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# Line 6 | Line 6 | behind classical mechanics. Firstly, One can determine
6   Closely related to Classical Mechanics, Molecular Dynamics
7   simulations are carried out by integrating the equations of motion
8   for a given system of particles. There are three fundamental ideas
9 < behind classical mechanics. Firstly, One can determine the state of
9 > behind classical mechanics. Firstly, one can determine the state of
10   a mechanical system at any time of interest; Secondly, all the
11   mechanical properties of the system at that time can be determined
12   by combining the knowledge of the properties of the system with the
# Line 17 | Line 17 | Newton¡¯s first law defines a class of inertial frames
17   \subsection{\label{introSection:newtonian}Newtonian Mechanics}
18   The discovery of Newton's three laws of mechanics which govern the
19   motion of particles is the foundation of the classical mechanics.
20 < Newton¡¯s first law defines a class of inertial frames. Inertial
20 > Newton's first law defines a class of inertial frames. Inertial
21   frames are reference frames where a particle not interacting with
22   other bodies will move with constant speed in the same direction.
23 < With respect to inertial frames Newton¡¯s second law has the form
23 > With respect to inertial frames, Newton's second law has the form
24   \begin{equation}
25 < F = \frac {dp}{dt} = \frac {mv}{dt}
25 > F = \frac {dp}{dt} = \frac {mdv}{dt}
26   \label{introEquation:newtonSecondLaw}
27   \end{equation}
28   A point mass interacting with other bodies moves with the
29   acceleration along the direction of the force acting on it. Let
30 < $F_ij$ be the force that particle $i$ exerts on particle $j$, and
31 < $F_ji$ be the force that particle $j$ exerts on particle $i$.
32 < Newton¡¯s third law states that
30 > $F_{ij}$ be the force that particle $i$ exerts on particle $j$, and
31 > $F_{ji}$ be the force that particle $j$ exerts on particle $i$.
32 > Newton's third law states that
33   \begin{equation}
34 < F_ij = -F_ji
34 > F_{ij} = -F_{ji}
35   \label{introEquation:newtonThirdLaw}
36   \end{equation}
37  
# Line 46 | Line 46 | N \equiv r \times F \label{introEquation:torqueDefinit
46   \end{equation}
47   The torque $\tau$ with respect to the same origin is defined to be
48   \begin{equation}
49 < N \equiv r \times F \label{introEquation:torqueDefinition}
49 > \tau \equiv r \times F \label{introEquation:torqueDefinition}
50   \end{equation}
51   Differentiating Eq.~\ref{introEquation:angularMomentumDefinition},
52   \[
# Line 59 | Line 59 | thus,
59   \]
60   thus,
61   \begin{equation}
62 < \dot L = r \times \dot p = N
62 > \dot L = r \times \dot p = \tau
63   \end{equation}
64   If there are no external torques acting on a body, the angular
65   momentum of it is conserved. The last conservation theorem state
# Line 68 | Line 68 | scheme for rigid body \cite{Dullweber1997}.
68   \end{equation}
69   is conserved. All of these conserved quantities are
70   important factors to determine the quality of numerical integration
71 < scheme for rigid body \cite{Dullweber1997}.
71 > schemes for rigid bodies \cite{Dullweber1997}.
72  
73   \subsection{\label{introSection:lagrangian}Lagrangian Mechanics}
74  
75 < Newtonian Mechanics suffers from two important limitations: it
76 < describes their motion in special cartesian coordinate systems.
77 < Another limitation of Newtonian mechanics becomes obvious when we
78 < try to describe systems with large numbers of particles. It becomes
79 < very difficult to predict the properties of the system by carrying
80 < out calculations involving the each individual interaction between
81 < all the particles, even if we know all of the details of the
82 < interaction. In order to overcome some of the practical difficulties
83 < which arise in attempts to apply Newton's equation to complex
84 < system, alternative procedures may be developed.
75 > Newtonian Mechanics suffers from two important limitations: motions
76 > can only be described in cartesian coordinate systems. Moreover, It
77 > 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.
82  
83 < \subsubsection{\label{introSection:halmiltonPrinciple}Hamilton's
84 < Principle}
83 > \subsubsection{\label{introSection:halmiltonPrinciple}\textbf{Hamilton's
84 > Principle}}
85  
86   Hamilton introduced the dynamical principle upon which it is
87 < possible to base all of mechanics and, indeed, most of classical
88 < physics. Hamilton's Principle may be stated as follow,
87 > possible to base all of mechanics and most of classical physics.
88 > Hamilton's Principle may be stated as follows,
89  
90   The actual trajectory, along which a dynamical system may move from
91   one point to another within a specified time, is derived by finding
92   the path which minimizes the time integral of the difference between
93 < the kinetic, $K$, and potential energies, $U$ \cite{tolman79}.
93 > the kinetic, $K$, and potential energies, $U$.
94   \begin{equation}
95   \delta \int_{t_1 }^{t_2 } {(K - U)dt = 0} ,
96   \label{introEquation:halmitonianPrinciple1}
97   \end{equation}
98  
99   For simple mechanical systems, where the forces acting on the
100 < different part are derivable from a potential and the velocities are
101 < small compared with that of light, the Lagrangian function $L$ can
102 < be define as the difference between the kinetic energy of the system
106 < and its potential energy,
100 > different parts are derivable from a potential, the Lagrangian
101 > function $L$ can be defined as the difference between the kinetic
102 > energy of the system and its potential energy,
103   \begin{equation}
104   L \equiv K - U = L(q_i ,\dot q_i ) ,
105   \label{introEquation:lagrangianDef}
# Line 114 | Line 110 | then Eq.~\ref{introEquation:halmitonianPrinciple1} bec
110   \label{introEquation:halmitonianPrinciple2}
111   \end{equation}
112  
113 < \subsubsection{\label{introSection:equationOfMotionLagrangian}The
114 < Equations of Motion in Lagrangian Mechanics}
113 > \subsubsection{\label{introSection:equationOfMotionLagrangian}\textbf{The
114 > Equations of Motion in Lagrangian Mechanics}}
115  
116 < for a holonomic system of $f$ degrees of freedom, the equations of
117 < motion in the Lagrangian form is
116 > For a system of $f$ degrees of freedom, the equations of motion in
117 > the Lagrangian form is
118   \begin{equation}
119   \frac{d}{{dt}}\frac{{\partial L}}{{\partial \dot q_i }} -
120   \frac{{\partial L}}{{\partial q_i }} = 0,{\rm{ }}i = 1, \ldots,f
# Line 132 | Line 128 | independent of generalized velocities, the generalized
128   Arising from Lagrangian Mechanics, Hamiltonian Mechanics was
129   introduced by William Rowan Hamilton in 1833 as a re-formulation of
130   classical mechanics. If the potential energy of a system is
131 < independent of generalized velocities, the generalized momenta can
136 < be defined as
131 > independent of velocities, the momenta can be defined as
132   \begin{equation}
133   p_i = \frac{\partial L}{\partial \dot q_i}
134   \label{introEquation:generalizedMomenta}
# Line 172 | Line 167 | find
167   By identifying the coefficients of $dq_k$, $dp_k$ and dt, we can
168   find
169   \begin{equation}
170 < \frac{{\partial H}}{{\partial p_k }} = q_k
170 > \frac{{\partial H}}{{\partial p_k }} = \dot {q_k}
171   \label{introEquation:motionHamiltonianCoordinate}
172   \end{equation}
173   \begin{equation}
174 < \frac{{\partial H}}{{\partial q_k }} =  - p_k
174 > \frac{{\partial H}}{{\partial q_k }} =  - \dot {p_k}
175   \label{introEquation:motionHamiltonianMomentum}
176   \end{equation}
177   and
# Line 189 | Line 184 | known as the canonical equations of motions \cite{Gold
184   Eq.~\ref{introEquation:motionHamiltonianCoordinate} and
185   Eq.~\ref{introEquation:motionHamiltonianMomentum} are Hamilton's
186   equation of motion. Due to their symmetrical formula, they are also
187 < known as the canonical equations of motions \cite{Goldstein01}.
187 > known as the canonical equations of motions \cite{Goldstein2001}.
188  
189   An important difference between Lagrangian approach and the
190   Hamiltonian approach is that the Lagrangian is considered to be a
191 < function of the generalized velocities $\dot q_i$ and the
192 < generalized coordinates $q_i$, while the Hamiltonian is considered
193 < to be a function of the generalized momenta $p_i$ and the conjugate
194 < generalized coordinate $q_i$. Hamiltonian Mechanics is more
195 < appropriate for application to statistical mechanics and quantum
196 < mechanics, since it treats the coordinate and its time derivative as
197 < independent variables and it only works with 1st-order differential
203 < equations\cite{Marion90}.
191 > function of the generalized velocities $\dot q_i$ and coordinates
192 > $q_i$, while the Hamiltonian is considered to be a function of the
193 > generalized momenta $p_i$ and the conjugate coordinates $q_i$.
194 > Hamiltonian Mechanics is more appropriate for application to
195 > statistical mechanics and quantum mechanics, since it treats the
196 > coordinate and its time derivative as independent variables and it
197 > only works with 1st-order differential equations\cite{Marion1990}.
198  
199   In Newtonian Mechanics, a system described by conservative forces
200   conserves the total energy \ref{introEquation:energyConservation}.
# Line 212 | Line 206 | q_i }}} \right) = 0}
206   }}\dot p_i } \right)}  = \sum\limits_i {\left( {\frac{{\partial
207   H}}{{\partial q_i }}\frac{{\partial H}}{{\partial p_i }} -
208   \frac{{\partial H}}{{\partial p_i }}\frac{{\partial H}}{{\partial
209 < q_i }}} \right) = 0}
216 < \label{introEquation:conserveHalmitonian}
209 > q_i }}} \right) = 0} \label{introEquation:conserveHalmitonian}
210   \end{equation}
211  
212 < When studying Hamiltonian system, it is more convenient to use
213 < notation
221 < \begin{equation}
222 < r = r(q,p)^T
223 < \end{equation}
224 < and to introduce a $2n \times 2n$ canonical structure matrix $J$,
225 < \begin{equation}
226 < J = \left( {\begin{array}{*{20}c}
227 <   0 & I  \\
228 <   { - I} & 0  \\
229 < \end{array}} \right)
230 < \label{introEquation:canonicalMatrix}
231 < \end{equation}
232 < where $I$ is a $n \times n$ identity matrix and $J$ is a
233 < skew-symmetric matrix ($ J^T  =  - J $). Thus, Hamiltonian system
234 < can be rewritten as,
235 < \begin{equation}
236 < \frac{d}{{dt}}r = J\nabla _r H(r)
237 < \label{introEquation:compactHamiltonian}
238 < \end{equation}
212 > \section{\label{introSection:statisticalMechanics}Statistical
213 > Mechanics}
214  
215 < \section{\label{introSection:geometricIntegratos}Geometric Integrators}
215 > The thermodynamic behaviors and properties of Molecular Dynamics
216 > simulation are governed by the principle of Statistical Mechanics.
217 > The following section will give a brief introduction to some of the
218 > Statistical Mechanics concepts and theorem presented in this
219 > dissertation.
220  
221 < \subsection{\label{introSection:symplecticManifold}Symplectic Manifold}
243 < A \emph{manifold} is an abstract mathematical space. It locally
244 < looks like Euclidean space, but when viewed globally, it may have
245 < more complicate structure. A good example of manifold is the surface
246 < of Earth. It seems to be flat locally, but it is round if viewed as
247 < a whole. A \emph{differentiable manifold} (also known as
248 < \emph{smooth manifold}) is a manifold with an open cover in which
249 < the covering neighborhoods are all smoothly isomorphic to one
250 < another. In other words,it is possible to apply calculus on
251 < \emph{differentiable manifold}. A \emph{symplectic manifold} is
252 < defined as a pair $(M, \omega)$ consisting of a \emph{differentiable
253 < manifold} $M$ and a close, non-degenerated, bilinear symplectic
254 < form, $\omega$. One of the motivation to study \emph{symplectic
255 < manifold} in Hamiltonian Mechanics is that a symplectic manifold can
256 < represent all possible configurations of the system and the phase
257 < space of the system can be described by it's cotangent bundle. Every
258 < symplectic manifold is even dimensional. For instance, in Hamilton
259 < equations, coordinate and momentum always appear in pairs.
221 > \subsection{\label{introSection:ensemble}Phase Space and Ensemble}
222  
223 < A \emph{symplectomorphism} is also known as a \emph{canonical
224 < transformation}.
223 > Mathematically, phase space is the space which represents all
224 > possible states. Each possible state of the system corresponds to
225 > one unique point in the phase space. For mechanical systems, the
226 > phase space usually consists of all possible values of position and
227 > momentum variables. Consider a dynamic system of $f$ particles in a
228 > cartesian space, where each of the $6f$ coordinates and momenta is
229 > assigned to one of $6f$ mutually orthogonal axes, the phase space of
230 > this system is a $6f$ dimensional space. A point, $x = (q_1 , \ldots
231 > ,q_f ,p_1 , \ldots ,p_f )$, with a unique set of values of $6f$
232 > coordinates and momenta is a phase space vector.
233  
234 < Any real-valued differentiable function H on a symplectic manifold
235 < can serve as an energy function or Hamiltonian. Associated to any
236 < Hamiltonian is a Hamiltonian vector field; the integral curves of
237 < the Hamiltonian vector field are solutions to the Hamilton-Jacobi
238 < equations. The Hamiltonian vector field defines a flow on the
239 < symplectic manifold, called a Hamiltonian flow or symplectomorphism.
240 < By Liouville's theorem, Hamiltonian flows preserve the volume form
241 < on the phase space.
