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1 \chapter{\label{chapt:introduction}INTRODUCTION AND THEORETICAL BACKGROUND}
2
3 \section{\label{introSection:classicalMechanics}Classical
4 Mechanics}
5
6 Using equations of motion derived from Classical Mechanics,
7 Molecular Dynamics simulations are carried out by integrating the
8 equations of motion for a given system of particles. There are three
9 fundamental ideas behind classical mechanics. Firstly, one can
10 determine the state of a mechanical system at any time of interest;
11 Secondly, all the mechanical properties of the system at that time
12 can be determined by combining the knowledge of the properties of
13 the system with the specification of this state; Finally, the
14 specification of the state when further combined with the laws of
15 mechanics will also be sufficient to predict the future behavior of
16 the system.
17
18 \subsection{\label{introSection:newtonian}Newtonian Mechanics}
19 The discovery of Newton's three laws of mechanics which govern the
20 motion of particles is the foundation of the classical mechanics.
21 Newton's first law defines a class of inertial frames. Inertial
22 frames are reference frames where a particle not interacting with
23 other bodies will move with constant speed in the same direction.
24 With respect to inertial frames, Newton's second law has the form
25 \begin{equation}
26 F = \frac {dp}{dt} = \frac {mdv}{dt}
27 \label{introEquation:newtonSecondLaw}
28 \end{equation}
29 A point mass interacting with other bodies moves with the
30 acceleration along the direction of the force acting on it. Let
31 $F_{ij}$ be the force that particle $i$ exerts on particle $j$, and
32 $F_{ji}$ be the force that particle $j$ exerts on particle $i$.
33 Newton's third law states that
34 \begin{equation}
35 F_{ij} = -F_{ji}.
36 \label{introEquation:newtonThirdLaw}
37 \end{equation}
38 Conservation laws of Newtonian Mechanics play very important roles
39 in solving mechanics problems. The linear momentum of a particle is
40 conserved if it is free or it experiences no force. The second
41 conservation theorem concerns the angular momentum of a particle.
42 The angular momentum $L$ of a particle with respect to an origin
43 from which $r$ is measured is defined to be
44 \begin{equation}
45 L \equiv r \times p \label{introEquation:angularMomentumDefinition}
46 \end{equation}
47 The torque $\tau$ with respect to the same origin is defined to be
48 \begin{equation}
49 \tau \equiv r \times F \label{introEquation:torqueDefinition}
50 \end{equation}
51 Differentiating Eq.~\ref{introEquation:angularMomentumDefinition},
52 \[
53 \dot L = \frac{d}{{dt}}(r \times p) = (\dot r \times p) + (r \times
54 \dot p)
55 \]
56 since
57 \[
58 \dot r \times p = \dot r \times mv = m\dot r \times \dot r \equiv 0
59 \]
60 thus,
61 \begin{equation}
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
66 that if all forces are conservative, energy is conserved,
67 \begin{equation}E = T + V. \label{introEquation:energyConservation}
68 \end{equation}
69 All of these conserved quantities are important factors to determine
70 the quality of numerical integration schemes for rigid bodies
71 \cite{Dullweber1997}.
72
73 \subsection{\label{introSection:lagrangian}Lagrangian Mechanics}
74
75 Newtonian Mechanics suffers from an important limitation: motion can
76 only be described in cartesian coordinate systems which make it
77 impossible to predict analytically the properties of the system even
78 if we know all of the details of the interaction. In order to
79 overcome some of the practical difficulties which arise in attempts
80 to apply Newton's equation to complex systems, approximate numerical
81 procedures may be developed.
82
83 \subsubsection{\label{introSection:halmiltonPrinciple}\textbf{Hamilton's
84 Principle}}
85
86 Hamilton introduced the dynamical principle upon which it is
87 possible to base all of mechanics and most of classical physics.
88 Hamilton's Principle may be stated as follows: the trajectory, along
89 which a dynamical system may move from one point to another within a
90 specified time, is derived by finding the path which minimizes the
91 time integral of the difference between the kinetic $K$, and
92 potential energies $U$,
93 \begin{equation}
94 \delta \int_{t_1 }^{t_2 } {(K - U)dt = 0}.
95 \label{introEquation:halmitonianPrinciple1}
96 \end{equation}
97 For simple mechanical systems, where the forces acting on the
98 different parts are derivable from a potential, the Lagrangian
99 function $L$ can be defined as the difference between the kinetic
100 energy of the system and its potential energy,
101 \begin{equation}
102 L \equiv K - U = L(q_i ,\dot q_i ).
103 \label{introEquation:lagrangianDef}
104 \end{equation}
105 Thus, Eq.~\ref{introEquation:halmitonianPrinciple1} becomes
106 \begin{equation}
107 \delta \int_{t_1 }^{t_2 } {L dt = 0} .
108 \label{introEquation:halmitonianPrinciple2}
109 \end{equation}
110
111 \subsubsection{\label{introSection:equationOfMotionLagrangian}\textbf{The
112 Equations of Motion in Lagrangian Mechanics}}
113
114 For a system of $f$ degrees of freedom, the equations of motion in
115 the Lagrangian form is
116 \begin{equation}
117 \frac{d}{{dt}}\frac{{\partial L}}{{\partial \dot q_i }} -
118 \frac{{\partial L}}{{\partial q_i }} = 0,{\rm{ }}i = 1, \ldots,f
119 \label{introEquation:eqMotionLagrangian}
120 \end{equation}
121 where $q_{i}$ is generalized coordinate and $\dot{q_{i}}$ is
122 generalized velocity.
123
124 \subsection{\label{introSection:hamiltonian}Hamiltonian Mechanics}
125
126 Arising from Lagrangian Mechanics, Hamiltonian Mechanics was
127 introduced by William Rowan Hamilton in 1833 as a re-formulation of
128 classical mechanics. If the potential energy of a system is
129 independent of velocities, the momenta can be defined as
130 \begin{equation}
131 p_i = \frac{\partial L}{\partial \dot q_i}
132 \label{introEquation:generalizedMomenta}
133 \end{equation}
134 The Lagrange equations of motion are then expressed by
135 \begin{equation}
136 p_i = \frac{{\partial L}}{{\partial q_i }}
137 \label{introEquation:generalizedMomentaDot}
138 \end{equation}
139 With the help of the generalized momenta, we may now define a new
140 quantity $H$ by the equation
141 \begin{equation}
142 H = \sum\limits_k {p_k \dot q_k } - L ,
143 \label{introEquation:hamiltonianDefByLagrangian}
144 \end{equation}
145 where $ \dot q_1 \ldots \dot q_f $ are generalized velocities and
146 $L$ is the Lagrangian function for the system. Differentiating
147 Eq.~\ref{introEquation:hamiltonianDefByLagrangian}, one can obtain
148 \begin{equation}
149 dH = \sum\limits_k {\left( {p_k d\dot q_k + \dot q_k dp_k -
150 \frac{{\partial L}}{{\partial q_k }}dq_k - \frac{{\partial
151 L}}{{\partial \dot q_k }}d\dot q_k } \right)} - \frac{{\partial
152 L}}{{\partial t}}dt . \label{introEquation:diffHamiltonian1}
153 \end{equation}
154 Making use of Eq.~\ref{introEquation:generalizedMomenta}, the second
155 and fourth terms in the parentheses cancel. Therefore,
156 Eq.~\ref{introEquation:diffHamiltonian1} can be rewritten as
157 \begin{equation}
158 dH = \sum\limits_k {\left( {\dot q_k dp_k - \dot p_k dq_k }
159 \right)} - \frac{{\partial L}}{{\partial t}}dt .
160 \label{introEquation:diffHamiltonian2}
161 \end{equation}
162 By identifying the coefficients of $dq_k$, $dp_k$ and dt, we can
163 find
164 \begin{equation}
165 \frac{{\partial H}}{{\partial p_k }} = \dot {q_k}
166 \label{introEquation:motionHamiltonianCoordinate}
167 \end{equation}
168 \begin{equation}
169 \frac{{\partial H}}{{\partial q_k }} = - \dot {p_k}
170 \label{introEquation:motionHamiltonianMomentum}
171 \end{equation}
172 and
173 \begin{equation}
174 \frac{{\partial H}}{{\partial t}} = - \frac{{\partial L}}{{\partial
175 t}}
176 \label{introEquation:motionHamiltonianTime}
177 \end{equation}
178 where Eq.~\ref{introEquation:motionHamiltonianCoordinate} and
179 Eq.~\ref{introEquation:motionHamiltonianMomentum} are Hamilton's
180 equation of motion. Due to their symmetrical formula, they are also
181 known as the canonical equations of motions \cite{Goldstein2001}.
182
183 An important difference between Lagrangian approach and the
184 Hamiltonian approach is that the Lagrangian is considered to be a
185 function of the generalized velocities $\dot q_i$ and coordinates
186 $q_i$, while the Hamiltonian is considered to be a function of the
187 generalized momenta $p_i$ and the conjugate coordinates $q_i$.
188 Hamiltonian Mechanics is more appropriate for application to
189 statistical mechanics and quantum mechanics, since it treats the
190 coordinate and its time derivative as independent variables and it
191 only works with 1st-order differential equations\cite{Marion1990}.
192 In Newtonian Mechanics, a system described by conservative forces
193 conserves the total energy
194 (Eq.~\ref{introEquation:energyConservation}). It follows that
195 Hamilton's equations of motion conserve the total Hamiltonian
196 \begin{equation}
197 \frac{{dH}}{{dt}} = \sum\limits_i {\left( {\frac{{\partial
198 H}}{{\partial q_i }}\dot q_i + \frac{{\partial H}}{{\partial p_i
199 }}\dot p_i } \right)} = \sum\limits_i {\left( {\frac{{\partial
200 H}}{{\partial q_i }}\frac{{\partial H}}{{\partial p_i }} -
201 \frac{{\partial H}}{{\partial p_i }}\frac{{\partial H}}{{\partial
202 q_i }}} \right) = 0}. \label{introEquation:conserveHalmitonian}
203 \end{equation}
204
205 \section{\label{introSection:statisticalMechanics}Statistical
206 Mechanics}
207
208 The thermodynamic behaviors and properties of Molecular Dynamics
209 simulation are governed by the principle of Statistical Mechanics.
210 The following section will give a brief introduction to some of the
211 Statistical Mechanics concepts and theorem presented in this
212 dissertation.
213
214 \subsection{\label{introSection:ensemble}Phase Space and Ensemble}
215
216 Mathematically, phase space is the space which represents all
217 possible states of a system. Each possible state of the system
218 corresponds to one unique point in the phase space. For mechanical
219 systems, the phase space usually consists of all possible values of
220 position and momentum variables. Consider a dynamic system of $f$
221 particles in a cartesian space, where each of the $6f$ coordinates
222 and momenta is assigned to one of $6f$ mutually orthogonal axes, the
223 phase space of this system is a $6f$ dimensional space. A point, $x
224 =
225 (\mathord{\buildrel{\lower3pt\hbox{$\scriptscriptstyle\rightharpoonup$}}
226 \over q} _1 , \ldots
227 ,\mathord{\buildrel{\lower3pt\hbox{$\scriptscriptstyle\rightharpoonup$}}
228 \over q} _f
229 ,\mathord{\buildrel{\lower3pt\hbox{$\scriptscriptstyle\rightharpoonup$}}
230 \over p} _1 \ldots
231 ,\mathord{\buildrel{\lower3pt\hbox{$\scriptscriptstyle\rightharpoonup$}}
232 \over p} _f )$ , with a unique set of values of $6f$ coordinates and
233 momenta is a phase space vector.
