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# Line 3 | Line 3 | Closely related to Classical Mechanics, Molecular Dyna
3   \section{\label{introSection:classicalMechanics}Classical
4   Mechanics}
5  
6 < Closely related to Classical Mechanics, Molecular Dynamics
7 < simulations are carried out by integrating the equations of motion
8 < for a given system of particles. There are three fundamental ideas
9 < behind classical mechanics. Firstly, one can determine the state of
10 < a mechanical system at any time of interest; Secondly, all the
11 < mechanical properties of the system at that time can be determined
12 < by combining the knowledge of the properties of the system with the
13 < specification of this state; Finally, the specification of the state
14 < when further combine with the laws of mechanics will also be
15 < sufficient to predict the future behavior of the system.
6 > Using equations of motion derived from Classical Mechanics,
7 > Molecular Dynamics simulations are carried out by integrating the
8 > equations of motion for a given system of particles. There are three
9 > fundamental ideas behind classical mechanics. Firstly, one can
10 > determine the state of a mechanical system at any time of interest;
11 > Secondly, all the mechanical properties of the system at that time
12 > can be determined by combining the knowledge of the properties of
13 > the system with the specification of this state; Finally, the
14 > specification of the state when further combined with the laws of
15 > mechanics will also be sufficient to predict the future behavior of
16 > the system.
17  
18   \subsection{\label{introSection:newtonian}Newtonian Mechanics}
19   The discovery of Newton's three laws of mechanics which govern the
# Line 31 | Line 32 | F_{ij} = -F_{ji}
32   $F_{ji}$ be the force that particle $j$ exerts on particle $i$.
33   Newton's third law states that
34   \begin{equation}
35 < F_{ij} = -F_{ji}
35 > F_{ij} = -F_{ji}.
36   \label{introEquation:newtonThirdLaw}
37   \end{equation}
37
38   Conservation laws of Newtonian Mechanics play very important roles
39   in solving mechanics problems. The linear momentum of a particle is
40   conserved if it is free or it experiences no force. The second
# Line 63 | Line 63 | that if all forces are conservative, Energy
63   \end{equation}
64   If there are no external torques acting on a body, the angular
65   momentum of it is conserved. The last conservation theorem state
66 < that if all forces are conservative, Energy
67 < \begin{equation}E = T + V \label{introEquation:energyConservation}
66 > that if all forces are conservative, energy is conserved,
67 > \begin{equation}E = T + V. \label{introEquation:energyConservation}
68   \end{equation}
69 < is conserved. All of these conserved quantities are
70 < important factors to determine the quality of numerical integration
71 < schemes for rigid bodies \cite{Dullweber1997}.
69 > All of these conserved quantities are important factors to determine
70 > the quality of numerical integration schemes for rigid
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 | $L$ is the Lagrangian function for the system.
143   \label{introEquation:hamiltonianDefByLagrangian}
144   \end{equation}
145   where $ \dot q_1  \ldots \dot q_f $ are generalized velocities and
146 < $L$ is the Lagrangian function for the system.
147 <
151 < Differentiating Eq.~\ref{introEquation:hamiltonianDefByLagrangian},
152 < one can obtain
146 > $L$ is the Lagrangian function for the system. Differentiating
147 > Eq.~\ref{introEquation:hamiltonianDefByLagrangian}, one can obtain
148   \begin{equation}
149   dH = \sum\limits_k {\left( {p_k d\dot q_k  + \dot q_k dp_k  -
150   \frac{{\partial L}}{{\partial q_k }}dq_k  - \frac{{\partial
151   L}}{{\partial \dot q_k }}d\dot q_k } \right)}  - \frac{{\partial
152 < L}}{{\partial t}}dt \label{introEquation:diffHamiltonian1}
152 > L}}{{\partial t}}dt . \label{introEquation:diffHamiltonian1}
153   \end{equation}
154 < Making use of  Eq.~\ref{introEquation:generalizedMomenta}, the
155 < second and fourth terms in the parentheses cancel. Therefore,
154 > Making use of Eq.~\ref{introEquation:generalizedMomenta}, the second
155 > and fourth terms in the parentheses cancel. Therefore,
156   Eq.~\ref{introEquation:diffHamiltonian1} can be rewritten as
157   \begin{equation}
158   dH = \sum\limits_k {\left( {\dot q_k dp_k  - \dot p_k dq_k }
159 < \right)}  - \frac{{\partial L}}{{\partial t}}dt
159 > \right)}  - \frac{{\partial L}}{{\partial t}}dt .
160   \label{introEquation:diffHamiltonian2}
161   \end{equation}
162   By identifying the coefficients of $dq_k$, $dp_k$ and dt, we can
# Line 180 | Line 175 | t}}
175   t}}
176   \label{introEquation:motionHamiltonianTime}
177   \end{equation}
178 <
184 < Eq.~\ref{introEquation:motionHamiltonianCoordinate} and
178 > where Eq.~\ref{introEquation:motionHamiltonianCoordinate} and
179   Eq.~\ref{introEquation:motionHamiltonianMomentum} are Hamilton's
180   equation of motion. Due to their symmetrical formula, they are also
181 < known as the canonical equations of motions \cite{Goldstein2001}.
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 | only works with 1st-order differential equations\cite{
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 | Statistical Mechanics concepts and theorem presented i
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, $x = (\rightarrow
224 < q_1 , \ldots ,\rightarrow q_f ,\rightarrow p_1 , \ldots ,\rightarrow
225 < p_f )$, with a unique set of values of $6f$ coordinates and momenta
226 < is a phase space vector.
217 > possible states of a system. Each possible state of the system
218 > corresponds to one unique point in the phase space. For mechanical
219 > systems, the phase space usually consists of all possible values of
220 > position and momentum variables. Consider a dynamic system of $f$
221 > particles in a cartesian space, where each of the $6f$ coordinates
222 > and momenta is assigned to one of $6f$ mutually orthogonal axes, the
223 > phase space of this system is a $6f$ dimensional space. A point, $x
224 > =
225 > (\mathord{\buildrel{\lower3pt\hbox{$\scriptscriptstyle\rightharpoonup$}}
226 > \over q} _1 , \ldots
227 > ,\mathord{\buildrel{\lower3pt\hbox{$\scriptscriptstyle\rightharpoonup$}}
228 > \over q} _f
229 > ,\mathord{\buildrel{\lower3pt\hbox{$\scriptscriptstyle\rightharpoonup$}}
230 > \over p} _1  \ldots
231 > ,\mathord{\buildrel{\lower3pt\hbox{$\scriptscriptstyle\rightharpoonup$}}
232 > \over p} _f )$ , with a unique set of values of $6f$ coordinates and
233 > momenta is a phase space vector.
234   %%%fix me
235  
236   In statistical mechanics, the condition of an ensemble at any time
# Line 243 | Line 243 | their locations which would change the density at any
243   \label{introEquation:densityDistribution}
244   \end{equation}
245   Governed by the principles of mechanics, the phase points change
246 < their locations which would change the density at any time at phase
246 > their locations which changes the density at any time at phase
247   space. Hence, the density distribution is also to be taken as a
248 < function of the time.
249 <
250 < The number of systems $\delta N$ at time $t$ can be determined by,
248 > function of the time. The number of systems $\delta N$ at time $t$
249 > can be determined by,
250   \begin{equation}
251   \delta N = \rho (q,p,t)dq_1  \ldots dq_f dp_1  \ldots dp_f.
252   \label{introEquation:deltaN}
253   \end{equation}
254 < Assuming a large enough population of systems, we can sufficiently
254 > Assuming enough copies of the systems, we can sufficiently
255   approximate $\delta N$ without introducing discontinuity when we go
256   from one region in the phase space to another. By integrating over
257   the whole phase space,
# Line 260 | Line 259 | gives us an expression for the total number of the sys
259   N = \int { \ldots \int {\rho (q,p,t)dq_1 } ...dq_f dp_1 } ...dp_f
260   \label{introEquation:totalNumberSystem}
261   \end{equation}
262 < gives us an expression for the total number of the systems. Hence,
263 < the probability per unit in the phase space can be obtained by,
262 > gives us an expression for the total number of copies. Hence, the
263 > probability per unit volume in the phase space can be obtained by,
264   \begin{equation}
265   \frac{{\rho (q,p,t)}}{N} = \frac{{\rho (q,p,t)}}{{\int { \ldots \int
266   {\rho (q,p,t)dq_1 } ...dq_f dp_1 } ...dp_f }}.
# Line 270 | Line 269 | momenta of the system. Even when the dynamics of the r
269   With the help of Eq.~\ref{introEquation:unitProbability} and the
270   knowledge of the system, it is possible to calculate the average
271   value of any desired quantity which depends on the coordinates and
272 < momenta of the system. Even when the dynamics of the real system is
272 > momenta of the system. Even when the dynamics of the real system are
273   complex, or stochastic, or even discontinuous, the average
274 < properties of the ensemble of possibilities as a whole remaining
275 < well defined. For a classical system in thermal equilibrium with its
274 > properties of the ensemble of possibilities as a whole remain well
275 > defined. For a classical system in thermal equilibrium with its
276   environment, the ensemble average of a mechanical quantity, $\langle
277   A(q , p) \rangle_t$, takes the form of an integral over the phase
278   space of the system,
279   \begin{equation}
280   \langle  A(q , p) \rangle_t = \frac{{\int { \ldots \int {A(q,p)\rho
281   (q,p,t)dq_1 } ...dq_f dp_1 } ...dp_f }}{{\int { \ldots \int {\rho
282 < (q,p,t)dq_1 } ...dq_f dp_1 } ...dp_f }}
282 > (q,p,t)dq_1 } ...dq_f dp_1 } ...dp_f }}.
283   \label{introEquation:ensembelAverage}
284   \end{equation}
285  
287 There are several different types of ensembles with different
288 statistical characteristics. As a function of macroscopic
289 parameters, such as temperature \textit{etc}, the partition function
290 can be used to describe the statistical properties of a system in
291 thermodynamic equilibrium.
292
293 As an ensemble of systems, each of which is known to be thermally
294 isolated and conserve energy, the Microcanonical ensemble (NVE) has
295 a partition function like,
296 \begin{equation}
297 \Omega (N,V,E) = e^{\beta TS} \label{introEquation:NVEPartition}.
298 \end{equation}
299 A canonical ensemble (NVT)is an ensemble of systems, each of which
300 can share its energy with a large heat reservoir. The distribution
301 of the total energy amongst the possible dynamical states is given
302 by the partition function,
303 \begin{equation}
304 \Omega (N,V,T) = e^{ - \beta A}
305 \label{introEquation:NVTPartition}
306 \end{equation}
307 Here, $A$ is the Helmholtz free energy which is defined as $ A = U -
308 TS$. Since most experiments are carried out under constant pressure
309 condition, the isothermal-isobaric ensemble (NPT) plays a very
310 important role in molecular simulations. The isothermal-isobaric
311 ensemble allow the system to exchange energy with a heat bath of
312 temperature $T$ and to change the volume as well. Its partition
313 function is given as
314 \begin{equation}
315 \Delta (N,P,T) =  - e^{\beta G}.
316 \label{introEquation:NPTPartition}
317 \end{equation}
318 Here, $G = U - TS + PV$, and $G$ is called Gibbs free energy.
319
286   \subsection{\label{introSection:liouville}Liouville's theorem}
287  
288   Liouville's theorem is the foundation on which statistical mechanics
# Line 358 | Line 324 | simple form,
324   \frac{{\partial \rho }}{{\partial p_i }}\dot p_i } \right)}  = 0 .
325   \label{introEquation:liouvilleTheorem}
326   \end{equation}
361
327   Liouville's theorem states that the distribution function is
328   constant along any trajectory in phase space. In classical
329 < statistical mechanics, since the number of members in an ensemble is
330 < huge and constant, we can assume the local density has no reason
331 < (other than classical mechanics) to change,
329 > statistical mechanics, since the number of system copies in an
330 > ensemble is huge and constant, we can assume the local density has
331 > no reason (other than classical mechanics) to change,
332   \begin{equation}
333   \frac{{\partial \rho }}{{\partial t}} = 0.