234 > %%%fix me
235 > A microscopic state or microstate of a classical system is
236 > specification of the complete phase space vector of a system at any
237 > instant in time. An ensemble is defined as a collection of systems
238 > sharing one or more macroscopic characteristics but each being in a
239 > unique microstate. The complete ensemble is specified by giving all
240 > systems or microstates consistent with the common macroscopic
241 > characteristics of the ensemble. Although the state of each
242 > individual system in the ensemble could be precisely described at
243 > any instance in time by a suitable phase space vector, when using
244 > ensembles for statistical purposes, there is no need to maintain
245 > distinctions between individual systems, since the numbers of
246 > systems at any time in the different states which correspond to
247 > different regions of the phase space are more interesting. Moreover,
248 > in the point of view of statistical mechanics, one would prefer to
249 > use ensembles containing a large enough population of separate
250 > members so that the numbers of systems in such different states can
251 > be regarded as changing continuously as we traverse different
252 > regions of the phase space. The condition of an ensemble at any time
253 > can be regarded as appropriately specified by the density $\rho$
254 > with which representative points are distributed over the phase
255 > space. The density distribution for an ensemble with $f$ degrees of
256 > freedom is defined as,
257 > \begin{equation}
258 > \rho  = \rho (q_1 , \ldots ,q_f ,p_1 , \ldots ,p_f ,t).
259 > \label{introEquation:densityDistribution}
260 > \end{equation}
261 > Governed by the principles of mechanics, the phase points change
262 > their locations which would change the density at any time at phase
263 > space. Hence, the density distribution is also to be taken as a
264 > function of the time.
265 >
266 > The number of systems $\delta N$ at time $t$ can be determined by,
267 > \begin{equation}
268 > \delta N = \rho (q,p,t)dq_1  \ldots dq_f dp_1  \ldots dp_f.
269 > \label{introEquation:deltaN}
270 > \end{equation}
271 > Assuming a large enough population of systems, we can sufficiently
272 > approximate $\delta N$ without introducing discontinuity when we go
273 > from one region in the phase space to another. By integrating over
274 > the whole phase space,
275 > \begin{equation}
276 > N = \int { \ldots \int {\rho (q,p,t)dq_1 } ...dq_f dp_1 } ...dp_f
277 > \label{introEquation:totalNumberSystem}
278 > \end{equation}
279 > gives us an expression for the total number of the systems. Hence,
280 > the probability per unit in the phase space can be obtained by,
281 > \begin{equation}
282 > \frac{{\rho (q,p,t)}}{N} = \frac{{\rho (q,p,t)}}{{\int { \ldots \int
283 > {\rho (q,p,t)dq_1 } ...dq_f dp_1 } ...dp_f }}.
284 > \label{introEquation:unitProbability}
285 > \end{equation}
286 > With the help of Eq.~\ref{introEquation:unitProbability} and the
287 > knowledge of the system, it is possible to calculate the average
288 > value of any desired quantity which depends on the coordinates and
289 > momenta of the system. Even when the dynamics of the real system is
290 > complex, or stochastic, or even discontinuous, the average
291 > properties of the ensemble of possibilities as a whole remaining
292 > well defined. For a classical system in thermal equilibrium with its
293 > environment, the ensemble average of a mechanical quantity, $\langle
294 > A(q , p) \rangle_t$, takes the form of an integral over the phase
295 > space of the system,
296 > \begin{equation}
297 > \langle  A(q , p) \rangle_t = \frac{{\int { \ldots \int {A(q,p)\rho
298 > (q,p,t)dq_1 } ...dq_f dp_1 } ...dp_f }}{{\int { \ldots \int {\rho
299 > (q,p,t)dq_1 } ...dq_f dp_1 } ...dp_f }}
300 > \label{introEquation:ensembelAverage}
301 > \end{equation}
302 >
303 > There are several different types of ensembles with different
304 > statistical characteristics. As a function of macroscopic
305 > parameters, such as temperature \textit{etc}, the partition function
306 > can be used to describe the statistical properties of a system in
307 > thermodynamic equilibrium.
308 >
309 > As an ensemble of systems, each of which is known to be thermally
310 > isolated and conserve energy, the Microcanonical ensemble (NVE) has
311 > a partition function like,
312 > \begin{equation}
313 > \Omega (N,V,E) = e^{\beta TS} \label{introEquation:NVEPartition}.
314 > \end{equation}
315 > A canonical ensemble (NVT)is an ensemble of systems, each of which
316 > can share its energy with a large heat reservoir. The distribution
317 > of the total energy amongst the possible dynamical states is given
318 > by the partition function,
319 > \begin{equation}
320 > \Omega (N,V,T) = e^{ - \beta A}
321 > \label{introEquation:NVTPartition}
322 > \end{equation}
323 > Here, $A$ is the Helmholtz free energy which is defined as $ A = U -
324 > TS$. Since most experiments are carried out under constant pressure
325 > condition, the isothermal-isobaric ensemble (NPT) plays a very
326 > important role in molecular simulations. The isothermal-isobaric
327 > ensemble allow the system to exchange energy with a heat bath of
328 > temperature $T$ and to change the volume as well. Its partition
329 > function is given as
330 > \begin{equation}
331 > \Delta (N,P,T) =  - e^{\beta G}.
332 > \label{introEquation:NPTPartition}
333 > \end{equation}
334 > Here, $G = U - TS + PV$, and $G$ is called Gibbs free energy.
335 >
336 > \subsection{\label{introSection:liouville}Liouville's theorem}
337  
338 < \subsection{\label{Construction of Symplectic Methods}}
338 > Liouville's theorem is the foundation on which statistical mechanics
339 > rests. It describes the time evolution of the phase space
340 > distribution function. In order to calculate the rate of change of
341 > $\rho$, we begin from Eq.~\ref{introEquation:deltaN}. If we consider
342 > the two faces perpendicular to the $q_1$ axis, which are located at
343 > $q_1$ and $q_1 + \delta q_1$, the number of phase points leaving the
344 > opposite face is given by the expression,
345 > \begin{equation}
346 > \left( {\rho  + \frac{{\partial \rho }}{{\partial q_1 }}\delta q_1 }
347 > \right)\left( {\dot q_1  + \frac{{\partial \dot q_1 }}{{\partial q_1
348 > }}\delta q_1 } \right)\delta q_2  \ldots \delta q_f \delta p_1
349 > \ldots \delta p_f .
350 > \end{equation}
351 > Summing all over the phase space, we obtain
352 > \begin{equation}
353 > \frac{{d(\delta N)}}{{dt}} =  - \sum\limits_{i = 1}^f {\left[ {\rho
354 > \left( {\frac{{\partial \dot q_i }}{{\partial q_i }} +
355 > \frac{{\partial \dot p_i }}{{\partial p_i }}} \right) + \left(
356 > {\frac{{\partial \rho }}{{\partial q_i }}\dot q_i  + \frac{{\partial
357 > \rho }}{{\partial p_i }}\dot p_i } \right)} \right]} \delta q_1
358 > \ldots \delta q_f \delta p_1  \ldots \delta p_f .
359 > \end{equation}
360 > Differentiating the equations of motion in Hamiltonian formalism
361 > (\ref{introEquation:motionHamiltonianCoordinate},
362 > \ref{introEquation:motionHamiltonianMomentum}), we can show,
363 > \begin{equation}
364 > \sum\limits_i {\left( {\frac{{\partial \dot q_i }}{{\partial q_i }}
365 > + \frac{{\partial \dot p_i }}{{\partial p_i }}} \right)}  = 0 ,
366 > \end{equation}
367 > which cancels the first terms of the right hand side. Furthermore,
368 > dividing $ \delta q_1  \ldots \delta q_f \delta p_1  \ldots \delta
369 > p_f $ in both sides, we can write out Liouville's theorem in a
370 > simple form,
371 > \begin{equation}
372 > \frac{{\partial \rho }}{{\partial t}} + \sum\limits_{i = 1}^f
373 > {\left( {\frac{{\partial \rho }}{{\partial q_i }}\dot q_i  +
374 > \frac{{\partial \rho }}{{\partial p_i }}\dot p_i } \right)}  = 0 .
375 > \label{introEquation:liouvilleTheorem}
376 > \end{equation}
377  
378 < \section{\label{introSection:statisticalMechanics}Statistical
379 < Mechanics}
378 > Liouville's theorem states that the distribution function is
379 > constant along any trajectory in phase space. In classical
380 > statistical mechanics, since the number of members in an ensemble is
381 > huge and constant, we can assume the local density has no reason
382 > (other than classical mechanics) to change,
383 > \begin{equation}
384 > \frac{{\partial \rho }}{{\partial t}} = 0.
385 > \label{introEquation:stationary}
386 > \end{equation}
387 > In such stationary system, the density of distribution $\rho$ can be
388 > connected to the Hamiltonian $H$ through Maxwell-Boltzmann
389 > distribution,
390 > \begin{equation}
391 > \rho  \propto e^{ - \beta H}
392 > \label{introEquation:densityAndHamiltonian}
393 > \end{equation}
394  
395 < The thermodynamic behaviors and properties of Molecular Dynamics
396 < simulation are governed by the principle of Statistical Mechanics.
397 < The following section will give a brief introduction to some of the
398 < Statistical Mechanics concepts presented in this dissertation.
395 > \subsubsection{\label{introSection:phaseSpaceConservation}\textbf{Conservation of Phase Space}}
396 > Lets consider a region in the phase space,
397 > \begin{equation}
398 > \delta v = \int { \ldots \int {dq_1 } ...dq_f dp_1 } ..dp_f .
399 > \end{equation}
400 > If this region is small enough, the density $\rho$ can be regarded
401 > as uniform over the whole integral. Thus, the number of phase points
402 > inside this region is given by,
403 > \begin{equation}
404 > \delta N = \rho \delta v = \rho \int { \ldots \int {dq_1 } ...dq_f
405 > dp_1 } ..dp_f.
406 > \end{equation}
407  
408 < \subsection{\label{introSection:ensemble}Ensemble and Phase Space}
408 > \begin{equation}
409 > \frac{{d(\delta N)}}{{dt}} = \frac{{d\rho }}{{dt}}\delta v + \rho
410 > \frac{d}{{dt}}(\delta v) = 0.
411 > \end{equation}
412 > With the help of stationary assumption
413 > (\ref{introEquation:stationary}), we obtain the principle of the
414 > \emph{conservation of volume in phase space},
415 > \begin{equation}
416 > \frac{d}{{dt}}(\delta v) = \frac{d}{{dt}}\int { \ldots \int {dq_1 }
417 > ...dq_f dp_1 } ..dp_f  = 0.
418 > \label{introEquation:volumePreserving}
419 > \end{equation}
420  
421 + \subsubsection{\label{introSection:liouvilleInOtherForms}\textbf{Liouville's Theorem in Other Forms}}
422 +
423 + Liouville's theorem can be expresses in a variety of different forms
424 + which are convenient within different contexts. For any two function
425 + $F$ and $G$ of the coordinates and momenta of a system, the Poisson
426 + bracket ${F, G}$ is defined as
427 + \begin{equation}
428 + \left\{ {F,G} \right\} = \sum\limits_i {\left( {\frac{{\partial
429 + F}}{{\partial q_i }}\frac{{\partial G}}{{\partial p_i }} -
430 + \frac{{\partial F}}{{\partial p_i }}\frac{{\partial G}}{{\partial
431 + q_i }}} \right)}.
432 + \label{introEquation:poissonBracket}
433 + \end{equation}
434 + Substituting equations of motion in Hamiltonian formalism(
435 + Eq.~\ref{introEquation:motionHamiltonianCoordinate} ,
436 + Eq.~\ref{introEquation:motionHamiltonianMomentum} ) into
437 + (Eq.~\ref{introEquation:liouvilleTheorem}), we can rewrite
438 + Liouville's theorem using Poisson bracket notion,
439 + \begin{equation}
440 + \left( {\frac{{\partial \rho }}{{\partial t}}} \right) =  - \left\{
441 + {\rho ,H} \right\}.
442 + \label{introEquation:liouvilleTheromInPoissin}
443 + \end{equation}
444 + Moreover, the Liouville operator is defined as
445 + \begin{equation}
446 + iL = \sum\limits_{i = 1}^f {\left( {\frac{{\partial H}}{{\partial
447 + p_i }}\frac{\partial }{{\partial q_i }} - \frac{{\partial
448 + H}}{{\partial q_i }}\frac{\partial }{{\partial p_i }}} \right)}
449 + \label{introEquation:liouvilleOperator}
450 + \end{equation}
451 + In terms of Liouville operator, Liouville's equation can also be
452 + expressed as
453 + \begin{equation}
454 + \left( {\frac{{\partial \rho }}{{\partial t}}} \right) =  - iL\rho
455 + \label{introEquation:liouvilleTheoremInOperator}
456 + \end{equation}
457 +
458   \subsection{\label{introSection:ergodic}The Ergodic Hypothesis}
459  
460   Various thermodynamic properties can be calculated from Molecular
461   Dynamics simulation. By comparing experimental values with the
462   calculated properties, one can determine the accuracy of the
463 < simulation and the quality of the underlying model. However, both of
464 < experiment and computer simulation are usually performed during a
463 > simulation and the quality of the underlying model. However, both
464 > experiments and computer simulations are usually performed during a
465   certain time interval and the measurements are averaged over a
466   period of them which is different from the average behavior of
467 < many-body system in Statistical Mechanics. Fortunately, Ergodic
468 < Hypothesis is proposed to make a connection between time average and
469 < ensemble average. It states that time average and average over the
470 < statistical ensemble are identical \cite{Frenkel1996, leach01:mm}.
467 > many-body system in Statistical Mechanics. Fortunately, the Ergodic
468 > Hypothesis makes a connection between time average and the ensemble
469 > average. It states that the time average and average over the
470 > statistical ensemble are identical \cite{Frenkel1996, Leach2001}.
471   \begin{equation}
472 < \langle A \rangle_t = \mathop {\lim }\limits_{t \to \infty }
473 < \frac{1}{t}\int\limits_0^t {A(p(t),q(t))dt = \int\limits_\Gamma
474 < {A(p(t),q(t))} } \rho (p(t), q(t)) dpdq
472 > \langle A(q , p) \rangle_t = \mathop {\lim }\limits_{t \to \infty }
473 > \frac{1}{t}\int\limits_0^t {A(q(t),p(t))dt = \int\limits_\Gamma
474 > {A(q(t),p(t))} } \rho (q(t), p(t)) dqdp
475   \end{equation}
476 < where $\langle A \rangle_t$ is an equilibrium value of a physical
477 < quantity and $\rho (p(t), q(t))$ is the equilibrium distribution
478 < function. If an observation is averaged over a sufficiently long
479 < time (longer than relaxation time), all accessible microstates in
480 < phase space are assumed to be equally probed, giving a properly
481 < weighted statistical average. This allows the researcher freedom of
482 < choice when deciding how best to measure a given observable. In case
483 < an ensemble averaged approach sounds most reasonable, the Monte
484 < Carlo techniques\cite{metropolis:1949} can be utilized. Or if the
485 < system lends itself to a time averaging approach, the Molecular
486 < Dynamics techniques in Sec.~\ref{introSection:molecularDynamics}
487 < will be the best choice\cite{Frenkel1996}.
