe the
1104   rotational degrees of freedom. However, due to $\frac {1}{sin
1105   \theta}$ singularities, the numerical integration of corresponding
1106 < equations of motion is very inefficient and inaccurate. Although an
1107 < alternative integrator using multiple sets of Euler angles can
1108 < overcome this difficulty\cite{Barojas1973}, the computational
1109 < penalty and the loss of angular momentum conservation still remain.
1110 < A singularity-free representation utilizing quaternions was
1111 < developed by Evans in 1977\cite{Evans1977}. Unfortunately, this
1112 < approach uses a nonseparable Hamiltonian resulting from the
1113 < quaternion representation, which prevents the symplectic algorithm
1114 < to be utilized. Another different approach is to apply holonomic
1115 < constraints to the atoms belonging to the rigid body. Each atom
1116 < moves independently under the normal forces deriving from potential
1117 < energy and constraint forces which are used to guarantee the
1118 < rigidness. However, due to their iterative nature, the SHAKE and
1119 < Rattle algorithms also converge very slowly when the number of
1120 < constraints increases\cite{Ryckaert1977, Andersen1983}.
1106 > equations of these motion is very inefficient and inaccurate.
1107 > Although an alternative integrator using multiple sets of Euler
1108 > angles can overcome this difficulty\cite{Barojas1973}, the
1109 > computational penalty and the loss of angular momentum conservation
1110 > still remain. A singularity-free representation utilizing
1111 > quaternions was developed by Evans in 1977.\cite{Evans1977}
1112 > Unfortunately, this approach used a nonseparable Hamiltonian
1113 > resulting from the quaternion representation, which prevented the
1114 > symplectic algorithm from being utilized. Another different approach
1115 > is to apply holonomic constraints to the atoms belonging to the
1116 > rigid body. Each atom moves independently under the normal forces
1117 > deriving from potential energy and constraint forces which are used
1118 > to guarantee the rigidness. However, due to their iterative nature,
1119 > the SHAKE and Rattle algorithms also converge very slowly when the
1120 > number of constraints increases.\cite{Ryckaert1977, Andersen1983}
1121  
1122   A break-through in geometric literature suggests that, in order to
1123   develop a long-term integration scheme, one should preserve the
1124 < symplectic structure of the flow. By introducing a conjugate
1124 > symplectic structure of the propagator. By introducing a conjugate
1125   momentum to the rotation matrix $Q$ and re-formulating Hamiltonian's
1126   equation, a symplectic integrator, RSHAKE\cite{Kol1997}, was
1127   proposed to evolve the Hamiltonian system in a constraint manifold
1128   by iteratively satisfying the orthogonality constraint $Q^T Q = 1$.