334   \label{introEquation:stationary}
# Line 393 | Line 358 | With the help of stationary assumption
358   \frac{{d(\delta N)}}{{dt}} = \frac{{d\rho }}{{dt}}\delta v + \rho
359   \frac{d}{{dt}}(\delta v) = 0.
360   \end{equation}
361 < With the help of stationary assumption
362 < (\ref{introEquation:stationary}), we obtain the principle of the
361 > With the help of the stationary assumption
362 > (Eq.~\ref{introEquation:stationary}), we obtain the principle of
363   \emph{conservation of volume in phase space},
364   \begin{equation}
365   \frac{d}{{dt}}(\delta v) = \frac{d}{{dt}}\int { \ldots \int {dq_1 }
# Line 404 | Line 369 | Liouville's theorem can be expresses in a variety of d
369  
370   \subsubsection{\label{introSection:liouvilleInOtherForms}\textbf{Liouville's Theorem in Other Forms}}
371  
372 < Liouville's theorem can be expresses in a variety of different forms
372 > Liouville's theorem can be expressed in a variety of different forms
373   which are convenient within different contexts. For any two function
374   $F$ and $G$ of the coordinates and momenta of a system, the Poisson
375 < bracket ${F, G}$ is defined as
375 > bracket $\{F,G\}$ is defined as
376   \begin{equation}
377   \left\{ {F,G} \right\} = \sum\limits_i {\left( {\frac{{\partial
378   F}}{{\partial q_i }}\frac{{\partial G}}{{\partial p_i }} -
# Line 415 | Line 380 | Substituting equations of motion in Hamiltonian formal
380   q_i }}} \right)}.
381   \label{introEquation:poissonBracket}
382   \end{equation}
383 < Substituting equations of motion in Hamiltonian formalism(
384 < Eq.~\ref{introEquation:motionHamiltonianCoordinate} ,
385 < Eq.~\ref{introEquation:motionHamiltonianMomentum} ) into
383 > Substituting equations of motion in Hamiltonian formalism
384 > (Eq.~\ref{introEquation:motionHamiltonianCoordinate} ,
385 > Eq.~\ref{introEquation:motionHamiltonianMomentum}) into
386   (Eq.~\ref{introEquation:liouvilleTheorem}), we can rewrite
387   Liouville's theorem using Poisson bracket notion,
388   \begin{equation}
# Line 438 | Line 403 | expressed as
403   \left( {\frac{{\partial \rho }}{{\partial t}}} \right) =  - iL\rho
404   \label{introEquation:liouvilleTheoremInOperator}
405   \end{equation}
406 <
406 > which can help define a propagator $\rho (t) = e^{-iLt} \rho (0)$.
407   \subsection{\label{introSection:ergodic}The Ergodic Hypothesis}
408  
409   Various thermodynamic properties can be calculated from Molecular
# Line 447 | Line 412 | period of them which is different from the average beh
412   simulation and the quality of the underlying model. However, both
413   experiments and computer simulations are usually performed during a
414   certain time interval and the measurements are averaged over a
415 < period of them which is different from the average behavior of
415 > period of time which is different from the average behavior of
416   many-body system in Statistical Mechanics. Fortunately, the Ergodic
417   Hypothesis makes a connection between time average and the ensemble
418   average. It states that the time average and average over the
419 < statistical ensemble are identical \cite{Frenkel1996, Leach2001}.
419 > statistical ensemble are identical:\cite{Frenkel1996, Leach2001}
420   \begin{equation}
421   \langle A(q , p) \rangle_t = \mathop {\lim }\limits_{t \to \infty }
422   \frac{1}{t}\int\limits_0^t {A(q(t),p(t))dt = \int\limits_\Gamma
# Line 460 | Line 425 | sufficiently long time (longer than relaxation time),
425   where $\langle  A(q , p) \rangle_t$ is an equilibrium value of a
426   physical quantity and $\rho (p(t), q(t))$ is the equilibrium
427   distribution function. If an observation is averaged over a
428 < sufficiently long time (longer than relaxation time), all accessible
429 < microstates in phase space are assumed to be equally probed, giving
430 < a properly weighted statistical average. This allows the researcher
431 < freedom of choice when deciding how best to measure a given
432 < observable. In case an ensemble averaged approach sounds most
433 < reasonable, the Monte Carlo techniques\cite{Metropolis1949} can be
428 > sufficiently long time (longer than the relaxation time), all
429 > accessible microstates in phase space are assumed to be equally
430 > probed, giving a properly weighted statistical average. This allows
431 > the researcher freedom of choice when deciding how best to measure a
432 > given observable. In case an ensemble averaged approach sounds most
433 > reasonable, the Monte Carlo methods\cite{Metropolis1949} can be
434   utilized. Or if the system lends itself to a time averaging
435   approach, the Molecular Dynamics techniques in
436   Sec.~\ref{introSection:molecularDynamics} will be the best
437 < choice\cite{Frenkel1996}.
437 > choice.\cite{Frenkel1996}
438  
439   \section{\label{introSection:geometricIntegratos}Geometric Integrators}
440   A variety of numerical integrators have been proposed to simulate
441   the motions of atoms in MD simulation. They usually begin with
442 < initial conditionals and move the objects in the direction governed
443 < by the differential equations. However, most of them ignore the
444 < hidden physical laws contained within the equations. Since 1990,
445 < geometric integrators, which preserve various phase-flow invariants
446 < such as symplectic structure, volume and time reversal symmetry, are
447 < developed to address this issue\cite{Dullweber1997, McLachlan1998,
448 < Leimkuhler1999}. The velocity Verlet method, which happens to be a
442 > initial conditions and move the objects in the direction governed by
443 > the differential equations. However, most of them ignore the hidden
444 > physical laws contained within the equations. Since 1990, geometric
445 > integrators, which preserve various phase-flow invariants such as
446 > symplectic structure, volume and time reversal symmetry, were
447 > developed to address this issue.\cite{Dullweber1997, McLachlan1998,
448 > Leimkuhler1999} The velocity Verlet method, which happens to be a
449   simple example of symplectic integrator, continues to gain
450   popularity in the molecular dynamics community. This fact can be
451   partly explained by its geometric nature.
452  
453 < \subsection{\label{introSection:symplecticManifold}Symplectic Manifolds}
453 > \subsection{\label{introSection:symplecticManifold}Manifolds and Bundles}
454   A \emph{manifold} is an abstract mathematical space. It looks
455   locally like Euclidean space, but when viewed globally, it may have
456   more complicated structure. A good example of manifold is the
457   surface of Earth. It seems to be flat locally, but it is round if
458   viewed as a whole. A \emph{differentiable manifold} (also known as
459   \emph{smooth manifold}) is a manifold on which it is possible to
460 < apply calculus on \emph{differentiable manifold}. A \emph{symplectic
461 < manifold} is defined as a pair $(M, \omega)$ which consists of a
462 < \emph{differentiable manifold} $M$ and a close, non-degenerated,
460 > apply calculus.\cite{Hirsch1997} A \emph{symplectic manifold} is
461 > defined as a pair $(M, \omega)$ which consists of a
462 > \emph{differentiable manifold} $M$ and a close, non-degenerate,
463   bilinear symplectic form, $\omega$. A symplectic form on a vector
464   space $V$ is a function $\omega(x, y)$ which satisfies
465   $\omega(\lambda_1x_1+\lambda_2x_2, y) = \lambda_1\omega(x_1, y)+
466   \lambda_2\omega(x_2, y)$, $\omega(x, y) = - \omega(y, x)$ and
467 < $\omega(x, x) = 0$. The cross product operation in vector field is
468 < an example of symplectic form.
467 > $\omega(x, x) = 0$.\cite{McDuff1998} The cross product operation in
468 > vector field is an example of symplectic form.
469 > Given vector spaces $V$ and $W$ over same field $F$, $f: V \to W$ is a linear transformation if
470 > \begin{eqnarray*}
471 > f(x+y) & = & f(x) + f(y) \\
472 > f(ax) & = & af(x)      
473 > \end{eqnarray*}
474 > 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:
475 > \begin{eqnarray*}
476 > (\phi+\psi)(x) & = & \phi(x)+\psi(x) \\
477 > (a\phi)(x) & = & a \phi(x)
478 > \end{eqnarray*}
479 > 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 $q$
480 > \begin{equation}
481 > \dot q = \mathop {\lim }\limits_{t \to 0} \frac{{\phi (t) - \phi (0)}}{t}      
482 > \end{equation}
483 > 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.
484 > 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 $(q,p)$.
485  
505 One of the motivations to study \emph{symplectic manifolds} in
506 Hamiltonian Mechanics is that a symplectic manifold can represent
507 all possible configurations of the system and the phase space of the
508 system can be described by it's cotangent bundle. Every symplectic
509 manifold is even dimensional. For instance, in Hamilton equations,
510 coordinate and momentum always appear in pairs.
511
486   \subsection{\label{introSection:ODE}Ordinary Differential Equations}
487  
488   For an ordinary differential system defined as
489   \begin{equation}
490   \dot x = f(x)
491   \end{equation}
492 < where $x = x(q,p)^T$, this system is a canonical Hamiltonian, if
492 > where $x = x(q,p)$, this system is a canonical Hamiltonian, if
493 > $f(x) = J\nabla _x H(x)$. Here, $H = H (q, p)$ is Hamiltonian
494 > function and $J$ is the skew-symmetric matrix
495   \begin{equation}
520 f(r) = J\nabla _x H(r).
521 \end{equation}
522 $H = H (q, p)$ is Hamiltonian function and $J$ is the skew-symmetric
523 matrix
524 \begin{equation}
496   J = \left( {\begin{array}{*{20}c}
497     0 & I  \\
498     { - I} & 0  \\
# Line 531 | Line 502 | system can be rewritten as,
502   where $I$ is an identity matrix. Using this notation, Hamiltonian
503   system can be rewritten as,
504   \begin{equation}
505 < \frac{d}{{dt}}x = J\nabla _x H(x)
505 > \frac{d}{{dt}}x = J\nabla _x H(x).
506   \label{introEquation:compactHamiltonian}
507   \end{equation}In this case, $f$ is
508 < called a \emph{Hamiltonian vector field}.
509 <
539 < Another generalization of Hamiltonian dynamics is Poisson
540 < Dynamics\cite{Olver1986},
508 > called a \emph{Hamiltonian vector field}. Another generalization of
509 > Hamiltonian dynamics is Poisson Dynamics,\cite{Olver1986}
510   \begin{equation}
511   \dot x = J(x)\nabla _x H \label{introEquation:poissonHamiltonian}
512   \end{equation}
513 < The most obvious change being that matrix $J$ now depends on $x$.
513 > where the most obvious change being that matrix $J$ now depends on
514 > $x$.
515  
516 < \subsection{\label{introSection:exactFlow}Exact Flow}
516 > \subsection{\label{introSection:exactFlow}Exact Propagator}
517  
518 < Let $x(t)$ be the exact solution of the ODE system,
518 > Let $x(t)$ be the exact solution of the ODE
519 > system,
520   \begin{equation}
521 < \frac{{dx}}{{dt}} = f(x) \label{introEquation:ODE}
522 < \end{equation}
523 < The exact flow(solution) $\varphi_\tau$ is defined by
524 < \[
525 < x(t+\tau) =\varphi_\tau(x(t))
521 > \frac{{dx}}{{dt}} = f(x), \label{introEquation:ODE}
522 > \end{equation} we can
523 > define its exact propagator $\varphi_\tau$:
524 > \[ x(t+\tau)
525 > =\varphi_\tau(x(t))
526   \]
527   where $\tau$ is a fixed time step and $\varphi$ is a map from phase
528 < space to itself. The flow has the continuous group property,
528 > space to itself. The propagator has the continuous group property,
529   \begin{equation}
530   \varphi _{\tau _1 }  \circ \varphi _{\tau _2 }  = \varphi _{\tau _1
531   + \tau _2 } .
# Line 563 | Line 534 | Therefore, the exact flow is self-adjoint,
534   \begin{equation}
535   \varphi _\tau   \circ \varphi _{ - \tau }  = I
536   \end{equation}
537 < Therefore, the exact flow is self-adjoint,
537 > Therefore, the exact propagator is self-adjoint,
538   \begin{equation}
539   \varphi _\tau   = \varphi _{ - \tau }^{ - 1}.