476 > where $\langle  A(q , p) \rangle_t$ is an equilibrium value of a
477 > physical quantity and $\rho (p(t), q(t))$ is the equilibrium
478 > distribution function. If an observation is averaged over a
479 > sufficiently long time (longer than relaxation time), all accessible
480 > microstates in phase space are assumed to be equally probed, giving
481 > a properly weighted statistical average. This allows the researcher
482 > freedom of choice when deciding how best to measure a given
483 > observable. In case an ensemble averaged approach sounds most
484 > reasonable, the Monte Carlo techniques\cite{Metropolis1949} can be
485 > utilized. Or if the system lends itself to a time averaging
486 > approach, the Molecular Dynamics techniques in
487 > Sec.~\ref{introSection:molecularDynamics} will be the best
488 > choice\cite{Frenkel1996}.
489  
490 < \section{\label{introSection:molecularDynamics}Molecular Dynamics}
490 > \section{\label{introSection:geometricIntegratos}Geometric Integrators}
491 > A variety of numerical integrators have been proposed to simulate
492 > the motions of atoms in MD simulation. They usually begin with
493 > initial conditionals and move the objects in the direction governed
494 > by the differential equations. However, most of them ignore the
495 > hidden physical laws contained within the equations. Since 1990,
496 > geometric integrators, which preserve various phase-flow invariants
497 > such as symplectic structure, volume and time reversal symmetry, are
498 > developed to address this issue\cite{Dullweber1997, McLachlan1998,
499 > Leimkuhler1999}. The velocity Verlet method, which happens to be a
500 > simple example of symplectic integrator, continues to gain
501 > popularity in the molecular dynamics community. This fact can be
502 > partly explained by its geometric nature.
503  
504 < As a special discipline of molecular modeling, Molecular dynamics
505 < has proven to be a powerful tool for studying the functions of
506 < biological systems, providing structural, thermodynamic and
507 < dynamical information.
504 > \subsection{\label{introSection:symplecticManifold}Symplectic Manifolds}
505 > A \emph{manifold} is an abstract mathematical space. It looks
506 > locally like Euclidean space, but when viewed globally, it may have
507 > more complicated structure. A good example of manifold is the
508 > surface of Earth. It seems to be flat locally, but it is round if
509 > viewed as a whole. A \emph{differentiable manifold} (also known as
510 > \emph{smooth manifold}) is a manifold on which it is possible to
511 > apply calculus on \emph{differentiable manifold}. A \emph{symplectic
512 > manifold} is defined as a pair $(M, \omega)$ which consists of a
513 > \emph{differentiable manifold} $M$ and a close, non-degenerated,
514 > bilinear symplectic form, $\omega$. A symplectic form on a vector
515 > space $V$ is a function $\omega(x, y)$ which satisfies
516 > $\omega(\lambda_1x_1+\lambda_2x_2, y) = \lambda_1\omega(x_1, y)+
517 > \lambda_2\omega(x_2, y)$, $\omega(x, y) = - \omega(y, x)$ and
518 > $\omega(x, x) = 0$. The cross product operation in vector field is
519 > an example of symplectic form.
520  
521 < \subsection{\label{introSec:mdInit}Initialization}
521 > One of the motivations to study \emph{symplectic manifolds} in
522 > Hamiltonian Mechanics is that a symplectic manifold can represent
523 > all possible configurations of the system and the phase space of the
524 > system can be described by it's cotangent bundle. Every symplectic
525 > manifold is even dimensional. For instance, in Hamilton equations,
526 > coordinate and momentum always appear in pairs.
527  
528 < \subsection{\label{introSection:mdIntegration} Integration of the Equations of Motion}
528 > \subsection{\label{introSection:ODE}Ordinary Differential Equations}
529  
530 < \section{\label{introSection:rigidBody}Dynamics of Rigid Bodies}
531 <
532 < A rigid body is a body in which the distance between any two given
533 < points of a rigid body remains constant regardless of external
534 < forces exerted on it. A rigid body therefore conserves its shape
535 < during its motion.
536 <
537 < Applications of dynamics of rigid bodies.
538 <
539 < \subsection{\label{introSection:lieAlgebra}Lie Algebra}
540 <
541 < \subsection{\label{introSection:DLMMotionEquation}The Euler Equations of Rigid Body Motion}
542 <
543 < \subsection{\label{introSection:otherRBMotionEquation}Other Formulations for Rigid Body Motion}
544 <
545 < %\subsection{\label{introSection:poissonBrackets}Poisson Brackets}
546 <
547 < \section{\label{introSection:correlationFunctions}Correlation Functions}
548 <
549 < \section{\label{introSection:langevinDynamics}Langevin Dynamics}
550 <
551 < \subsection{\label{introSection:LDIntroduction}Introduction and application of Langevin Dynamics}
530 > For an ordinary differential system defined as
531 > \begin{equation}
532 > \dot x = f(x)
533 > \end{equation}
534 > where $x = x(q,p)^T$, this system is a canonical Hamiltonian, if
535 > \begin{equation}
536 > f(r) = J\nabla _x H(r).
537 > \end{equation}
538 > $H = H (q, p)$ is Hamiltonian function and $J$ is the skew-symmetric
539 > matrix
540 > \begin{equation}
541 > J = \left( {\begin{array}{*{20}c}
542 >   0 & I  \\
543 >   { - I} & 0  \\
544 > \end{array}} \right)
545 > \label{introEquation:canonicalMatrix}
546 > \end{equation}
547 > where $I$ is an identity matrix. Using this notation, Hamiltonian
548 > system can be rewritten as,
549 > \begin{equation}
550 > \frac{d}{{dt}}x = J\nabla _x H(x)
551 > \label{introEquation:compactHamiltonian}
552 > \end{equation}In this case, $f$ is
553 > called a \emph{Hamiltonian vector field}.
554  
555 < \subsection{\label{introSection:generalizedLangevinDynamics}Generalized Langevin Dynamics}
555 > Another generalization of Hamiltonian dynamics is Poisson
556 > Dynamics\cite{Olver1986},
557 > \begin{equation}
558 > \dot x = J(x)\nabla _x H \label{introEquation:poissonHamiltonian}
559 > \end{equation}
560 > The most obvious change being that matrix $J$ now depends on $x$.
561  
562 + \subsection{\label{introSection:exactFlow}Exact Flow}
563 +
564 + Let $x(t)$ be the exact solution of the ODE system,
565   \begin{equation}
566 < H = \frac{{p^2 }}{{2m}} + U(x) + H_B  + \Delta U(x,x_1 , \ldots x_N)
354 < \label{introEquation:bathGLE}
566 > \frac{{dx}}{{dt}} = f(x) \label{introEquation:ODE}
567   \end{equation}
568 < where $H_B$ is harmonic bath Hamiltonian,
568 > The exact flow(solution) $\varphi_\tau$ is defined by
569   \[
570 < H_B  =\sum\limits_{\alpha  = 1}^N {\left\{ {\frac{{p_\alpha ^2
359 < }}{{2m_\alpha  }} + \frac{1}{2}m_\alpha  w_\alpha ^2 } \right\}}
570 > x(t+\tau) =\varphi_\tau(x(t))
571   \]
572 < and $\Delta U$ is bilinear system-bath coupling,
572 > where $\tau$ is a fixed time step and $\varphi$ is a map from phase
573 > space to itself. The flow has the continuous group property,
574 > \begin{equation}
575 > \varphi _{\tau _1 }  \circ \varphi _{\tau _2 }  = \varphi _{\tau _1
576 > + \tau _2 } .
577 > \end{equation}
578 > In particular,
579 > \begin{equation}
580 > \varphi _\tau   \circ \varphi _{ - \tau }  = I
581 > \end{equation}
582 > Therefore, the exact flow is self-adjoint,
583 > \begin{equation}
584 > \varphi _\tau   = \varphi _{ - \tau }^{ - 1}.
585 > \end{equation}
586 > The exact flow can also be written in terms of the of an operator,
587 > \begin{equation}
588 > \varphi _\tau  (x) = e^{\tau \sum\limits_i {f_i (x)\frac{\partial
589 > }{{\partial x_i }}} } (x) \equiv \exp (\tau f)(x).
590 > \label{introEquation:exponentialOperator}
591 > \end{equation}
592 >
593 > In most cases, it is not easy to find the exact flow $\varphi_\tau$.
594 > Instead, we use an approximate map, $\psi_\tau$, which is usually
595 > called integrator. The order of an integrator $\psi_\tau$ is $p$, if
596 > the Taylor series of $\psi_\tau$ agree to order $p$,
597 > \begin{equation}
598 > \psi_\tau(x) = x + \tau f(x) + O(\tau^{p+1})
599 > \end{equation}
600 >
601 > \subsection{\label{introSection:geometricProperties}Geometric Properties}
602 >
603 > The hidden geometric properties\cite{Budd1999, Marsden1998} of an
604 > ODE and its flow play important roles in numerical studies. Many of
605 > them can be found in systems which occur naturally in applications.
606 >
607 > Let $\varphi$ be the flow of Hamiltonian vector field, $\varphi$ is
608 > a \emph{symplectic} flow if it satisfies,
609 > \begin{equation}
610 > {\varphi '}^T J \varphi ' = J.
611 > \end{equation}
612 > According to Liouville's theorem, the symplectic volume is invariant
613 > under a Hamiltonian flow, which is the basis for classical
614 > statistical mechanics. Furthermore, the flow of a Hamiltonian vector
615 > field on a symplectic manifold can be shown to be a
616 > symplectomorphism. As to the Poisson system,
617 > \begin{equation}
618 > {\varphi '}^T J \varphi ' = J \circ \varphi
619 > \end{equation}
620 > is the property that must be preserved by the integrator.
621 >
622 > It is possible to construct a \emph{volume-preserving} flow for a
623 > source free ODE ($ \nabla \cdot f = 0 $), if the flow satisfies $
624 > \det d\varphi  = 1$. One can show easily that a symplectic flow will
625 > be volume-preserving.
626 >
627 > Changing the variables $y = h(x)$ in an ODE
628 > (Eq.~\ref{introEquation:ODE}) will result in a new system,
629   \[
630 < \Delta U =  - \sum\limits_{\alpha  = 1}^N {g_\alpha  x_\alpha  x}
630 > \dot y = \tilde f(y) = ((dh \cdot f)h^{ - 1} )(y).
631   \]
632 < Completing the square,
632 > The vector filed $f$ has reversing symmetry $h$ if $f = - \tilde f$.
633 > In other words, the flow of this vector field is reversible if and
634 > only if $ h \circ \varphi ^{ - 1}  = \varphi  \circ h $.
635 >
636 > A \emph{first integral}, or conserved quantity of a general
637 > differential function is a function $ G:R^{2d}  \to R^d $ which is
638 > constant for all solutions of the ODE $\frac{{dx}}{{dt}} = f(x)$ ,
639   \[
640 < H_B  + \Delta U = \sum\limits_{\alpha  = 1}^N {\left\{
368 < {\frac{{p_\alpha ^2 }}{{2m_\alpha  }} + \frac{1}{2}m_\alpha
369 < w_\alpha ^2 \left( {x_\alpha   - \frac{{g_\alpha  }}{{m_\alpha
370 < w_\alpha ^2 }}x} \right)^2 } \right\}}  - \sum\limits_{\alpha  =
371 < 1}^N {\frac{{g_\alpha ^2 }}{{2m_\alpha  w_\alpha ^2 }}} x^2
640 > \frac{{dG(x(t))}}{{dt}} = 0.
641   \]
642 < and putting it back into Eq.~\ref{introEquation:bathGLE},
642 > Using chain rule, one may obtain,
643   \[
644 < H = \frac{{p^2 }}{{2m}} + W(x) + \sum\limits_{\alpha  = 1}^N
376 < {\left\{ {\frac{{p_\alpha ^2 }}{{2m_\alpha  }} + \frac{1}{2}m_\alpha
377 < w_\alpha ^2 \left( {x_\alpha   - \frac{{g_\alpha  }}{{m_\alpha
378 < w_\alpha ^2 }}x} \right)^2 } \right\}}
644 > \sum\limits_i {\frac{{dG}}{{dx_i }}} f_i (x) = f \bullet \nabla G,
645   \]
646 < where
647 < \[
648 < W(x) = U(x) - \sum\limits_{\alpha  = 1}^N {\frac{{g_\alpha ^2
383 < }}{{2m_\alpha  w_\alpha ^2 }}} x^2
384 < \]
385 < Since the first two terms of the new Hamiltonian depend only on the
386 < system coordinates, we can get the equations of motion for
387 < Generalized Langevin Dynamics by Hamilton's equations
388 < \ref{introEquation:motionHamiltonianCoordinate,
389 < introEquation:motionHamiltonianMomentum},
390 < \begin{align}
391 < \dot p &=  - \frac{{\partial H}}{{\partial x}}
392 <       &= m\ddot x
393 <       &= - \frac{{\partial W(x)}}{{\partial x}} - \sum\limits_{\alpha  = 1}^N {g_\alpha  \left( {x_\alpha   - \frac{{g_\alpha  }}{{m_\alpha  w_\alpha ^2 }}x} \right)}
394 < \label{introEq:Lp5}
395 < \end{align}
396 < , and
397 < \begin{align}
398 < \dot p_\alpha   &=  - \frac{{\partial H}}{{\partial x_\alpha  }}
399 <                &= m\ddot x_\alpha
400 <                &= \- m_\alpha  w_\alpha ^2 \left( {x_\alpha   - \frac{{g_\alpha}}{{m_\alpha  w_\alpha ^2 }}x} \right)
401 < \end{align}
646 > which is the condition for conserving \emph{first integral}. For a
647 > canonical Hamiltonian system, the time evolution of an arbitrary
648 > smooth function $G$ is given by,
649  
650 < \subsection{\label{introSection:laplaceTransform}The Laplace Transform}
650 > \begin{eqnarray}
651 > \frac{{dG(x(t))}}{{dt}} & = & [\nabla _x G(x(t))]^T \dot x(t) \\
652 >                        & = & [\nabla _x G(x(t))]^T J\nabla _x H(x(t)). \\
653 > \label{introEquation:firstIntegral1}
654 > \end{eqnarray}
655  
405 \[
406 L(x) = \int_0^\infty  {x(t)e^{ - pt} dt}
407 \]
656  
657 + Using poisson bracket notion, Equation
658 + \ref{introEquation:firstIntegral1} can be rewritten as
659   \[
660 < L(x + y) = L(x) + L(y)
660 > \frac{d}{{dt}}G(x(t)) = \left\{ {G,H} \right\}(x(t)).