234 %%%fix me
235
236 In statistical mechanics, the condition of an ensemble at any time
237 can be regarded as appropriately specified by the density $\rho$
238 with which representative points are distributed over the phase
239 space. The density distribution for an ensemble with $f$ degrees of
240 freedom is defined as,
241 \begin{equation}
242 \rho = \rho (q_1 , \ldots ,q_f ,p_1 , \ldots ,p_f ,t).
243 \label{introEquation:densityDistribution}
244 \end{equation}
245 Governed by the principles of mechanics, the phase points change
246 their locations which changes the density at any time at phase
247 space. Hence, the density distribution is also to be taken as a
248 function of the time. The number of systems $\delta N$ at time $t$
249 can be determined by,
250 \begin{equation}
251 \delta N = \rho (q,p,t)dq_1 \ldots dq_f dp_1 \ldots dp_f.
252 \label{introEquation:deltaN}
253 \end{equation}
254 Assuming enough copies of the systems, we can sufficiently
255 approximate $\delta N$ without introducing discontinuity when we go
256 from one region in the phase space to another. By integrating over
257 the whole phase space,
258 \begin{equation}
259 N = \int { \ldots \int {\rho (q,p,t)dq_1 } ...dq_f dp_1 } ...dp_f
260 \label{introEquation:totalNumberSystem}
261 \end{equation}
262 gives us an expression for the total number of copies. Hence, the
263 probability per unit volume in the phase space can be obtained by,
264 \begin{equation}
265 \frac{{\rho (q,p,t)}}{N} = \frac{{\rho (q,p,t)}}{{\int { \ldots \int
266 {\rho (q,p,t)dq_1 } ...dq_f dp_1 } ...dp_f }}.
267 \label{introEquation:unitProbability}
268 \end{equation}
269 With the help of Eq.~\ref{introEquation:unitProbability} and the
270 knowledge of the system, it is possible to calculate the average
271 value of any desired quantity which depends on the coordinates and
272 momenta of the system. Even when the dynamics of the real system are
273 complex, or stochastic, or even discontinuous, the average
274 properties of the ensemble of possibilities as a whole remain well
275 defined. For a classical system in thermal equilibrium with its
276 environment, the ensemble average of a mechanical quantity, $\langle
277 A(q , p) \rangle_t$, takes the form of an integral over the phase
278 space of the system,
279 \begin{equation}
280 \langle A(q , p) \rangle_t = \frac{{\int { \ldots \int {A(q,p)\rho
281 (q,p,t)dq_1 } ...dq_f dp_1 } ...dp_f }}{{\int { \ldots \int {\rho
282 (q,p,t)dq_1 } ...dq_f dp_1 } ...dp_f }}.
283 \label{introEquation:ensembelAverage}
284 \end{equation}
285
286 There are several different types of ensembles with different
287 statistical characteristics. As a function of macroscopic
288 parameters, such as temperature \textit{etc}, the partition function
289 can be used to describe the statistical properties of a system in
290 thermodynamic equilibrium. As an ensemble of systems, each of which
291 is known to be thermally isolated and conserve energy, the
292 Microcanonical ensemble (NVE) has a partition function like,
293 \begin{equation}
294 \Omega (N,V,E) = e^{\beta TS}. \label{introEquation:NVEPartition}
295 \end{equation}
296 A canonical ensemble (NVT) is an ensemble of systems, each of which
297 can share its energy with a large heat reservoir. The distribution
298 of the total energy amongst the possible dynamical states is given
299 by the partition function,
300 \begin{equation}
301 \Omega (N,V,T) = e^{ - \beta A}.
302 \label{introEquation:NVTPartition}
303 \end{equation}
304 Here, $A$ is the Helmholtz free energy which is defined as $ A = U -
305 TS$. Since most experiments are carried out under constant pressure
306 condition, the isothermal-isobaric ensemble (NPT) plays a very
307 important role in molecular simulations. The isothermal-isobaric
308 ensemble allow the system to exchange energy with a heat bath of
309 temperature $T$ and to change the volume as well. Its partition
310 function is given as
311 \begin{equation}
312 \Delta (N,P,T) = - e^{\beta G}.
313 \label{introEquation:NPTPartition}
314 \end{equation}
315 Here, $G = U - TS + PV$, and $G$ is called Gibbs free energy.
316
317 \subsection{\label{introSection:liouville}Liouville's theorem}
318
319 Liouville's theorem is the foundation on which statistical mechanics
320 rests. It describes the time evolution of the phase space
321 distribution function. In order to calculate the rate of change of
322 $\rho$, we begin from Eq.~\ref{introEquation:deltaN}. If we consider
323 the two faces perpendicular to the $q_1$ axis, which are located at
324 $q_1$ and $q_1 + \delta q_1$, the number of phase points leaving the
325 opposite face is given by the expression,
326 \begin{equation}
327 \left( {\rho + \frac{{\partial \rho }}{{\partial q_1 }}\delta q_1 }
328 \right)\left( {\dot q_1 + \frac{{\partial \dot q_1 }}{{\partial q_1
329 }}\delta q_1 } \right)\delta q_2 \ldots \delta q_f \delta p_1
330 \ldots \delta p_f .
331 \end{equation}
332 Summing all over the phase space, we obtain
333 \begin{equation}
334 \frac{{d(\delta N)}}{{dt}} = - \sum\limits_{i = 1}^f {\left[ {\rho
335 \left( {\frac{{\partial \dot q_i }}{{\partial q_i }} +
336 \frac{{\partial \dot p_i }}{{\partial p_i }}} \right) + \left(
337 {\frac{{\partial \rho }}{{\partial q_i }}\dot q_i + \frac{{\partial
338 \rho }}{{\partial p_i }}\dot p_i } \right)} \right]} \delta q_1
339 \ldots \delta q_f \delta p_1 \ldots \delta p_f .
340 \end{equation}
341 Differentiating the equations of motion in Hamiltonian formalism
342 (\ref{introEquation:motionHamiltonianCoordinate},
343 \ref{introEquation:motionHamiltonianMomentum}), we can show,
344 \begin{equation}
345 \sum\limits_i {\left( {\frac{{\partial \dot q_i }}{{\partial q_i }}
346 + \frac{{\partial \dot p_i }}{{\partial p_i }}} \right)} = 0 ,
347 \end{equation}
348 which cancels the first terms of the right hand side. Furthermore,
349 dividing $ \delta q_1 \ldots \delta q_f \delta p_1 \ldots \delta
350 p_f $ in both sides, we can write out Liouville's theorem in a
351 simple form,
352 \begin{equation}
353 \frac{{\partial \rho }}{{\partial t}} + \sum\limits_{i = 1}^f
354 {\left( {\frac{{\partial \rho }}{{\partial q_i }}\dot q_i +
355 \frac{{\partial \rho }}{{\partial p_i }}\dot p_i } \right)} = 0 .
356 \label{introEquation:liouvilleTheorem}
357 \end{equation}
358 Liouville's theorem states that the distribution function is
359 constant along any trajectory in phase space. In classical
360 statistical mechanics, since the number of system copies in an
361 ensemble is huge and constant, we can assume the local density has
362 no reason (other than classical mechanics) to change,
363 \begin{equation}
364 \frac{{\partial \rho }}{{\partial t}} = 0.
365 \label{introEquation:stationary}
366 \end{equation}
367 In such stationary system, the density of distribution $\rho$ can be
368 connected to the Hamiltonian $H$ through Maxwell-Boltzmann
369 distribution,
370 \begin{equation}
371 \rho \propto e^{ - \beta H}
372 \label{introEquation:densityAndHamiltonian}
373 \end{equation}
374
375 \subsubsection{\label{introSection:phaseSpaceConservation}\textbf{Conservation of Phase Space}}
376 Lets consider a region in the phase space,
377 \begin{equation}
378 \delta v = \int { \ldots \int {dq_1 } ...dq_f dp_1 } ..dp_f .
379 \end{equation}
380 If this region is small enough, the density $\rho$ can be regarded
381 as uniform over the whole integral. Thus, the number of phase points
382 inside this region is given by,
383 \begin{equation}
384 \delta N = \rho \delta v = \rho \int { \ldots \int {dq_1 } ...dq_f
385 dp_1 } ..dp_f.
386 \end{equation}
387
388 \begin{equation}
389 \frac{{d(\delta N)}}{{dt}} = \frac{{d\rho }}{{dt}}\delta v + \rho
390 \frac{d}{{dt}}(\delta v) = 0.
391 \end{equation}
392 With the help of the stationary assumption
393 (Eq.~\ref{introEquation:stationary}), we obtain the principle of
394 \emph{conservation of volume in phase space},
395 \begin{equation}
396 \frac{d}{{dt}}(\delta v) = \frac{d}{{dt}}\int { \ldots \int {dq_1 }
397 ...dq_f dp_1 } ..dp_f = 0.
398 \label{introEquation:volumePreserving}
399 \end{equation}
400
401 \subsubsection{\label{introSection:liouvilleInOtherForms}\textbf{Liouville's Theorem in Other Forms}}
402
403 Liouville's theorem can be expressed in a variety of different forms
404 which are convenient within different contexts. For any two function
405 $F$ and $G$ of the coordinates and momenta of a system, the Poisson
406 bracket ${F, G}$ is defined as
407 \begin{equation}
408 \left\{ {F,G} \right\} = \sum\limits_i {\left( {\frac{{\partial
409 F}}{{\partial q_i }}\frac{{\partial G}}{{\partial p_i }} -
410 \frac{{\partial F}}{{\partial p_i }}\frac{{\partial G}}{{\partial
411 q_i }}} \right)}.
412 \label{introEquation:poissonBracket}
413 \end{equation}
414 Substituting equations of motion in Hamiltonian formalism
415 (Eq.~\ref{introEquation:motionHamiltonianCoordinate} ,
416 Eq.~\ref{introEquation:motionHamiltonianMomentum}) into
417 (Eq.~\ref{introEquation:liouvilleTheorem}), we can rewrite
418 Liouville's theorem using Poisson bracket notion,
419 \begin{equation}
420 \left( {\frac{{\partial \rho }}{{\partial t}}} \right) = - \left\{
421 {\rho ,H} \right\}.
422 \label{introEquation:liouvilleTheromInPoissin}
423 \end{equation}
424 Moreover, the Liouville operator is defined as
425 \begin{equation}
426 iL = \sum\limits_{i = 1}^f {\left( {\frac{{\partial H}}{{\partial
427 p_i }}\frac{\partial }{{\partial q_i }} - \frac{{\partial
428 H}}{{\partial q_i }}\frac{\partial }{{\partial p_i }}} \right)}
429 \label{introEquation:liouvilleOperator}
430 \end{equation}
431 In terms of Liouville operator, Liouville's equation can also be
432 expressed as
433 \begin{equation}
434 \left( {\frac{{\partial \rho }}{{\partial t}}} \right) = - iL\rho
435 \label{introEquation:liouvilleTheoremInOperator}
436 \end{equation}
437 which can help define a propagator $\rho (t) = e^{-iLt} \rho (0)$.