540   \end{equation}
541 < The exact flow can also be written in terms of the of an operator,
541 > In most cases, it is not easy to find the exact propagator
542 > $\varphi_\tau$. Instead, we use an approximate map, $\psi_\tau$,
543 > which is usually called an integrator. The order of an integrator
544 > $\psi_\tau$ is $p$, if the Taylor series of $\psi_\tau$ agree to
545 > order $p$,
546   \begin{equation}
572 \varphi _\tau  (x) = e^{\tau \sum\limits_i {f_i (x)\frac{\partial
573 }{{\partial x_i }}} } (x) \equiv \exp (\tau f)(x).
574 \label{introEquation:exponentialOperator}
575 \end{equation}
576
577 In most cases, it is not easy to find the exact flow $\varphi_\tau$.
578 Instead, we use an approximate map, $\psi_\tau$, which is usually
579 called integrator. The order of an integrator $\psi_\tau$ is $p$, if
580 the Taylor series of $\psi_\tau$ agree to order $p$,
581 \begin{equation}
547   \psi_\tau(x) = x + \tau f(x) + O(\tau^{p+1})
548   \end{equation}
549  
550   \subsection{\label{introSection:geometricProperties}Geometric Properties}
551  
552   The hidden geometric properties\cite{Budd1999, Marsden1998} of an
553 < ODE and its flow play important roles in numerical studies. Many of
554 < them can be found in systems which occur naturally in applications.
555 <
556 < Let $\varphi$ be the flow of Hamiltonian vector field, $\varphi$ is
592 < a \emph{symplectic} flow if it satisfies,
553 > ODE and its propagator play important roles in numerical studies.
554 > Many of them can be found in systems which occur naturally in
555 > applications. Let $\varphi$ be the propagator of Hamiltonian vector
556 > field, $\varphi$ is a \emph{symplectic} propagator if it satisfies,
557   \begin{equation}
558   {\varphi '}^T J \varphi ' = J.
559   \end{equation}
560   According to Liouville's theorem, the symplectic volume is invariant
561 < under a Hamiltonian flow, which is the basis for classical
562 < statistical mechanics. Furthermore, the flow of a Hamiltonian vector
563 < field on a symplectic manifold can be shown to be a
561 > under a Hamiltonian propagator, which is the basis for classical
562 > statistical mechanics. Furthermore, the propagator of a Hamiltonian
563 > vector field on a symplectic manifold can be shown to be a
564   symplectomorphism. As to the Poisson system,
565   \begin{equation}
566   {\varphi '}^T J \varphi ' = J \circ \varphi
567   \end{equation}
568 < is the property that must be preserved by the integrator.
569 <
570 < It is possible to construct a \emph{volume-preserving} flow for a
571 < source free ODE ($ \nabla \cdot f = 0 $), if the flow satisfies $
572 < \det d\varphi  = 1$. One can show easily that a symplectic flow will
573 < be volume-preserving.
574 <
611 < Changing the variables $y = h(x)$ in an ODE
612 < (Eq.~\ref{introEquation:ODE}) will result in a new system,
568 > is the property that must be preserved by the integrator. It is
569 > possible to construct a \emph{volume-preserving} propagator for a
570 > source free ODE ($ \nabla \cdot f = 0 $), if the propagator
571 > satisfies $ \det d\varphi  = 1$. One can show easily that a
572 > symplectic propagator will be volume-preserving. Changing the
573 > variables $y = h(x)$ in an ODE (Eq.~\ref{introEquation:ODE}) will
574 > result in a new system,
575   \[
576   \dot y = \tilde f(y) = ((dh \cdot f)h^{ - 1} )(y).
577   \]
578   The vector filed $f$ has reversing symmetry $h$ if $f = - \tilde f$.
579 < In other words, the flow of this vector field is reversible if and
580 < only if $ h \circ \varphi ^{ - 1}  = \varphi  \circ h $.
581 <
582 < A \emph{first integral}, or conserved quantity of a general
583 < differential function is a function $ G:R^{2d}  \to R^d $ which is
622 < constant for all solutions of the ODE $\frac{{dx}}{{dt}} = f(x)$ ,
579 > In other words, the propagator of this vector field is reversible if
580 > and only if $ h \circ \varphi ^{ - 1}  = \varphi  \circ h $. A
581 > conserved quantity of a general differential function is a function
582 > $ G:R^{2d}  \to R^d $ which is constant for all solutions of the ODE
583 > $\frac{{dx}}{{dt}} = f(x)$ ,
584   \[
585   \frac{{dG(x(t))}}{{dt}} = 0.
586   \]
587 < Using chain rule, one may obtain,
587 > Using the chain rule, one may obtain,
588   \[
589 < \sum\limits_i {\frac{{dG}}{{dx_i }}} f_i (x) = f \bullet \nabla G,
589 > \sum\limits_i {\frac{{dG}}{{dx_i }}} f_i (x) = f \cdot \nabla G,
590   \]
591 < which is the condition for conserving \emph{first integral}. For a
592 < canonical Hamiltonian system, the time evolution of an arbitrary
593 < smooth function $G$ is given by,
633 <
591 > which is the condition for conserved quantities. For a canonical
592 > Hamiltonian system, the time evolution of an arbitrary smooth
593 > function $G$ is given by,
594   \begin{eqnarray}
595 < \frac{{dG(x(t))}}{{dt}} & = & [\nabla _x G(x(t))]^T \dot x(t) \\
596 <                        & = & [\nabla _x G(x(t))]^T J\nabla _x H(x(t)). \\
595 > \frac{{dG(x(t))}}{{dt}} & = & [\nabla _x G(x(t))]^T \dot x(t) \notag\\
596 >                        & = & [\nabla _x G(x(t))]^T J\nabla _x H(x(t)).
597   \label{introEquation:firstIntegral1}
598   \end{eqnarray}
599 <
600 <
641 < Using poisson bracket notion, Equation
642 < \ref{introEquation:firstIntegral1} can be rewritten as
599 > Using poisson bracket notion, Eq.~\ref{introEquation:firstIntegral1}
600 > can be rewritten as
601   \[
602   \frac{d}{{dt}}G(x(t)) = \left\{ {G,H} \right\}(x(t)).
603   \]
604 < Therefore, the sufficient condition for $G$ to be the \emph{first
605 < integral} of a Hamiltonian system is
606 < \[
607 < \left\{ {G,H} \right\} = 0.
650 < \]
651 < As well known, the Hamiltonian (or energy) H of a Hamiltonian system
652 < is a \emph{first integral}, which is due to the fact $\{ H,H\}  =
653 < 0$.
654 <
604 > Therefore, the sufficient condition for $G$ to be a conserved
605 > quantity of a Hamiltonian system is $\left\{ {G,H} \right\} = 0.$ As
606 > is well known, the Hamiltonian (or energy) H of a Hamiltonian system
607 > is a conserved quantity, which is due to the fact $\{ H,H\}  = 0$.
608   When designing any numerical methods, one should always try to
609 < preserve the structural properties of the original ODE and its flow.
609 > preserve the structural properties of the original ODE and its
610 > propagator.
611  
612   \subsection{\label{introSection:constructionSymplectic}Construction of Symplectic Methods}
613   A lot of well established and very effective numerical methods have
614 < been successful precisely because of their symplecticities even
614 > been successful precisely because of their symplectic nature even
615   though this fact was not recognized when they were first
616   constructed. The most famous example is the Verlet-leapfrog method
617   in molecular dynamics. In general, symplectic integrators can be
# Line 668 | Line 622 | constructed using one of four different methods.
622   \item Runge-Kutta methods
623   \item Splitting methods
624   \end{enumerate}
625 <
672 < Generating function\cite{Channell1990} tends to lead to methods
625 > Generating functions\cite{Channell1990} tend to lead to methods
626   which are cumbersome and difficult to use. In dissipative systems,
627   variational methods can capture the decay of energy
628 < accurately\cite{Kane2000}. Since their geometrically unstable nature
628 > accurately.\cite{Kane2000} Since they are geometrically unstable
629   against non-Hamiltonian perturbations, ordinary implicit Runge-Kutta
630 < methods are not suitable for Hamiltonian system. Recently, various
631 < high-order explicit Runge-Kutta methods
632 < \cite{Owren1992,Chen2003}have been developed to overcome this
633 < instability. However, due to computational penalty involved in
634 < implementing the Runge-Kutta methods, they have not attracted much
635 < attention from the Molecular Dynamics community. Instead, splitting
636 < methods have been widely accepted since they exploit natural
637 < decompositions of the system\cite{Tuckerman1992, McLachlan1998}.
630 > methods are not suitable for Hamiltonian
631 > system.\cite{Cartwright1992} Recently, various high-order explicit
632 > Runge-Kutta methods \cite{Owren1992,Chen2003} have been developed to
633 > overcome this instability. However, due to computational penalty
634 > involved in implementing the Runge-Kutta methods, they have not
635 > attracted much attention from the Molecular Dynamics community.
636 > Instead, splitting methods have been widely accepted since they
637 > exploit natural decompositions of the system.\cite{McLachlan1998,
638 > Tuckerman1992}
639  
640   \subsubsection{\label{introSection:splittingMethod}\textbf{Splitting Methods}}
641  
642   The main idea behind splitting methods is to decompose the discrete
643 < $\varphi_h$ as a composition of simpler flows,
643 > $\varphi_h$ as a composition of simpler propagators,
644   \begin{equation}
645   \varphi _h  = \varphi _{h_1 }  \circ \varphi _{h_2 }  \ldots  \circ
646   \varphi _{h_n }
647   \label{introEquation:FlowDecomposition}
648   \end{equation}
649 < where each of the sub-flow is chosen such that each represent a
650 < simpler integration of the system.
651 <
698 < Suppose that a Hamiltonian system takes the form,
649 > where each of the sub-propagator is chosen such that each represent
650 > a simpler integration of the system. Suppose that a Hamiltonian
651 > system takes the form,
652   \[
653   H = H_1 + H_2.
654   \]
655   Here, $H_1$ and $H_2$ may represent different physical processes of
656   the system. For instance, they may relate to kinetic and potential
657   energy respectively, which is a natural decomposition of the
658 < problem. If $H_1$ and $H_2$ can be integrated using exact flows
659 < $\varphi_1(t)$ and $\varphi_2(t)$, respectively, a simple first
660 < order expression is then given by the Lie-Trotter formula
658 > problem. If $H_1$ and $H_2$ can be integrated using exact
659 > propagators $\varphi_1(t)$ and $\varphi_2(t)$, respectively, a
660 > simple first order expression is then given by the Lie-Trotter
661 > formula\cite{Trotter1959}
662   \begin{equation}
663   \varphi _h  = \varphi _{1,h}  \circ \varphi _{2,h},
664   \label{introEquation:firstOrderSplitting}
# Line 713 | Line 667 | It is easy to show that any composition of symplectic
667   continuous $\varphi _i$ over a time $h$. By definition, as
668   $\varphi_i(t)$ is the exact solution of a Hamiltonian system, it
669   must follow that each operator $\varphi_i(t)$ is a symplectic map.
670 < It is easy to show that any composition of symplectic flows yields a
671 < symplectic map,
670 > It is easy to show that any composition of symplectic propagators
671 > yields a symplectic map,
672   \begin{equation}
673   (\varphi '\phi ')^T J\varphi '\phi ' = \phi '^T \varphi '^T J\varphi
674   '\phi ' = \phi '^T J\phi ' = J,
# Line 722 | Line 676 | splitting in this context automatically generates a sy
676   \end{equation}
677   where $\phi$ and $\psi$ both are symplectic maps. Thus operator
678   splitting in this context automatically generates a symplectic map.