661   \]
662 <
662 > Therefore, the sufficient condition for $G$ to be the \emph{first
663 > integral} of a Hamiltonian system is
664   \[
665 < L(ax) = aL(x)
665 > \left\{ {G,H} \right\} = 0.
666   \]
667 + As well known, the Hamiltonian (or energy) H of a Hamiltonian system
668 + is a \emph{first integral}, which is due to the fact $\{ H,H\}  =
669 + 0$.
670  
671 + When designing any numerical methods, one should always try to
672 + preserve the structural properties of the original ODE and its flow.
673 +
674 + \subsection{\label{introSection:constructionSymplectic}Construction of Symplectic Methods}
675 + A lot of well established and very effective numerical methods have
676 + been successful precisely because of their symplecticities even
677 + though this fact was not recognized when they were first
678 + constructed. The most famous example is the Verlet-leapfrog method
679 + in molecular dynamics. In general, symplectic integrators can be
680 + constructed using one of four different methods.
681 + \begin{enumerate}
682 + \item Generating functions
683 + \item Variational methods
684 + \item Runge-Kutta methods
685 + \item Splitting methods
686 + \end{enumerate}
687 +
688 + Generating function\cite{Channell1990} tends to lead to methods
689 + which are cumbersome and difficult to use. In dissipative systems,
690 + variational methods can capture the decay of energy
691 + accurately\cite{Kane2000}. Since their geometrically unstable nature
692 + against non-Hamiltonian perturbations, ordinary implicit Runge-Kutta
693 + methods are not suitable for Hamiltonian system. Recently, various
694 + high-order explicit Runge-Kutta methods
695 + \cite{Owren1992,Chen2003}have been developed to overcome this
696 + instability. However, due to computational penalty involved in
697 + implementing the Runge-Kutta methods, they have not attracted much
698 + attention from the Molecular Dynamics community. Instead, splitting
699 + methods have been widely accepted since they exploit natural
700 + decompositions of the system\cite{Tuckerman1992, McLachlan1998}.
701 +
702 + \subsubsection{\label{introSection:splittingMethod}\textbf{Splitting Methods}}
703 +
704 + The main idea behind splitting methods is to decompose the discrete
705 + $\varphi_h$ as a composition of simpler flows,
706 + \begin{equation}
707 + \varphi _h  = \varphi _{h_1 }  \circ \varphi _{h_2 }  \ldots  \circ
708 + \varphi _{h_n }
709 + \label{introEquation:FlowDecomposition}
710 + \end{equation}
711 + where each of the sub-flow is chosen such that each represent a
712 + simpler integration of the system.
713 +
714 + Suppose that a Hamiltonian system takes the form,
715   \[
716 < L(\dot x) = pL(x) - px(0)
716 > H = H_1 + H_2.
717   \]
718 + Here, $H_1$ and $H_2$ may represent different physical processes of
719 + the system. For instance, they may relate to kinetic and potential
720 + energy respectively, which is a natural decomposition of the
721 + problem. If $H_1$ and $H_2$ can be integrated using exact flows
722 + $\varphi_1(t)$ and $\varphi_2(t)$, respectively, a simple first
723 + order expression is then given by the Lie-Trotter formula
724 + \begin{equation}
725 + \varphi _h  = \varphi _{1,h}  \circ \varphi _{2,h},
726 + \label{introEquation:firstOrderSplitting}
727 + \end{equation}
728 + where $\varphi _h$ is the result of applying the corresponding
729 + continuous $\varphi _i$ over a time $h$. By definition, as
730 + $\varphi_i(t)$ is the exact solution of a Hamiltonian system, it
731 + must follow that each operator $\varphi_i(t)$ is a symplectic map.
732 + It is easy to show that any composition of symplectic flows yields a
733 + symplectic map,
734 + \begin{equation}
735 + (\varphi '\phi ')^T J\varphi '\phi ' = \phi '^T \varphi '^T J\varphi
736 + '\phi ' = \phi '^T J\phi ' = J,
737 + \label{introEquation:SymplecticFlowComposition}
738 + \end{equation}
739 + where $\phi$ and $\psi$ both are symplectic maps. Thus operator
740 + splitting in this context automatically generates a symplectic map.
741  
742 + The Lie-Trotter splitting(\ref{introEquation:firstOrderSplitting})
743 + introduces local errors proportional to $h^2$, while Strang
744 + splitting gives a second-order decomposition,
745 + \begin{equation}
746 + \varphi _h  = \varphi _{1,h/2}  \circ \varphi _{2,h}  \circ \varphi
747 + _{1,h/2} , \label{introEquation:secondOrderSplitting}
748 + \end{equation}
749 + which has a local error proportional to $h^3$. The Sprang
750 + splitting's popularity in molecular simulation community attribute
751 + to its symmetric property,
752 + \begin{equation}
753 + \varphi _h^{ - 1} = \varphi _{ - h}.
754 + \label{introEquation:timeReversible}
755 + \end{equation}
756 +
757 + \subsubsection{\label{introSection:exampleSplittingMethod}\textbf{Examples of the Splitting Method}}
758 + The classical equation for a system consisting of interacting
759 + particles can be written in Hamiltonian form,
760   \[
761 < L(\ddot x) = p^2 L(x) - px(0) - \dot x(0)
761 > H = T + V
762   \]
763 + where $T$ is the kinetic energy and $V$ is the potential energy.
764 + Setting $H_1 = T, H_2 = V$ and applying the Strang splitting, one
765 + obtains the following:
766 + \begin{align}
767 + q(\Delta t) &= q(0) + \dot{q}(0)\Delta t +
768 +    \frac{F[q(0)]}{m}\frac{\Delta t^2}{2}, %
769 + \label{introEquation:Lp10a} \\%
770 + %
771 + \dot{q}(\Delta t) &= \dot{q}(0) + \frac{\Delta t}{2m}
772 +    \biggl [F[q(0)] + F[q(\Delta t)] \biggr]. %
773 + \label{introEquation:Lp10b}
774 + \end{align}
775 + where $F(t)$ is the force at time $t$. This integration scheme is
776 + known as \emph{velocity verlet} which is
777 + symplectic(\ref{introEquation:SymplecticFlowComposition}),
778 + time-reversible(\ref{introEquation:timeReversible}) and
779 + volume-preserving (\ref{introEquation:volumePreserving}). These
780 + geometric properties attribute to its long-time stability and its
781 + popularity in the community. However, the most commonly used
782 + velocity verlet integration scheme is written as below,
783 + \begin{align}
784 + \dot{q}\biggl (\frac{\Delta t}{2}\biggr ) &=
785 +    \dot{q}(0) + \frac{\Delta t}{2m}\, F[q(0)], \label{introEquation:Lp9a}\\%
786 + %
787 + q(\Delta t) &= q(0) + \Delta t\, \dot{q}\biggl (\frac{\Delta t}{2}\biggr ),%
788 +    \label{introEquation:Lp9b}\\%
789 + %
790 + \dot{q}(\Delta t) &= \dot{q}\biggl (\frac{\Delta t}{2}\biggr ) +
791 +    \frac{\Delta t}{2m}\, F[q(t)]. \label{introEquation:Lp9c}
792 + \end{align}
793 + From the preceding splitting, one can see that the integration of
794 + the equations of motion would follow:
795 + \begin{enumerate}
796 + \item calculate the velocities at the half step, $\frac{\Delta t}{2}$, from the forces calculated at the initial position.
797  
798 + \item Use the half step velocities to move positions one whole step, $\Delta t$.
799 +
800 + \item Evaluate the forces at the new positions, $\mathbf{q}(\Delta t)$, and use the new forces to complete the velocity move.
801 +
802 + \item Repeat from step 1 with the new position, velocities, and forces assuming the roles of the initial values.
803 + \end{enumerate}
804 +
805 + By simply switching the order of the propagators in the splitting
806 + and composing a new integrator, the \emph{position verlet}
807 + integrator, can be generated,
808 + \begin{align}
809 + \dot q(\Delta t) &= \dot q(0) + \Delta tF(q(0))\left[ {q(0) +
810 + \frac{{\Delta t}}{{2m}}\dot q(0)} \right], %
811 + \label{introEquation:positionVerlet1} \\%
812 + %
813 + q(\Delta t) &= q(0) + \frac{{\Delta t}}{2}\left[ {\dot q(0) + \dot
814 + q(\Delta t)} \right]. %
815 + \label{introEquation:positionVerlet2}
816 + \end{align}
817 +
818 + \subsubsection{\label{introSection:errorAnalysis}\textbf{Error Analysis and Higher Order Methods}}
819 +
820 + The Baker-Campbell-Hausdorff formula can be used to determine the
821 + local error of splitting method in terms of the commutator of the
822 + operators(\ref{introEquation:exponentialOperator}) associated with
823 + the sub-flow. For operators $hX$ and $hY$ which are associated with
824 + $\varphi_1(t)$ and $\varphi_2(t)$ respectively , we have
825 + \begin{equation}
826 + \exp (hX + hY) = \exp (hZ)
827 + \end{equation}
828 + where
829 + \begin{equation}
830 + hZ = hX + hY + \frac{{h^2 }}{2}[X,Y] + \frac{{h^3 }}{2}\left(
831 + {[X,[X,Y]] + [Y,[Y,X]]} \right) +  \ldots .
832 + \end{equation}
833 + Here, $[X,Y]$ is the commutators of operator $X$ and $Y$ given by
834   \[
835 < L\left( {\int_0^t {g(t - \tau )h(\tau )d\tau } } \right) = G(p)H(p)
835 > [X,Y] = XY - YX .
836   \]
837 <
838 < Some relatively important transformation,
837 > Applying the Baker-Campbell-Hausdorff formula\cite{Varadarajan1974}
838 > to the Sprang splitting, we can obtain
839 > \begin{eqnarray*}
840 > \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 \\
841 >                                   &   & \mbox{} + h^2 [X,X]/8 + h^2 [Y,Y]/8 \\
842 >                                   &   & \mbox{} + h^3 [Y,[Y,X]]/12 - h^3[X,[X,Y]]/24 + \ldots )
843 > \end{eqnarray*}
844 > Since \[ [X,Y] + [Y,X] = 0\] and \[ [X,X] = 0,\] the dominant local
845 > error of Spring splitting is proportional to $h^3$. The same
846 > procedure can be applied to a general splitting,  of the form
847 > \begin{equation}
848 > \varphi _{b_m h}^2  \circ \varphi _{a_m h}^1  \circ \varphi _{b_{m -
849 > 1} h}^2  \circ  \ldots  \circ \varphi _{a_1 h}^1 .
850 > \end{equation}
851 > A careful choice of coefficient $a_1 \ldots b_m$ will lead to higher
852 > order methods. Yoshida proposed an elegant way to compose higher
853 > order methods based on symmetric splitting\cite{Yoshida1990}. Given
854 > a symmetric second order base method $ \varphi _h^{(2)} $, a
855 > fourth-order symmetric method can be constructed by composing,
856   \[
857 < L(\cos at) = \frac{p}{{p^2  + a^2 }}
857 > \varphi _h^{(4)}  = \varphi _{\alpha h}^{(2)}  \circ \varphi _{\beta
858 > h}^{(2)}  \circ \varphi _{\alpha h}^{(2)}
859   \]
860 <
860 > where $ \alpha  =  - \frac{{2^{1/3} }}{{2 - 2^{1/3} }}$ and $ \beta
861 > = \frac{{2^{1/3} }}{{2 - 2^{1/3} }}$. Moreover, a symmetric
862 > integrator $ \varphi _h^{(2n + 2)}$ can be composed by
863 > \begin{equation}
864 > \varphi _h^{(2n + 2)}  = \varphi _{\alpha h}^{(2n)}  \circ \varphi
865 > _{\beta h}^{(2n)}  \circ \varphi _{\alpha h}^{(2n)},
866 > \end{equation}
867 > if the weights are chosen as
868   \[
869 < L(\sin at) = \frac{a}{{p^2  + a^2 }}
869 > \alpha  =  - \frac{{2^{1/(2n + 1)} }}{{2 - 2^{1/(2n + 1)} }},\beta =
870 > \frac{{2^{1/(2n + 1)} }}{{2 - 2^{1/(2n + 1)} }} .
871   \]
872  
873 + \section{\label{introSection:molecularDynamics}Molecular Dynamics}
874 +
875 + As one of the principal tools of molecular modeling, Molecular
876 + dynamics has proven to be a powerful tool for studying the functions
877 + of biological systems, providing structural, thermodynamic and
878 + dynamical information. The basic idea of molecular dynamics is that
879 + macroscopic properties are related to microscopic behavior and
880 + microscopic behavior can be calculated from the trajectories in
881 + simulations. For instance, instantaneous temperature of an
882 + Hamiltonian system of $N$ particle can be measured by
883   \[
884 < L(1) = \frac{1}{p}
884 > T = \sum\limits_{i = 1}^N {\frac{{m_i v_i^2 }}{{fk_B }}}
885   \]
886 + where $m_i$ and $v_i$ are the mass and velocity of $i$th particle
887 + respectively, $f$ is the number of degrees of freedom, and $k_B$ is
888 + the boltzman constant.
