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# Line 27 | Line 27 | $F_ij$ be the force that particle $i$ exerts on partic
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 $i$.
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 117 | Line 117 | for a holonomic system of $f$ degrees of freedom, the
117   \subsubsection{\label{introSection:equationOfMotionLagrangian}The
118   Equations of Motion in Lagrangian Mechanics}
119  
120 < for a holonomic system of $f$ degrees of freedom, the equations of
120 > For a holonomic system of $f$ degrees of freedom, the equations of
121   motion in the Lagrangian form is
122   \begin{equation}
123   \frac{d}{{dt}}\frac{{\partial L}}{{\partial \dot q_i }} -
# Line 212 | Line 212 | q_i }}} \right) = 0}
212   }}\dot p_i } \right)}  = \sum\limits_i {\left( {\frac{{\partial
213   H}}{{\partial q_i }}\frac{{\partial H}}{{\partial p_i }} -
214   \frac{{\partial H}}{{\partial p_i }}\frac{{\partial H}}{{\partial
215 < q_i }}} \right) = 0}
216 < \label{introEquation:conserveHalmitonian}
215 > q_i }}} \right) = 0} \label{introEquation:conserveHalmitonian}
216   \end{equation}
217  
218 < When studying Hamiltonian system, it is more convenient to use
219 < notation
218 > \section{\label{introSection:statisticalMechanics}Statistical
219 > Mechanics}
220 >
221 > The thermodynamic behaviors and properties of Molecular Dynamics
222 > simulation are governed by the principle of Statistical Mechanics.
223 > The following section will give a brief introduction to some of the
224 > Statistical Mechanics concepts and theorem presented in this
225 > dissertation.
226 >
227 > \subsection{\label{introSection:ensemble}Phase Space and Ensemble}
228 >
229 > Mathematically, phase space is the space which represents all
230 > possible states. Each possible state of the system corresponds to
231 > one unique point in the phase space. For mechanical systems, the
232 > phase space usually consists of all possible values of position and
233 > momentum variables. Consider a dynamic system in a cartesian space,
234 > where each of the $6f$ coordinates and momenta is assigned to one of
235 > $6f$ mutually orthogonal axes, the phase space of this system is a
236 > $6f$ dimensional space. A point, $x = (q_1 , \ldots ,q_f ,p_1 ,
237 > \ldots ,p_f )$, with a unique set of values of $6f$ coordinates and
238 > momenta is a phase space vector.
239 >
240 > A microscopic state or microstate of a classical system is
241 > specification of the complete phase space vector of a system at any
242 > instant in time. An ensemble is defined as a collection of systems
243 > sharing one or more macroscopic characteristics but each being in a
244 > unique microstate. The complete ensemble is specified by giving all
245 > systems or microstates consistent with the common macroscopic
246 > characteristics of the ensemble. Although the state of each
247 > individual system in the ensemble could be precisely described at
248 > any instance in time by a suitable phase space vector, when using
249 > ensembles for statistical purposes, there is no need to maintain
250 > distinctions between individual systems, since the numbers of
251 > systems at any time in the different states which correspond to
252 > different regions of the phase space are more interesting. Moreover,
253 > in the point of view of statistical mechanics, one would prefer to
254 > use ensembles containing a large enough population of separate
255 > members so that the numbers of systems in such different states can
256 > be regarded as changing continuously as we traverse different
257 > regions of the phase space. The condition of an ensemble at any time
258 > can be regarded as appropriately specified by the density $\rho$
259 > with which representative points are distributed over the phase
260 > space. The density of distribution for an ensemble with $f$ degrees
261 > of freedom is defined as,
262   \begin{equation}
263 < r = r(q,p)^T
264 < \end{equation}
265 < and to introduce a $2n \times 2n$ canonical structure matrix $J$,
263 > \rho  = \rho (q_1 , \ldots ,q_f ,p_1 , \ldots ,p_f ,t).
264 > \label{introEquation:densityDistribution}
265 > \end{equation}
266 > Governed by the principles of mechanics, the phase points change
267 > their value which would change the density at any time at phase
268 > space. Hence, the density of distribution is also to be taken as a
269 > function of the time.