1129   An alternative method using the quaternion representation was
1130 < developed by Omelyan\cite{Omelyan1998}. However, both of these
1130 > developed by Omelyan.\cite{Omelyan1998} However, both of these
1131   methods are iterative and inefficient. In this section, we descibe a
1132 < symplectic Lie-Poisson integrator for rigid body developed by
1132 > symplectic Lie-Poisson integrator for rigid bodies developed by
1133   Dullweber and his coworkers\cite{Dullweber1997} in depth.
1134  
1135   \subsection{\label{introSection:constrainedHamiltonianRB}Constrained Hamiltonian for Rigid Bodies}
1136 < The motion of a rigid body is Hamiltonian with the Hamiltonian
1210 < function
1136 > The Hamiltonian of a rigid body is given by
1137   \begin{equation}
1138   H = \frac{1}{2}(p^T m^{ - 1} p) + \frac{1}{2}tr(PJ^{ - 1} P) +
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 1225 | Line 1151 | Q^T Q = 1, \label{introEquation:orthogonalConstraint}
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
1156 < \ref{introEquation:RBMotionMomentum}, one may obtain,
1231 < \begin{equation}
1232 < Q^T PJ^{ - 1}  + J^{ - 1} P^T Q = 0 . \\
1233 < \label{introEquation:RBFirstOrderConstraint}
1234 < \end{equation}
1235 <
1236 < Using Equation (\ref{introEquation:motionHamiltonianCoordinate},
1237 < \ref{introEquation:motionHamiltonianMomentum}), one can write down
1154 > which is used to ensure the rotation matrix's unitarity. Using
1155 > Eq.~\ref{introEquation:motionHamiltonianCoordinate} and Eq.~
1156 > \ref{introEquation:motionHamiltonianMomentum}, one can write down
1157   the equations of motion,
1239
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 < $T_{\star}SO(3)$. However, it turns out that under symplectic
1184 < transformation, the cotangent space and the phase space are
1262 < 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   \[
1186   \tilde Q = Q,\tilde P = \frac{1}{2}\left( {P - QP^T Q} \right),
1187   \]
1188 < the mechanical system subject to a holonomic constraint manifold $M$
1188 > the mechanical system subjected to a holonomic constraint manifold $M$
1189   can be re-formulated as a Hamiltonian system on the cotangent space
1190   \[
1191   T^* SO(3) = \left\{ {(\tilde Q,\tilde P):\tilde Q^T \tilde Q =
1192   1,\tilde Q^T \tilde PJ^{ - 1}  + J^{ - 1} P^T \tilde Q = 0} \right\}
1193   \]
1272
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
1195 > the rigid body, its corresponding lab fixed vector $X_i^{lab}$  is
1196   given as
1197   \begin{equation}
1198   X_i^{lab} = Q X_i + q.
# Line 1288 | Line 1209 | and
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
1294 < body, the angular momentum on the body fixed frame $\Pi  = Q^t P$ is
1295 < 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 < \mathop \Pi \limits^ \bullet   = J^{ - 1} \Pi ^T \Pi  + Q^T \sum\limits_i {F_i (q,Q)X_i^T }  - \Lambda  \\
1218 < \mathop Q\limits^{{\rm{   }} \bullet }  = 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 < \[
1224 < \begin{array}{l}
1306 < \Pi J^{ - 1}  + J^{ - 1} \Pi ^t  = 0 \\
1307 < Q^T Q = 1 \\
1308 < \end{array}
1309 < \]
1310 <
1311 < For a vector $v(v_1 ,v_2 ,v_3 ) \in R^3$ and a matrix $\hat v \in
1312 < so(3)^ \star$, 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 1322 | 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 + \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
1253   \begin{equation}
1330 (\mathop \Pi \limits^ \bullet   - \mathop \Pi \limits^ {\bullet  ^T}
1331 ){\rm{ }} = {\rm{ }}(\Pi  - \Pi ^T ){\rm{ }}(J^{ - 1} \Pi  + \Pi J^{
1332 - 1} ) + \sum\limits_i {[Q^T F_i (r,Q)X_i^T  - X_i F_i (r,Q)^T Q]} -
1333 (\Lambda  - \Lambda ^T ) . \label{introEquation:skewMatrixPI}
1334 \end{equation}
1335 Since $\Lambda$ is symmetric, the last term of Equation
1336 \ref{introEquation:skewMatrixPI} is zero, which implies the Lagrange
1337 multiplier $\Lambda$ is absent from the equations of motion. This
1338 unique property eliminates the requirement of iterations which can
1339 not be avoided in other methods\cite{Kol1997, Omelyan1998}.
1340
1341 Applying the hat-map isomorphism, we obtain the equation of motion
1342 for angular momentum on body frame
1343 \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 }.
1256   \label{introEquation:bodyAngularMotion}
# Line 1348 | 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 1370 | 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
1382 < 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   \[
1305   \pi (\Delta t) = e^{\Delta tR_1 } \pi (0),Q(\Delta t) =
1306   Q(0)e^{\Delta tR_1 }
# Line 1405 | Line 1314 | To reduce the cost of computing expensive functions in
1314   \end{array}} \right),\theta _1  = \frac{{\pi _1 }}{{I_1 }}\Delta t.