889  
890 < First, the bath coordinates,
891 < \[
892 < p^2 L(x_\alpha  ) - px_\alpha  (0) - \dot x_\alpha  (0) =  - \omega
893 < _\alpha ^2 L(x_\alpha  ) + \frac{{g_\alpha  }}{{\omega _\alpha
894 < }}L(x)
890 > A typical molecular dynamics run consists of three essential steps:
891 > \begin{enumerate}
892 >  \item Initialization
893 >    \begin{enumerate}
894 >    \item Preliminary preparation
895 >    \item Minimization
896 >    \item Heating
897 >    \item Equilibration
898 >    \end{enumerate}
899 >  \item Production
900 >  \item Analysis
901 > \end{enumerate}
902 > These three individual steps will be covered in the following
903 > sections. Sec.~\ref{introSec:initialSystemSettings} deals with the
904 > initialization of a simulation. Sec.~\ref{introSection:production}
905 > will discusse issues in production run.
906 > Sec.~\ref{introSection:Analysis} provides the theoretical tools for
907 > trajectory analysis.
908 >
909 > \subsection{\label{introSec:initialSystemSettings}Initialization}
910 >
911 > \subsubsection{\textbf{Preliminary preparation}}
912 >
913 > When selecting the starting structure of a molecule for molecular
914 > simulation, one may retrieve its Cartesian coordinates from public
915 > databases, such as RCSB Protein Data Bank \textit{etc}. Although
916 > thousands of crystal structures of molecules are discovered every
917 > year, many more remain unknown due to the difficulties of
918 > purification and crystallization. Even for molecules with known
919 > structure, some important information is missing. For example, a
920 > missing hydrogen atom which acts as donor in hydrogen bonding must
921 > be added. Moreover, in order to include electrostatic interaction,
922 > one may need to specify the partial charges for individual atoms.
923 > Under some circumstances, we may even need to prepare the system in
924 > a special configuration. For instance, when studying transport
925 > phenomenon in membrane systems, we may prepare the lipids in a
926 > bilayer structure instead of placing lipids randomly in solvent,
927 > since we are not interested in the slow self-aggregation process.
928 >
929 > \subsubsection{\textbf{Minimization}}
930 >
931 > It is quite possible that some of molecules in the system from
932 > preliminary preparation may be overlapping with each other. This
933 > close proximity leads to high initial potential energy which
934 > consequently jeopardizes any molecular dynamics simulations. To
935 > remove these steric overlaps, one typically performs energy
936 > minimization to find a more reasonable conformation. Several energy
937 > minimization methods have been developed to exploit the energy
938 > surface and to locate the local minimum. While converging slowly
939 > near the minimum, steepest descent method is extremely robust when
940 > systems are strongly anharmonic. Thus, it is often used to refine
941 > structure from crystallographic data. Relied on the gradient or
942 > hessian, advanced methods like Newton-Raphson converge rapidly to a
943 > local minimum, but become unstable if the energy surface is far from
944 > quadratic. Another factor that must be taken into account, when
945 > choosing energy minimization method, is the size of the system.
946 > Steepest descent and conjugate gradient can deal with models of any
947 > size. Because of the limits on computer memory to store the hessian
948 > matrix and the computing power needed to diagonalized these
949 > matrices, most Newton-Raphson methods can not be used with very
950 > large systems.
951 >
952 > \subsubsection{\textbf{Heating}}
953 >
954 > Typically, Heating is performed by assigning random velocities
955 > according to a Maxwell-Boltzman distribution for a desired
956 > temperature. Beginning at a lower temperature and gradually
957 > increasing the temperature by assigning larger random velocities, we
958 > end up with setting the temperature of the system to a final
959 > temperature at which the simulation will be conducted. In heating
960 > phase, we should also keep the system from drifting or rotating as a
961 > whole. To do this, the net linear momentum and angular momentum of
962 > the system is shifted to zero after each resampling from the Maxwell
963 > -Boltzman distribution.
964 >
965 > \subsubsection{\textbf{Equilibration}}
966 >
967 > The purpose of equilibration is to allow the system to evolve
968 > spontaneously for a period of time and reach equilibrium. The
969 > procedure is continued until various statistical properties, such as
970 > temperature, pressure, energy, volume and other structural
971 > properties \textit{etc}, become independent of time. Strictly
972 > speaking, minimization and heating are not necessary, provided the
973 > equilibration process is long enough. However, these steps can serve
974 > as a means to arrive at an equilibrated structure in an effective
975 > way.
976 >
977 > \subsection{\label{introSection:production}Production}
978 >
979 > The production run is the most important step of the simulation, in
980 > which the equilibrated structure is used as a starting point and the
981 > motions of the molecules are collected for later analysis. In order
982 > to capture the macroscopic properties of the system, the molecular
983 > dynamics simulation must be performed by sampling correctly and
984 > efficiently from the relevant thermodynamic ensemble.
985 >
986 > The most expensive part of a molecular dynamics simulation is the
987 > calculation of non-bonded forces, such as van der Waals force and
988 > Coulombic forces \textit{etc}. For a system of $N$ particles, the
989 > complexity of the algorithm for pair-wise interactions is $O(N^2 )$,
990 > which making large simulations prohibitive in the absence of any
991 > algorithmic tricks.
992 >
993 > A natural approach to avoid system size issues is to represent the
994 > bulk behavior by a finite number of the particles. However, this
995 > approach will suffer from the surface effect at the edges of the
996 > simulation. To offset this, \textit{Periodic boundary conditions}
997 > (see Fig.~\ref{introFig:pbc}) is developed to simulate bulk
998 > properties with a relatively small number of particles. In this
999 > method, the simulation box is replicated throughout space to form an
1000 > infinite lattice. During the simulation, when a particle moves in
1001 > the primary cell, its image in other cells move in exactly the same
1002 > direction with exactly the same orientation. Thus, as a particle
1003 > leaves the primary cell, one of its images will enter through the
1004 > opposite face.
1005 > \begin{figure}
1006 > \centering
1007 > \includegraphics[width=\linewidth]{pbc.eps}
1008 > \caption[An illustration of periodic boundary conditions]{A 2-D
1009 > illustration of periodic boundary conditions. As one particle leaves
1010 > the left of the simulation box, an image of it enters the right.}
1011 > \label{introFig:pbc}
1012 > \end{figure}
1013 >
1014 > %cutoff and minimum image convention
1015 > Another important technique to improve the efficiency of force
1016 > evaluation is to apply spherical cutoff where particles farther than
1017 > a predetermined distance are not included in the calculation
1018 > \cite{Frenkel1996}. The use of a cutoff radius will cause a
1019 > discontinuity in the potential energy curve. Fortunately, one can
1020 > shift simple radial potential to ensure the potential curve go
1021 > smoothly to zero at the cutoff radius. The cutoff strategy works
1022 > well for Lennard-Jones interaction because of its short range
1023 > nature. However, simply truncating the electrostatic interaction
1024 > with the use of cutoffs has been shown to lead to severe artifacts
1025 > in simulations. The Ewald summation, in which the slowly decaying
1026 > Coulomb potential is transformed into direct and reciprocal sums
1027 > with rapid and absolute convergence, has proved to minimize the
1028 > periodicity artifacts in liquid simulations. Taking the advantages
1029 > of the fast Fourier transform (FFT) for calculating discrete Fourier
1030 > transforms, the particle mesh-based
1031 > methods\cite{Hockney1981,Shimada1993, Luty1994} are accelerated from
1032 > $O(N^{3/2})$ to $O(N logN)$. An alternative approach is the
1033 > \emph{fast multipole method}\cite{Greengard1987, Greengard1994},
1034 > which treats Coulombic interactions exactly at short range, and
1035 > approximate the potential at long range through multipolar
1036 > expansion. In spite of their wide acceptance at the molecular
1037 > simulation community, these two methods are difficult to implement
1038 > correctly and efficiently. Instead, we use a damped and
1039 > charge-neutralized Coulomb potential method developed by Wolf and
1040 > his coworkers\cite{Wolf1999}. The shifted Coulomb potential for
1041 > particle $i$ and particle $j$ at distance $r_{rj}$ is given by:
1042 > \begin{equation}
1043 > V(r_{ij})= \frac{q_i q_j \textrm{erfc}(\alpha
1044 > r_{ij})}{r_{ij}}-\lim_{r_{ij}\rightarrow
1045 > R_\textrm{c}}\left\{\frac{q_iq_j \textrm{erfc}(\alpha
1046 > r_{ij})}{r_{ij}}\right\}. \label{introEquation:shiftedCoulomb}
1047 > \end{equation}
1048 > where $\alpha$ is the convergence parameter. Due to the lack of
1049 > inherent periodicity and rapid convergence,this method is extremely
1050 > efficient and easy to implement.
1051 > \begin{figure}
1052 > \centering
1053 > \includegraphics[width=\linewidth]{shifted_coulomb.eps}
1054 > \caption[An illustration of shifted Coulomb potential]{An
1055 > illustration of shifted Coulomb potential.}
1056 > \label{introFigure:shiftedCoulomb}
1057 > \end{figure}
1058 >
1059 > %multiple time step
1060 >
1061 > \subsection{\label{introSection:Analysis} Analysis}
1062 >
1063 > Recently, advanced visualization technique have become applied to
1064 > monitor the motions of molecules. Although the dynamics of the
1065 > system can be described qualitatively from animation, quantitative
1066 > trajectory analysis are more useful. According to the principles of
1067 > Statistical Mechanics, Sec.~\ref{introSection:statisticalMechanics},
1068 > one can compute thermodynamic properties, analyze fluctuations of
1069 > structural parameters, and investigate time-dependent processes of
1070 > the molecule from the trajectories.
1071 >
1072 > \subsubsection{\label{introSection:thermodynamicsProperties}\textbf{Thermodynamic Properties}}
1073 >
1074 > Thermodynamic properties, which can be expressed in terms of some
1075 > function of the coordinates and momenta of all particles in the
1076 > system, can be directly computed from molecular dynamics. The usual
1077 > way to measure the pressure is based on virial theorem of Clausius
1078 > which states that the virial is equal to $-3Nk_BT$. For a system
1079 > with forces between particles, the total virial, $W$, contains the
1080 > contribution from external pressure and interaction between the
1081 > particles:
1082 > \[
1083 > W =  - 3PV + \left\langle {\sum\limits_{i < j} {r{}_{ij} \cdot
1084 > f_{ij} } } \right\rangle
1085   \]
1086 + where $f_{ij}$ is the force between particle $i$ and $j$ at a
1087 + distance $r_{ij}$. Thus, the expression for the pressure is given
1088 + by:
1089 + \begin{equation}
1090 + P = \frac{{Nk_B T}}{V} - \frac{1}{{3V}}\left\langle {\sum\limits_{i
1091 + < j} {r{}_{ij} \cdot f_{ij} } } \right\rangle
1092 + \end{equation}
1093 +
1094 + \subsubsection{\label{introSection:structuralProperties}\textbf{Structural Properties}}
1095 +
1096 + Structural Properties of a simple fluid can be described by a set of
1097 + distribution functions. Among these functions,the \emph{pair
1098 + distribution function}, also known as \emph{radial distribution
1099 + function}, is of most fundamental importance to liquid theory.
1100 + Experimentally, pair distribution function can be gathered by
1101 + Fourier transforming raw data from a series of neutron diffraction
1102 + experiments and integrating over the surface factor
1103 + \cite{Powles1973}. The experimental results can serve as a criterion
1104 + to justify the correctness of a liquid model. Moreover, various
1105 + equilibrium thermodynamic and structural properties can also be
1106 + expressed in terms of radial distribution function \cite{Allen1987}.
1107 +
1108 + The pair distribution functions $g(r)$ gives the probability that a
1109 + particle $i$ will be located at a distance $r$ from a another
1110 + particle $j$ in the system
1111   \[
1112 < L(x_\alpha  ) = \frac{{\frac{{g_\alpha  }}{{\omega _\alpha  }}L(x) +
1113 < px_\alpha  (0) + \dot x_\alpha  (0)}}{{p^2  + \omega _\alpha ^2 }}
1112 > g(r) = \frac{V}{{N^2 }}\left\langle {\sum\limits_i {\sum\limits_{j
1113 > \ne i} {\delta (r - r_{ij} )} } } \right\rangle = \frac{\rho
1114 > (r)}{\rho}.
1115   \]
1116 < Then, the system coordinates,
1117 < \begin{align}
1118 < mL(\ddot x) &=  - \frac{1}{p}\frac{{\partial W(x)}}{{\partial x}} -
1119 < \sum\limits_{\alpha  = 1}^N {\left\{ {\frac{{\frac{{g_\alpha
456 < }}{{\omega _\alpha  }}L(x) + px_\alpha  (0) + \dot x_\alpha
457 < (0)}}{{p^2  + \omega _\alpha ^2 }} - \frac{{g_\alpha ^2 }}{{m_\alpha
458 < }}\omega _\alpha ^2 L(x)} \right\}}
459 < %
460 < &= - \frac{1}{p}\frac{{\partial W(x)}}{{\partial x}} -
461 < \sum\limits_{\alpha  = 1}^N {\left\{ { - \frac{{g_\alpha ^2 }}{{m_\alpha  \omega _\alpha ^2 }}\frac{p}{{p^2  + \omega _\alpha ^2 }}pL(x)
462 < - \frac{p}{{p^2  + \omega _\alpha ^2 }}g_\alpha  x_\alpha  (0)
463 < - \frac{1}{{p^2  + \omega _\alpha ^2 }}g_\alpha  \dot x_\alpha  (0)} \right\}}
464 < \end{align}
465 < Then, the inverse transform,
1116 > Note that the delta function can be replaced by a histogram in
1117 > computer simulation. Peaks in $g(r)$ represent solvent shells, and
1118 > the height of these peaks gradually decreases to 1 as the liquid of
1119 > large distance approaches the bulk density.