270 >
271 > The number of systems $\delta N$ at time $t$ can be determined by,
272   \begin{equation}
273 < J = \left( {\begin{array}{*{20}c}
274 <   0 & I  \\
228 <   { - I} & 0  \\
229 < \end{array}} \right)
230 < \label{introEquation:canonicalMatrix}
273 > \delta N = \rho (q,p,t)dq_1  \ldots dq_f dp_1  \ldots dp_f.
274 > \label{introEquation:deltaN}
275   \end{equation}
276 < where $I$ is a $n \times n$ identity matrix and $J$ is a
277 < skew-symmetric matrix ($ J^T  =  - J $). Thus, Hamiltonian system
278 < can be rewritten as,
276 > Assuming a large enough population of systems are exploited, we can
277 > sufficiently approximate $\delta N$ without introducing
278 > discontinuity when we go from one region in the phase space to
279 > another. By integrating over the whole phase space,
280   \begin{equation}
281 < \frac{d}{{dt}}r = J\nabla _r H(r)
282 < \label{introEquation:compactHamiltonian}
281 > N = \int { \ldots \int {\rho (q,p,t)dq_1 } ...dq_f dp_1 } ...dp_f
282 > \label{introEquation:totalNumberSystem}
283   \end{equation}
284 + gives us an expression for the total number of the systems. Hence,
285 + the probability per unit in the phase space can be obtained by,
286 + \begin{equation}
287 + \frac{{\rho (q,p,t)}}{N} = \frac{{\rho (q,p,t)}}{{\int { \ldots \int
288 + {\rho (q,p,t)dq_1 } ...dq_f dp_1 } ...dp_f }}.
289 + \label{introEquation:unitProbability}
290 + \end{equation}
291 + With the help of Equation(\ref{introEquation:unitProbability}) and
292 + the knowledge of the system, it is possible to calculate the average
293 + value of any desired quantity which depends on the coordinates and
294 + momenta of the system. Even when the dynamics of the real system is
295 + complex, or stochastic, or even discontinuous, the average
296 + properties of the ensemble of possibilities as a whole may still
297 + remain well defined. For a classical system in thermal equilibrium
298 + with its environment, the ensemble average of a mechanical quantity,
299 + $\langle A(q , p) \rangle_t$, takes the form of an integral over the
300 + phase space of the system,
301 + \begin{equation}
302 + \langle  A(q , p) \rangle_t = \frac{{\int { \ldots \int {A(q,p)\rho
303 + (q,p,t)dq_1 } ...dq_f dp_1 } ...dp_f }}{{\int { \ldots \int {\rho
304 + (q,p,t)dq_1 } ...dq_f dp_1 } ...dp_f }}
305 + \label{introEquation:ensembelAverage}
306 + \end{equation}
307  
308 < \section{\label{introSection:geometricIntegratos}Geometric Integrators}
308 > There are several different types of ensembles with different
309 > statistical characteristics. As a function of macroscopic
310 > parameters, such as temperature \textit{etc}, partition function can
311 > be used to describe the statistical properties of a system in
312 > thermodynamic equilibrium.
313  
314 < \subsection{\label{introSection:symplecticManifold}Symplectic Manifold}
315 < A \emph{manifold} is an abstract mathematical space. It locally
316 < looks like Euclidean space, but when viewed globally, it may have
317 < more complicate structure. A good example of manifold is the surface
318 < of Earth. It seems to be flat locally, but it is round if viewed as
319 < a whole. A \emph{differentiable manifold} (also known as
320 < \emph{smooth manifold}) is a manifold with an open cover in which
321 < the covering neighborhoods are all smoothly isomorphic to one
322 < another. In other words,it is possible to apply calculus on
323 < \emph{differentiable manifold}. A \emph{symplectic manifold} is
324 < defined as a pair $(M, \omega)$ consisting of a \emph{differentiable
325 < manifold} $M$ and a close, non-degenerated, bilinear symplectic
326 < form, $\omega$. One of the motivation to study \emph{symplectic
327 < manifold} in Hamiltonian Mechanics is that a symplectic manifold can
328 < represent all possible configurations of the system and the phase
329 < space of the system can be described by it's cotangent bundle. Every
330 < symplectic manifold is even dimensional. For instance, in Hamilton
331 < equations, coordinate and momentum always appear in pairs.