438 \subsection{\label{introSection:ergodic}The Ergodic Hypothesis}
439
440 Various thermodynamic properties can be calculated from Molecular
441 Dynamics simulation. By comparing experimental values with the
442 calculated properties, one can determine the accuracy of the
443 simulation and the quality of the underlying model. However, both
444 experiments and computer simulations are usually performed during a
445 certain time interval and the measurements are averaged over a
446 period of time which is different from the average behavior of
447 many-body system in Statistical Mechanics. Fortunately, the Ergodic
448 Hypothesis makes a connection between time average and the ensemble
449 average. It states that the time average and average over the
450 statistical ensemble are identical \cite{Frenkel1996, Leach2001}:
451 \begin{equation}
452 \langle A(q , p) \rangle_t = \mathop {\lim }\limits_{t \to \infty }
453 \frac{1}{t}\int\limits_0^t {A(q(t),p(t))dt = \int\limits_\Gamma
454 {A(q(t),p(t))} } \rho (q(t), p(t)) dqdp
455 \end{equation}
456 where $\langle A(q , p) \rangle_t$ is an equilibrium value of a
457 physical quantity and $\rho (p(t), q(t))$ is the equilibrium
458 distribution function. If an observation is averaged over a
459 sufficiently long time (longer than the relaxation time), all
460 accessible microstates in phase space are assumed to be equally
461 probed, giving a properly weighted statistical average. This allows
462 the researcher freedom of choice when deciding how best to measure a
463 given observable. In case an ensemble averaged approach sounds most
464 reasonable, the Monte Carlo methods\cite{Metropolis1949} can be
465 utilized. Or if the system lends itself to a time averaging
466 approach, the Molecular Dynamics techniques in
467 Sec.~\ref{introSection:molecularDynamics} will be the best
468 choice\cite{Frenkel1996}.
469
470 \section{\label{introSection:geometricIntegratos}Geometric Integrators}
471 A variety of numerical integrators have been proposed to simulate
472 the motions of atoms in MD simulation. They usually begin with
473 initial conditionals and move the objects in the direction governed
474 by the differential equations. However, most of them ignore the
475 hidden physical laws contained within the equations. Since 1990,
476 geometric integrators, which preserve various phase-flow invariants
477 such as symplectic structure, volume and time reversal symmetry,
478 were developed to address this issue\cite{Dullweber1997,
479 McLachlan1998, Leimkuhler1999}. The velocity Verlet method, which
480 happens to be a simple example of symplectic integrator, continues
481 to gain popularity in the molecular dynamics community. This fact
482 can be partly explained by its geometric nature.
483
484 \subsection{\label{introSection:symplecticManifold}Symplectic Manifolds}
485 A \emph{manifold} is an abstract mathematical space. It looks
486 locally like Euclidean space, but when viewed globally, it may have
487 more complicated structure. A good example of manifold is the
488 surface of Earth. It seems to be flat locally, but it is round if
489 viewed as a whole. A \emph{differentiable manifold} (also known as
490 \emph{smooth manifold}) is a manifold on which it is possible to
491 apply calculus\cite{Hirsch1997}. A \emph{symplectic manifold} is
492 defined as a pair $(M, \omega)$ which consists of a
493 \emph{differentiable manifold} $M$ and a close, non-degenerated,
494 bilinear symplectic form, $\omega$. A symplectic form on a vector
495 space $V$ is a function $\omega(x, y)$ which satisfies
496 $\omega(\lambda_1x_1+\lambda_2x_2, y) = \lambda_1\omega(x_1, y)+
497 \lambda_2\omega(x_2, y)$, $\omega(x, y) = - \omega(y, x)$ and
498 $\omega(x, x) = 0$\cite{McDuff1998}. The cross product operation in
499 vector field is an example of symplectic form. One of the
500 motivations to study \emph{symplectic manifolds} in Hamiltonian
501 Mechanics is that a symplectic manifold can represent all possible
502 configurations of the system and the phase space of the system can
503 be described by it's cotangent bundle\cite{Jost2002}. Every
504 symplectic manifold is even dimensional. For instance, in Hamilton
505 equations, coordinate and momentum always appear in pairs.
506
507 \subsection{\label{introSection:ODE}Ordinary Differential Equations}
508
509 For an ordinary differential system defined as
510 \begin{equation}
511 \dot x = f(x)
512 \end{equation}
513 where $x = x(q,p)^T$, this system is a canonical Hamiltonian, if
514 $f(x) = J\nabla _x H(x)$. Here, $H = H (q, p)$ is Hamiltonian
515 function and $J$ is the skew-symmetric matrix
516 \begin{equation}
517 J = \left( {\begin{array}{*{20}c}
518 0 & I \\
519 { - I} & 0 \\
520 \end{array}} \right)
521 \label{introEquation:canonicalMatrix}
522 \end{equation}
523 where $I$ is an identity matrix. Using this notation, Hamiltonian
524 system can be rewritten as,
525 \begin{equation}
526 \frac{d}{{dt}}x = J\nabla _x H(x).
527 \label{introEquation:compactHamiltonian}
528 \end{equation}In this case, $f$ is
529 called a \emph{Hamiltonian vector field}. Another generalization of
530 Hamiltonian dynamics is Poisson Dynamics\cite{Olver1986},
531 \begin{equation}
532 \dot x = J(x)\nabla _x H \label{introEquation:poissonHamiltonian}
533 \end{equation}
534 The most obvious change being that matrix $J$ now depends on $x$.
535
536 \subsection{\label{introSection:exactFlow}Exact Propagator}
537
538 Let $x(t)$ be the exact solution of the ODE
539 system,$\frac{{dx}}{{dt}} = f(x) \label{introEquation:ODE}$, we can
540 define its exact propagator(solution) $\varphi_\tau$
541 \[ x(t+\tau)
542 =\varphi_\tau(x(t))
543 \]
544 where $\tau$ is a fixed time step and $\varphi$ is a map from phase
545 space to itself. The propagator has the continuous group property,
546 \begin{equation}
547 \varphi _{\tau _1 } \circ \varphi _{\tau _2 } = \varphi _{\tau _1
548 + \tau _2 } .
549 \end{equation}
550 In particular,
551 \begin{equation}
552 \varphi _\tau \circ \varphi _{ - \tau } = I
553 \end{equation}
554 Therefore, the exact propagator is self-adjoint,
555 \begin{equation}
556 \varphi _\tau = \varphi _{ - \tau }^{ - 1}.
557 \end{equation}
558 The exact propagator can also be written in terms of operator,
559 \begin{equation}
560 \varphi _\tau (x) = e^{\tau \sum\limits_i {f_i (x)\frac{\partial
561 }{{\partial x_i }}} } (x) \equiv \exp (\tau f)(x).
562 \label{introEquation:exponentialOperator}
563 \end{equation}
564 In most cases, it is not easy to find the exact propagator
565 $\varphi_\tau$. Instead, we use an approximate map, $\psi_\tau$,
566 which is usually called an integrator. The order of an integrator
567 $\psi_\tau$ is $p$, if the Taylor series of $\psi_\tau$ agree to
568 order $p$,
569 \begin{equation}
570 \psi_\tau(x) = x + \tau f(x) + O(\tau^{p+1})
571 \end{equation}
572
573 \subsection{\label{introSection:geometricProperties}Geometric Properties}
574
575 The hidden geometric properties\cite{Budd1999, Marsden1998} of an
576 ODE and its propagator play important roles in numerical studies.
577 Many of them can be found in systems which occur naturally in
578 applications. Let $\varphi$ be the propagator of Hamiltonian vector
579 field, $\varphi$ is a \emph{symplectic} propagator if it satisfies,
580 \begin{equation}
581 {\varphi '}^T J \varphi ' = J.
582 \end{equation}
583 According to Liouville's theorem, the symplectic volume is invariant
584 under a Hamiltonian propagator, which is the basis for classical
585 statistical mechanics. Furthermore, the propagator of a Hamiltonian
586 vector field on a symplectic manifold can be shown to be a
587 symplectomorphism. As to the Poisson system,
588 \begin{equation}
589 {\varphi '}^T J \varphi ' = J \circ \varphi
590 \end{equation}
591 is the property that must be preserved by the integrator. It is
592 possible to construct a \emph{volume-preserving} propagator for a
593 source free ODE ($ \nabla \cdot f = 0 $), if the propagator
594 satisfies $ \det d\varphi = 1$. One can show easily that a
595 symplectic propagator will be volume-preserving. Changing the
596 variables $y = h(x)$ in an ODE (Eq.~\ref{introEquation:ODE}) will
597 result in a new system,
598 \[
599 \dot y = \tilde f(y) = ((dh \cdot f)h^{ - 1} )(y).
600 \]
601 The vector filed $f$ has reversing symmetry $h$ if $f = - \tilde f$.
602 In other words, the propagator of this vector field is reversible if
603 and only if $ h \circ \varphi ^{ - 1} = \varphi \circ h $. A
604 conserved quantity of a general differential function is a function
605 $ G:R^{2d} \to R^d $ which is constant for all solutions of the ODE
606 $\frac{{dx}}{{dt}} = f(x)$ ,
607 \[
608 \frac{{dG(x(t))}}{{dt}} = 0.
609 \]
610 Using the chain rule, one may obtain,
611 \[
612 \sum\limits_i {\frac{{dG}}{{dx_i }}} f_i (x) = f \dot \nabla G,
613 \]
614 which is the condition for conserved quantities. For a canonical
615 Hamiltonian system, the time evolution of an arbitrary smooth
616 function $G$ is given by,
617 \begin{eqnarray}
618 \frac{{dG(x(t))}}{{dt}} & = & [\nabla _x G(x(t))]^T \dot x(t) \notag\\
619 & = & [\nabla _x G(x(t))]^T J\nabla _x H(x(t)).
620 \label{introEquation:firstIntegral1}
621 \end{eqnarray}
622 Using poisson bracket notion, Eq.~\ref{introEquation:firstIntegral1}
623 can be rewritten as
624 \[
625 \frac{d}{{dt}}G(x(t)) = \left\{ {G,H} \right\}(x(t)).
626 \]
627 Therefore, the sufficient condition for $G$ to be a conserved
628 quantity of a Hamiltonian system is $\left\{ {G,H} \right\} = 0.$ As
629 is well known, the Hamiltonian (or energy) H of a Hamiltonian system
630 is a conserved quantity, which is due to the fact $\{ H,H\} = 0$.
631 When designing any numerical methods, one should always try to
632 preserve the structural properties of the original ODE and its
633 propagator.
634
635 \subsection{\label{introSection:constructionSymplectic}Construction of Symplectic Methods}
636 A lot of well established and very effective numerical methods have
637 been successful precisely because of their symplectic nature even
638 though this fact was not recognized when they were first
639 constructed. The most famous example is the Verlet-leapfrog method
640 in molecular dynamics. In general, symplectic integrators can be
641 constructed using one of four different methods.
642 \begin{enumerate}
643 \item Generating functions
644 \item Variational methods
645 \item Runge-Kutta methods
646 \item Splitting methods
647 \end{enumerate}
648 Generating functions\cite{Channell1990} tend to lead to methods
649 which are cumbersome and difficult to use. In dissipative systems,
650 variational methods can capture the decay of energy
651 accurately\cite{Kane2000}. Since they are geometrically unstable
652 against non-Hamiltonian perturbations, ordinary implicit Runge-Kutta
653 methods are not suitable for Hamiltonian system. Recently, various
654 high-order explicit Runge-Kutta methods \cite{Owren1992,Chen2003}
655 have been developed to overcome this instability. However, due to
656 computational penalty involved in implementing the Runge-Kutta
657 methods, they have not attracted much attention from the Molecular
658 Dynamics community. Instead, splitting methods have been widely
659 accepted since they exploit natural decompositions of the
660 system\cite{Tuckerman1992, McLachlan1998}.