679 <
680 < The Lie-Trotter splitting(\ref{introEquation:firstOrderSplitting})
681 < introduces local errors proportional to $h^2$, while Strang
682 < splitting gives a second-order decomposition,
679 > The Lie-Trotter
680 > splitting(Eq.~\ref{introEquation:firstOrderSplitting}) introduces
681 > local errors proportional to $h^2$, while the Strang splitting gives
682 > a second-order decomposition,\cite{Strang1968}
683   \begin{equation}
684   \varphi _h  = \varphi _{1,h/2}  \circ \varphi _{2,h}  \circ \varphi
685   _{1,h/2} , \label{introEquation:secondOrderSplitting}
686   \end{equation}
687 < which has a local error proportional to $h^3$. The Sprang
687 > which has a local error proportional to $h^3$. The Strang
688   splitting's popularity in molecular simulation community attribute
689   to its symmetric property,
690   \begin{equation}
# Line 758 | Line 712 | symplectic(\ref{introEquation:SymplecticFlowCompositio
712   \end{align}
713   where $F(t)$ is the force at time $t$. This integration scheme is
714   known as \emph{velocity verlet} which is
715 < symplectic(\ref{introEquation:SymplecticFlowComposition}),
716 < time-reversible(\ref{introEquation:timeReversible}) and
717 < volume-preserving (\ref{introEquation:volumePreserving}). These
715 > symplectic(Eq.~\ref{introEquation:SymplecticFlowComposition}),
716 > time-reversible(Eq.~\ref{introEquation:timeReversible}) and
717 > volume-preserving (Eq.~\ref{introEquation:volumePreserving}). These
718   geometric properties attribute to its long-time stability and its
719   popularity in the community. However, the most commonly used
720   velocity verlet integration scheme is written as below,
# Line 781 | Line 735 | the equations of motion would follow:
735  
736   \item Use the half step velocities to move positions one whole step, $\Delta t$.
737  
738 < \item Evaluate the forces at the new positions, $\mathbf{q}(\Delta t)$, and use the new forces to complete the velocity move.
738 > \item Evaluate the forces at the new positions, $q(\Delta t)$, and use the new forces to complete the velocity move.
739  
740   \item Repeat from step 1 with the new position, velocities, and forces assuming the roles of the initial values.
741   \end{enumerate}
788
742   By simply switching the order of the propagators in the splitting
743   and composing a new integrator, the \emph{position verlet}
744   integrator, can be generated,
# Line 801 | Line 754 | The Baker-Campbell-Hausdorff formula can be used to de
754  
755   \subsubsection{\label{introSection:errorAnalysis}\textbf{Error Analysis and Higher Order Methods}}
756  
757 < The Baker-Campbell-Hausdorff formula can be used to determine the
758 < local error of splitting method in terms of the commutator of the
759 < operators(\ref{introEquation:exponentialOperator}) associated with
760 < the sub-flow. For operators $hX$ and $hY$ which are associated with
761 < $\varphi_1(t)$ and $\varphi_2(t)$ respectively , we have
757 > The Baker-Campbell-Hausdorff formula\cite{Gilmore1974} can be used
758 > to determine the local error of a splitting method in terms of the
759 > commutator of the
760 > operators(Eq.~\ref{introEquation:exponentialOperator}) associated
761 > with the sub-propagator. For operators $hX$ and $hY$ which are
762 > associated with $\varphi_1(t)$ and $\varphi_2(t)$ respectively , we
763 > have
764   \begin{equation}
765   \exp (hX + hY) = \exp (hZ)
766   \end{equation}
# Line 814 | Line 769 | Here, $[X,Y]$ is the commutators of operator $X$ and $
769   hZ = hX + hY + \frac{{h^2 }}{2}[X,Y] + \frac{{h^3 }}{2}\left(
770   {[X,[X,Y]] + [Y,[Y,X]]} \right) +  \ldots .
771   \end{equation}
772 < Here, $[X,Y]$ is the commutators of operator $X$ and $Y$ given by
772 > Here, $[X,Y]$ is the commutator of operator $X$ and $Y$ given by
773   \[
774   [X,Y] = XY - YX .
775   \]
776   Applying the Baker-Campbell-Hausdorff formula\cite{Varadarajan1974}
777 < to the Sprang splitting, we can obtain
777 > to the Strang splitting, we can obtain
778   \begin{eqnarray*}
779   \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 \\
780                                     &   & \mbox{} + h^2 [X,X]/8 + h^2 [Y,Y]/8 \\
781 <                                   &   & \mbox{} + h^3 [Y,[Y,X]]/12 - h^3[X,[X,Y]]/24 + \ldots )
781 >                                   &   & \mbox{} + h^3 [Y,[Y,X]]/12 - h^3[X,[X,Y]]/24 + \ldots
782 >                                   ).
783   \end{eqnarray*}
784 < Since \[ [X,Y] + [Y,X] = 0\] and \[ [X,X] = 0,\] the dominant local
785 < error of Spring splitting is proportional to $h^3$. The same
786 < procedure can be applied to a general splitting,  of the form
784 > Since $ [X,Y] + [Y,X] = 0$ and $ [X,X] = 0$, the dominant local
785 > error of Strang splitting is proportional to $h^3$. The same
786 > procedure can be applied to a general splitting of the form
787   \begin{equation}
788   \varphi _{b_m h}^2  \circ \varphi _{a_m h}^1  \circ \varphi _{b_{m -
789   1} h}^2  \circ  \ldots  \circ \varphi _{a_1 h}^1 .
790   \end{equation}
791   A careful choice of coefficient $a_1 \ldots b_m$ will lead to higher
792   order methods. Yoshida proposed an elegant way to compose higher
793 < order methods based on symmetric splitting\cite{Yoshida1990}. Given
793 > order methods based on symmetric splitting.\cite{Yoshida1990} Given
794   a symmetric second order base method $ \varphi _h^{(2)} $, a
795   fourth-order symmetric method can be constructed by composing,
796   \[
# Line 862 | Line 818 | simulations. For instance, instantaneous temperature o
818   dynamical information. The basic idea of molecular dynamics is that
819   macroscopic properties are related to microscopic behavior and
820   microscopic behavior can be calculated from the trajectories in
821 < simulations. For instance, instantaneous temperature of an
822 < Hamiltonian system of $N$ particle can be measured by
821 > simulations. For instance, instantaneous temperature of a
822 > Hamiltonian system of $N$ particles can be measured by
823   \[
824   T = \sum\limits_{i = 1}^N {\frac{{m_i v_i^2 }}{{fk_B }}}
825   \]
826   where $m_i$ and $v_i$ are the mass and velocity of $i$th particle
827   respectively, $f$ is the number of degrees of freedom, and $k_B$ is
828 < the boltzman constant.
828 > the Boltzman constant.
829  
830   A typical molecular dynamics run consists of three essential steps:
831   \begin{enumerate}
# Line 886 | Line 842 | will discusse issues in production run.
842   These three individual steps will be covered in the following
843   sections. Sec.~\ref{introSec:initialSystemSettings} deals with the
844   initialization of a simulation. Sec.~\ref{introSection:production}
845 < will discusse issues in production run.
845 > discusses issues of production runs.
846   Sec.~\ref{introSection:Analysis} provides the theoretical tools for
847 < trajectory analysis.
847 > analysis of trajectories.
848  
849   \subsection{\label{introSec:initialSystemSettings}Initialization}
850  
# Line 900 | Line 856 | structure, some important information is missing. For
856   thousands of crystal structures of molecules are discovered every
857   year, many more remain unknown due to the difficulties of
858   purification and crystallization. Even for molecules with known
859 < structure, some important information is missing. For example, a
859 > structures, some important information is missing. For example, a
860   missing hydrogen atom which acts as donor in hydrogen bonding must
861 < be added. Moreover, in order to include electrostatic interaction,
861 > be added. Moreover, in order to include electrostatic interactions,
862   one may need to specify the partial charges for individual atoms.
863   Under some circumstances, we may even need to prepare the system in
864   a special configuration. For instance, when studying transport
# Line 920 | Line 876 | near the minimum, steepest descent method is extremely
876   minimization to find a more reasonable conformation. Several energy
877   minimization methods have been developed to exploit the energy
878   surface and to locate the local minimum. While converging slowly
879 < near the minimum, steepest descent method is extremely robust when
879 > near the minimum, the steepest descent method is extremely robust when
880   systems are strongly anharmonic. Thus, it is often used to refine
881 < structure from crystallographic data. Relied on the gradient or
882 < hessian, advanced methods like Newton-Raphson converge rapidly to a
883 < local minimum, but become unstable if the energy surface is far from
881 > structures from crystallographic data. Relying on the Hessian,
882 > advanced methods like Newton-Raphson converge rapidly to a local
883 > minimum, but become unstable if the energy surface is far from
884   quadratic. Another factor that must be taken into account, when
885   choosing energy minimization method, is the size of the system.
886   Steepest descent and conjugate gradient can deal with models of any
887   size. Because of the limits on computer memory to store the hessian
888 < matrix and the computing power needed to diagonalized these
889 < matrices, most Newton-Raphson methods can not be used with very
934 < large systems.
888 > matrix and the computing power needed to diagonalize these matrices,
889 > most Newton-Raphson methods can not be used with very large systems.
890  
891   \subsubsection{\textbf{Heating}}
892  
893 < Typically, Heating is performed by assigning random velocities
893 > Typically, heating is performed by assigning random velocities
894   according to a Maxwell-Boltzman distribution for a desired
895   temperature. Beginning at a lower temperature and gradually
896   increasing the temperature by assigning larger random velocities, we
897 < end up with setting the temperature of the system to a final
898 < temperature at which the simulation will be conducted. In heating
899 < phase, we should also keep the system from drifting or rotating as a
900 < whole. To do this, the net linear momentum and angular momentum of
901 < the system is shifted to zero after each resampling from the Maxwell
902 < -Boltzman distribution.
897 > end up setting the temperature of the system to a final temperature
898 > at which the simulation will be conducted. In the heating phase, we
899 > should also keep the system from drifting or rotating as a whole. To
900 > do this, the net linear momentum and angular momentum of the system
901 > is shifted to zero after each resampling from the Maxwell -Boltzman
902 > distribution.
903  
904   \subsubsection{\textbf{Equilibration}}
905  
# Line 955 | Line 910 | as a means to arrive at an equilibrated structure in a
910   properties \textit{etc}, become independent of time. Strictly
911   speaking, minimization and heating are not necessary, provided the
912   equilibration process is long enough. However, these steps can serve
913 < as a means to arrive at an equilibrated structure in an effective
913 > as a mean to arrive at an equilibrated structure in an effective
914   way.
915  
916   \subsection{\label{introSection:production}Production}
# Line 971 | Line 926 | which making large simulations prohibitive in the abse
926   calculation of non-bonded forces, such as van der Waals force and
927   Coulombic forces \textit{etc}. For a system of $N$ particles, the
928   complexity of the algorithm for pair-wise interactions is $O(N^2 )$,
929 < which making large simulations prohibitive in the absence of any
930 < algorithmic tricks.
931 <
932 < A natural approach to avoid system size issues is to represent the
933 < bulk behavior by a finite number of the particles. However, this
934 < approach will suffer from the surface effect at the edges of the
935 < simulation. To offset this, \textit{Periodic boundary conditions}
936 < (see Fig.~\ref{introFig:pbc}) is developed to simulate bulk
937 < properties with a relatively small number of particles. In this
938 < method, the simulation box is replicated throughout space to form an
939 < infinite lattice. During the simulation, when a particle moves in
940 < the primary cell, its image in other cells move in exactly the same
941 < direction with exactly the same orientation. Thus, as a particle
987 < leaves the primary cell, one of its images will enter through the
988 < opposite face.
929 > which makes large simulations prohibitive in the absence of any
930 > algorithmic tricks. A natural approach to avoid system size issues
931 > is to represent the bulk behavior by a finite number of the
932 > particles. However, this approach will suffer from surface effects
933 > at the edges of the simulation. To offset this, \textit{Periodic
934 > boundary conditions} (see Fig.~\ref{introFig:pbc}) were developed to
935 > simulate bulk properties with a relatively small number of
936 > particles. In this method, the simulation box is replicated
937 > throughout space to form an infinite lattice. During the simulation,
938 > when a particle moves in the primary cell, its image in other cells
939 > move in exactly the same direction with exactly the same
940 > orientation. Thus, as a particle leaves the primary cell, one of its
941 > images will enter through the opposite face.