314 > As an ensemble of systems, each of which is known to be thermally
315 > isolated and conserve energy, Microcanonical ensemble(NVE) has a
316 > partition function like,
317 > \begin{equation}
318 > \Omega (N,V,E) = e^{\beta TS} \label{introEquation:NVEPartition}.
319 > \end{equation}
320 > A canonical ensemble(NVT)is an ensemble of systems, each of which
321 > can share its energy with a large heat reservoir. The distribution
322 > of the total energy amongst the possible dynamical states is given
323 > by the partition function,
324 > \begin{equation}
325 > \Omega (N,V,T) = e^{ - \beta A}
326 > \label{introEquation:NVTPartition}
327 > \end{equation}
328 > Here, $A$ is the Helmholtz free energy which is defined as $ A = U -
329 > TS$. Since most experiment are carried out under constant pressure
330 > condition, isothermal-isobaric ensemble(NPT) play a very important
331 > role in molecular simulation. The isothermal-isobaric ensemble allow
332 > the system to exchange energy with a heat bath of temperature $T$
333 > and to change the volume as well. Its partition function is given as
334 > \begin{equation}
335 > \Delta (N,P,T) =  - e^{\beta G}.
336 > \label{introEquation:NPTPartition}
337 > \end{equation}
338 > Here, $G = U - TS + PV$, and $G$ is called Gibbs free energy.
339  
340 < A \emph{symplectomorphism} is also known as a \emph{canonical
262 < transformation}.
340 > \subsection{\label{introSection:liouville}Liouville's theorem}
341  
342 < Any real-valued differentiable function H on a symplectic manifold
343 < can serve as an energy function or Hamiltonian. Associated to any
344 < Hamiltonian is a Hamiltonian vector field; the integral curves of
345 < the Hamiltonian vector field are solutions to the Hamilton-Jacobi
346 < equations. The Hamiltonian vector field defines a flow on the
347 < symplectic manifold, called a Hamiltonian flow or symplectomorphism.
348 < By Liouville's theorem, Hamiltonian flows preserve the volume form
349 < on the phase space.
342 > The Liouville's theorem is the foundation on which statistical
343 > mechanics rests. It describes the time evolution of phase space
344 > distribution function. In order to calculate the rate of change of
345 > $\rho$, we begin from Equation(\ref{introEquation:deltaN}). If we
346 > consider the two faces perpendicular to the $q_1$ axis, which are
347 > located at $q_1$ and $q_1 + \delta q_1$, the number of phase points
348 > leaving the opposite face is given by the expression,
349 > \begin{equation}
350 > \left( {\rho  + \frac{{\partial \rho }}{{\partial q_1 }}\delta q_1 }
351 > \right)\left( {\dot q_1  + \frac{{\partial \dot q_1 }}{{\partial q_1
352 > }}\delta q_1 } \right)\delta q_2  \ldots \delta q_f \delta p_1
353 > \ldots \delta p_f .
354 > \end{equation}
355 > Summing all over the phase space, we obtain
356 > \begin{equation}
357 > \frac{{d(\delta N)}}{{dt}} =  - \sum\limits_{i = 1}^f {\left[ {\rho
358 > \left( {\frac{{\partial \dot q_i }}{{\partial q_i }} +
359 > \frac{{\partial \dot p_i }}{{\partial p_i }}} \right) + \left(
360 > {\frac{{\partial \rho }}{{\partial q_i }}\dot q_i  + \frac{{\partial
361 > \rho }}{{\partial p_i }}\dot p_i } \right)} \right]} \delta q_1
362 > \ldots \delta q_f \delta p_1  \ldots \delta p_f .