661
662 \subsubsection{\label{introSection:splittingMethod}\textbf{Splitting Methods}}
663
664 The main idea behind splitting methods is to decompose the discrete
665 $\varphi_h$ as a composition of simpler propagators,
666 \begin{equation}
667 \varphi _h = \varphi _{h_1 } \circ \varphi _{h_2 } \ldots \circ
668 \varphi _{h_n }
669 \label{introEquation:FlowDecomposition}
670 \end{equation}
671 where each of the sub-propagator is chosen such that each represent
672 a simpler integration of the system. Suppose that a Hamiltonian
673 system takes the form,
674 \[
675 H = H_1 + H_2.
676 \]
677 Here, $H_1$ and $H_2$ may represent different physical processes of
678 the system. For instance, they may relate to kinetic and potential
679 energy respectively, which is a natural decomposition of the
680 problem. If $H_1$ and $H_2$ can be integrated using exact
681 propagators $\varphi_1(t)$ and $\varphi_2(t)$, respectively, a
682 simple first order expression is then given by the Lie-Trotter
683 formula
684 \begin{equation}
685 \varphi _h = \varphi _{1,h} \circ \varphi _{2,h},
686 \label{introEquation:firstOrderSplitting}
687 \end{equation}
688 where $\varphi _h$ is the result of applying the corresponding
689 continuous $\varphi _i$ over a time $h$. By definition, as
690 $\varphi_i(t)$ is the exact solution of a Hamiltonian system, it
691 must follow that each operator $\varphi_i(t)$ is a symplectic map.
692 It is easy to show that any composition of symplectic propagators
693 yields a symplectic map,
694 \begin{equation}
695 (\varphi '\phi ')^T J\varphi '\phi ' = \phi '^T \varphi '^T J\varphi
696 '\phi ' = \phi '^T J\phi ' = J,
697 \label{introEquation:SymplecticFlowComposition}
698 \end{equation}
699 where $\phi$ and $\psi$ both are symplectic maps. Thus operator
700 splitting in this context automatically generates a symplectic map.
701 The Lie-Trotter
702 splitting(Eq.~\ref{introEquation:firstOrderSplitting}) introduces
703 local errors proportional to $h^2$, while the Strang splitting gives
704 a second-order decomposition,
705 \begin{equation}
706 \varphi _h = \varphi _{1,h/2} \circ \varphi _{2,h} \circ \varphi
707 _{1,h/2} , \label{introEquation:secondOrderSplitting}
708 \end{equation}
709 which has a local error proportional to $h^3$. The Strang
710 splitting's popularity in molecular simulation community attribute
711 to its symmetric property,
712 \begin{equation}
713 \varphi _h^{ - 1} = \varphi _{ - h}.
714 \label{introEquation:timeReversible}
715 \end{equation}
716
717 \subsubsection{\label{introSection:exampleSplittingMethod}\textbf{Examples of the Splitting Method}}
718 The classical equation for a system consisting of interacting
719 particles can be written in Hamiltonian form,
720 \[
721 H = T + V
722 \]
723 where $T$ is the kinetic energy and $V$ is the potential energy.
724 Setting $H_1 = T, H_2 = V$ and applying the Strang splitting, one
725 obtains the following:
726 \begin{align}
727 q(\Delta t) &= q(0) + \dot{q}(0)\Delta t +
728 \frac{F[q(0)]}{m}\frac{\Delta t^2}{2}, %
729 \label{introEquation:Lp10a} \\%
730 %
731 \dot{q}(\Delta t) &= \dot{q}(0) + \frac{\Delta t}{2m}
732 \biggl [F[q(0)] + F[q(\Delta t)] \biggr]. %
733 \label{introEquation:Lp10b}
734 \end{align}
735 where $F(t)$ is the force at time $t$. This integration scheme is
736 known as \emph{velocity verlet} which is
737 symplectic(\ref{introEquation:SymplecticFlowComposition}),
738 time-reversible(\ref{introEquation:timeReversible}) and
739 volume-preserving (\ref{introEquation:volumePreserving}). These
740 geometric properties attribute to its long-time stability and its
741 popularity in the community. However, the most commonly used
742 velocity verlet integration scheme is written as below,
743 \begin{align}
744 \dot{q}\biggl (\frac{\Delta t}{2}\biggr ) &=
745 \dot{q}(0) + \frac{\Delta t}{2m}\, F[q(0)], \label{introEquation:Lp9a}\\%
746 %
747 q(\Delta t) &= q(0) + \Delta t\, \dot{q}\biggl (\frac{\Delta t}{2}\biggr ),%
748 \label{introEquation:Lp9b}\\%
749 %
750 \dot{q}(\Delta t) &= \dot{q}\biggl (\frac{\Delta t}{2}\biggr ) +
751 \frac{\Delta t}{2m}\, F[q(t)]. \label{introEquation:Lp9c}
752 \end{align}
753 From the preceding splitting, one can see that the integration of
754 the equations of motion would follow:
755 \begin{enumerate}
756 \item calculate the velocities at the half step, $\frac{\Delta t}{2}$, from the forces calculated at the initial position.
757
758 \item Use the half step velocities to move positions one whole step, $\Delta t$.
759
760 \item Evaluate the forces at the new positions, $\mathbf{q}(\Delta t)$, and use the new forces to complete the velocity move.
761
762 \item Repeat from step 1 with the new position, velocities, and forces assuming the roles of the initial values.
763 \end{enumerate}
764 By simply switching the order of the propagators in the splitting
765 and composing a new integrator, the \emph{position verlet}
766 integrator, can be generated,
767 \begin{align}
768 \dot q(\Delta t) &= \dot q(0) + \Delta tF(q(0))\left[ {q(0) +
769 \frac{{\Delta t}}{{2m}}\dot q(0)} \right], %
770 \label{introEquation:positionVerlet1} \\%
771 %
772 q(\Delta t) &= q(0) + \frac{{\Delta t}}{2}\left[ {\dot q(0) + \dot
773 q(\Delta t)} \right]. %
774 \label{introEquation:positionVerlet2}
775 \end{align}
776
777 \subsubsection{\label{introSection:errorAnalysis}\textbf{Error Analysis and Higher Order Methods}}
778
779 The Baker-Campbell-Hausdorff formula can be used to determine the
780 local error of a splitting method in terms of the commutator of the
781 operators(\ref{introEquation:exponentialOperator}) associated with
782 the sub-propagator. For operators $hX$ and $hY$ which are associated
783 with $\varphi_1(t)$ and $\varphi_2(t)$ respectively , we have
784 \begin{equation}
785 \exp (hX + hY) = \exp (hZ)
786 \end{equation}
787 where
788 \begin{equation}
789 hZ = hX + hY + \frac{{h^2 }}{2}[X,Y] + \frac{{h^3 }}{2}\left(
790 {[X,[X,Y]] + [Y,[Y,X]]} \right) + \ldots .
791 \end{equation}
792 Here, $[X,Y]$ is the commutator of operator $X$ and $Y$ given by
793 \[
794 [X,Y] = XY - YX .
795 \]
796 Applying the Baker-Campbell-Hausdorff formula\cite{Varadarajan1974}
797 to the Strang splitting, we can obtain
798 \begin{eqnarray*}
799 \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 \\
800 & & \mbox{} + h^2 [X,X]/8 + h^2 [Y,Y]/8 \\
801 & & \mbox{} + h^3 [Y,[Y,X]]/12 - h^3[X,[X,Y]]/24 + \ldots
802 ).
803 \end{eqnarray*}
804 Since $ [X,Y] + [Y,X] = 0$ and $ [X,X] = 0$, the dominant local
805 error of Strang splitting is proportional to $h^3$. The same
806 procedure can be applied to a general splitting of the form
807 \begin{equation}
808 \varphi _{b_m h}^2 \circ \varphi _{a_m h}^1 \circ \varphi _{b_{m -
809 1} h}^2 \circ \ldots \circ \varphi _{a_1 h}^1 .
810 \end{equation}
811 A careful choice of coefficient $a_1 \ldots b_m$ will lead to higher
812 order methods. Yoshida proposed an elegant way to compose higher
813 order methods based on symmetric splitting\cite{Yoshida1990}. Given
814 a symmetric second order base method $ \varphi _h^{(2)} $, a
815 fourth-order symmetric method can be constructed by composing,
816 \[
817 \varphi _h^{(4)} = \varphi _{\alpha h}^{(2)} \circ \varphi _{\beta
818 h}^{(2)} \circ \varphi _{\alpha h}^{(2)}
819 \]
820 where $ \alpha = - \frac{{2^{1/3} }}{{2 - 2^{1/3} }}$ and $ \beta
821 = \frac{{2^{1/3} }}{{2 - 2^{1/3} }}$. Moreover, a symmetric
822 integrator $ \varphi _h^{(2n + 2)}$ can be composed by
823 \begin{equation}
824 \varphi _h^{(2n + 2)} = \varphi _{\alpha h}^{(2n)} \circ \varphi
825 _{\beta h}^{(2n)} \circ \varphi _{\alpha h}^{(2n)},
826 \end{equation}
827 if the weights are chosen as
828 \[
829 \alpha = - \frac{{2^{1/(2n + 1)} }}{{2 - 2^{1/(2n + 1)} }},\beta =
830 \frac{{2^{1/(2n + 1)} }}{{2 - 2^{1/(2n + 1)} }} .
831 \]
832
833 \section{\label{introSection:molecularDynamics}Molecular Dynamics}
834
835 As one of the principal tools of molecular modeling, Molecular
836 dynamics has proven to be a powerful tool for studying the functions
837 of biological systems, providing structural, thermodynamic and
838 dynamical information. The basic idea of molecular dynamics is that
839 macroscopic properties are related to microscopic behavior and
840 microscopic behavior can be calculated from the trajectories in
841 simulations. For instance, instantaneous temperature of a
842 Hamiltonian system of $N$ particles can be measured by
843 \[
844 T = \sum\limits_{i = 1}^N {\frac{{m_i v_i^2 }}{{fk_B }}}
845 \]
846 where $m_i$ and $v_i$ are the mass and velocity of $i$th particle
847 respectively, $f$ is the number of degrees of freedom, and $k_B$ is
848 the Boltzman constant.
849
850 A typical molecular dynamics run consists of three essential steps:
851 \begin{enumerate}
852 \item Initialization
853 \begin{enumerate}
854 \item Preliminary preparation
855 \item Minimization
856 \item Heating
857 \item Equilibration
858 \end{enumerate}
859 \item Production
860 \item Analysis
861 \end{enumerate}
862 These three individual steps will be covered in the following
863 sections. Sec.~\ref{introSec:initialSystemSettings} deals with the
864 initialization of a simulation. Sec.~\ref{introSection:production}
865 will discuss issues of production runs.
866 Sec.~\ref{introSection:Analysis} provides the theoretical tools for
867 analysis of trajectories.
868
869 \subsection{\label{introSec:initialSystemSettings}Initialization}
870
871 \subsubsection{\textbf{Preliminary preparation}}
872
873 When selecting the starting structure of a molecule for molecular
874 simulation, one may retrieve its Cartesian coordinates from public
875 databases, such as RCSB Protein Data Bank \textit{etc}. Although
876 thousands of crystal structures of molecules are discovered every
877 year, many more remain unknown due to the difficulties of
878 purification and crystallization. Even for molecules with known
879 structures, some important information is missing. For example, a
880 missing hydrogen atom which acts as donor in hydrogen bonding must
881 be added. Moreover, in order to include electrostatic interactions,
882 one may need to specify the partial charges for individual atoms.