942   \begin{figure}
943   \centering
944   \includegraphics[width=\linewidth]{pbc.eps}
# Line 997 | Line 950 | evaluation is to apply spherical cutoff where particle
950  
951   %cutoff and minimum image convention
952   Another important technique to improve the efficiency of force
953 < evaluation is to apply spherical cutoff where particles farther than
954 < a predetermined distance are not included in the calculation
955 < \cite{Frenkel1996}. The use of a cutoff radius will cause a
956 < discontinuity in the potential energy curve. Fortunately, one can
957 < shift simple radial potential to ensure the potential curve go
953 > evaluation is to apply spherical cutoffs where particles farther
954 > than a predetermined distance are not included in the
955 > calculation.\cite{Frenkel1996} The use of a cutoff radius will cause
956 > a discontinuity in the potential energy curve. Fortunately, one can
957 > shift a simple radial potential to ensure the potential curve go
958   smoothly to zero at the cutoff radius. The cutoff strategy works
959   well for Lennard-Jones interaction because of its short range
960   nature. However, simply truncating the electrostatic interaction
# Line 1009 | Line 962 | periodicity artifacts in liquid simulations. Taking th
962   in simulations. The Ewald summation, in which the slowly decaying
963   Coulomb potential is transformed into direct and reciprocal sums
964   with rapid and absolute convergence, has proved to minimize the
965 < periodicity artifacts in liquid simulations. Taking the advantages
966 < of the fast Fourier transform (FFT) for calculating discrete Fourier
967 < transforms, the particle mesh-based
965 > periodicity artifacts in liquid simulations. Taking advantage of
966 > fast Fourier transform (FFT) techniques for calculating discrete
967 > Fourier transforms, the particle mesh-based
968   methods\cite{Hockney1981,Shimada1993, Luty1994} are accelerated from
969   $O(N^{3/2})$ to $O(N logN)$. An alternative approach is the
970   \emph{fast multipole method}\cite{Greengard1987, Greengard1994},
# Line 1021 | Line 974 | his coworkers\cite{Wolf1999}. The shifted Coulomb pote
974   simulation community, these two methods are difficult to implement
975   correctly and efficiently. Instead, we use a damped and
976   charge-neutralized Coulomb potential method developed by Wolf and
977 < his coworkers\cite{Wolf1999}. The shifted Coulomb potential for
977 > his coworkers.\cite{Wolf1999} The shifted Coulomb potential for
978   particle $i$ and particle $j$ at distance $r_{rj}$ is given by:
979   \begin{equation}
980   V(r_{ij})= \frac{q_i q_j \textrm{erfc}(\alpha
981   r_{ij})}{r_{ij}}-\lim_{r_{ij}\rightarrow
982   R_\textrm{c}}\left\{\frac{q_iq_j \textrm{erfc}(\alpha
983 < r_{ij})}{r_{ij}}\right\}. \label{introEquation:shiftedCoulomb}
983 > r_{ij})}{r_{ij}}\right\}, \label{introEquation:shiftedCoulomb}
984   \end{equation}
985   where $\alpha$ is the convergence parameter. Due to the lack of
986   inherent periodicity and rapid convergence,this method is extremely
# Line 1044 | Line 997 | Recently, advanced visualization technique have become
997  
998   \subsection{\label{introSection:Analysis} Analysis}
999  
1000 < Recently, advanced visualization technique have become applied to
1000 > Recently, advanced visualization techniques have been applied to
1001   monitor the motions of molecules. Although the dynamics of the
1002   system can be described qualitatively from animation, quantitative
1003 < trajectory analysis are more useful. According to the principles of
1004 < Statistical Mechanics, Sec.~\ref{introSection:statisticalMechanics},
1005 < one can compute thermodynamic properties, analyze fluctuations of
1006 < structural parameters, and investigate time-dependent processes of
1007 < the molecule from the trajectories.
1003 > trajectory analysis is more useful. According to the principles of
1004 > Statistical Mechanics in
1005 > Sec.~\ref{introSection:statisticalMechanics}, one can compute
1006 > thermodynamic properties, analyze fluctuations of structural
1007 > parameters, and investigate time-dependent processes of the molecule
1008 > from the trajectories.
1009  
1010   \subsubsection{\label{introSection:thermodynamicsProperties}\textbf{Thermodynamic Properties}}
1011  
# Line 1081 | Line 1035 | Experimentally, pair distribution function can be gath
1035   distribution functions. Among these functions,the \emph{pair
1036   distribution function}, also known as \emph{radial distribution
1037   function}, is of most fundamental importance to liquid theory.
1038 < Experimentally, pair distribution function can be gathered by
1038 > Experimentally, pair distribution functions can be gathered by
1039   Fourier transforming raw data from a series of neutron diffraction
1040 < experiments and integrating over the surface factor
1041 < \cite{Powles1973}. The experimental results can serve as a criterion
1042 < to justify the correctness of a liquid model. Moreover, various
1043 < equilibrium thermodynamic and structural properties can also be
1044 < expressed in terms of radial distribution function \cite{Allen1987}.
1045 <
1046 < The pair distribution functions $g(r)$ gives the probability that a
1047 < particle $i$ will be located at a distance $r$ from a another
1048 < particle $j$ in the system
1095 < \[
1040 > experiments and integrating over the surface
1041 > factor.\cite{Powles1973} The experimental results can serve as a
1042 > criterion to justify the correctness of a liquid model. Moreover,
1043 > various equilibrium thermodynamic and structural properties can also
1044 > be expressed in terms of the radial distribution
1045 > function.\cite{Allen1987} The pair distribution functions $g(r)$
1046 > gives the probability that a particle $i$ will be located at a
1047 > distance $r$ from a another particle $j$ in the system
1048 > \begin{equation}
1049   g(r) = \frac{V}{{N^2 }}\left\langle {\sum\limits_i {\sum\limits_{j
1050   \ne i} {\delta (r - r_{ij} )} } } \right\rangle = \frac{\rho
1051   (r)}{\rho}.
1052 < \]
1052 > \end{equation}
1053   Note that the delta function can be replaced by a histogram in
1054   computer simulation. Peaks in $g(r)$ represent solvent shells, and
1055   the height of these peaks gradually decreases to 1 as the liquid of
# Line 1114 | Line 1067 | function is called an \emph{autocorrelation function}.
1067   \label{introEquation:timeCorrelationFunction}
1068   \end{equation}
1069   If $A$ and $B$ refer to same variable, this kind of correlation
1070 < function is called an \emph{autocorrelation function}. One example
1118 < of an auto correlation function is the velocity auto-correlation
1070 > functions are called \emph{autocorrelation functions}. One typical example is the velocity autocorrelation
1071   function which is directly related to transport properties of
1072   molecular liquids:
1073 < \[
1073 > \begin{equation}
1074   D = \frac{1}{3}\int\limits_0^\infty  {\left\langle {v(t) \cdot v(0)}
1075   \right\rangle } dt
1076 < \]
1076 > \end{equation}
1077   where $D$ is diffusion constant. Unlike the velocity autocorrelation
1078 < function, which is averaging over time origins and over all the
1079 < atoms, the dipole autocorrelation functions are calculated for the
1078 > function, which is averaged over time origins and over all the
1079 > atoms, the dipole autocorrelation functions is calculated for the
1080   entire system. The dipole autocorrelation function is given by:
1081 < \[
1081 > \begin{equation}
1082   c_{dipole}  = \left\langle {u_{tot} (t) \cdot u_{tot} (t)}
1083   \right\rangle
1084 < \]
1084 > \end{equation}
1085   Here $u_{tot}$ is the net dipole of the entire system and is given
1086   by
1087 < \[
1088 < u_{tot} (t) = \sum\limits_i {u_i (t)}
1089 < \]
1090 < In principle, many time correlation functions can be related with
1087 > \begin{equation}
1088 > u_{tot} (t) = \sum\limits_i {u_i (t)}.
1089 > \end{equation}
1090 > In principle, many time correlation functions can be related to
1091   Fourier transforms of the infrared, Raman, and inelastic neutron
1092   scattering spectra of molecular liquids. In practice, one can
1093 < extract the IR spectrum from the intensity of dipole fluctuation at
1094 < each frequency using the following relationship:
1095 < \[
1093 > extract the IR spectrum from the intensity of the molecular dipole
1094 > fluctuation at each frequency using the following relationship:
1095 > \begin{equation}
1096   \hat c_{dipole} (v) = \int_{ - \infty }^\infty  {c_{dipole} (t)e^{ -
1097 < i2\pi vt} dt}
1098 < \]
1097 > i2\pi vt} dt}.
1098 > \end{equation}
1099  
1100   \section{\label{introSection:rigidBody}Dynamics of Rigid Bodies}
1101  
1102   Rigid bodies are frequently involved in the modeling of different
1103 < areas, from engineering, physics, to chemistry. For example,
1104 < missiles and vehicle are usually modeled by rigid bodies.  The
1105 < movement of the objects in 3D gaming engine or other physics
1106 < simulator is governed by rigid body dynamics. In molecular
1103 > areas, including engineering, physics and chemistry. For example,
1104 > missiles and vehicles are usually modeled by rigid bodies.  The
1105 > movement of the objects in 3D gaming engines or other physics
1106 > simulators is governed by rigid body dynamics. In molecular
1107   simulations, rigid bodies are used to simplify protein-protein
1108 < docking studies\cite{Gray2003}.
1108 > docking studies.\cite{Gray2003}
1109  
1110   It is very important to develop stable and efficient methods to
1111   integrate the equations of motion for orientational degrees of
1112   freedom. Euler angles are the natural choice to describe the
1113   rotational degrees of freedom. However, due to $\frac {1}{sin
1114   \theta}$ singularities, the numerical integration of corresponding
1115 < equations of motion is very inefficient and inaccurate. Although an
1116 < alternative integrator using multiple sets of Euler angles can
1117 < overcome this difficulty\cite{Barojas1973}, the computational
1118 < penalty and the loss of angular momentum conservation still remain.
1119 < A singularity-free representation utilizing quaternions was
1120 < developed by Evans in 1977\cite{Evans1977}. Unfortunately, this
1121 < approach uses a nonseparable Hamiltonian resulting from the
1122 < quaternion representation, which prevents the symplectic algorithm
1123 < to be utilized. Another different approach is to apply holonomic
1124 < constraints to the atoms belonging to the rigid body. Each atom
1125 < moves independently under the normal forces deriving from potential
1126 < energy and constraint forces which are used to guarantee the
1127 < rigidness. However, due to their iterative nature, the SHAKE and
1128 < Rattle algorithms also converge very slowly when the number of
1129 < constraints increases\cite{Ryckaert1977, Andersen1983}.
1115 > equations of these motion is very inefficient and inaccurate.
1116 > Although an alternative integrator using multiple sets of Euler
1117 > angles can overcome this difficulty\cite{Barojas1973}, the
1118 > computational penalty and the loss of angular momentum conservation
1119 > still remain. A singularity-free representation utilizing
1120 > quaternions was developed by Evans in 1977.\cite{Evans1977}
1121 > Unfortunately, this approach used a nonseparable Hamiltonian
1122 > resulting from the quaternion representation, which prevented the
1123 > symplectic algorithm from being utilized. Another different approach
1124 > is to apply holonomic constraints to the atoms belonging to the
1125 > rigid body. Each atom moves independently under the normal forces
1126 > deriving from potential energy and constraint forces which are used
1127 > to guarantee the rigidness. However, due to their iterative nature,
1128 > the SHAKE and Rattle algorithms also converge very slowly when the
1129 > number of constraints increases.\cite{Ryckaert1977, Andersen1983}
1130  
1131   A break-through in geometric literature suggests that, in order to
1132   develop a long-term integration scheme, one should preserve the
1133 < symplectic structure of the flow. By introducing a conjugate
1133 > symplectic structure of the propagator. By introducing a conjugate
1134   momentum to the rotation matrix $Q$ and re-formulating Hamiltonian's
1135   equation, a symplectic integrator, RSHAKE\cite{Kol1997}, was
1136   proposed to evolve the Hamiltonian system in a constraint manifold
1137   by iteratively satisfying the orthogonality constraint $Q^T Q = 1$.