1120  
467 \begin{align}
468 m\ddot x &=  - \frac{{\partial W(x)}}{{\partial x}} -
469 \sum\limits_{\alpha  = 1}^N {\left\{ {\left( { - \frac{{g_\alpha ^2
470 }}{{m_\alpha  \omega _\alpha ^2 }}} \right)\int_0^t {\cos (\omega
471 _\alpha  t)\dot x(t - \tau )d\tau  - \left[ {g_\alpha  x_\alpha  (0)
472 - \frac{{g_\alpha  }}{{m_\alpha  \omega _\alpha  }}} \right]\cos
473 (\omega _\alpha  t) - \frac{{g_\alpha  \dot x_\alpha  (0)}}{{\omega
474 _\alpha  }}\sin (\omega _\alpha  t)} } \right\}}
475 %
476 &= - \frac{{\partial W(x)}}{{\partial x}} - \int_0^t
477 {\sum\limits_{\alpha  = 1}^N {\left( { - \frac{{g_\alpha ^2
478 }}{{m_\alpha  \omega _\alpha ^2 }}} \right)\cos (\omega _\alpha
479 t)\dot x(t - \tau )d} \tau }  + \sum\limits_{\alpha  = 1}^N {\left\{
480 {\left[ {g_\alpha  x_\alpha  (0) - \frac{{g_\alpha  }}{{m_\alpha
481 \omega _\alpha  }}} \right]\cos (\omega _\alpha  t) +
482 \frac{{g_\alpha  \dot x_\alpha  (0)}}{{\omega _\alpha  }}\sin
483 (\omega _\alpha  t)} \right\}}
484 \end{align}
1121  
1122 + \subsubsection{\label{introSection:timeDependentProperties}\textbf{Time-dependent
1123 + Properties}}
1124 +
1125 + Time-dependent properties are usually calculated using \emph{time
1126 + correlation functions}, which correlate random variables $A$ and $B$
1127 + at two different times,
1128   \begin{equation}
1129 < m\ddot x =  - \frac{{\partial W}}{{\partial x}} - \int_0^t {\xi
1130 < (t)\dot x(t - \tau )d\tau }  + R(t)
489 < \label{introEuqation:GeneralizedLangevinDynamics}
1129 > C_{AB} (t) = \left\langle {A(t)B(0)} \right\rangle.
1130 > \label{introEquation:timeCorrelationFunction}
1131   \end{equation}
1132 < %where $ {\xi (t)}$ is friction kernel, $R(t)$ is random force and
1133 < %$W$ is the potential of mean force. $W(x) =  - kT\ln p(x)$
1132 > If $A$ and $B$ refer to same variable, this kind of correlation
1133 > function is called an \emph{autocorrelation function}. One example
1134 > of an auto correlation function is the velocity auto-correlation
1135 > function which is directly related to transport properties of
1136 > molecular liquids:
1137   \[
1138 < \xi (t) = \sum\limits_{\alpha  = 1}^N {\left( { - \frac{{g_\alpha ^2
1139 < }}{{m_\alpha  \omega _\alpha ^2 }}} \right)\cos (\omega _\alpha  t)}
1138 > D = \frac{1}{3}\int\limits_0^\infty  {\left\langle {v(t) \cdot v(0)}
1139 > \right\rangle } dt
1140   \]
1141 < For an infinite harmonic bath, we can use the spectral density and
1142 < an integral over frequencies.
1141 > where $D$ is diffusion constant. Unlike the velocity autocorrelation
1142 > function, which is averaging over time origins and over all the
1143 > atoms, the dipole autocorrelation functions are calculated for the
1144 > entire system. The dipole autocorrelation function is given by:
1145 > \[
1146 > c_{dipole}  = \left\langle {u_{tot} (t) \cdot u_{tot} (t)}
1147 > \right\rangle
1148 > \]
1149 > Here $u_{tot}$ is the net dipole of the entire system and is given
1150 > by
1151 > \[
1152 > u_{tot} (t) = \sum\limits_i {u_i (t)}
1153 > \]
1154 > In principle, many time correlation functions can be related with
1155 > Fourier transforms of the infrared, Raman, and inelastic neutron
1156 > scattering spectra of molecular liquids. In practice, one can
1157 > extract the IR spectrum from the intensity of dipole fluctuation at
1158 > each frequency using the following relationship:
1159 > \[
1160 > \hat c_{dipole} (v) = \int_{ - \infty }^\infty  {c_{dipole} (t)e^{ -
1161 > i2\pi vt} dt}
1162 > \]
1163  
1164 + \section{\label{introSection:rigidBody}Dynamics of Rigid Bodies}
1165 +
1166 + Rigid bodies are frequently involved in the modeling of different
1167 + areas, from engineering, physics, to chemistry. For example,
1168 + missiles and vehicle are usually modeled by rigid bodies.  The
1169 + movement of the objects in 3D gaming engine or other physics
1170 + simulator is governed by rigid body dynamics. In molecular
1171 + simulations, rigid bodies are used to simplify protein-protein
1172 + docking studies\cite{Gray2003}.
1173 +
1174 + It is very important to develop stable and efficient methods to
1175 + integrate the equations of motion for orientational degrees of
1176 + freedom. Euler angles are the natural choice to describe the
1177 + rotational degrees of freedom. However, due to $\frac {1}{sin
1178 + \theta}$ singularities, the numerical integration of corresponding
1179 + equations of motion is very inefficient and inaccurate. Although an
1180 + alternative integrator using multiple sets of Euler angles can
1181 + overcome this difficulty\cite{Barojas1973}, the computational
1182 + penalty and the loss of angular momentum conservation still remain.
1183 + A singularity-free representation utilizing quaternions was
1184 + developed by Evans in 1977\cite{Evans1977}. Unfortunately, this
1185 + approach uses a nonseparable Hamiltonian resulting from the
1186 + quaternion representation, which prevents the symplectic algorithm
1187 + to be utilized. Another different approach is to apply holonomic
1188 + constraints to the atoms belonging to the rigid body. Each atom
1189 + moves independently under the normal forces deriving from potential
1190 + energy and constraint forces which are used to guarantee the
1191 + rigidness. However, due to their iterative nature, the SHAKE and
1192 + Rattle algorithms also converge very slowly when the number of
1193 + constraints increases\cite{Ryckaert1977, Andersen1983}.
1194 +
1195 + A break-through in geometric literature suggests that, in order to
1196 + develop a long-term integration scheme, one should preserve the
1197 + symplectic structure of the flow. By introducing a conjugate
1198 + momentum to the rotation matrix $Q$ and re-formulating Hamiltonian's
1199 + equation, a symplectic integrator, RSHAKE\cite{Kol1997}, was
1200 + proposed to evolve the Hamiltonian system in a constraint manifold
1201 + by iteratively satisfying the orthogonality constraint $Q^T Q = 1$.
1202 + An alternative method using the quaternion representation was
1203 + developed by Omelyan\cite{Omelyan1998}. However, both of these
1204 + methods are iterative and inefficient. In this section, we descibe a
1205 + symplectic Lie-Poisson integrator for rigid body developed by
1206 + Dullweber and his coworkers\cite{Dullweber1997} in depth.
1207 +
1208 + \subsection{\label{introSection:constrainedHamiltonianRB}Constrained Hamiltonian for Rigid Bodies}
1209 + The motion of a rigid body is Hamiltonian with the Hamiltonian
1210 + function
1211 + \begin{equation}
1212 + H = \frac{1}{2}(p^T m^{ - 1} p) + \frac{1}{2}tr(PJ^{ - 1} P) +
1213 + V(q,Q) + \frac{1}{2}tr[(QQ^T  - 1)\Lambda ].
1214 + \label{introEquation:RBHamiltonian}
1215 + \end{equation}
1216 + Here, $q$ and $Q$  are the position and rotation matrix for the
1217 + rigid-body, $p$ and $P$  are conjugate momenta to $q$  and $Q$ , and
1218 + $J$, a diagonal matrix, is defined by
1219   \[
1220 < R(t) = \sum\limits_{\alpha  = 1}^N {\left( {g_\alpha  x_\alpha  (0)
502 < - \frac{{g_\alpha ^2 }}{{m_\alpha  \omega _\alpha ^2 }}x(0)}
503 < \right)\cos (\omega _\alpha  t)}  + \frac{{\dot x_\alpha
504 < (0)}}{{\omega _\alpha  }}\sin (\omega _\alpha  t)
1220 > I_{ii}^{ - 1}  = \frac{1}{2}\sum\limits_{i \ne j} {J_{jj}^{ - 1} }
1221   \]
1222 < The random forces depend only on initial conditions.
1222 > where $I_{ii}$ is the diagonal element of the inertia tensor. This
1223 > constrained Hamiltonian equation is subjected to a holonomic
1224 > constraint,
1225 > \begin{equation}
1226 > Q^T Q = 1, \label{introEquation:orthogonalConstraint}
1227 > \end{equation}
1228 > which is used to ensure rotation matrix's unitarity. Differentiating
1229 > \ref{introEquation:orthogonalConstraint} and using Equation
1230 > \ref{introEquation:RBMotionMomentum}, one may obtain,
1231 > \begin{equation}
1232 > Q^T PJ^{ - 1}  + J^{ - 1} P^T Q = 0 . \\
1233 > \label{introEquation:RBFirstOrderConstraint}
1234 > \end{equation}
1235  
1236 < \subsubsection{\label{introSection:secondFluctuationDissipation}The Second Fluctuation Dissipation Theorem}
1237 < So we can define a new set of coordinates,
1236 > Using Equation (\ref{introEquation:motionHamiltonianCoordinate},
1237 > \ref{introEquation:motionHamiltonianMomentum}), one can write down
1238 > the equations of motion,
1239 >
1240 > \begin{eqnarray}
1241 > \frac{{dq}}{{dt}} & = & \frac{p}{m} \label{introEquation:RBMotionPosition}\\
1242 > \frac{{dp}}{{dt}} & = & - \nabla _q V(q,Q) \label{introEquation:RBMotionMomentum}\\
1243 > \frac{{dQ}}{{dt}} & = & PJ^{ - 1}  \label{introEquation:RBMotionRotation}\\
1244 > \frac{{dP}}{{dt}} & = & - \nabla _Q V(q,Q) - 2Q\Lambda . \label{introEquation:RBMotionP}
1245 > \end{eqnarray}
1246 >
1247 > In general, there are two ways to satisfy the holonomic constraints.
1248 > We can use a constraint force provided by a Lagrange multiplier on
1249 > the normal manifold to keep the motion on constraint space. Or we
1250 > can simply evolve the system on the constraint manifold. These two
1251 > methods have been proved to be equivalent. The holonomic constraint
1252 > and equations of motions define a constraint manifold for rigid
1253 > bodies
1254   \[
1255 < q_\alpha  (t) = x_\alpha  (t) - \frac{1}{{m_\alpha  \omega _\alpha
1256 < ^2 }}x(0)
1255 > M = \left\{ {(Q,P):Q^T Q = 1,Q^T PJ^{ - 1}  + J^{ - 1} P^T Q = 0}
1256 > \right\}.
1257   \]
1258 < This makes
1258 >
1259 > Unfortunately, this constraint manifold is not the cotangent bundle
1260 > $T_{\star}SO(3)$. However, it turns out that under symplectic
1261 > transformation, the cotangent space and the phase space are
1262 > diffeomorphic. By introducing
1263   \[
1264 < R(t) = \sum\limits_{\alpha  = 1}^N {g_\alpha  q_\alpha  (t)}
1264 > \tilde Q = Q,\tilde P = \frac{1}{2}\left( {P - QP^T Q} \right),
1265   \]
1266 < And since the $q$ coordinates are harmonic oscillators,
1266 > the mechanical system subject to a holonomic constraint manifold $M$
1267 > can be re-formulated as a Hamiltonian system on the cotangent space
1268   \[
1269 < \begin{array}{l}
1270 < \left\langle {q_\alpha  (t)q_\alpha  (0)} \right\rangle  = \left\langle {q_\alpha ^2 (0)} \right\rangle \cos (\omega _\alpha  t) \\
522 < \left\langle {q_\alpha  (t)q_\beta  (0)} \right\rangle  = \delta _{\alpha \beta } \left\langle {q_\alpha  (t)q_\alpha  (0)} \right\rangle  \\
523 < \end{array}
1269 > T^* SO(3) = \left\{ {(\tilde Q,\tilde P):\tilde Q^T \tilde Q =
1270 > 1,\tilde Q^T \tilde PJ^{ - 1}  + J^{ - 1} P^T \tilde Q = 0} \right\}
1271   \]
1272  
1273 < \begin{align}
1274 < \left\langle {R(t)R(0)} \right\rangle  &= \sum\limits_\alpha
1275 < {\sum\limits_\beta  {g_\alpha  g_\beta  \left\langle {q_\alpha
1276 < (t)q_\beta  (0)} \right\rangle } }
1277 < %
1278 < &= \sum\limits_\alpha  {g_\alpha ^2 \left\langle {q_\alpha ^2 (0)}
1279 < \right\rangle \cos (\omega _\alpha  t)}
1280 < %
1281 < &= kT\xi (t)
1282 < \end{align}
1273 > For a body fixed vector $X_i$ with respect to the center of mass of
1274 > the rigid body, its corresponding lab fixed vector $X_0^{lab}$  is
1275 > given as
1276 > \begin{equation}
1277 > X_i^{lab} = Q X_i + q.
1278 > \end{equation}
1279 > Therefore, potential energy $V(q,Q)$ is defined by
1280 > \[
1281 > V(q,Q) = V(Q X_0 + q).
1282 > \]
1283 > Hence, the force and torque are given by
1284 > \[
1285 > \nabla _q V(q,Q) = F(q,Q) = \sum\limits_i {F_i (q,Q)},
1286 > \]
1287 > and
1288 > \[
1289 > \nabla _Q V(q,Q) = F(q,Q)X_i^t
1290 > \]
1291 > respectively.