363 > \end{equation}
364 > Differentiating the equations of motion in Hamiltonian formalism
365 > (\ref{introEquation:motionHamiltonianCoordinate},
366 > \ref{introEquation:motionHamiltonianMomentum}), we can show,
367 > \begin{equation}
368 > \sum\limits_i {\left( {\frac{{\partial \dot q_i }}{{\partial q_i }}
369 > + \frac{{\partial \dot p_i }}{{\partial p_i }}} \right)}  = 0 ,
370 > \end{equation}
371 > which cancels the first terms of the right hand side. Furthermore,
372 > divining $ \delta q_1  \ldots \delta q_f \delta p_1  \ldots \delta
373 > p_f $ in both sides, we can write out Liouville's theorem in a
374 > simple form,
375 > \begin{equation}
376 > \frac{{\partial \rho }}{{\partial t}} + \sum\limits_{i = 1}^f
377 > {\left( {\frac{{\partial \rho }}{{\partial q_i }}\dot q_i  +
378 > \frac{{\partial \rho }}{{\partial p_i }}\dot p_i } \right)}  = 0 .
379 > \label{introEquation:liouvilleTheorem}
380 > \end{equation}
381  
382 < \subsection{\label{Construction of Symplectic Methods}}
383 <
384 < \section{\label{introSection:statisticalMechanics}Statistical
385 < Mechanics}
386 <
387 < The thermodynamic behaviors and properties of Molecular Dynamics
388 < simulation are governed by the principle of Statistical Mechanics.
389 < The following section will give a brief introduction to some of the
390 < Statistical Mechanics concepts presented in this dissertation.
382 > Liouville's theorem states that the distribution function is
383 > constant along any trajectory in phase space. In classical
384 > statistical mechanics, since the number of particles in the system
385 > is huge, we may be able to believe the system is stationary,
386 > \begin{equation}
387 > \frac{{\partial \rho }}{{\partial t}} = 0.
388 > \label{introEquation:stationary}
389 > \end{equation}
390 > In such stationary system, the density of distribution $\rho$ can be
391 > connected to the Hamiltonian $H$ through Maxwell-Boltzmann
392 > distribution,
393 > \begin{equation}
394 > \rho  \propto e^{ - \beta H}
395 > \label{introEquation:densityAndHamiltonian}
396 > \end{equation}
397  
398 < \subsection{\label{introSection:ensemble}Ensemble and Phase Space}
398 > \subsubsection{\label{introSection:phaseSpaceConservation}Conservation of Phase Space}
399 > Lets consider a region in the phase space,
400 > \begin{equation}
401 > \delta v = \int { \ldots \int {dq_1 } ...dq_f dp_1 } ..dp_f .
402 > \end{equation}
403 > If this region is small enough, the density $\rho$ can be regarded
404 > as uniform over the whole phase space. Thus, the number of phase
405 > points inside this region is given by,
406 > \begin{equation}
407 > \delta N = \rho \delta v = \rho \int { \ldots \int {dq_1 } ...dq_f
408 > dp_1 } ..dp_f.
409 > \end{equation}
410  
411 + \begin{equation}
412 + \frac{{d(\delta N)}}{{dt}} = \frac{{d\rho }}{{dt}}\delta v + \rho
413 + \frac{d}{{dt}}(\delta v) = 0.
414 + \end{equation}
415 + With the help of stationary assumption
416 + (\ref{introEquation:stationary}), we obtain the principle of the
417 + \emph{conservation of extension in phase space},
418 + \begin{equation}
419 + \frac{d}{{dt}}(\delta v) = \frac{d}{{dt}}\int { \ldots \int {dq_1 }
420 + ...dq_f dp_1 } ..dp_f  = 0.
421 + \label{introEquation:volumePreserving}
422 + \end{equation}
423 +
424 + \subsubsection{\label{introSection:liouvilleInOtherForms}Liouville's Theorem in Other Forms}
425 +
426 + Liouville's theorem can be expresses in a variety of different forms
427 + which are convenient within different contexts. For any two function
428 + $F$ and $G$ of the coordinates and momenta of a system, the Poisson
429 + bracket ${F, G}$ is defined as
430 + \begin{equation}
431 + \left\{ {F,G} \right\} = \sum\limits_i {\left( {\frac{{\partial
432 + F}}{{\partial q_i }}\frac{{\partial G}}{{\partial p_i }} -
433 + \frac{{\partial F}}{{\partial p_i }}\frac{{\partial G}}{{\partial
434 + q_i }}} \right)}.