1138   An alternative method using the quaternion representation was
1139 < developed by Omelyan\cite{Omelyan1998}. However, both of these
1139 > developed by Omelyan.\cite{Omelyan1998} However, both of these
1140   methods are iterative and inefficient. In this section, we descibe a
1141 < symplectic Lie-Poisson integrator for rigid body developed by
1141 > symplectic Lie-Poisson integrator for rigid bodies developed by
1142   Dullweber and his coworkers\cite{Dullweber1997} in depth.
1143  
1144   \subsection{\label{introSection:constrainedHamiltonianRB}Constrained Hamiltonian for Rigid Bodies}
1145 < The motion of a rigid body is Hamiltonian with the Hamiltonian
1194 < function
1145 > The Hamiltonian of a rigid body is given by
1146   \begin{equation}
1147   H = \frac{1}{2}(p^T m^{ - 1} p) + \frac{1}{2}tr(PJ^{ - 1} P) +
1148   V(q,Q) + \frac{1}{2}tr[(QQ^T  - 1)\Lambda ].
1149   \label{introEquation:RBHamiltonian}
1150   \end{equation}
1151 < Here, $q$ and $Q$  are the position and rotation matrix for the
1152 < rigid-body, $p$ and $P$  are conjugate momenta to $q$  and $Q$ , and
1153 < $J$, a diagonal matrix, is defined by
1151 > Here, $q$ and $Q$  are the position vector and rotation matrix for
1152 > the rigid-body, $p$ and $P$  are conjugate momenta to $q$  and $Q$ ,
1153 > and $J$, a diagonal matrix, is defined by
1154   \[
1155   I_{ii}^{ - 1}  = \frac{1}{2}\sum\limits_{i \ne j} {J_{jj}^{ - 1} }
1156   \]
# Line 1209 | Line 1160 | which is used to ensure rotation matrix's unitarity. D
1160   \begin{equation}
1161   Q^T Q = 1, \label{introEquation:orthogonalConstraint}
1162   \end{equation}
1163 < which is used to ensure rotation matrix's unitarity. Differentiating
1164 < \ref{introEquation:orthogonalConstraint} and using Equation
1165 < \ref{introEquation:RBMotionMomentum}, one may obtain,
1215 < \begin{equation}
1216 < Q^T PJ^{ - 1}  + J^{ - 1} P^T Q = 0 . \\
1217 < \label{introEquation:RBFirstOrderConstraint}
1218 < \end{equation}
1219 <
1220 < Using Equation (\ref{introEquation:motionHamiltonianCoordinate},
1221 < \ref{introEquation:motionHamiltonianMomentum}), one can write down
1163 > which is used to ensure the rotation matrix's unitarity. Using
1164 > Eq.~\ref{introEquation:motionHamiltonianCoordinate} and Eq.~
1165 > \ref{introEquation:motionHamiltonianMomentum}, one can write down
1166   the equations of motion,
1223
1167   \begin{eqnarray}
1168 < \frac{{dq}}{{dt}} & = & \frac{p}{m} \label{introEquation:RBMotionPosition}\\
1169 < \frac{{dp}}{{dt}} & = & - \nabla _q V(q,Q) \label{introEquation:RBMotionMomentum}\\
1170 < \frac{{dQ}}{{dt}} & = & PJ^{ - 1}  \label{introEquation:RBMotionRotation}\\
1168 > \frac{{dq}}{{dt}} & = & \frac{p}{m}, \label{introEquation:RBMotionPosition}\\
1169 > \frac{{dp}}{{dt}} & = & - \nabla _q V(q,Q), \label{introEquation:RBMotionMomentum}\\
1170 > \frac{{dQ}}{{dt}} & = & PJ^{ - 1},  \label{introEquation:RBMotionRotation}\\
1171   \frac{{dP}}{{dt}} & = & - \nabla _Q V(q,Q) - 2Q\Lambda . \label{introEquation:RBMotionP}
1172   \end{eqnarray}
1173 <
1173 > Differentiating Eq.~\ref{introEquation:orthogonalConstraint} and
1174 > using Eq.~\ref{introEquation:RBMotionMomentum}, one may obtain,
1175 > \begin{equation}
1176 > Q^T PJ^{ - 1}  + J^{ - 1} P^T Q = 0 . \\
1177 > \label{introEquation:RBFirstOrderConstraint}
1178 > \end{equation}
1179   In general, there are two ways to satisfy the holonomic constraints.
1180   We can use a constraint force provided by a Lagrange multiplier on
1181 < the normal manifold to keep the motion on constraint space. Or we
1182 < can simply evolve the system on the constraint manifold. These two
1183 < methods have been proved to be equivalent. The holonomic constraint
1184 < and equations of motions define a constraint manifold for rigid
1185 < bodies
1181 > the normal manifold to keep the motion on the constraint space. Or
1182 > we can simply evolve the system on the constraint manifold. These
1183 > two methods have been proved to be equivalent. The holonomic
1184 > constraint and equations of motions define a constraint manifold for
1185 > rigid bodies
1186   \[
1187   M = \left\{ {(Q,P):Q^T Q = 1,Q^T PJ^{ - 1}  + J^{ - 1} P^T Q = 0}
1188   \right\}.
1189   \]
1190 <
1191 < Unfortunately, this constraint manifold is not the cotangent bundle
1192 < $T^* SO(3)$ which can be consider as a symplectic manifold on Lie
1193 < rotation group $SO(3)$. However, it turns out that under symplectic
1246 < transformation, the cotangent space and the phase space are
1247 < diffeomorphic. By introducing
1190 > Unfortunately, this constraint manifold is not $T^* SO(3)$ which is
1191 > a symplectic manifold on Lie rotation group $SO(3)$. However, it
1192 > turns out that under symplectic transformation, the cotangent space
1193 > and the phase space are diffeomorphic. By introducing
1194   \[
1195   \tilde Q = Q,\tilde P = \frac{1}{2}\left( {P - QP^T Q} \right),
1196   \]
1197 < the mechanical system subject to a holonomic constraint manifold $M$
1197 > the mechanical system subjected to a holonomic constraint manifold $M$
1198   can be re-formulated as a Hamiltonian system on the cotangent space
1199   \[
1200   T^* SO(3) = \left\{ {(\tilde Q,\tilde P):\tilde Q^T \tilde Q =
1201   1,\tilde Q^T \tilde PJ^{ - 1}  + J^{ - 1} P^T \tilde Q = 0} \right\}
1202   \]
1257
1203   For a body fixed vector $X_i$ with respect to the center of mass of
1204 < the rigid body, its corresponding lab fixed vector $X_0^{lab}$  is
1204 > the rigid body, its corresponding lab fixed vector $X_i^{lab}$  is
1205   given as
1206   \begin{equation}
1207   X_i^{lab} = Q X_i + q.
# Line 1273 | Line 1218 | respectively.
1218   \[
1219   \nabla _Q V(q,Q) = F(q,Q)X_i^t
1220   \]
1221 < respectively.
1222 <
1223 < As a common choice to describe the rotation dynamics of the rigid
1279 < body, the angular momentum on the body fixed frame $\Pi  = Q^t P$ is
1280 < introduced to rewrite the equations of motion,
1221 > respectively. As a common choice to describe the rotation dynamics
1222 > of the rigid body, the angular momentum on the body fixed frame $\Pi
1223 > = Q^t P$ is introduced to rewrite the equations of motion,
1224   \begin{equation}
1225   \begin{array}{l}
1226 < \dot \Pi  = J^{ - 1} \Pi ^T \Pi  + Q^T \sum\limits_i {F_i (q,Q)X_i^T }  - \Lambda  \\
1227 < \dot Q  = Q\Pi {\rm{ }}J^{ - 1}  \\
1226 > \dot \Pi  = J^{ - 1} \Pi ^T \Pi  + Q^T \sum\limits_i {F_i (q,Q)X_i^T }  - \Lambda,  \\
1227 > \dot Q  = Q\Pi {\rm{ }}J^{ - 1},  \\
1228   \end{array}
1229   \label{introEqaution:RBMotionPI}
1230   \end{equation}
1231 < , as well as holonomic constraints,
1232 < \[
1233 < \begin{array}{l}
1291 < \Pi J^{ - 1}  + J^{ - 1} \Pi ^t  = 0 \\
1292 < Q^T Q = 1 \\
1293 < \end{array}
1294 < \]
1295 <
1296 < For a vector $v(v_1 ,v_2 ,v_3 ) \in R^3$ and a matrix $\hat v \in
1297 < so(3)^ \star$, the hat-map isomorphism,
1231 > as well as holonomic constraints $\Pi J^{ - 1}  + J^{ - 1} \Pi ^t  =
1232 > 0$ and $Q^T Q = 1$. For a vector $v(v_1 ,v_2 ,v_3 ) \in R^3$ and a
1233 > matrix $\hat v \in so(3)^ \star$, the hat-map isomorphism,
1234   \begin{equation}
1235   v(v_1 ,v_2 ,v_3 ) \Leftrightarrow \hat v = \left(
1236   {\begin{array}{*{20}c}
# Line 1307 | Line 1243 | operations
1243   will let us associate the matrix products with traditional vector
1244   operations
1245   \[
1246 < \hat vu = v \times u
1246 > \hat vu = v \times u.
1247   \]
1248 < Using \ref{introEqaution:RBMotionPI}, one can construct a skew
1248 > Using Eq.~\ref{introEqaution:RBMotionPI}, one can construct a skew
1249   matrix,
1250 <
1251 < \begin{eqnarry*}
1252 < (\dot \Pi  - \dot \Pi ^T ){\rm{ }} = {\rm{ }}(\Pi  - \Pi ^T ){\rm{
1253 < }}(J^{ - 1} \Pi  + \Pi J^{ - 1} ) + \sum\limits_i {[Q^T F_i
1254 < (r,Q)X_i^T  - X_i F_i (r,Q)^T Q]}  - (\Lambda  - \Lambda ^T ).
1255 < \label{introEquation:skewMatrixPI}
1256 < \end{eqnarray*}
1257 <
1258 < Since $\Lambda$ is symmetric, the last term of Equation
1259 < \ref{introEquation:skewMatrixPI} is zero, which implies the Lagrange
1260 < multiplier $\Lambda$ is absent from the equations of motion. This
1261 < unique property eliminates the requirement of iterations which can
1326 < not be avoided in other methods\cite{Kol1997, Omelyan1998}.
1327 <
1328 < Applying the hat-map isomorphism, we obtain the equation of motion
1329 < for angular momentum on body frame
1250 > \begin{eqnarray}
1251 > (\dot \Pi  - \dot \Pi ^T )&= &(\Pi  - \Pi ^T )(J^{ - 1} \Pi  + \Pi J^{ - 1} ) \notag \\
1252 > & & + \sum\limits_i {[Q^T F_i (r,Q)X_i^T  - X_i F_i (r,Q)^T Q]}  -
1253 > (\Lambda  - \Lambda ^T ). \label{introEquation:skewMatrixPI}
1254 > \end{eqnarray}
1255 > Since $\Lambda$ is symmetric, the last term of
1256 > Eq.~\ref{introEquation:skewMatrixPI} is zero, which implies the
1257 > Lagrange multiplier $\Lambda$ is absent from the equations of
1258 > motion. This unique property eliminates the requirement of
1259 > iterations which can not be avoided in other methods.\cite{Kol1997,
1260 > Omelyan1998} Applying the hat-map isomorphism, we obtain the
1261 > equation of motion for angular momentum in the body frame
1262   \begin{equation}
1263   \dot \pi  = \pi  \times I^{ - 1} \pi  + \sum\limits_i {\left( {Q^T
1264   F_i (r,Q)} \right) \times X_i }.
# Line 1335 | Line 1267 | given by
1267   In the same manner, the equation of motion for rotation matrix is
1268   given by
1269   \[
1270 < \dot Q = Qskew(I^{ - 1} \pi )
1270 > \dot Q = Qskew(I^{ - 1} \pi ).