883 Under some circumstances, we may even need to prepare the system in
884 a special configuration. For instance, when studying transport
885 phenomenon in membrane systems, we may prepare the lipids in a
886 bilayer structure instead of placing lipids randomly in solvent,
887 since we are not interested in the slow self-aggregation process.
888
889 \subsubsection{\textbf{Minimization}}
890
891 It is quite possible that some of molecules in the system from
892 preliminary preparation may be overlapping with each other. This
893 close proximity leads to high initial potential energy which
894 consequently jeopardizes any molecular dynamics simulations. To
895 remove these steric overlaps, one typically performs energy
896 minimization to find a more reasonable conformation. Several energy
897 minimization methods have been developed to exploit the energy
898 surface and to locate the local minimum. While converging slowly
899 near the minimum, steepest descent method is extremely robust when
900 systems are strongly anharmonic. Thus, it is often used to refine
901 structures from crystallographic data. Relying on the Hessian,
902 advanced methods like Newton-Raphson converge rapidly to a local
903 minimum, but become unstable if the energy surface is far from
904 quadratic. Another factor that must be taken into account, when
905 choosing energy minimization method, is the size of the system.
906 Steepest descent and conjugate gradient can deal with models of any
907 size. Because of the limits on computer memory to store the hessian
908 matrix and the computing power needed to diagonalize these matrices,
909 most Newton-Raphson methods can not be used with very large systems.
910
911 \subsubsection{\textbf{Heating}}
912
913 Typically, heating is performed by assigning random velocities
914 according to a Maxwell-Boltzman distribution for a desired
915 temperature. Beginning at a lower temperature and gradually
916 increasing the temperature by assigning larger random velocities, we
917 end up setting the temperature of the system to a final temperature
918 at which the simulation will be conducted. In heating phase, we
919 should also keep the system from drifting or rotating as a whole. To
920 do this, the net linear momentum and angular momentum of the system
921 is shifted to zero after each resampling from the Maxwell -Boltzman
922 distribution.
923
924 \subsubsection{\textbf{Equilibration}}
925
926 The purpose of equilibration is to allow the system to evolve
927 spontaneously for a period of time and reach equilibrium. The
928 procedure is continued until various statistical properties, such as
929 temperature, pressure, energy, volume and other structural
930 properties \textit{etc}, become independent of time. Strictly
931 speaking, minimization and heating are not necessary, provided the
932 equilibration process is long enough. However, these steps can serve
933 as a means to arrive at an equilibrated structure in an effective
934 way.
935
936 \subsection{\label{introSection:production}Production}
937
938 The production run is the most important step of the simulation, in
939 which the equilibrated structure is used as a starting point and the
940 motions of the molecules are collected for later analysis. In order
941 to capture the macroscopic properties of the system, the molecular
942 dynamics simulation must be performed by sampling correctly and
943 efficiently from the relevant thermodynamic ensemble.
944
945 The most expensive part of a molecular dynamics simulation is the
946 calculation of non-bonded forces, such as van der Waals force and
947 Coulombic forces \textit{etc}. For a system of $N$ particles, the
948 complexity of the algorithm for pair-wise interactions is $O(N^2 )$,
949 which makes large simulations prohibitive in the absence of any
950 algorithmic tricks. A natural approach to avoid system size issues
951 is to represent the bulk behavior by a finite number of the
952 particles. However, this approach will suffer from surface effects
953 at the edges of the simulation. To offset this, \textit{Periodic
954 boundary conditions} (see Fig.~\ref{introFig:pbc}) were developed to
955 simulate bulk properties with a relatively small number of
956 particles. In this method, the simulation box is replicated
957 throughout space to form an infinite lattice. During the simulation,
958 when a particle moves in the primary cell, its image in other cells
959 move in exactly the same direction with exactly the same
960 orientation. Thus, as a particle leaves the primary cell, one of its
961 images will enter through the opposite face.
962 \begin{figure}
963 \centering
964 \includegraphics[width=\linewidth]{pbc.eps}
965 \caption[An illustration of periodic boundary conditions]{A 2-D
966 illustration of periodic boundary conditions. As one particle leaves
967 the left of the simulation box, an image of it enters the right.}
968 \label{introFig:pbc}
969 \end{figure}
970
971 %cutoff and minimum image convention
972 Another important technique to improve the efficiency of force
973 evaluation is to apply spherical cutoffs where particles farther
974 than a predetermined distance are not included in the calculation
975 \cite{Frenkel1996}. The use of a cutoff radius will cause a
976 discontinuity in the potential energy curve. Fortunately, one can
977 shift a simple radial potential to ensure the potential curve go
978 smoothly to zero at the cutoff radius. The cutoff strategy works
979 well for Lennard-Jones interaction because of its short range
980 nature. However, simply truncating the electrostatic interaction
981 with the use of cutoffs has been shown to lead to severe artifacts
982 in simulations. The Ewald summation, in which the slowly decaying
983 Coulomb potential is transformed into direct and reciprocal sums
984 with rapid and absolute convergence, has proved to minimize the
985 periodicity artifacts in liquid simulations. Taking the advantages
986 of the fast Fourier transform (FFT) for calculating discrete Fourier
987 transforms, the particle mesh-based
988 methods\cite{Hockney1981,Shimada1993, Luty1994} are accelerated from
989 $O(N^{3/2})$ to $O(N logN)$. An alternative approach is the
990 \emph{fast multipole method}\cite{Greengard1987, Greengard1994},
991 which treats Coulombic interactions exactly at short range, and
992 approximate the potential at long range through multipolar
993 expansion. In spite of their wide acceptance at the molecular
994 simulation community, these two methods are difficult to implement
995 correctly and efficiently. Instead, we use a damped and
996 charge-neutralized Coulomb potential method developed by Wolf and
997 his coworkers\cite{Wolf1999}. The shifted Coulomb potential for
998 particle $i$ and particle $j$ at distance $r_{rj}$ is given by:
999 \begin{equation}
1000 V(r_{ij})= \frac{q_i q_j \textrm{erfc}(\alpha
1001 r_{ij})}{r_{ij}}-\lim_{r_{ij}\rightarrow
1002 R_\textrm{c}}\left\{\frac{q_iq_j \textrm{erfc}(\alpha
1003 r_{ij})}{r_{ij}}\right\}. \label{introEquation:shiftedCoulomb}
1004 \end{equation}
1005 where $\alpha$ is the convergence parameter. Due to the lack of
1006 inherent periodicity and rapid convergence,this method is extremely
1007 efficient and easy to implement.
1008 \begin{figure}
1009 \centering
1010 \includegraphics[width=\linewidth]{shifted_coulomb.eps}
1011 \caption[An illustration of shifted Coulomb potential]{An
1012 illustration of shifted Coulomb potential.}
1013 \label{introFigure:shiftedCoulomb}
1014 \end{figure}
1015
1016 %multiple time step
1017
1018 \subsection{\label{introSection:Analysis} Analysis}
1019
1020 Recently, advanced visualization technique have become applied to
1021 monitor the motions of molecules. Although the dynamics of the
1022 system can be described qualitatively from animation, quantitative
1023 trajectory analysis is more useful. According to the principles of
1024 Statistical Mechanics in
1025 Sec.~\ref{introSection:statisticalMechanics}, one can compute
1026 thermodynamic properties, analyze fluctuations of structural
1027 parameters, and investigate time-dependent processes of the molecule
1028 from the trajectories.
1029
1030 \subsubsection{\label{introSection:thermodynamicsProperties}\textbf{Thermodynamic Properties}}
1031
1032 Thermodynamic properties, which can be expressed in terms of some
1033 function of the coordinates and momenta of all particles in the
1034 system, can be directly computed from molecular dynamics. The usual
1035 way to measure the pressure is based on virial theorem of Clausius
1036 which states that the virial is equal to $-3Nk_BT$. For a system
1037 with forces between particles, the total virial, $W$, contains the
1038 contribution from external pressure and interaction between the
1039 particles:
1040 \[
1041 W = - 3PV + \left\langle {\sum\limits_{i < j} {r{}_{ij} \cdot
1042 f_{ij} } } \right\rangle
1043 \]
1044 where $f_{ij}$ is the force between particle $i$ and $j$ at a
1045 distance $r_{ij}$. Thus, the expression for the pressure is given
1046 by:
1047 \begin{equation}
1048 P = \frac{{Nk_B T}}{V} - \frac{1}{{3V}}\left\langle {\sum\limits_{i
1049 < j} {r{}_{ij} \cdot f_{ij} } } \right\rangle
1050 \end{equation}
1051
1052 \subsubsection{\label{introSection:structuralProperties}\textbf{Structural Properties}}
1053
1054 Structural Properties of a simple fluid can be described by a set of
1055 distribution functions. Among these functions,the \emph{pair
1056 distribution function}, also known as \emph{radial distribution
1057 function}, is of most fundamental importance to liquid theory.
1058 Experimentally, pair distribution functions can be gathered by
1059 Fourier transforming raw data from a series of neutron diffraction
1060 experiments and integrating over the surface factor
1061 \cite{Powles1973}. The experimental results can serve as a criterion
1062 to justify the correctness of a liquid model. Moreover, various
1063 equilibrium thermodynamic and structural properties can also be
1064 expressed in terms of the radial distribution function
1065 \cite{Allen1987}. The pair distribution functions $g(r)$ gives the
1066 probability that a particle $i$ will be located at a distance $r$
1067 from a another particle $j$ in the system
1068 \begin{equation}
1069 g(r) = \frac{V}{{N^2 }}\left\langle {\sum\limits_i {\sum\limits_{j
1070 \ne i} {\delta (r - r_{ij} )} } } \right\rangle = \frac{\rho
1071 (r)}{\rho}.
1072 \end{equation}
1073 Note that the delta function can be replaced by a histogram in
1074 computer simulation. Peaks in $g(r)$ represent solvent shells, and
1075 the height of these peaks gradually decreases to 1 as the liquid of
1076 large distance approaches the bulk density.
1077
1078
1079 \subsubsection{\label{introSection:timeDependentProperties}\textbf{Time-dependent
1080 Properties}}
1081
1082 Time-dependent properties are usually calculated using \emph{time
1083 correlation functions}, which correlate random variables $A$ and $B$
1084 at two different times,
1085 \begin{equation}
1086 C_{AB} (t) = \left\langle {A(t)B(0)} \right\rangle.
1087 \label{introEquation:timeCorrelationFunction}
1088 \end{equation}
1089 If $A$ and $B$ refer to same variable, this kind of correlation
1090 function is called an \emph{autocorrelation function}. One example
1091 of an auto correlation function is the velocity auto-correlation
1092 function which is directly related to transport properties of
1093 molecular liquids:
1094 \[
1095 D = \frac{1}{3}\int\limits_0^\infty {\left\langle {v(t) \cdot v(0)}
1096 \right\rangle } dt
1097 \]
1098 where $D$ is diffusion constant. Unlike the velocity autocorrelation
1099 function, which is averaged over time origins and over all the
1100 atoms, the dipole autocorrelation functions is calculated for the
1101 entire system. The dipole autocorrelation function is given by:
1102 \[
1103 c_{dipole} = \left\langle {u_{tot} (t) \cdot u_{tot} (t)}
1104 \right\rangle
1105 \]
1106 Here $u_{tot}$ is the net dipole of the entire system and is given
1107 by
1108 \[
1109 u_{tot} (t) = \sum\limits_i {u_i (t)}.