435 + \label{introEquation:poissonBracket}
436 + \end{equation}
437 + Substituting equations of motion in Hamiltonian formalism(
438 + \ref{introEquation:motionHamiltonianCoordinate} ,
439 + \ref{introEquation:motionHamiltonianMomentum} ) into
440 + (\ref{introEquation:liouvilleTheorem}), we can rewrite Liouville's
441 + theorem using Poisson bracket notion,
442 + \begin{equation}
443 + \left( {\frac{{\partial \rho }}{{\partial t}}} \right) =  - \left\{
444 + {\rho ,H} \right\}.
445 + \label{introEquation:liouvilleTheromInPoissin}
446 + \end{equation}
447 + Moreover, the Liouville operator is defined as
448 + \begin{equation}
449 + iL = \sum\limits_{i = 1}^f {\left( {\frac{{\partial H}}{{\partial
450 + p_i }}\frac{\partial }{{\partial q_i }} - \frac{{\partial
451 + H}}{{\partial q_i }}\frac{\partial }{{\partial p_i }}} \right)}
452 + \label{introEquation:liouvilleOperator}
453 + \end{equation}
454 + In terms of Liouville operator, Liouville's equation can also be
455 + expressed as
456 + \begin{equation}
457 + \left( {\frac{{\partial \rho }}{{\partial t}}} \right) =  - iL\rho
458 + \label{introEquation:liouvilleTheoremInOperator}
459 + \end{equation}
460 +
461   \subsection{\label{introSection:ergodic}The Ergodic Hypothesis}
462  
463   Various thermodynamic properties can be calculated from Molecular
# Line 296 | Line 472 | statistical ensemble are identical \cite{Frenkel1996,
472   ensemble average. It states that time average and average over the
473   statistical ensemble are identical \cite{Frenkel1996, leach01:mm}.
474   \begin{equation}
475 < \langle A \rangle_t = \mathop {\lim }\limits_{t \to \infty }
476 < \frac{1}{t}\int\limits_0^t {A(p(t),q(t))dt = \int\limits_\Gamma
477 < {A(p(t),q(t))} } \rho (p(t), q(t)) dpdq
475 > \langle A(q , p) \rangle_t = \mathop {\lim }\limits_{t \to \infty }
476 > \frac{1}{t}\int\limits_0^t {A(q(t),p(t))dt = \int\limits_\Gamma
477 > {A(q(t),p(t))} } \rho (q(t), p(t)) dqdp
478   \end{equation}
479 < where $\langle A \rangle_t$ is an equilibrium value of a physical
480 < quantity and $\rho (p(t), q(t))$ is the equilibrium distribution
481 < function. If an observation is averaged over a sufficiently long
482 < time (longer than relaxation time), all accessible microstates in
483 < phase space are assumed to be equally probed, giving a properly
484 < weighted statistical average. This allows the researcher freedom of
485 < choice when deciding how best to measure a given observable. In case
486 < an ensemble averaged approach sounds most reasonable, the Monte
487 < Carlo techniques\cite{metropolis:1949} can be utilized. Or if the
488 < system lends itself to a time averaging approach, the Molecular
489 < Dynamics techniques in Sec.~\ref{introSection:molecularDynamics}
490 < will be the best choice\cite{Frenkel1996}.
479 > where $\langle  A(q , p) \rangle_t$ is an equilibrium value of a
480 > physical quantity and $\rho (p(t), q(t))$ is the equilibrium
481 > distribution function. If an observation is averaged over a
482 > sufficiently long time (longer than relaxation time), all accessible
483 > microstates in phase space are assumed to be equally probed, giving
484 > a properly weighted statistical average. This allows the researcher
485 > freedom of choice when deciding how best to measure a given
486 > observable. In case an ensemble averaged approach sounds most
487 > reasonable, the Monte Carlo techniques\cite{metropolis:1949} can be
488 > utilized. Or if the system lends itself to a time averaging
489 > approach, the Molecular Dynamics techniques in
490 > Sec.~\ref{introSection:molecularDynamics} will be the best
491 > choice\cite{Frenkel1996}.