1315   \]
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   \[
1336   T^r (\pi ) = \frac{1}{2}T_1 ^r (\pi _1 ) + \frac{1}{2}T_2^r (\pi _2
1337   ) + T_3^r (\pi _3 ) + \frac{1}{2}T_2^r (\pi _2 ) + \frac{1}{2}T_1 ^r
# Line 1427 | Line 1345 | _1 }.
1345   \circ \varphi _{\Delta t/2,\pi _2 }  \circ \varphi _{\Delta t/2,\pi
1346   _1 }.
1347   \]
1348 <
1431 < The non-canonical Lie-Poisson bracket ${F, G}$ of two function
1432 < $F(\pi )$ and $G(\pi )$ is defined by
1348 > The non-canonical Lie-Poisson bracket $\{F, G\}$ of two functions $F(\pi )$ and $G(\pi )$ is defined by
1349   \[
1350   \{ F,G\} (\pi ) = [\nabla _\pi  F(\pi )]^T J(\pi )\nabla _\pi  G(\pi
1351 < )
1351 > ).
1352   \]
1353   If the Poisson bracket of a function $F$ with an arbitrary smooth
1354   function $G$ is zero, $F$ is a \emph{Casimir}, which is the
1355   conserved quantity in Poisson system. We can easily verify that the
1356   norm of the angular momentum, $\parallel \pi
1357 < \parallel$, is a \emph{Casimir}. Let$ F(\pi ) = S(\frac{{\parallel
1357 > \parallel$, is a \emph{Casimir}.\cite{McLachlan1993} Let $F(\pi ) = S(\frac{{\parallel
1358   \pi \parallel ^2 }}{2})$ for an arbitrary function $ S:R \to R$ ,
1359   then by the chain rule
1360   \[
1361   \nabla _\pi  F(\pi ) = S'(\frac{{\parallel \pi \parallel ^2
1362 < }}{2})\pi
1362 > }}{2})\pi.
1363   \]
1364 < Thus $ [\nabla _\pi  F(\pi )]^T J(\pi ) =  - S'(\frac{{\parallel \pi
1364 > Thus, $ [\nabla _\pi  F(\pi )]^T J(\pi ) =  - S'(\frac{{\parallel
1365 > \pi
1366   \parallel ^2 }}{2})\pi  \times \pi  = 0 $. This explicit
1367   Lie-Poisson integrator is found to be both extremely efficient and
1368   stable. These properties can be explained by the fact the small
# Line 1456 | Line 1373 | The Hamiltonian of rigid body can be separated in term
1373   Splitting for Rigid Body}
1374  
1375   The Hamiltonian of rigid body can be separated in terms of kinetic
1376 < energy and potential energy,
1377 < \[
1378 < H = T(p,\pi ) + V(q,Q)
1462 < \]
1463 < The equations of motion corresponding to potential energy and
1464 < kinetic energy are listed in the below table,
1376 > energy and potential energy, $H = T(p,\pi ) + V(q,Q)$. The equations
1377 > of motion corresponding to potential energy and kinetic energy are
1378 > listed in Table~\ref{introTable:rbEquations}.
1379   \begin{table}
1380 < \caption{Equations of motion due to Potential and Kinetic Energies}
1380 > \caption{EQUATIONS OF MOTION DUE TO POTENTIAL AND KINETIC ENERGIES}
1381 > \label{introTable:rbEquations}
1382   \begin{center}
1383   \begin{tabular}{|l|l|}
1384    \hline
# Line 1499 | Line 1414 | where $ T^t (p) = \frac{1}{2}p^T m^{ - 1} p $ and $T^r
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 }  \\
1514 <  \circ \varphi _{\Delta t/2,\tau }  \circ \varphi _{\Delta t/2,F}  .\\
1515 < \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
1434   mimics a simple heat bath with stochastic and dissipative forces,
1435   has been applied in a variety of studies. This section will review
1436 < the theory of Langevin dynamics. A brief derivation of generalized
1436 > the theory of Langevin dynamics. A brief derivation of the generalized
1437   Langevin equation will be given first. Following that, we will
1438 < discuss the physical meaning of the terms appearing in the equation
1526 < as well as the calculation of friction tensor from hydrodynamics
1527 < theory.