1110 \]
1111 In principle, many time correlation functions can be related to
1112 Fourier transforms of the infrared, Raman, and inelastic neutron
1113 scattering spectra of molecular liquids. In practice, one can
1114 extract the IR spectrum from the intensity of the molecular dipole
1115 fluctuation at each frequency using the following relationship:
1116 \[
1117 \hat c_{dipole} (v) = \int_{ - \infty }^\infty {c_{dipole} (t)e^{ -
1118 i2\pi vt} dt}.
1119 \]
1120
1121 \section{\label{introSection:rigidBody}Dynamics of Rigid Bodies}
1122
1123 Rigid bodies are frequently involved in the modeling of different
1124 areas, from engineering, physics, to chemistry. For example,
1125 missiles and vehicles are usually modeled by rigid bodies. The
1126 movement of the objects in 3D gaming engines or other physics
1127 simulators is governed by rigid body dynamics. In molecular
1128 simulations, rigid bodies are used to simplify protein-protein
1129 docking studies\cite{Gray2003}.
1130
1131 It is very important to develop stable and efficient methods to
1132 integrate the equations of motion for orientational degrees of
1133 freedom. Euler angles are the natural choice to describe the
1134 rotational degrees of freedom. However, due to $\frac {1}{sin
1135 \theta}$ singularities, the numerical integration of corresponding
1136 equations of these motion is very inefficient and inaccurate.
1137 Although an alternative integrator using multiple sets of Euler
1138 angles can overcome this difficulty\cite{Barojas1973}, the
1139 computational penalty and the loss of angular momentum conservation
1140 still remain. A singularity-free representation utilizing
1141 quaternions was developed by Evans in 1977\cite{Evans1977}.
1142 Unfortunately, this approach uses a nonseparable Hamiltonian
1143 resulting from the quaternion representation, which prevents the
1144 symplectic algorithm from being utilized. Another different approach
1145 is to apply holonomic constraints to the atoms belonging to the
1146 rigid body. Each atom moves independently under the normal forces
1147 deriving from potential energy and constraint forces which are used
1148 to guarantee the rigidness. However, due to their iterative nature,
1149 the SHAKE and Rattle algorithms also converge very slowly when the
1150 number of constraints increases\cite{Ryckaert1977, Andersen1983}.
1151
1152 A break-through in geometric literature suggests that, in order to
1153 develop a long-term integration scheme, one should preserve the
1154 symplectic structure of the propagator. By introducing a conjugate
1155 momentum to the rotation matrix $Q$ and re-formulating Hamiltonian's
1156 equation, a symplectic integrator, RSHAKE\cite{Kol1997}, was
1157 proposed to evolve the Hamiltonian system in a constraint manifold
1158 by iteratively satisfying the orthogonality constraint $Q^T Q = 1$.
1159 An alternative method using the quaternion representation was
1160 developed by Omelyan\cite{Omelyan1998}. However, both of these
1161 methods are iterative and inefficient. In this section, we descibe a
1162 symplectic Lie-Poisson integrator for rigid bodies developed by
1163 Dullweber and his coworkers\cite{Dullweber1997} in depth.
1164
1165 \subsection{\label{introSection:constrainedHamiltonianRB}Constrained Hamiltonian for Rigid Bodies}
1166 The motion of a rigid body is Hamiltonian with the Hamiltonian
1167 function
1168 \begin{equation}
1169 H = \frac{1}{2}(p^T m^{ - 1} p) + \frac{1}{2}tr(PJ^{ - 1} P) +
1170 V(q,Q) + \frac{1}{2}tr[(QQ^T - 1)\Lambda ].
1171 \label{introEquation:RBHamiltonian}
1172 \end{equation}
1173 Here, $q$ and $Q$ are the position and rotation matrix for the
1174 rigid-body, $p$ and $P$ are conjugate momenta to $q$ and $Q$ , and
1175 $J$, a diagonal matrix, is defined by
1176 \[
1177 I_{ii}^{ - 1} = \frac{1}{2}\sum\limits_{i \ne j} {J_{jj}^{ - 1} }
1178 \]
1179 where $I_{ii}$ is the diagonal element of the inertia tensor. This
1180 constrained Hamiltonian equation is subjected to a holonomic
1181 constraint,
1182 \begin{equation}
1183 Q^T Q = 1, \label{introEquation:orthogonalConstraint}
1184 \end{equation}
1185 which is used to ensure rotation matrix's unitarity. Differentiating
1186 Eq.~\ref{introEquation:orthogonalConstraint} and using
1187 Eq.~\ref{introEquation:RBMotionMomentum}, one may obtain,
1188 \begin{equation}
1189 Q^T PJ^{ - 1} + J^{ - 1} P^T Q = 0 . \\
1190 \label{introEquation:RBFirstOrderConstraint}
1191 \end{equation}
1192 Using Equation (\ref{introEquation:motionHamiltonianCoordinate},
1193 \ref{introEquation:motionHamiltonianMomentum}), one can write down
1194 the equations of motion,
1195 \begin{eqnarray}
1196 \frac{{dq}}{{dt}} & = & \frac{p}{m}, \label{introEquation:RBMotionPosition}\\
1197 \frac{{dp}}{{dt}} & = & - \nabla _q V(q,Q), \label{introEquation:RBMotionMomentum}\\
1198 \frac{{dQ}}{{dt}} & = & PJ^{ - 1}, \label{introEquation:RBMotionRotation}\\
1199 \frac{{dP}}{{dt}} & = & - \nabla _Q V(q,Q) - 2Q\Lambda . \label{introEquation:RBMotionP}
1200 \end{eqnarray}
1201 In general, there are two ways to satisfy the holonomic constraints.
1202 We can use a constraint force provided by a Lagrange multiplier on
1203 the normal manifold to keep the motion on constraint space. Or we
1204 can simply evolve the system on the constraint manifold. These two
1205 methods have been proved to be equivalent. The holonomic constraint
1206 and equations of motions define a constraint manifold for rigid
1207 bodies
1208 \[
1209 M = \left\{ {(Q,P):Q^T Q = 1,Q^T PJ^{ - 1} + J^{ - 1} P^T Q = 0}
1210 \right\}.
1211 \]
1212 Unfortunately, this constraint manifold is not the cotangent bundle
1213 $T^* SO(3)$ which can be consider as a symplectic manifold on Lie
1214 rotation group $SO(3)$. However, it turns out that under symplectic
1215 transformation, the cotangent space and the phase space are
1216 diffeomorphic. By introducing
1217 \[
1218 \tilde Q = Q,\tilde P = \frac{1}{2}\left( {P - QP^T Q} \right),
1219 \]
1220 the mechanical system subject to a holonomic constraint manifold $M$
1221 can be re-formulated as a Hamiltonian system on the cotangent space
1222 \[
1223 T^* SO(3) = \left\{ {(\tilde Q,\tilde P):\tilde Q^T \tilde Q =
1224 1,\tilde Q^T \tilde PJ^{ - 1} + J^{ - 1} P^T \tilde Q = 0} \right\}
1225 \]
1226 For a body fixed vector $X_i$ with respect to the center of mass of
1227 the rigid body, its corresponding lab fixed vector $X_0^{lab}$ is
1228 given as
1229 \begin{equation}
1230 X_i^{lab} = Q X_i + q.
1231 \end{equation}
1232 Therefore, potential energy $V(q,Q)$ is defined by
1233 \[
1234 V(q,Q) = V(Q X_0 + q).
1235 \]
1236 Hence, the force and torque are given by
1237 \[
1238 \nabla _q V(q,Q) = F(q,Q) = \sum\limits_i {F_i (q,Q)},
1239 \]
1240 and
1241 \[
1242 \nabla _Q V(q,Q) = F(q,Q)X_i^t
1243 \]
1244 respectively. As a common choice to describe the rotation dynamics
1245 of the rigid body, the angular momentum on the body fixed frame $\Pi
1246 = Q^t P$ is introduced to rewrite the equations of motion,
1247 \begin{equation}
1248 \begin{array}{l}
1249 \dot \Pi = J^{ - 1} \Pi ^T \Pi + Q^T \sum\limits_i {F_i (q,Q)X_i^T } - \Lambda, \\
1250 \dot Q = Q\Pi {\rm{ }}J^{ - 1}, \\
1251 \end{array}
1252 \label{introEqaution:RBMotionPI}
1253 \end{equation}
1254 as well as holonomic constraints $\Pi J^{ - 1} + J^{ - 1} \Pi ^t =
1255 0$ and $Q^T Q = 1$. For a vector $v(v_1 ,v_2 ,v_3 ) \in R^3$ and a
1256 matrix $\hat v \in so(3)^ \star$, the hat-map isomorphism,
1257 \begin{equation}
1258 v(v_1 ,v_2 ,v_3 ) \Leftrightarrow \hat v = \left(
1259 {\begin{array}{*{20}c}
1260 0 & { - v_3 } & {v_2 } \\
1261 {v_3 } & 0 & { - v_1 } \\
1262 { - v_2 } & {v_1 } & 0 \\
1263 \end{array}} \right),
1264 \label{introEquation:hatmapIsomorphism}
1265 \end{equation}
1266 will let us associate the matrix products with traditional vector
1267 operations
1268 \[
1269 \hat vu = v \times u.
1270 \]
1271 Using Eq.~\ref{introEqaution:RBMotionPI}, one can construct a skew
1272 matrix,
1273 \begin{eqnarray}
1274 (\dot \Pi - \dot \Pi ^T )&= &(\Pi - \Pi ^T )(J^{ - 1} \Pi + \Pi J^{ - 1} ) \notag \\
1275 & & + \sum\limits_i {[Q^T F_i (r,Q)X_i^T - X_i F_i (r,Q)^T Q]} -
1276 (\Lambda - \Lambda ^T ). \label{introEquation:skewMatrixPI}
1277 \end{eqnarray}
1278 Since $\Lambda$ is symmetric, the last term of
1279 Eq.~\ref{introEquation:skewMatrixPI} is zero, which implies the
1280 Lagrange multiplier $\Lambda$ is absent from the equations of
1281 motion. This unique property eliminates the requirement of
1282 iterations which can not be avoided in other methods\cite{Kol1997,
1283 Omelyan1998}. Applying the hat-map isomorphism, we obtain the
1284 equation of motion for angular momentum on body frame
1285 \begin{equation}
1286 \dot \pi = \pi \times I^{ - 1} \pi + \sum\limits_i {\left( {Q^T
1287 F_i (r,Q)} \right) \times X_i }.
1288 \label{introEquation:bodyAngularMotion}
1289 \end{equation}
1290 In the same manner, the equation of motion for rotation matrix is
1291 given by
1292 \[
1293 \dot Q = Qskew(I^{ - 1} \pi ).
1294 \]
1295
1296 \subsection{\label{introSection:SymplecticFreeRB}Symplectic
1297 Lie-Poisson Integrator for Free Rigid Body}
1298
1299 If there are no external forces exerted on the rigid body, the only
1300 contribution to the rotational motion is from the kinetic energy
1301 (the first term of \ref{introEquation:bodyAngularMotion}). The free
1302 rigid body is an example of a Lie-Poisson system with Hamiltonian
1303 function
1304 \begin{equation}
1305 T^r (\pi ) = T_1 ^r (\pi _1 ) + T_2^r (\pi _2 ) + T_3^r (\pi _3 )
1306 \label{introEquation:rotationalKineticRB}
1307 \end{equation}
1308 where $T_i^r (\pi _i ) = \frac{{\pi _i ^2 }}{{2I_i }}$ and
1309 Lie-Poisson structure matrix,
1310 \begin{equation}
1311 J(\pi ) = \left( {\begin{array}{*{20}c}
1312 0 & {\pi _3 } & { - \pi _2 } \\
1313 { - \pi _3 } & 0 & {\pi _1 } \\
1314 {\pi _2 } & { - \pi _1 } & 0 \\
1315 \end{array}} \right).