492  
493 < \section{\label{introSection:molecularDynamics}Molecular Dynamics}
493 > \section{\label{introSection:geometricIntegratos}Geometric Integrators}
494 > A variety of numerical integrators were proposed to simulate the
495 > motions. They usually begin with an initial conditionals and move
496 > the objects in the direction governed by the differential equations.
497 > However, most of them ignore the hidden physical law contained
498 > within the equations. Since 1990, geometric integrators, which
499 > preserve various phase-flow invariants such as symplectic structure,
500 > volume and time reversal symmetry, are developed to address this
501 > issue. The velocity verlet method, which happens to be a simple
502 > example of symplectic integrator, continues to gain its popularity
503 > in molecular dynamics community. This fact can be partly explained
504 > by its geometric nature.
505 >
506 > \subsection{\label{introSection:symplecticManifold}Symplectic Manifold}
507 > A \emph{manifold} is an abstract mathematical space. It locally
508 > looks like Euclidean space, but when viewed globally, it may have
509 > more complicate structure. A good example of manifold is the surface
510 > of Earth. It seems to be flat locally, but it is round if viewed as
511 > a whole. A \emph{differentiable manifold} (also known as
512 > \emph{smooth manifold}) is a manifold with an open cover in which
513 > the covering neighborhoods are all smoothly isomorphic to one
514 > another. In other words,it is possible to apply calculus on
515 > \emph{differentiable manifold}. A \emph{symplectic manifold} is
516 > defined as a pair $(M, \omega)$ which consisting of a
517 > \emph{differentiable manifold} $M$ and a close, non-degenerated,
518 > bilinear symplectic form, $\omega$. A symplectic form on a vector
519 > space $V$ is a function $\omega(x, y)$ which satisfies
520 > $\omega(\lambda_1x_1+\lambda_2x_2, y) = \lambda_1\omega(x_1, y)+
521 > \lambda_2\omega(x_2, y)$, $\omega(x, y) = - \omega(y, x)$ and
522 > $\omega(x, x) = 0$. Cross product operation in vector field is an
523 > example of symplectic form.
524 >
525 > One of the motivations to study \emph{symplectic manifold} in
526 > Hamiltonian Mechanics is that a symplectic manifold can represent
527 > all possible configurations of the system and the phase space of the
528 > system can be described by it's cotangent bundle. Every symplectic
529 > manifold is even dimensional. For instance, in Hamilton equations,
530 > coordinate and momentum always appear in pairs.
531 >
532 > Let  $(M,\omega)$ and $(N, \eta)$ be symplectic manifolds. A map
533 > \[
534 > f : M \rightarrow N
535 > \]
536 > is a \emph{symplectomorphism} if it is a \emph{diffeomorphims} and
537 > the \emph{pullback} of $\eta$ under f is equal to $\omega$.
538 > Canonical transformation is an example of symplectomorphism in
539 > classical mechanics.
540 >
541 > \subsection{\label{introSection:ODE}Ordinary Differential Equations}
542 >
543 > For a ordinary differential system defined as
544 > \begin{equation}
545 > \dot x = f(x)
546 > \end{equation}
547 > where $x = x(q,p)^T$, this system is canonical Hamiltonian, if
548 > \begin{equation}
549 > f(r) = J\nabla _x H(r).
550 > \end{equation}
551 > $H = H (q, p)$ is Hamiltonian function and $J$ is the skew-symmetric
552 > matrix
553 > \begin{equation}
554 > J = \left( {\begin{array}{*{20}c}
555 >   0 & I  \\
556 >   { - I} & 0  \\
557 > \end{array}} \right)
558 > \label{introEquation:canonicalMatrix}
559 > \end{equation}
560 > where $I$ is an identity matrix. Using this notation, Hamiltonian
561 > system can be rewritten as,
562 > \begin{equation}
563 > \frac{d}{{dt}}x = J\nabla _x H(x)
564 > \label{introEquation:compactHamiltonian}
565 > \end{equation}In this case, $f$ is
566 > called a \emph{Hamiltonian vector field}.