1438 > discuss the physical meaning of the terms appearing in the equation.
1439  
1440   \subsection{\label{introSection:generalizedLangevinDynamics}Derivation of Generalized Langevin Equation}
1441  
# Line 1533 | Line 1444 | Harmonic bath model is the derivation of the Generaliz
1444   environment, has been widely used in quantum chemistry and
1445   statistical mechanics. One of the successful applications of
1446   Harmonic bath model is the derivation of the Generalized Langevin
1447 < Dynamics (GLE). Lets consider a system, in which the degree of
1447 > Dynamics (GLE). Consider a system, in which the degree of
1448   freedom $x$ is assumed to couple to the bath linearly, giving a
1449   Hamiltonian of the form
1450   \begin{equation}
# Line 1544 | Line 1455 | H_B  = \sum\limits_{\alpha  = 1}^N {\left\{ {\frac{{p_
1455   with this degree of freedom, $H_B$ is a harmonic bath Hamiltonian,
1456   \[
1457   H_B  = \sum\limits_{\alpha  = 1}^N {\left\{ {\frac{{p_\alpha ^2
1458 < }}{{2m_\alpha  }} + \frac{1}{2}m_\alpha  \omega _\alpha ^2 }
1458 > }}{{2m_\alpha  }} + \frac{1}{2}m_\alpha  x_\alpha ^2 }
1459   \right\}}
1460   \]
1461   where the index $\alpha$ runs over all the bath degrees of freedom,
# Line 1560 | Line 1471 | W(x) = U(x) - \sum\limits_{\alpha  = 1}^N {\frac{{g_\a
1471   \[
1472   W(x) = U(x) - \sum\limits_{\alpha  = 1}^N {\frac{{g_\alpha ^2
1473   }}{{2m_\alpha  w_\alpha ^2 }}} x^2
1474 < \] and combining the last two terms in Equation
1475 < \ref{introEquation:bathGLE}, we may rewrite the Harmonic bath
1565 < Hamiltonian as
1474 > \]
1475 > and combining the last two terms in Eq.~\ref{introEquation:bathGLE}, we may rewrite the Harmonic bath Hamiltonian as
1476   \[
1477   H = \frac{{p^2 }}{{2m}} + W(x) + \sum\limits_{\alpha  = 1}^N
1478   {\left\{ {\frac{{p_\alpha ^2 }}{{2m_\alpha  }} + \frac{1}{2}m_\alpha
1479   w_\alpha ^2 \left( {x_\alpha   - \frac{{g_\alpha  }}{{m_\alpha
1480 < w_\alpha ^2 }}x} \right)^2 } \right\}}
1480 > w_\alpha ^2 }}x} \right)^2 } \right\}}.
1481   \]
1482   Since the first two terms of the new Hamiltonian depend only on the
1483   system coordinates, we can get the equations of motion for
# Line 1584 | Line 1494 | m\ddot x_\alpha   =  - m_\alpha  w_\alpha ^2 \left( {x
1494   \frac{{g_\alpha  }}{{m_\alpha  w_\alpha ^2 }}x} \right).
1495   \label{introEquation:bathMotionGLE}
1496   \end{equation}
1587
1497   In order to derive an equation for $x$, the dynamics of the bath
1498   variables $x_\alpha$ must be solved exactly first. As an integral
1499   transform which is particularly useful in solving linear ordinary
1500   differential equations,the Laplace transform is the appropriate tool
1501   to solve this problem. The basic idea is to transform the difficult
1502   differential equations into simple algebra problems which can be
1503 < solved easily. Then, by applying the inverse Laplace transform, also
1504 < known as the Bromwich integral, we can retrieve the solutions of the
1505 < original problems.