1316 \end{equation}
1317 Thus, the dynamics of free rigid body is governed by
1318 \begin{equation}
1319 \frac{d}{{dt}}\pi = J(\pi )\nabla _\pi T^r (\pi ).
1320 \end{equation}
1321 One may notice that each $T_i^r$ in
1322 Eq.~\ref{introEquation:rotationalKineticRB} can be solved exactly.
1323 For instance, the equations of motion due to $T_1^r$ are given by
1324 \begin{equation}
1325 \frac{d}{{dt}}\pi = R_1 \pi ,\frac{d}{{dt}}Q = QR_1
1326 \label{introEqaution:RBMotionSingleTerm}
1327 \end{equation}
1328 with
1329 \[ R_1 = \left( {\begin{array}{*{20}c}
1330 0 & 0 & 0 \\
1331 0 & 0 & {\pi _1 } \\
1332 0 & { - \pi _1 } & 0 \\
1333 \end{array}} \right).
1334 \]
1335 The solutions of Eq.~\ref{introEqaution:RBMotionSingleTerm} is
1336 \[
1337 \pi (\Delta t) = e^{\Delta tR_1 } \pi (0),Q(\Delta t) =
1338 Q(0)e^{\Delta tR_1 }
1339 \]
1340 with
1341 \[
1342 e^{\Delta tR_1 } = \left( {\begin{array}{*{20}c}
1343 0 & 0 & 0 \\
1344 0 & {\cos \theta _1 } & {\sin \theta _1 } \\
1345 0 & { - \sin \theta _1 } & {\cos \theta _1 } \\
1346 \end{array}} \right),\theta _1 = \frac{{\pi _1 }}{{I_1 }}\Delta t.
1347 \]
1348 To reduce the cost of computing expensive functions in $e^{\Delta
1349 tR_1 }$, we can use Cayley transformation to obtain a single-aixs
1350 propagator,
1351 \[
1352 e^{\Delta tR_1 } \approx (1 - \Delta tR_1 )^{ - 1} (1 + \Delta tR_1
1353 ).
1354 \]
1355 The propagator maps for $T_2^r$ and $T_3^r$ can be found in the same
1356 manner. In order to construct a second-order symplectic method, we
1357 split the angular kinetic Hamiltonian function into five terms
1358 \[
1359 T^r (\pi ) = \frac{1}{2}T_1 ^r (\pi _1 ) + \frac{1}{2}T_2^r (\pi _2
1360 ) + T_3^r (\pi _3 ) + \frac{1}{2}T_2^r (\pi _2 ) + \frac{1}{2}T_1 ^r
1361 (\pi _1 ).
1362 \]
1363 By concatenating the propagators corresponding to these five terms,
1364 we can obtain an symplectic integrator,
1365 \[
1366 \varphi _{\Delta t,T^r } = \varphi _{\Delta t/2,\pi _1 } \circ
1367 \varphi _{\Delta t/2,\pi _2 } \circ \varphi _{\Delta t,\pi _3 }
1368 \circ \varphi _{\Delta t/2,\pi _2 } \circ \varphi _{\Delta t/2,\pi
1369 _1 }.
1370 \]
1371 The non-canonical Lie-Poisson bracket ${F, G}$ of two function
1372 $F(\pi )$ and $G(\pi )$ is defined by
1373 \[
1374 \{ F,G\} (\pi ) = [\nabla _\pi F(\pi )]^T J(\pi )\nabla _\pi G(\pi
1375 ).
1376 \]
1377 If the Poisson bracket of a function $F$ with an arbitrary smooth
1378 function $G$ is zero, $F$ is a \emph{Casimir}, which is the
1379 conserved quantity in Poisson system. We can easily verify that the
1380 norm of the angular momentum, $\parallel \pi
1381 \parallel$, is a \emph{Casimir}. Let$ F(\pi ) = S(\frac{{\parallel
1382 \pi \parallel ^2 }}{2})$ for an arbitrary function $ S:R \to R$ ,
1383 then by the chain rule
1384 \[
1385 \nabla _\pi F(\pi ) = S'(\frac{{\parallel \pi \parallel ^2
1386 }}{2})\pi.
1387 \]
1388 Thus, $ [\nabla _\pi F(\pi )]^T J(\pi ) = - S'(\frac{{\parallel
1389 \pi
1390 \parallel ^2 }}{2})\pi \times \pi = 0 $. This explicit
1391 Lie-Poisson integrator is found to be both extremely efficient and
1392 stable. These properties can be explained by the fact the small
1393 angle approximation is used and the norm of the angular momentum is
1394 conserved.
1395
1396 \subsection{\label{introSection:RBHamiltonianSplitting} Hamiltonian
1397 Splitting for Rigid Body}
1398
1399 The Hamiltonian of rigid body can be separated in terms of kinetic
1400 energy and potential energy,$H = T(p,\pi ) + V(q,Q)$. The equations
1401 of motion corresponding to potential energy and kinetic energy are
1402 listed in the below table,
1403 \begin{table}
1404 \caption{EQUATIONS OF MOTION DUE TO POTENTIAL AND KINETIC ENERGIES}
1405 \begin{center}
1406 \begin{tabular}{|l|l|}
1407 \hline
1408 % after \\: \hline or \cline{col1-col2} \cline{col3-col4} ...
1409 Potential & Kinetic \\
1410 $\frac{{dq}}{{dt}} = \frac{p}{m}$ & $\frac{d}{{dt}}q = p$ \\
1411 $\frac{d}{{dt}}p = - \frac{{\partial V}}{{\partial q}}$ & $ \frac{d}{{dt}}p = 0$ \\
1412 $\frac{d}{{dt}}Q = 0$ & $ \frac{d}{{dt}}Q = Qskew(I^{ - 1} j)$ \\
1413 $ \frac{d}{{dt}}\pi = \sum\limits_i {\left( {Q^T F_i (r,Q)} \right) \times X_i }$ & $\frac{d}{{dt}}\pi = \pi \times I^{ - 1} \pi$\\
1414 \hline
1415 \end{tabular}
1416 \end{center}
1417 \end{table}
1418 A second-order symplectic method is now obtained by the composition
1419 of the position and velocity propagators,
1420 \[
1421 \varphi _{\Delta t} = \varphi _{\Delta t/2,V} \circ \varphi
1422 _{\Delta t,T} \circ \varphi _{\Delta t/2,V}.
1423 \]
1424 Moreover, $\varphi _{\Delta t/2,V}$ can be divided into two
1425 sub-propagators which corresponding to force and torque
1426 respectively,
1427 \[
1428 \varphi _{\Delta t/2,V} = \varphi _{\Delta t/2,F} \circ \varphi
1429 _{\Delta t/2,\tau }.
1430 \]
1431 Since the associated operators of $\varphi _{\Delta t/2,F} $ and
1432 $\circ \varphi _{\Delta t/2,\tau }$ commute, the composition order
1433 inside $\varphi _{\Delta t/2,V}$ does not matter. Furthermore, the
1434 kinetic energy can be separated to translational kinetic term, $T^t
1435 (p)$, and rotational kinetic term, $T^r (\pi )$,
1436 \begin{equation}
1437 T(p,\pi ) =T^t (p) + T^r (\pi ).
1438 \end{equation}
1439 where $ T^t (p) = \frac{1}{2}p^T m^{ - 1} p $ and $T^r (\pi )$ is
1440 defined by Eq.~\ref{introEquation:rotationalKineticRB}. Therefore,
1441 the corresponding propagators are given by
1442 \[
1443 \varphi _{\Delta t,T} = \varphi _{\Delta t,T^t } \circ \varphi
1444 _{\Delta t,T^r }.
1445 \]
1446 Finally, we obtain the overall symplectic propagators for freely
1447 moving rigid bodies
1448 \begin{eqnarray}
1449 \varphi _{\Delta t} &=& \varphi _{\Delta t/2,F} \circ \varphi _{\Delta t/2,\tau } \notag\\
1450 & & \circ \varphi _{\Delta t,T^t } \circ \varphi _{\Delta t/2,\pi _1 } \circ \varphi _{\Delta t/2,\pi _2 } \circ \varphi _{\Delta t,\pi _3 } \circ \varphi _{\Delta t/2,\pi _2 } \circ \varphi _{\Delta t/2,\pi _1 } \notag\\
1451 & & \circ \varphi _{\Delta t/2,\tau } \circ \varphi _{\Delta t/2,F} .
1452 \label{introEquation:overallRBFlowMaps}
1453 \end{eqnarray}
1454
1455 \section{\label{introSection:langevinDynamics}Langevin Dynamics}
1456 As an alternative to newtonian dynamics, Langevin dynamics, which
1457 mimics a simple heat bath with stochastic and dissipative forces,
1458 has been applied in a variety of studies. This section will review
1459 the theory of Langevin dynamics. A brief derivation of generalized
1460 Langevin equation will be given first. Following that, we will
1461 discuss the physical meaning of the terms appearing in the equation
1462 as well as the calculation of friction tensor from hydrodynamics
1463 theory.
1464
1465 \subsection{\label{introSection:generalizedLangevinDynamics}Derivation of Generalized Langevin Equation}
1466
1467 A harmonic bath model, in which an effective set of harmonic
1468 oscillators are used to mimic the effect of a linearly responding
1469 environment, has been widely used in quantum chemistry and
1470 statistical mechanics. One of the successful applications of
1471 Harmonic bath model is the derivation of the Generalized Langevin
1472 Dynamics (GLE). Lets consider a system, in which the degree of
1473 freedom $x$ is assumed to couple to the bath linearly, giving a
1474 Hamiltonian of the form
1475 \begin{equation}
1476 H = \frac{{p^2 }}{{2m}} + U(x) + H_B + \Delta U(x,x_1 , \ldots x_N)
1477 \label{introEquation:bathGLE}.
1478 \end{equation}
1479 Here $p$ is a momentum conjugate to $x$, $m$ is the mass associated
1480 with this degree of freedom, $H_B$ is a harmonic bath Hamiltonian,
1481 \[
1482 H_B = \sum\limits_{\alpha = 1}^N {\left\{ {\frac{{p_\alpha ^2
1483 }}{{2m_\alpha }} + \frac{1}{2}m_\alpha \omega _\alpha ^2 }
1484 \right\}}
1485 \]
1486 where the index $\alpha$ runs over all the bath degrees of freedom,
1487 $\omega _\alpha$ are the harmonic bath frequencies, $m_\alpha$ are
1488 the harmonic bath masses, and $\Delta U$ is a bilinear system-bath
1489 coupling,
1490 \[
1491 \Delta U = - \sum\limits_{\alpha = 1}^N {g_\alpha x_\alpha x}
1492 \]
1493 where $g_\alpha$ are the coupling constants between the bath
1494 coordinates ($x_ \alpha$) and the system coordinate ($x$).
1495 Introducing
1496 \[
1497 W(x) = U(x) - \sum\limits_{\alpha = 1}^N {\frac{{g_\alpha ^2
1498 }}{{2m_\alpha w_\alpha ^2 }}} x^2
1499 \]
1500 and combining the last two terms in Eq.~\ref{introEquation:bathGLE}, we may rewrite the Harmonic bath Hamiltonian as
1501 \[
1502 H = \frac{{p^2 }}{{2m}} + W(x) + \sum\limits_{\alpha = 1}^N
1503 {\left\{ {\frac{{p_\alpha ^2 }}{{2m_\alpha }} + \frac{1}{2}m_\alpha
1504 w_\alpha ^2 \left( {x_\alpha - \frac{{g_\alpha }}{{m_\alpha
1505 w_\alpha ^2 }}x} \right)^2 } \right\}}.