1292  
1293 + As a common choice to describe the rotation dynamics of the rigid
1294 + body, the angular momentum on the body fixed frame $\Pi  = Q^t P$ is
1295 + introduced to rewrite the equations of motion,
1296   \begin{equation}
1297 < \xi (t) = \left\langle {R(t)R(0)} \right\rangle
1298 < \label{introEquation:secondFluctuationDissipation}
1297 > \begin{array}{l}
1298 > \mathop \Pi \limits^ \bullet   = J^{ - 1} \Pi ^T \Pi  + Q^T \sum\limits_i {F_i (q,Q)X_i^T }  - \Lambda  \\
1299 > \mathop Q\limits^{{\rm{   }} \bullet }  = Q\Pi {\rm{ }}J^{ - 1}  \\
1300 > \end{array}
1301 > \label{introEqaution:RBMotionPI}
1302   \end{equation}
1303 + , as well as holonomic constraints,
1304 + \[
1305 + \begin{array}{l}
1306 + \Pi J^{ - 1}  + J^{ - 1} \Pi ^t  = 0 \\
1307 + Q^T Q = 1 \\
1308 + \end{array}
1309 + \]
1310  
1311 < \section{\label{introSection:hydroynamics}Hydrodynamics}
1312 <
1313 < \subsection{\label{introSection:frictionTensor} Friction Tensor}
1314 < \subsection{\label{introSection:analyticalApproach}Analytical
1315 < Approach}
1316 <
1317 < \subsection{\label{introSection:approximationApproach}Approximation
1318 < Approach}
1311 > For a vector $v(v_1 ,v_2 ,v_3 ) \in R^3$ and a matrix $\hat v \in
1312 > so(3)^ \star$, the hat-map isomorphism,
1313 > \begin{equation}
1314 > v(v_1 ,v_2 ,v_3 ) \Leftrightarrow \hat v = \left(
1315 > {\begin{array}{*{20}c}
1316 >   0 & { - v_3 } & {v_2 }  \\
1317 >   {v_3 } & 0 & { - v_1 }  \\
1318 >   { - v_2 } & {v_1 } & 0  \\
1319 > \end{array}} \right),
1320 > \label{introEquation:hatmapIsomorphism}
1321 > \end{equation}
1322 > will let us associate the matrix products with traditional vector
1323 > operations
1324 > \[
1325 > \hat vu = v \times u
1326 > \]
1327 > Using \ref{introEqaution:RBMotionPI}, one can construct a skew
1328 > matrix,
1329 > \begin{equation}
1330 > (\mathop \Pi \limits^ \bullet   - \mathop \Pi \limits^ {\bullet  ^T}
1331 > ){\rm{ }} = {\rm{ }}(\Pi  - \Pi ^T ){\rm{ }}(J^{ - 1} \Pi  + \Pi J^{
1332 > - 1} ) + \sum\limits_i {[Q^T F_i (r,Q)X_i^T  - X_i F_i (r,Q)^T Q]} -
1333 > (\Lambda  - \Lambda ^T ) . \label{introEquation:skewMatrixPI}
1334 > \end{equation}
1335 > Since $\Lambda$ is symmetric, the last term of Equation
1336 > \ref{introEquation:skewMatrixPI} is zero, which implies the Lagrange
1337 > multiplier $\Lambda$ is absent from the equations of motion. This
1338 > unique property eliminates the requirement of iterations which can
1339 > not be avoided in other methods\cite{Kol1997, Omelyan1998}.
1340  
1341 < \subsection{\label{introSection:centersRigidBody}Centers of Rigid
1342 < Body}
1341 > Applying the hat-map isomorphism, we obtain the equation of motion
1342 > for angular momentum on body frame
1343 > \begin{equation}
1344 > \dot \pi  = \pi  \times I^{ - 1} \pi  + \sum\limits_i {\left( {Q^T
1345 > F_i (r,Q)} \right) \times X_i }.
1346 > \label{introEquation:bodyAngularMotion}
1347 > \end{equation}
1348 > In the same manner, the equation of motion for rotation matrix is
1349 > given by
1350 > \[
1351 > \dot Q = Qskew(I^{ - 1} \pi )
1352 > \]
1353 >
1354 > \subsection{\label{introSection:SymplecticFreeRB}Symplectic
1355 > Lie-Poisson Integrator for Free Rigid Body}
1356 >
1357 > If there are no external forces exerted on the rigid body, the only
1358 > contribution to the rotational motion is from the kinetic energy
1359 > (the first term of \ref{introEquation:bodyAngularMotion}). The free
1360 > rigid body is an example of a Lie-Poisson system with Hamiltonian
1361 > function
1362 > \begin{equation}
1363 > T^r (\pi ) = T_1 ^r (\pi _1 ) + T_2^r (\pi _2 ) + T_3^r (\pi _3 )
1364 > \label{introEquation:rotationalKineticRB}
1365 > \end{equation}
1366 > where $T_i^r (\pi _i ) = \frac{{\pi _i ^2 }}{{2I_i }}$ and
1367 > Lie-Poisson structure matrix,
1368 > \begin{equation}
1369 > J(\pi ) = \left( {\begin{array}{*{20}c}
1370 >   0 & {\pi _3 } & { - \pi _2 }  \\
1371 >   { - \pi _3 } & 0 & {\pi _1 }  \\
1372 >   {\pi _2 } & { - \pi _1 } & 0  \\
1373 > \end{array}} \right)
1374 > \end{equation}
1375 > Thus, the dynamics of free rigid body is governed by
1376 > \begin{equation}
1377 > \frac{d}{{dt}}\pi  = J(\pi )\nabla _\pi  T^r (\pi )
1378 > \end{equation}
1379 >
1380 > One may notice that each $T_i^r$ in Equation
1381 > \ref{introEquation:rotationalKineticRB} can be solved exactly. For
1382 > instance, the equations of motion due to $T_1^r$ are given by
1383 > \begin{equation}
1384 > \frac{d}{{dt}}\pi  = R_1 \pi ,\frac{d}{{dt}}Q = QR_1
1385 > \label{introEqaution:RBMotionSingleTerm}
1386 > \end{equation}
1387 > where
1388 > \[ R_1  = \left( {\begin{array}{*{20}c}
1389 >   0 & 0 & 0  \\
1390 >   0 & 0 & {\pi _1 }  \\
1391 >   0 & { - \pi _1 } & 0  \\
1392 > \end{array}} \right).
1393 > \]
1394 > The solutions of Equation \ref{introEqaution:RBMotionSingleTerm} is
1395 > \[
1396 > \pi (\Delta t) = e^{\Delta tR_1 } \pi (0),Q(\Delta t) =
1397 > Q(0)e^{\Delta tR_1 }
1398 > \]
1399 > with
1400 > \[
1401 > e^{\Delta tR_1 }  = \left( {\begin{array}{*{20}c}
1402 >   0 & 0 & 0  \\
1403 >   0 & {\cos \theta _1 } & {\sin \theta _1 }  \\
1404 >   0 & { - \sin \theta _1 } & {\cos \theta _1 }  \\
1405 > \end{array}} \right),\theta _1  = \frac{{\pi _1 }}{{I_1 }}\Delta t.
1406 > \]
1407 > To reduce the cost of computing expensive functions in $e^{\Delta
1408 > tR_1 }$, we can use Cayley transformation to obtain a single-aixs
1409 > propagator,
1410 > \[
1411 > e^{\Delta tR_1 }  \approx (1 - \Delta tR_1 )^{ - 1} (1 + \Delta tR_1
1412 > )
1413 > \]
1414 > The flow maps for $T_2^r$ and $T_3^r$ can be found in the same
1415 > manner. In order to construct a second-order symplectic method, we
1416 > split the angular kinetic Hamiltonian function can into five terms
1417 > \[
1418 > T^r (\pi ) = \frac{1}{2}T_1 ^r (\pi _1 ) + \frac{1}{2}T_2^r (\pi _2
1419 > ) + T_3^r (\pi _3 ) + \frac{1}{2}T_2^r (\pi _2 ) + \frac{1}{2}T_1 ^r
1420 > (\pi _1 ).
1421 > \]
1422 > By concatenating the propagators corresponding to these five terms,
1423 > we can obtain an symplectic integrator,
1424 > \[
1425 > \varphi _{\Delta t,T^r }  = \varphi _{\Delta t/2,\pi _1 }  \circ
1426 > \varphi _{\Delta t/2,\pi _2 }  \circ \varphi _{\Delta t,\pi _3 }
1427 > \circ \varphi _{\Delta t/2,\pi _2 }  \circ \varphi _{\Delta t/2,\pi
1428 > _1 }.
1429 > \]
1430 >
1431 > The non-canonical Lie-Poisson bracket ${F, G}$ of two function
1432 > $F(\pi )$ and $G(\pi )$ is defined by
1433 > \[
1434 > \{ F,G\} (\pi ) = [\nabla _\pi  F(\pi )]^T J(\pi )\nabla _\pi  G(\pi
1435 > )
1436 > \]
1437 > If the Poisson bracket of a function $F$ with an arbitrary smooth
1438 > function $G$ is zero, $F$ is a \emph{Casimir}, which is the
1439 > conserved quantity in Poisson system. We can easily verify that the
1440 > norm of the angular momentum, $\parallel \pi
1441 > \parallel$, is a \emph{Casimir}. Let$ F(\pi ) = S(\frac{{\parallel
1442 > \pi \parallel ^2 }}{2})$ for an arbitrary function $ S:R \to R$ ,
1443 > then by the chain rule
1444 > \[
1445 > \nabla _\pi  F(\pi ) = S'(\frac{{\parallel \pi \parallel ^2
1446 > }}{2})\pi
1447 > \]
1448 > Thus $ [\nabla _\pi  F(\pi )]^T J(\pi ) =  - S'(\frac{{\parallel \pi
1449 > \parallel ^2 }}{2})\pi  \times \pi  = 0 $. This explicit
1450 > Lie-Poisson integrator is found to be both extremely efficient and
1451 > stable. These properties can be explained by the fact the small
1452 > angle approximation is used and the norm of the angular momentum is
1453 > conserved.
1454 >
1455 > \subsection{\label{introSection:RBHamiltonianSplitting} Hamiltonian
1456 > Splitting for Rigid Body}
1457 >
1458 > The Hamiltonian of rigid body can be separated in terms of kinetic
1459 > energy and potential energy,
1460 > \[
1461 > H = T(p,\pi ) + V(q,Q)
1462 > \]
1463 > The equations of motion corresponding to potential energy and
1464 > kinetic energy are listed in the below table,
1465 > \begin{table}
1466 > \caption{Equations of motion due to Potential and Kinetic Energies}
1467 > \begin{center}
1468 > \begin{tabular}{|l|l|}
1469 >  \hline
1470 >  % after \\: \hline or \cline{col1-col2} \cline{col3-col4} ...
1471 >  Potential & Kinetic \\
1472 >  $\frac{{dq}}{{dt}} = \frac{p}{m}$ & $\frac{d}{{dt}}q = p$ \\
1473 >  $\frac{d}{{dt}}p =  - \frac{{\partial V}}{{\partial q}}$ & $ \frac{d}{{dt}}p = 0$ \\
1474 >  $\frac{d}{{dt}}Q = 0$ & $ \frac{d}{{dt}}Q = Qskew(I^{ - 1} j)$ \\
1475 >  $ \frac{d}{{dt}}\pi  = \sum\limits_i {\left( {Q^T F_i (r,Q)} \right) \times X_i }$ & $\frac{d}{{dt}}\pi  = \pi  \times I^{ - 1} \pi$\\
1476 >  \hline
1477 > \end{tabular}
1478 > \end{center}
1479 > \end{table}
1480 > A second-order symplectic method is now obtained by the composition
1481 > of the position and velocity propagators,
1482 > \[
1483 > \varphi _{\Delta t}  = \varphi _{\Delta t/2,V}  \circ \varphi
1484 > _{\Delta t,T}  \circ \varphi _{\Delta t/2,V}.
1485 > \]
1486 > Moreover, $\varphi _{\Delta t/2,V}$ can be divided into two
1487 > sub-propagators which corresponding to force and torque
1488 > respectively,
1489 > \[
1490 > \varphi _{\Delta t/2,V}  = \varphi _{\Delta t/2,F}  \circ \varphi
1491 > _{\Delta t/2,\tau }.
1492 > \]
1493 > Since the associated operators of $\varphi _{\Delta t/2,F} $ and
1494 > $\circ \varphi _{\Delta t/2,\tau }$ commute, the composition order
1495 > inside $\varphi _{\Delta t/2,V}$ does not matter. Furthermore, the
1496 > kinetic energy can be separated to translational kinetic term, $T^t
1497 > (p)$, and rotational kinetic term, $T^r (\pi )$,
1498 > \begin{equation}
1499 > T(p,\pi ) =T^t (p) + T^r (\pi ).
1500 > \end{equation}
1501 > where $ T^t (p) = \frac{1}{2}p^T m^{ - 1} p $ and $T^r (\pi )$ is
1502 > defined by \ref{introEquation:rotationalKineticRB}. Therefore, the
1503 > corresponding propagators are given by
1504 > \[
1505 > \varphi _{\Delta t,T}  = \varphi _{\Delta t,T^t }  \circ \varphi
1506 > _{\Delta t,T^r }.
1507 > \]
1508 > Finally, we obtain the overall symplectic propagators for freely
1509 > moving rigid bodies
1510 > \begin{equation}
1511 > \begin{array}{c}
1512 > \varphi _{\Delta t}  = \varphi _{\Delta t/2,F}  \circ \varphi _{\Delta t/2,\tau }  \\
1513 >  \circ \varphi _{\Delta t,T^t }  \circ \varphi _{\Delta t/2,\pi _1 }  \circ \varphi _{\Delta t/2,\pi _2 }  \circ \varphi _{\Delta t,\pi _3 }  \circ \varphi _{\Delta t/2,\pi _2 }  \circ \varphi _{\Delta t/2,\pi _1 }  \\
1514 >  \circ \varphi _{\Delta t/2,\tau }  \circ \varphi _{\Delta t/2,F}  .\\
1515 > \end{array}
1516 > \label{introEquation:overallRBFlowMaps}
1517 > \end{equation}
1518 >
1519 > \section{\label{introSection:langevinDynamics}Langevin Dynamics}
1520 > As an alternative to newtonian dynamics, Langevin dynamics, which
1521 > mimics a simple heat bath with stochastic and dissipative forces,
1522 > has been applied in a variety of studies. This section will review
1523 > the theory of Langevin dynamics. A brief derivation of generalized
1524 > Langevin equation will be given first. Following that, we will
1525 > discuss the physical meaning of the terms appearing in the equation
1526 > as well as the calculation of friction tensor from hydrodynamics
1527 > theory.
1528 >
1529 > \subsection{\label{introSection:generalizedLangevinDynamics}Derivation of Generalized Langevin Equation}
1530 >
1531 > A harmonic bath model, in which an effective set of harmonic
1532 > oscillators are used to mimic the effect of a linearly responding
1533 > environment, has been widely used in quantum chemistry and
1534 > statistical mechanics. One of the successful applications of
1535 > Harmonic bath model is the derivation of the Generalized Langevin
1536 > Dynamics (GLE). Lets consider a system, in which the degree of
1537 > freedom $x$ is assumed to couple to the bath linearly, giving a
1538 > Hamiltonian of the form
1539 > \begin{equation}
1540 > H = \frac{{p^2 }}{{2m}} + U(x) + H_B  + \Delta U(x,x_1 , \ldots x_N)
1541 > \label{introEquation:bathGLE}.