1506 <
1598 < Let $f(t)$ be a function defined on $ [0,\infty ) $. The Laplace
1599 < transform of f(t) is a new function defined as
1503 > solved easily. Then, by applying the inverse Laplace transform, we
1504 > can retrieve the solutions of the original problems. Let $f(t)$ be a
1505 > function defined on $ [0,\infty ) $, the Laplace transform of $f(t)$
1506 > is a new function defined as
1507   \[
1508   L(f(t)) \equiv F(p) = \int_0^\infty  {f(t)e^{ - pt} dt}
1509   \]
1510   where  $p$ is real and  $L$ is called the Laplace Transform
1511 < Operator. Below are some important properties of Laplace transform
1605 <
1511 > Operator. Below are some important properties of the Laplace transform
1512   \begin{eqnarray*}
1513   L(x + y)  & = & L(x) + L(y) \\
1514   L(ax)     & = & aL(x) \\
# Line 1610 | Line 1516 | Operator. Below are some important properties of Lapla
1516   L(\ddot x)& = & p^2 L(x) - px(0) - \dot x(0) \\
1517   L\left( {\int_0^t {g(t - \tau )h(\tau )d\tau } } \right)& = & G(p)H(p) \\
1518   \end{eqnarray*}
1613
1614
1519   Applying the Laplace transform to the bath coordinates, we obtain
1520   \begin{eqnarray*}
1521 < 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) \\
1522 < L(x_\alpha  ) & = & \frac{{\frac{{g_\alpha  }}{{\omega _\alpha  }}L(x) + px_\alpha  (0) + \dot x_\alpha  (0)}}{{p^2  + \omega _\alpha ^2 }} \\
1521 > 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), \\
1522 > L(x_\alpha  ) & = & \frac{{\frac{{g_\alpha  }}{{\omega _\alpha  }}L(x) + px_\alpha  (0) + \dot x_\alpha  (0)}}{{p^2  + \omega _\alpha ^2 }}. \\
1523   \end{eqnarray*}
1524 <
1621 < By the same way, the system coordinates become
1524 > In the same way, the system coordinates become
1525   \begin{eqnarray*}
1526 < mL(\ddot x) & = & - \frac{1}{p}\frac{{\partial W(x)}}{{\partial x}} \\
1527 <  & & \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\}}  \\
1526 > mL(\ddot x) & = &
1527 >  - \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 >  & & - \frac{1}{p}\frac{{\partial W(x)}}{{\partial x}}.