1506 \]
1507 Since the first two terms of the new Hamiltonian depend only on the
1508 system coordinates, we can get the equations of motion for
1509 Generalized Langevin Dynamics by Hamilton's equations,
1510 \begin{equation}
1511 m\ddot x = - \frac{{\partial W(x)}}{{\partial x}} -
1512 \sum\limits_{\alpha = 1}^N {g_\alpha \left( {x_\alpha -
1513 \frac{{g_\alpha }}{{m_\alpha w_\alpha ^2 }}x} \right)},
1514 \label{introEquation:coorMotionGLE}
1515 \end{equation}
1516 and
1517 \begin{equation}
1518 m\ddot x_\alpha = - m_\alpha w_\alpha ^2 \left( {x_\alpha -
1519 \frac{{g_\alpha }}{{m_\alpha w_\alpha ^2 }}x} \right).
1520 \label{introEquation:bathMotionGLE}
1521 \end{equation}
1522 In order to derive an equation for $x$, the dynamics of the bath
1523 variables $x_\alpha$ must be solved exactly first. As an integral
1524 transform which is particularly useful in solving linear ordinary
1525 differential equations,the Laplace transform is the appropriate tool
1526 to solve this problem. The basic idea is to transform the difficult
1527 differential equations into simple algebra problems which can be
1528 solved easily. Then, by applying the inverse Laplace transform, also
1529 known as the Bromwich integral, we can retrieve the solutions of the
1530 original problems. Let $f(t)$ be a function defined on $ [0,\infty )
1531 $, the Laplace transform of $f(t)$ is a new function defined as
1532 \[
1533 L(f(t)) \equiv F(p) = \int_0^\infty {f(t)e^{ - pt} dt}
1534 \]
1535 where $p$ is real and $L$ is called the Laplace Transform
1536 Operator. Below are some important properties of Laplace transform
1537 \begin{eqnarray*}
1538 L(x + y) & = & L(x) + L(y) \\
1539 L(ax) & = & aL(x) \\
1540 L(\dot x) & = & pL(x) - px(0) \\
1541 L(\ddot x)& = & p^2 L(x) - px(0) - \dot x(0) \\
1542 L\left( {\int_0^t {g(t - \tau )h(\tau )d\tau } } \right)& = & G(p)H(p) \\
1543 \end{eqnarray*}
1544 Applying the Laplace transform to the bath coordinates, we obtain
1545 \begin{eqnarray*}
1546 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), \\
1547 L(x_\alpha ) & = & \frac{{\frac{{g_\alpha }}{{\omega _\alpha }}L(x) + px_\alpha (0) + \dot x_\alpha (0)}}{{p^2 + \omega _\alpha ^2 }}. \\
1548 \end{eqnarray*}
1549 By the same way, the system coordinates become
1550 \begin{eqnarray*}
1551 mL(\ddot x) & = &
1552 - \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\}} \\
1553 & & - \frac{1}{p}\frac{{\partial W(x)}}{{\partial x}}.
1554 \end{eqnarray*}
1555 With the help of some relatively important inverse Laplace
1556 transformations:
1557 \[
1558 \begin{array}{c}
1559 L(\cos at) = \frac{p}{{p^2 + a^2 }} \\
1560 L(\sin at) = \frac{a}{{p^2 + a^2 }} \\
1561 L(1) = \frac{1}{p} \\
1562 \end{array}
1563 \]
1564 we obtain
1565 \begin{eqnarray*}
1566 m\ddot x & = & - \frac{{\partial W(x)}}{{\partial x}} -
1567 \sum\limits_{\alpha = 1}^N {\left\{ {\left( { - \frac{{g_\alpha ^2
1568 }}{{m_\alpha \omega _\alpha ^2 }}} \right)\int_0^t {\cos (\omega
1569 _\alpha t)\dot x(t - \tau )d\tau } } \right\}} \\
1570 & & + \sum\limits_{\alpha = 1}^N {\left\{ {\left[ {g_\alpha
1571 x_\alpha (0) - \frac{{g_\alpha }}{{m_\alpha \omega _\alpha }}}
1572 \right]\cos (\omega _\alpha t) + \frac{{g_\alpha \dot x_\alpha
1573 (0)}}{{\omega _\alpha }}\sin (\omega _\alpha t)} \right\}}
1574 \end{eqnarray*}
1575 \begin{eqnarray*}
1576 m\ddot x & = & - \frac{{\partial W(x)}}{{\partial x}} - \int_0^t
1577 {\sum\limits_{\alpha = 1}^N {\left( { - \frac{{g_\alpha ^2
1578 }}{{m_\alpha \omega _\alpha ^2 }}} \right)\cos (\omega _\alpha
1579 t)\dot x(t - \tau )d} \tau } \\
1580 & & + \sum\limits_{\alpha = 1}^N {\left\{ {\left[ {g_\alpha
1581 x_\alpha (0) - \frac{{g_\alpha }}{{m_\alpha \omega _\alpha }}}
1582 \right]\cos (\omega _\alpha t) + \frac{{g_\alpha \dot x_\alpha
1583 (0)}}{{\omega _\alpha }}\sin (\omega _\alpha t)} \right\}}
1584 \end{eqnarray*}
1585 Introducing a \emph{dynamic friction kernel}
1586 \begin{equation}
1587 \xi (t) = \sum\limits_{\alpha = 1}^N {\left( { - \frac{{g_\alpha ^2
1588 }}{{m_\alpha \omega _\alpha ^2 }}} \right)\cos (\omega _\alpha t)}
1589 \label{introEquation:dynamicFrictionKernelDefinition}
1590 \end{equation}
1591 and \emph{a random force}
1592 \begin{equation}
1593 R(t) = \sum\limits_{\alpha = 1}^N {\left( {g_\alpha x_\alpha (0)
1594 - \frac{{g_\alpha ^2 }}{{m_\alpha \omega _\alpha ^2 }}x(0)}
1595 \right)\cos (\omega _\alpha t)} + \frac{{\dot x_\alpha
1596 (0)}}{{\omega _\alpha }}\sin (\omega _\alpha t),
1597 \label{introEquation:randomForceDefinition}
1598 \end{equation}
1599 the equation of motion can be rewritten as
1600 \begin{equation}
1601 m\ddot x = - \frac{{\partial W}}{{\partial x}} - \int_0^t {\xi
1602 (t)\dot x(t - \tau )d\tau } + R(t)
1603 \label{introEuqation:GeneralizedLangevinDynamics}
1604 \end{equation}
1605 which is known as the \emph{generalized Langevin equation}.
1606
1607 \subsubsection{\label{introSection:randomForceDynamicFrictionKernel}\textbf{Random Force and Dynamic Friction Kernel}}
1608
1609 One may notice that $R(t)$ depends only on initial conditions, which
1610 implies it is completely deterministic within the context of a
1611 harmonic bath. However, it is easy to verify that $R(t)$ is totally
1612 uncorrelated to $x$ and $\dot x$,$\left\langle {x(t)R(t)}
1613 \right\rangle = 0, \left\langle {\dot x(t)R(t)} \right\rangle =
1614 0.$ This property is what we expect from a truly random process. As
1615 long as the model chosen for $R(t)$ was a gaussian distribution in
1616 general, the stochastic nature of the GLE still remains.
1617 %dynamic friction kernel
1618 The convolution integral
1619 \[
1620 \int_0^t {\xi (t)\dot x(t - \tau )d\tau }
1621 \]
1622 depends on the entire history of the evolution of $x$, which implies
1623 that the bath retains memory of previous motions. In other words,
1624 the bath requires a finite time to respond to change in the motion
1625 of the system. For a sluggish bath which responds slowly to changes
1626 in the system coordinate, we may regard $\xi(t)$ as a constant
1627 $\xi(t) = \Xi_0$. Hence, the convolution integral becomes
1628 \[
1629 \int_0^t {\xi (t)\dot x(t - \tau )d\tau } = \xi _0 (x(t) - x(0))
1630 \]
1631 and Eq.~\ref{introEuqation:GeneralizedLangevinDynamics} becomes
1632 \[
1633 m\ddot x = - \frac{\partial }{{\partial x}}\left( {W(x) +
1634 \frac{1}{2}\xi _0 (x - x_0 )^2 } \right) + R(t),
1635 \]
1636 which can be used to describe the effect of dynamic caging in
1637 viscous solvents. The other extreme is the bath that responds
1638 infinitely quickly to motions in the system. Thus, $\xi (t)$ can be
1639 taken as a $delta$ function in time:
1640 \[
1641 \xi (t) = 2\xi _0 \delta (t)
1642 \]
1643 Hence, the convolution integral becomes
1644 \[
1645 \int_0^t {\xi (t)\dot x(t - \tau )d\tau } = 2\xi _0 \int_0^t
1646 {\delta (t)\dot x(t - \tau )d\tau } = \xi _0 \dot x(t),
1647 \]
1648 and Eq.~\ref{introEuqation:GeneralizedLangevinDynamics} becomes
1649 \begin{equation}
1650 m\ddot x = - \frac{{\partial W(x)}}{{\partial x}} - \xi _0 \dot
1651 x(t) + R(t) \label{introEquation:LangevinEquation}
1652 \end{equation}
1653 which is known as the Langevin equation. The static friction
1654 coefficient $\xi _0$ can either be calculated from spectral density
1655 or be determined by Stokes' law for regular shaped particles. A
1656 briefly review on calculating friction tensor for arbitrary shaped
1657 particles is given in Sec.~\ref{introSection:frictionTensor}.
1658
1659 \subsubsection{\label{introSection:secondFluctuationDissipation}\textbf{The Second Fluctuation Dissipation Theorem}}
1660
1661 Defining a new set of coordinates
1662 \[
1663 q_\alpha (t) = x_\alpha (t) - \frac{1}{{m_\alpha \omega _\alpha
1664 ^2 }}x(0),
1665 \]
1666 we can rewrite $R(T)$ as
1667 \[
1668 R(t) = \sum\limits_{\alpha = 1}^N {g_\alpha q_\alpha (t)}.
1669 \]
1670 And since the $q$ coordinates are harmonic oscillators,
1671 \begin{eqnarray*}
1672 \left\langle {q_\alpha ^2 } \right\rangle & = & \frac{{kT}}{{m_\alpha \omega _\alpha ^2 }} \\
1673 \left\langle {q_\alpha (t)q_\alpha (0)} \right\rangle & = & \left\langle {q_\alpha ^2 (0)} \right\rangle \cos (\omega _\alpha t) \\
1674 \left\langle {q_\alpha (t)q_\beta (0)} \right\rangle & = &\delta _{\alpha \beta } \left\langle {q_\alpha (t)q_\alpha (0)} \right\rangle \\
1675 \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 } } \\
1676 & = &\sum\limits_\alpha {g_\alpha ^2 \left\langle {q_\alpha ^2 (0)} \right\rangle \cos (\omega _\alpha t)} \\
1677 & = &kT\xi (t)
1678 \end{eqnarray*}
1679 Thus, we recover the \emph{second fluctuation dissipation theorem}
1680 \begin{equation}
1681 \xi (t) = \left\langle {R(t)R(0)} \right\rangle
1682 \label{introEquation:secondFluctuationDissipation},
1683 \end{equation}
1684 which acts as a constraint on the possible ways in which one can
1685 model the random force and friction kernel.