1542 > \end{equation}
1543 > Here $p$ is a momentum conjugate to $x$, $m$ is the mass associated
1544 > with this degree of freedom, $H_B$ is a harmonic bath Hamiltonian,
1545 > \[
1546 > H_B  = \sum\limits_{\alpha  = 1}^N {\left\{ {\frac{{p_\alpha ^2
1547 > }}{{2m_\alpha  }} + \frac{1}{2}m_\alpha  \omega _\alpha ^2 }
1548 > \right\}}
1549 > \]
1550 > where the index $\alpha$ runs over all the bath degrees of freedom,
1551 > $\omega _\alpha$ are the harmonic bath frequencies, $m_\alpha$ are
1552 > the harmonic bath masses, and $\Delta U$ is a bilinear system-bath
1553 > coupling,
1554 > \[
1555 > \Delta U =  - \sum\limits_{\alpha  = 1}^N {g_\alpha  x_\alpha  x}
1556 > \]
1557 > where $g_\alpha$ are the coupling constants between the bath
1558 > coordinates ($x_ \alpha$) and the system coordinate ($x$).
1559 > Introducing
1560 > \[
1561 > W(x) = U(x) - \sum\limits_{\alpha  = 1}^N {\frac{{g_\alpha ^2
1562 > }}{{2m_\alpha  w_\alpha ^2 }}} x^2
1563 > \] and combining the last two terms in Equation
1564 > \ref{introEquation:bathGLE}, we may rewrite the Harmonic bath
1565 > Hamiltonian as
1566 > \[
1567 > H = \frac{{p^2 }}{{2m}} + W(x) + \sum\limits_{\alpha  = 1}^N
1568 > {\left\{ {\frac{{p_\alpha ^2 }}{{2m_\alpha  }} + \frac{1}{2}m_\alpha
1569 > w_\alpha ^2 \left( {x_\alpha   - \frac{{g_\alpha  }}{{m_\alpha
1570 > w_\alpha ^2 }}x} \right)^2 } \right\}}
1571 > \]
1572 > Since the first two terms of the new Hamiltonian depend only on the
1573 > system coordinates, we can get the equations of motion for
1574 > Generalized Langevin Dynamics by Hamilton's equations,
1575 > \begin{equation}
1576 > m\ddot x =  - \frac{{\partial W(x)}}{{\partial x}} -
1577 > \sum\limits_{\alpha  = 1}^N {g_\alpha  \left( {x_\alpha   -
1578 > \frac{{g_\alpha  }}{{m_\alpha  w_\alpha ^2 }}x} \right)},
1579 > \label{introEquation:coorMotionGLE}
1580 > \end{equation}
1581 > and
1582 > \begin{equation}
1583 > m\ddot x_\alpha   =  - m_\alpha  w_\alpha ^2 \left( {x_\alpha   -
1584 > \frac{{g_\alpha  }}{{m_\alpha  w_\alpha ^2 }}x} \right).
1585 > \label{introEquation:bathMotionGLE}
1586 > \end{equation}
1587 >
1588 > In order to derive an equation for $x$, the dynamics of the bath
1589 > variables $x_\alpha$ must be solved exactly first. As an integral
1590 > transform which is particularly useful in solving linear ordinary
1591 > differential equations,the Laplace transform is the appropriate tool
1592 > to solve this problem. The basic idea is to transform the difficult
1593 > differential equations into simple algebra problems which can be
1594 > solved easily. Then, by applying the inverse Laplace transform, also
1595 > known as the Bromwich integral, we can retrieve the solutions of the
1596 > original problems.
1597 >
1598 > Let $f(t)$ be a function defined on $ [0,\infty ) $. The Laplace
1599 > transform of f(t) is a new function defined as
1600 > \[
1601 > L(f(t)) \equiv F(p) = \int_0^\infty  {f(t)e^{ - pt} dt}
1602 > \]
1603 > where  $p$ is real and  $L$ is called the Laplace Transform
1604 > Operator. Below are some important properties of Laplace transform
1605 >
1606 > \begin{eqnarray*}
1607 > L(x + y)  & = & L(x) + L(y) \\
1608 > L(ax)     & = & aL(x) \\
1609 > L(\dot x) & = & pL(x) - px(0) \\
1610 > L(\ddot x)& = & p^2 L(x) - px(0) - \dot x(0) \\
1611 > L\left( {\int_0^t {g(t - \tau )h(\tau )d\tau } } \right)& = & G(p)H(p) \\
1612 > \end{eqnarray*}
1613 >
1614 >
1615 > Applying the Laplace transform to the bath coordinates, we obtain
1616 > \begin{eqnarray*}
1617 > 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) \\
1618 > L(x_\alpha  ) & = & \frac{{\frac{{g_\alpha  }}{{\omega _\alpha  }}L(x) + px_\alpha  (0) + \dot x_\alpha  (0)}}{{p^2  + \omega _\alpha ^2 }} \\
1619 > \end{eqnarray*}
1620 >
1621 > By the same way, the system coordinates become
1622 > \begin{eqnarray*}
1623 > mL(\ddot x) & = & - \frac{1}{p}\frac{{\partial W(x)}}{{\partial x}} \\
1624 >  & & \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\}}  \\
1625 > \end{eqnarray*}
1626 >
1627 > With the help of some relatively important inverse Laplace
1628 > transformations:
1629 > \[
1630 > \begin{array}{c}
1631 > L(\cos at) = \frac{p}{{p^2  + a^2 }} \\
1632 > L(\sin at) = \frac{a}{{p^2  + a^2 }} \\
1633 > L(1) = \frac{1}{p} \\
1634 > \end{array}
1635 > \]
1636 > , we obtain
1637 > \begin{eqnarray*}
1638 > m\ddot x & =  & - \frac{{\partial W(x)}}{{\partial x}} -
1639 > \sum\limits_{\alpha  = 1}^N {\left\{ {\left( { - \frac{{g_\alpha ^2
1640 > }}{{m_\alpha  \omega _\alpha ^2 }}} \right)\int_0^t {\cos (\omega
1641 > _\alpha  t)\dot x(t - \tau )d\tau } } \right\}}  \\
1642 > & & + \sum\limits_{\alpha  = 1}^N {\left\{ {\left[ {g_\alpha
1643 > x_\alpha (0) - \frac{{g_\alpha  }}{{m_\alpha  \omega _\alpha  }}}
1644 > \right]\cos (\omega _\alpha  t) + \frac{{g_\alpha  \dot x_\alpha
1645 > (0)}}{{\omega _\alpha  }}\sin (\omega _\alpha  t)} \right\}}
1646 > \end{eqnarray*}
1647 > \begin{eqnarray*}
1648 > m\ddot x & = & - \frac{{\partial W(x)}}{{\partial x}} - \int_0^t
1649 > {\sum\limits_{\alpha  = 1}^N {\left( { - \frac{{g_\alpha ^2
1650 > }}{{m_\alpha  \omega _\alpha ^2 }}} \right)\cos (\omega _\alpha
1651 > t)\dot x(t - \tau )d} \tau }  \\
1652 > & & + \sum\limits_{\alpha  = 1}^N {\left\{ {\left[ {g_\alpha
1653 > x_\alpha (0) - \frac{{g_\alpha }}{{m_\alpha \omega _\alpha  }}}
1654 > \right]\cos (\omega _\alpha  t) + \frac{{g_\alpha  \dot x_\alpha
1655 > (0)}}{{\omega _\alpha  }}\sin (\omega _\alpha  t)} \right\}}
1656 > \end{eqnarray*}
1657 > Introducing a \emph{dynamic friction kernel}
1658 > \begin{equation}
1659 > \xi (t) = \sum\limits_{\alpha  = 1}^N {\left( { - \frac{{g_\alpha ^2
1660 > }}{{m_\alpha  \omega _\alpha ^2 }}} \right)\cos (\omega _\alpha  t)}
1661 > \label{introEquation:dynamicFrictionKernelDefinition}
1662 > \end{equation}
1663 > and \emph{a random force}
1664 > \begin{equation}
1665 > R(t) = \sum\limits_{\alpha  = 1}^N {\left( {g_\alpha  x_\alpha  (0)
1666 > - \frac{{g_\alpha ^2 }}{{m_\alpha  \omega _\alpha ^2 }}x(0)}
1667 > \right)\cos (\omega _\alpha  t)}  + \frac{{\dot x_\alpha
1668 > (0)}}{{\omega _\alpha  }}\sin (\omega _\alpha  t),
1669 > \label{introEquation:randomForceDefinition}
1670 > \end{equation}
1671 > the equation of motion can be rewritten as
1672 > \begin{equation}
1673 > m\ddot x =  - \frac{{\partial W}}{{\partial x}} - \int_0^t {\xi
1674 > (t)\dot x(t - \tau )d\tau }  + R(t)
1675 > \label{introEuqation:GeneralizedLangevinDynamics}
1676 > \end{equation}
1677 > which is known as the \emph{generalized Langevin equation}.
1678 >
1679 > \subsubsection{\label{introSection:randomForceDynamicFrictionKernel}\textbf{Random Force and Dynamic Friction Kernel}}
1680 >
1681 > One may notice that $R(t)$ depends only on initial conditions, which
1682 > implies it is completely deterministic within the context of a
1683 > harmonic bath. However, it is easy to verify that $R(t)$ is totally
1684 > uncorrelated to $x$ and $\dot x$,
1685 > \[
1686 > \begin{array}{l}
1687 > \left\langle {x(t)R(t)} \right\rangle  = 0, \\
1688 > \left\langle {\dot x(t)R(t)} \right\rangle  = 0. \\
1689 > \end{array}
1690 > \]
1691 > This property is what we expect from a truly random process. As long
1692 > as the model chosen for $R(t)$ was a gaussian distribution in
1693 > general, the stochastic nature of the GLE still remains.
1694 >
1695 > %dynamic friction kernel
1696 > The convolution integral
1697 > \[
1698 > \int_0^t {\xi (t)\dot x(t - \tau )d\tau }
1699 > \]
1700 > depends on the entire history of the evolution of $x$, which implies
1701 > that the bath retains memory of previous motions. In other words,
1702 > the bath requires a finite time to respond to change in the motion
1703 > of the system. For a sluggish bath which responds slowly to changes
1704 > in the system coordinate, we may regard $\xi(t)$ as a constant
1705 > $\xi(t) = \Xi_0$. Hence, the convolution integral becomes
1706 > \[
1707 > \int_0^t {\xi (t)\dot x(t - \tau )d\tau }  = \xi _0 (x(t) - x(0))
1708 > \]
1709 > and Equation \ref{introEuqation:GeneralizedLangevinDynamics} becomes
1710 > \[
1711 > m\ddot x =  - \frac{\partial }{{\partial x}}\left( {W(x) +
1712 > \frac{1}{2}\xi _0 (x - x_0 )^2 } \right) + R(t),
1713 > \]
1714 > which can be used to describe the effect of dynamic caging in
1715 > viscous solvents. The other extreme is the bath that responds
1716 > infinitely quickly to motions in the system. Thus, $\xi (t)$ can be
1717 > taken as a $delta$ function in time:
1718 > \[
1719 > \xi (t) = 2\xi _0 \delta (t)
1720 > \]
1721 > Hence, the convolution integral becomes
1722 > \[
1723 > \int_0^t {\xi (t)\dot x(t - \tau )d\tau }  = 2\xi _0 \int_0^t
1724 > {\delta (t)\dot x(t - \tau )d\tau }  = \xi _0 \dot x(t),
1725 > \]
1726 > and Equation \ref{introEuqation:GeneralizedLangevinDynamics} becomes
1727 > \begin{equation}
1728 > m\ddot x =  - \frac{{\partial W(x)}}{{\partial x}} - \xi _0 \dot
1729 > x(t) + R(t) \label{introEquation:LangevinEquation}
1730 > \end{equation}
1731 > which is known as the Langevin equation. The static friction
1732 > coefficient $\xi _0$ can either be calculated from spectral density
1733 > or be determined by Stokes' law for regular shaped particles. A
1734 > briefly review on calculating friction tensor for arbitrary shaped
1735 > particles is given in Sec.~\ref{introSection:frictionTensor}.
1736 >
1737 > \subsubsection{\label{introSection:secondFluctuationDissipation}\textbf{The Second Fluctuation Dissipation Theorem}}
1738 >
1739 > Defining a new set of coordinates,
1740 > \[
1741 > q_\alpha  (t) = x_\alpha  (t) - \frac{1}{{m_\alpha  \omega _\alpha
1742 > ^2 }}x(0)
1743 > \],
1744 > we can rewrite $R(T)$ as
1745 > \[
1746 > R(t) = \sum\limits_{\alpha  = 1}^N {g_\alpha  q_\alpha  (t)}.
1747 > \]
1748 > And since the $q$ coordinates are harmonic oscillators,
1749 >
1750 > \begin{eqnarray*}
1751 > \left\langle {q_\alpha ^2 } \right\rangle  & = & \frac{{kT}}{{m_\alpha  \omega _\alpha ^2 }} \\
1752 > \left\langle {q_\alpha  (t)q_\alpha  (0)} \right\rangle & = & \left\langle {q_\alpha ^2 (0)} \right\rangle \cos (\omega _\alpha  t) \\
1753 > \left\langle {q_\alpha  (t)q_\beta  (0)} \right\rangle & = &\delta _{\alpha \beta } \left\langle {q_\alpha  (t)q_\alpha  (0)} \right\rangle  \\
1754 > \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 } }  \\
1755 >  & = &\sum\limits_\alpha  {g_\alpha ^2 \left\langle {q_\alpha ^2 (0)} \right\rangle \cos (\omega _\alpha  t)}  \\
1756 >  & = &kT\xi (t) \\
1757 > \end{eqnarray*}
1758 >
1759 > Thus, we recover the \emph{second fluctuation dissipation theorem}
1760 > \begin{equation}
1761 > \xi (t) = \left\langle {R(t)R(0)} \right\rangle
1762 > \label{introEquation:secondFluctuationDissipation}.
1763 > \end{equation}
1764 > In effect, it acts as a constraint on the possible ways in which one
1765 > can model the random force and friction kernel.

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