1529   \end{eqnarray*}
1626
1530   With the help of some relatively important inverse Laplace
1531   transformations:
1532   \[
# Line 1633 | Line 1536 | transformations:
1536   L(1) = \frac{1}{p} \\
1537   \end{array}
1538   \]
1539 < , we obtain
1539 > we obtain
1540   \begin{eqnarray*}
1541   m\ddot x & =  & - \frac{{\partial W(x)}}{{\partial x}} -
1542   \sum\limits_{\alpha  = 1}^N {\left\{ {\left( { - \frac{{g_\alpha ^2
# Line 1642 | Line 1545 | x_\alpha (0) - \frac{{g_\alpha  }}{{m_\alpha  \omega _
1545   & & + \sum\limits_{\alpha  = 1}^N {\left\{ {\left[ {g_\alpha
1546   x_\alpha (0) - \frac{{g_\alpha  }}{{m_\alpha  \omega _\alpha  }}}
1547   \right]\cos (\omega _\alpha  t) + \frac{{g_\alpha  \dot x_\alpha
1548 < (0)}}{{\omega _\alpha  }}\sin (\omega _\alpha  t)} \right\}}
1549 < \end{eqnarray*}
1550 < \begin{eqnarray*}
1551 < m\ddot x & = & - \frac{{\partial W(x)}}{{\partial x}} - \int_0^t
1552 < {\sum\limits_{\alpha  = 1}^N {\left( { - \frac{{g_\alpha ^2
1553 < }}{{m_\alpha  \omega _\alpha ^2 }}} \right)\cos (\omega _\alpha
1548 > (0)}}{{\omega _\alpha  }}\sin (\omega _\alpha  t)} \right\}}\\
1549 > %
1550 > & = & -
1551 > \frac{{\partial W(x)}}{{\partial x}} - \int_0^t {\sum\limits_{\alpha
1552 > = 1}^N {\left( { - \frac{{g_\alpha ^2 }}{{m_\alpha  \omega _\alpha
1553 > ^2 }}} \right)\cos (\omega _\alpha
1554   t)\dot x(t - \tau )d} \tau }  \\
1555   & & + \sum\limits_{\alpha  = 1}^N {\left\{ {\left[ {g_\alpha
1556   x_\alpha (0) - \frac{{g_\alpha }}{{m_\alpha \omega _\alpha  }}}
# Line 1674 | Line 1577 | m\ddot x =  - \frac{{\partial W}}{{\partial x}} - \int
1577   (t)\dot x(t - \tau )d\tau }  + R(t)
1578   \label{introEuqation:GeneralizedLangevinDynamics}
1579   \end{equation}
1580 < which is known as the \emph{generalized Langevin equation}.
1580 > which is known as the \emph{generalized Langevin equation} (GLE).
1581  
1582   \subsubsection{\label{introSection:randomForceDynamicFrictionKernel}\textbf{Random Force and Dynamic Friction Kernel}}
1583  
1584   One may notice that $R(t)$ depends only on initial conditions, which
1585   implies it is completely deterministic within the context of a
1586   harmonic bath. However, it is easy to verify that $R(t)$ is totally
1587 < uncorrelated to $x$ and $\dot x$,
1588 < \[
1589 < \begin{array}{l}
1590 < \left\langle {x(t)R(t)} \right\rangle  = 0, \\
1688 < \left\langle {\dot x(t)R(t)} \right\rangle  = 0. \\
1689 < \end{array}
1690 < \]
1691 < This property is what we expect from a truly random process. As long
1692 < as the model chosen for $R(t)$ was a gaussian distribution in
1587 > uncorrelated to $x$ and $\dot x$, $\left\langle {x(t)R(t)}
1588 > \right\rangle  = 0, \left\langle {\dot x(t)R(t)} \right\rangle  =
1589 > 0.$ This property is what we expect from a truly random process. As
1590 > long as the model chosen for $R(t)$ was a gaussian distribution in
1591   general, the stochastic nature of the GLE still remains.
1694
1592   %dynamic friction kernel
1593   The convolution integral
1594   \[
# Line 1706 | Line 1603 | $\xi(t) = \Xi_0$. Hence, the convolution integral beco
1603   \[
1604   \int_0^t {\xi (t)\dot x(t - \tau )d\tau }  = \xi _0 (x(t) - x(0))
1605   \]
1606 < and Equation \ref{introEuqation:GeneralizedLangevinDynamics} becomes
1606 > and Eq.~\ref{introEuqation:GeneralizedLangevinDynamics} becomes
1607   \[
1608   m\ddot x =  - \frac{\partial }{{\partial x}}\left( {W(x) +
1609   \frac{1}{2}\xi _0 (x - x_0 )^2 } \right) + R(t),
# Line 1716 | Line 1613 | taken as a $delta$ function in time:
1613   infinitely quickly to motions in the system. Thus, $\xi (t)$ can be
1614   taken as a $delta$ function in time:
1615   \[
1616 < \xi (t) = 2\xi _0 \delta (t)
1616 > \xi (t) = 2\xi _0 \delta (t).