1271   \]
1272  
1273   \subsection{\label{introSection:SymplecticFreeRB}Symplectic
1274 < Lie-Poisson Integrator for Free Rigid Body}
1274 > Lie-Poisson Integrator for Free Rigid Bodies}
1275  
1276   If there are no external forces exerted on the rigid body, the only
1277   contribution to the rotational motion is from the kinetic energy
# Line 1357 | Line 1289 | J(\pi ) = \left( {\begin{array}{*{20}c}
1289     0 & {\pi _3 } & { - \pi _2 }  \\
1290     { - \pi _3 } & 0 & {\pi _1 }  \\
1291     {\pi _2 } & { - \pi _1 } & 0  \\
1292 < \end{array}} \right)
1292 > \end{array}} \right).
1293   \end{equation}
1294   Thus, the dynamics of free rigid body is governed by
1295   \begin{equation}
1296 < \frac{d}{{dt}}\pi  = J(\pi )\nabla _\pi  T^r (\pi )
1296 > \frac{d}{{dt}}\pi  = J(\pi )\nabla _\pi  T^r (\pi ).
1297   \end{equation}
1298 <
1299 < One may notice that each $T_i^r$ in Equation
1300 < \ref{introEquation:rotationalKineticRB} can be solved exactly. For
1369 < instance, the equations of motion due to $T_1^r$ are given by
1298 > One may notice that each $T_i^r$ in
1299 > Eq.~\ref{introEquation:rotationalKineticRB} can be solved exactly.
1300 > For instance, the equations of motion due to $T_1^r$ are given by
1301   \begin{equation}
1302   \frac{d}{{dt}}\pi  = R_1 \pi ,\frac{d}{{dt}}Q = QR_1
1303   \label{introEqaution:RBMotionSingleTerm}
1304   \end{equation}
1305 < where
1305 > with
1306   \[ R_1  = \left( {\begin{array}{*{20}c}
1307     0 & 0 & 0  \\
1308     0 & 0 & {\pi _1 }  \\
1309     0 & { - \pi _1 } & 0  \\
1310   \end{array}} \right).
1311   \]
1312 < The solutions of Equation \ref{introEqaution:RBMotionSingleTerm} is
1312 > The solutions of Eq.~\ref{introEqaution:RBMotionSingleTerm} is
1313   \[
1314   \pi (\Delta t) = e^{\Delta tR_1 } \pi (0),Q(\Delta t) =
1315   Q(0)e^{\Delta tR_1 }
# Line 1392 | Line 1323 | tR_1 }$, we can use Cayley transformation to obtain a
1323   \end{array}} \right),\theta _1  = \frac{{\pi _1 }}{{I_1 }}\Delta t.
1324   \]
1325   To reduce the cost of computing expensive functions in $e^{\Delta
1326 < tR_1 }$, we can use Cayley transformation to obtain a single-aixs
1327 < propagator,
1328 < \[
1329 < e^{\Delta tR_1 }  \approx (1 - \Delta tR_1 )^{ - 1} (1 + \Delta tR_1
1330 < )
1331 < \]
1332 < The flow maps for $T_2^r$ and $T_3^r$ can be found in the same
1326 > tR_1 }$, we can use the Cayley transformation to obtain a
1327 > single-aixs propagator,
1328 > \begin{eqnarray*}
1329 > e^{\Delta tR_1 }  & \approx & (1 - \Delta tR_1 )^{ - 1} (1 + \Delta
1330 > tR_1 ) \\
1331 > %
1332 > & \approx & \left( \begin{array}{ccc}
1333 > 1 & 0 & 0 \\
1334 > 0 & \frac{1-\theta^2 / 4}{1 + \theta^2 / 4}  & -\frac{\theta}{1+
1335 > \theta^2 / 4} \\
1336 > 0 & \frac{\theta}{1+ \theta^2 / 4} & \frac{1-\theta^2 / 4}{1 +
1337 > \theta^2 / 4}
1338 > \end{array}
1339 > \right).
1340 > \end{eqnarray*}
1341 > The propagators for $T_2^r$ and $T_3^r$ can be found in the same
1342   manner. In order to construct a second-order symplectic method, we
1343 < split the angular kinetic Hamiltonian function can into five terms
1343 > split the angular kinetic Hamiltonian function into five terms
1344   \[
1345   T^r (\pi ) = \frac{1}{2}T_1 ^r (\pi _1 ) + \frac{1}{2}T_2^r (\pi _2
1346   ) + T_3^r (\pi _3 ) + \frac{1}{2}T_2^r (\pi _2 ) + \frac{1}{2}T_1 ^r
# Line 1414 | Line 1354 | _1 }.
1354   \circ \varphi _{\Delta t/2,\pi _2 }  \circ \varphi _{\Delta t/2,\pi
1355   _1 }.
1356   \]
1357 <
1418 < The non-canonical Lie-Poisson bracket ${F, G}$ of two function
1419 < $F(\pi )$ and $G(\pi )$ is defined by
1357 > The non-canonical Lie-Poisson bracket $\{F, G\}$ of two functions $F(\pi )$ and $G(\pi )$ is defined by
1358   \[
1359   \{ F,G\} (\pi ) = [\nabla _\pi  F(\pi )]^T J(\pi )\nabla _\pi  G(\pi
1360 < )
1360 > ).
1361   \]
1362   If the Poisson bracket of a function $F$ with an arbitrary smooth
1363   function $G$ is zero, $F$ is a \emph{Casimir}, which is the
1364   conserved quantity in Poisson system. We can easily verify that the
1365   norm of the angular momentum, $\parallel \pi
1366 < \parallel$, is a \emph{Casimir}. Let$ F(\pi ) = S(\frac{{\parallel
1366 > \parallel$, is a \emph{Casimir}.\cite{McLachlan1993} Let $F(\pi ) = S(\frac{{\parallel
1367   \pi \parallel ^2 }}{2})$ for an arbitrary function $ S:R \to R$ ,
1368   then by the chain rule
1369   \[
1370   \nabla _\pi  F(\pi ) = S'(\frac{{\parallel \pi \parallel ^2
1371 < }}{2})\pi
1371 > }}{2})\pi.
1372   \]
1373 < Thus $ [\nabla _\pi  F(\pi )]^T J(\pi ) =  - S'(\frac{{\parallel \pi
1373 > Thus, $ [\nabla _\pi  F(\pi )]^T J(\pi ) =  - S'(\frac{{\parallel
1374 > \pi
1375   \parallel ^2 }}{2})\pi  \times \pi  = 0 $. This explicit
1376   Lie-Poisson integrator is found to be both extremely efficient and
1377   stable. These properties can be explained by the fact the small
# Line 1443 | Line 1382 | energy and potential energy,
1382   Splitting for Rigid Body}
1383  
1384   The Hamiltonian of rigid body can be separated in terms of kinetic
1385 < energy and potential energy,
1386 < \[
1387 < H = T(p,\pi ) + V(q,Q)
1449 < \]
1450 < The equations of motion corresponding to potential energy and
1451 < kinetic energy are listed in the below table,
1385 > energy and potential energy, $H = T(p,\pi ) + V(q,Q)$. The equations
1386 > of motion corresponding to potential energy and kinetic energy are
1387 > listed in Table~\ref{introTable:rbEquations}.
1388   \begin{table}
1389   \caption{EQUATIONS OF MOTION DUE TO POTENTIAL AND KINETIC ENERGIES}
1390 + \label{introTable:rbEquations}
1391   \begin{center}
1392   \begin{tabular}{|l|l|}
1393    \hline
# Line 1486 | Line 1423 | defined by \ref{introEquation:rotationalKineticRB}. Th
1423   T(p,\pi ) =T^t (p) + T^r (\pi ).
1424   \end{equation}
1425   where $ T^t (p) = \frac{1}{2}p^T m^{ - 1} p $ and $T^r (\pi )$ is
1426 < defined by \ref{introEquation:rotationalKineticRB}. Therefore, the
1427 < corresponding propagators are given by
1426 > defined by Eq.~\ref{introEquation:rotationalKineticRB}. Therefore,
1427 > the corresponding propagators are given by
1428   \[
1429   \varphi _{\Delta t,T}  = \varphi _{\Delta t,T^t }  \circ \varphi
1430   _{\Delta t,T^r }.
1431   \]
1432   Finally, we obtain the overall symplectic propagators for freely
1433   moving rigid bodies
1434 < \begin{equation}
1435 < \begin{array}{c}
1436 < \varphi _{\Delta t}  = \varphi _{\Delta t/2,F}  \circ \varphi _{\Delta t/2,\tau }  \\
1437 <  \circ \varphi _{\Delta t,T^t }  \circ \varphi _{\Delta t/2,\pi _1 }  \circ \varphi _{\Delta t/2,\pi _2 }  \circ \varphi _{\Delta t,\pi _3 }  \circ \varphi _{\Delta t/2,\pi _2 }  \circ \varphi _{\Delta t/2,\pi _1 }  \\
1501 <  \circ \varphi _{\Delta t/2,\tau }  \circ \varphi _{\Delta t/2,F}  .\\
1502 < \end{array}
1434 > \begin{eqnarray}
1435 > \varphi _{\Delta t}  &=& \varphi _{\Delta t/2,F}  \circ \varphi _{\Delta t/2,\tau }  \notag\\
1436 >  & & \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\\
1437 >  & & \circ \varphi _{\Delta t/2,\tau }  \circ \varphi _{\Delta t/2,F}  .
1438   \label{introEquation:overallRBFlowMaps}
1439 < \end{equation}
1439 > \end{eqnarray}
1440  
1441   \section{\label{introSection:langevinDynamics}Langevin Dynamics}
1442   As an alternative to newtonian dynamics, Langevin dynamics, which
1443   mimics a simple heat bath with stochastic and dissipative forces,
1444   has been applied in a variety of studies. This section will review
1445 < the theory of Langevin dynamics. A brief derivation of generalized
1445 > the theory of Langevin dynamics. A brief derivation of the generalized
1446   Langevin equation will be given first. Following that, we will
1447 < discuss the physical meaning of the terms appearing in the equation
1513 < as well as the calculation of friction tensor from hydrodynamics
1514 < theory.
1447 > discuss the physical meaning of the terms appearing in the equation.
1448  
1449   \subsection{\label{introSection:generalizedLangevinDynamics}Derivation of Generalized Langevin Equation}
1450  
# Line 1520 | Line 1453 | Dynamics (GLE). Lets consider a system, in which the d
1453   environment, has been widely used in quantum chemistry and
1454   statistical mechanics. One of the successful applications of
1455   Harmonic bath model is the derivation of the Generalized Langevin
1456 < Dynamics (GLE). Lets consider a system, in which the degree of
1456 > Dynamics (GLE). Consider a system, in which the degree of
1457   freedom $x$ is assumed to couple to the bath linearly, giving a
1458   Hamiltonian of the form
1459   \begin{equation}
# Line 1531 | Line 1464 | H_B  = \sum\limits_{\alpha  = 1}^N {\left\{ {\frac{{p_
1464   with this degree of freedom, $H_B$ is a harmonic bath Hamiltonian,
1465   \[
1466   H_B  = \sum\limits_{\alpha  = 1}^N {\left\{ {\frac{{p_\alpha ^2
1467 < }}{{2m_\alpha  }} + \frac{1}{2}m_\alpha  \omega _\alpha ^2 }
1467 > }}{{2m_\alpha  }} + \frac{1}{2}m_\alpha  x_\alpha ^2 }
1468   \right\}}
1469   \]
1470   where the index $\alpha$ runs over all the bath degrees of freedom,
# Line 1547 | Line 1480 | W(x) = U(x) - \sum\limits_{\alpha  = 1}^N {\frac{{g_\a
1480   \[
1481   W(x) = U(x) - \sum\limits_{\alpha  = 1}^N {\frac{{g_\alpha ^2
1482   }}{{2m_\alpha  w_\alpha ^2 }}} x^2
1483 < \] and combining the last two terms in Equation
1484 < \ref{introEquation:bathGLE}, we may rewrite the Harmonic bath
1552 < Hamiltonian as
1483 > \]
1484 > and combining the last two terms in Eq.~\ref{introEquation:bathGLE}, we may rewrite the Harmonic bath Hamiltonian as
1485   \[
1486   H = \frac{{p^2 }}{{2m}} + W(x) + \sum\limits_{\alpha  = 1}^N
1487   {\left\{ {\frac{{p_\alpha ^2 }}{{2m_\alpha  }} + \frac{1}{2}m_\alpha
1488   w_\alpha ^2 \left( {x_\alpha   - \frac{{g_\alpha  }}{{m_\alpha
1489 < w_\alpha ^2 }}x} \right)^2 } \right\}}
1489 > w_\alpha ^2 }}x} \right)^2 } \right\}}.