1617   \]
1618   Hence, the convolution integral becomes
1619   \[
1620   \int_0^t {\xi (t)\dot x(t - \tau )d\tau }  = 2\xi _0 \int_0^t
1621   {\delta (t)\dot x(t - \tau )d\tau }  = \xi _0 \dot x(t),
1622   \]
1623 < and Equation \ref{introEuqation:GeneralizedLangevinDynamics} becomes
1623 > and Eq.~\ref{introEuqation:GeneralizedLangevinDynamics} becomes the
1624 > Langevin equation
1625   \begin{equation}
1626   m\ddot x =  - \frac{{\partial W(x)}}{{\partial x}} - \xi _0 \dot
1627 < x(t) + R(t) \label{introEquation:LangevinEquation}
1627 > x(t) + R(t) \label{introEquation:LangevinEquation}.
1628   \end{equation}
1629 < which is known as the Langevin equation. The static friction
1630 < coefficient $\xi _0$ can either be calculated from spectral density
1631 < or be determined by Stokes' law for regular shaped particles. A
1632 < briefly review on calculating friction tensor for arbitrary shaped
1633 < particles is given in Sec.~\ref{introSection:frictionTensor}.
1629 > The static friction coefficient $\xi _0$ can either be calculated
1630 > from spectral density or be determined by Stokes' law for regular
1631 > shaped particles. A brief review on calculating friction tensors for
1632 > arbitrary shaped particles is given in
1633 > Sec.~\ref{introSection:frictionTensor}.
1634  
1635   \subsubsection{\label{introSection:secondFluctuationDissipation}\textbf{The Second Fluctuation Dissipation Theorem}}
1636  
1637 < Defining a new set of coordinates,
1637 > Defining a new set of coordinates
1638   \[
1639   q_\alpha  (t) = x_\alpha  (t) - \frac{1}{{m_\alpha  \omega _\alpha
1640 < ^2 }}x(0)
1641 < \],
1642 < we can rewrite $R(T)$ as
1640 > ^2 }}x(0),
1641 > \]
1642 > we can rewrite $R(t)$ as
1643   \[
1644   R(t) = \sum\limits_{\alpha  = 1}^N {g_\alpha  q_\alpha  (t)}.
1645   \]
1646   And since the $q$ coordinates are harmonic oscillators,
1749
1647   \begin{eqnarray*}
1648   \left\langle {q_\alpha ^2 } \right\rangle  & = & \frac{{kT}}{{m_\alpha  \omega _\alpha ^2 }} \\
1649   \left\langle {q_\alpha  (t)q_\alpha  (0)} \right\rangle & = & \left\langle {q_\alpha ^2 (0)} \right\rangle \cos (\omega _\alpha  t) \\
1650   \left\langle {q_\alpha  (t)q_\beta  (0)} \right\rangle & = &\delta _{\alpha \beta } \left\langle {q_\alpha  (t)q_\alpha  (0)} \right\rangle  \\
1651   \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 } }  \\
1652    & = &\sum\limits_\alpha  {g_\alpha ^2 \left\langle {q_\alpha ^2 (0)} \right\rangle \cos (\omega _\alpha  t)}  \\
1653 <  & = &kT\xi (t) \\
1653 >  & = &kT\xi (t)
1654   \end{eqnarray*}
1758
1655   Thus, we recover the \emph{second fluctuation dissipation theorem}
1656   \begin{equation}
1657   \xi (t) = \left\langle {R(t)R(0)} \right\rangle
1658 < \label{introEquation:secondFluctuationDissipation}.
1658 > \label{introEquation:secondFluctuationDissipation},
1659   \end{equation}
1660 < In effect, it acts as a constraint on the possible ways in which one
1661 < can model the random force and friction kernel.
1660 > which acts as a constraint on the possible ways in which one can
1661 > model the random force and friction kernel.

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