1490   \]
1491   Since the first two terms of the new Hamiltonian depend only on the
1492   system coordinates, we can get the equations of motion for
# Line 1571 | Line 1503 | m\ddot x_\alpha   =  - m_\alpha  w_\alpha ^2 \left( {x
1503   \frac{{g_\alpha  }}{{m_\alpha  w_\alpha ^2 }}x} \right).
1504   \label{introEquation:bathMotionGLE}
1505   \end{equation}
1574
1506   In order to derive an equation for $x$, the dynamics of the bath
1507   variables $x_\alpha$ must be solved exactly first. As an integral
1508   transform which is particularly useful in solving linear ordinary
1509   differential equations,the Laplace transform is the appropriate tool
1510   to solve this problem. The basic idea is to transform the difficult
1511   differential equations into simple algebra problems which can be
1512 < solved easily. Then, by applying the inverse Laplace transform, also
1513 < known as the Bromwich integral, we can retrieve the solutions of the
1514 < original problems.
1515 <
1585 < Let $f(t)$ be a function defined on $ [0,\infty ) $. The Laplace
1586 < transform of f(t) is a new function defined as
1512 > solved easily. Then, by applying the inverse Laplace transform, we
1513 > can retrieve the solutions of the original problems. Let $f(t)$ be a
1514 > function defined on $ [0,\infty ) $, the Laplace transform of $f(t)$
1515 > is a new function defined as
1516   \[
1517   L(f(t)) \equiv F(p) = \int_0^\infty  {f(t)e^{ - pt} dt}
1518   \]
1519   where  $p$ is real and  $L$ is called the Laplace Transform
1520 < Operator. Below are some important properties of Laplace transform
1592 <
1520 > Operator. Below are some important properties of the Laplace transform
1521   \begin{eqnarray*}
1522   L(x + y)  & = & L(x) + L(y) \\
1523   L(ax)     & = & aL(x) \\
# Line 1597 | Line 1525 | Operator. Below are some important properties of Lapla
1525   L(\ddot x)& = & p^2 L(x) - px(0) - \dot x(0) \\
1526   L\left( {\int_0^t {g(t - \tau )h(\tau )d\tau } } \right)& = & G(p)H(p) \\
1527   \end{eqnarray*}
1600
1601
1528   Applying the Laplace transform to the bath coordinates, we obtain
1529   \begin{eqnarray*}
1530 < 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) \\
1531 < L(x_\alpha  ) & = & \frac{{\frac{{g_\alpha  }}{{\omega _\alpha  }}L(x) + px_\alpha  (0) + \dot x_\alpha  (0)}}{{p^2  + \omega _\alpha ^2 }} \\
1530 > 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), \\
1531 > L(x_\alpha  ) & = & \frac{{\frac{{g_\alpha  }}{{\omega _\alpha  }}L(x) + px_\alpha  (0) + \dot x_\alpha  (0)}}{{p^2  + \omega _\alpha ^2 }}. \\
1532   \end{eqnarray*}
1533 <
1608 < By the same way, the system coordinates become
1533 > In the same way, the system coordinates become
1534   \begin{eqnarray*}
1535 < mL(\ddot x) & = & - \frac{1}{p}\frac{{\partial W(x)}}{{\partial x}} \\
1536 <  & & \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\}}  \\
1535 > mL(\ddot x) & = &
1536 >  - \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\}}  \\
1537 >  & & - \frac{1}{p}\frac{{\partial W(x)}}{{\partial x}}.
1538   \end{eqnarray*}
1613
1539   With the help of some relatively important inverse Laplace
1540   transformations:
1541   \[
# Line 1620 | Line 1545 | transformations:
1545   L(1) = \frac{1}{p} \\
1546   \end{array}
1547   \]
1548 < , we obtain
1548 > we obtain
1549   \begin{eqnarray*}
1550   m\ddot x & =  & - \frac{{\partial W(x)}}{{\partial x}} -
1551   \sum\limits_{\alpha  = 1}^N {\left\{ {\left( { - \frac{{g_\alpha ^2
# Line 1629 | Line 1554 | x_\alpha (0) - \frac{{g_\alpha  }}{{m_\alpha  \omega _
1554   & & + \sum\limits_{\alpha  = 1}^N {\left\{ {\left[ {g_\alpha
1555   x_\alpha (0) - \frac{{g_\alpha  }}{{m_\alpha  \omega _\alpha  }}}
1556   \right]\cos (\omega _\alpha  t) + \frac{{g_\alpha  \dot x_\alpha
1557 < (0)}}{{\omega _\alpha  }}\sin (\omega _\alpha  t)} \right\}}
1558 < \end{eqnarray*}
1559 < \begin{eqnarray*}
1560 < m\ddot x & = & - \frac{{\partial W(x)}}{{\partial x}} - \int_0^t
1561 < {\sum\limits_{\alpha  = 1}^N {\left( { - \frac{{g_\alpha ^2
1562 < }}{{m_\alpha  \omega _\alpha ^2 }}} \right)\cos (\omega _\alpha
1557 > (0)}}{{\omega _\alpha  }}\sin (\omega _\alpha  t)} \right\}}\\
1558 > %
1559 > & = & -
1560 > \frac{{\partial W(x)}}{{\partial x}} - \int_0^t {\sum\limits_{\alpha
1561 > = 1}^N {\left( { - \frac{{g_\alpha ^2 }}{{m_\alpha  \omega _\alpha
1562 > ^2 }}} \right)\cos (\omega _\alpha
1563   t)\dot x(t - \tau )d} \tau }  \\
1564   & & + \sum\limits_{\alpha  = 1}^N {\left\{ {\left[ {g_\alpha
1565   x_\alpha (0) - \frac{{g_\alpha }}{{m_\alpha \omega _\alpha  }}}
# Line 1661 | Line 1586 | which is known as the \emph{generalized Langevin equat
1586   (t)\dot x(t - \tau )d\tau }  + R(t)
1587   \label{introEuqation:GeneralizedLangevinDynamics}
1588   \end{equation}
1589 < which is known as the \emph{generalized Langevin equation}.
1589 > which is known as the \emph{generalized Langevin equation} (GLE).
1590  
1591   \subsubsection{\label{introSection:randomForceDynamicFrictionKernel}\textbf{Random Force and Dynamic Friction Kernel}}
1592  
1593   One may notice that $R(t)$ depends only on initial conditions, which
1594   implies it is completely deterministic within the context of a
1595   harmonic bath. However, it is easy to verify that $R(t)$ is totally
1596 < uncorrelated to $x$ and $\dot x$,
1597 < \[
1598 < \begin{array}{l}
1599 < \left\langle {x(t)R(t)} \right\rangle  = 0, \\
1675 < \left\langle {\dot x(t)R(t)} \right\rangle  = 0. \\
1676 < \end{array}
1677 < \]
1678 < This property is what we expect from a truly random process. As long
1679 < as the model chosen for $R(t)$ was a gaussian distribution in
1596 > uncorrelated to $x$ and $\dot x$, $\left\langle {x(t)R(t)}
1597 > \right\rangle  = 0, \left\langle {\dot x(t)R(t)} \right\rangle  =
1598 > 0.$ This property is what we expect from a truly random process. As
1599 > long as the model chosen for $R(t)$ was a gaussian distribution in
1600   general, the stochastic nature of the GLE still remains.
1681
1601   %dynamic friction kernel
1602   The convolution integral
1603   \[
# Line 1693 | Line 1612 | and Equation \ref{introEuqation:GeneralizedLangevinDyn
1612   \[
1613   \int_0^t {\xi (t)\dot x(t - \tau )d\tau }  = \xi _0 (x(t) - x(0))
1614   \]
1615 < and Equation \ref{introEuqation:GeneralizedLangevinDynamics} becomes
1615 > and Eq.~\ref{introEuqation:GeneralizedLangevinDynamics} becomes
1616   \[
1617   m\ddot x =  - \frac{\partial }{{\partial x}}\left( {W(x) +
1618   \frac{1}{2}\xi _0 (x - x_0 )^2 } \right) + R(t),
# Line 1703 | Line 1622 | taken as a $delta$ function in time:
1622   infinitely quickly to motions in the system. Thus, $\xi (t)$ can be
1623   taken as a $delta$ function in time:
1624   \[
1625 < \xi (t) = 2\xi _0 \delta (t)
1625 > \xi (t) = 2\xi _0 \delta (t).
1626   \]
1627   Hence, the convolution integral becomes
1628   \[
1629   \int_0^t {\xi (t)\dot x(t - \tau )d\tau }  = 2\xi _0 \int_0^t
1630   {\delta (t)\dot x(t - \tau )d\tau }  = \xi _0 \dot x(t),
1631   \]
1632 < and Equation \ref{introEuqation:GeneralizedLangevinDynamics} becomes
1632 > and Eq.~\ref{introEuqation:GeneralizedLangevinDynamics} becomes
1633   \begin{equation}
1634   m\ddot x =  - \frac{{\partial W(x)}}{{\partial x}} - \xi _0 \dot
1635   x(t) + R(t) \label{introEquation:LangevinEquation}
# Line 1718 | Line 1637 | briefly review on calculating friction tensor for arbi
1637   which is known as the Langevin equation. The static friction
1638   coefficient $\xi _0$ can either be calculated from spectral density
1639   or be determined by Stokes' law for regular shaped particles. A
1640 < briefly review on calculating friction tensor for arbitrary shaped
1640 > brief review on calculating friction tensors for arbitrary shaped
1641   particles is given in Sec.~\ref{introSection:frictionTensor}.
1642  
1643   \subsubsection{\label{introSection:secondFluctuationDissipation}\textbf{The Second Fluctuation Dissipation Theorem}}
1644  
1645 < Defining a new set of coordinates,
1645 > Defining a new set of coordinates
1646   \[
1647   q_\alpha  (t) = x_\alpha  (t) - \frac{1}{{m_\alpha  \omega _\alpha
1648 < ^2 }}x(0)
1649 < \],
1650 < we can rewrite $R(T)$ as
1648 > ^2 }}x(0),
1649 > \]
1650 > we can rewrite $R(t)$ as
1651   \[
1652   R(t) = \sum\limits_{\alpha  = 1}^N {g_\alpha  q_\alpha  (t)}.
1653   \]
1654   And since the $q$ coordinates are harmonic oscillators,
1736
1655   \begin{eqnarray*}
1656   \left\langle {q_\alpha ^2 } \right\rangle  & = & \frac{{kT}}{{m_\alpha  \omega _\alpha ^2 }} \\
1657   \left\langle {q_\alpha  (t)q_\alpha  (0)} \right\rangle & = & \left\langle {q_\alpha ^2 (0)} \right\rangle \cos (\omega _\alpha  t) \\
1658   \left\langle {q_\alpha  (t)q_\beta  (0)} \right\rangle & = &\delta _{\alpha \beta } \left\langle {q_\alpha  (t)q_\alpha  (0)} \right\rangle  \\
1659   \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 } }  \\
1660    & = &\sum\limits_\alpha  {g_\alpha ^2 \left\langle {q_\alpha ^2 (0)} \right\rangle \cos (\omega _\alpha  t)}  \\
1661 <  & = &kT\xi (t) \\
1661 >  & = &kT\xi (t)
1662   \end{eqnarray*}
1745
1663   Thus, we recover the \emph{second fluctuation dissipation theorem}
1664   \begin{equation}
1665   \xi (t) = \left\langle {R(t)R(0)} \right\rangle
1666 < \label{introEquation:secondFluctuationDissipation}.
1666 > \label{introEquation:secondFluctuationDissipation},
1667   \end{equation}
1668 < In effect, it acts as a constraint on the possible ways in which one
1669 < can model the random force and friction kernel.
1668 > which acts as a constraint on the possible ways in which one can
1669 > model the random force and friction kernel.

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