567 >
568 > Another generalization of Hamiltonian dynamics is Poisson Dynamics,
569 > \begin{equation}
570 > \dot x = J(x)\nabla _x H \label{introEquation:poissonHamiltonian}
571 > \end{equation}
572 > The most obvious change being that matrix $J$ now depends on $x$.
573 >
574 > \subsection{\label{introSection:exactFlow}Exact Flow}
575 >
576 > Let $x(t)$ be the exact solution of the ODE system,
577 > \begin{equation}
578 > \frac{{dx}}{{dt}} = f(x) \label{introEquation:ODE}
579 > \end{equation}
580 > The exact flow(solution) $\varphi_\tau$ is defined by
581 > \[
582 > x(t+\tau) =\varphi_\tau(x(t))
583 > \]
584 > where $\tau$ is a fixed time step and $\varphi$ is a map from phase
585 > space to itself. The flow has the continuous group property,
586 > \begin{equation}
587 > \varphi _{\tau _1 }  \circ \varphi _{\tau _2 }  = \varphi _{\tau _1
588 > + \tau _2 } .
589 > \end{equation}
590 > In particular,
591 > \begin{equation}
592 > \varphi _\tau   \circ \varphi _{ - \tau }  = I
593 > \end{equation}
594 > Therefore, the exact flow is self-adjoint,
595 > \begin{equation}
596 > \varphi _\tau   = \varphi _{ - \tau }^{ - 1}.
597 > \end{equation}
598 > The exact flow can also be written in terms of the of an operator,
599 > \begin{equation}
600 > \varphi _\tau  (x) = e^{\tau \sum\limits_i {f_i (x)\frac{\partial
601 > }{{\partial x_i }}} } (x) \equiv \exp (\tau f)(x).
602 > \label{introEquation:exponentialOperator}
603 > \end{equation}
604 >
605 > In most cases, it is not easy to find the exact flow $\varphi_\tau$.
606 > Instead, we use a approximate map, $\psi_\tau$, which is usually
607 > called integrator. The order of an integrator $\psi_\tau$ is $p$, if
608 > the Taylor series of $\psi_\tau$ agree to order $p$,
609 > \begin{equation}
610 > \psi_tau(x) = x + \tau f(x) + O(\tau^{p+1})
611 > \end{equation}
612 >
613 > \subsection{\label{introSection:geometricProperties}Geometric Properties}
614 >
615 > The hidden geometric properties of ODE and its flow play important
616 > roles in numerical studies. Many of them can be found in systems
617 > which occur naturally in applications.
618  
619 < As a special discipline of molecular modeling, Molecular dynamics
620 < has proven to be a powerful tool for studying the functions of
621 < biological systems, providing structural, thermodynamic and
622 < dynamical information.
619 > Let $\varphi$ be the flow of Hamiltonian vector field, $\varphi$ is
620 > a \emph{symplectic} flow if it satisfies,
621 > \begin{equation}
622 > {\varphi '}^T J \varphi ' = J.
623 > \end{equation}
624 > According to Liouville's theorem, the symplectic volume is invariant
625 > under a Hamiltonian flow, which is the basis for classical
626 > statistical mechanics. Furthermore, the flow of a Hamiltonian vector
627 > field on a symplectic manifold can be shown to be a
628 > symplectomorphism. As to the Poisson system,
629 > \begin{equation}
630 > {\varphi '}^T J \varphi ' = J \circ \varphi
631 > \end{equation}
632 > is the property must be preserved by the integrator.
633  
634 < \subsection{\label{introSec:mdInit}Initialization}
634 > It is possible to construct a \emph{volume-preserving} flow for a
635 > source free($ \nabla \cdot f = 0 $) ODE, if the flow satisfies $
636 > \det d\varphi  = 1$. One can show easily that a symplectic flow will
637 > be volume-preserving.
638  
639 < \subsection{\label{introSection:mdIntegration} Integration of the Equations of Motion}
639 > Changing the variables $y = h(x)$ in a ODE\ref{introEquation:ODE}
640 > will result in a new system,
641 > \[
642 > \dot y = \tilde f(y) = ((dh \cdot f)h^{ - 1} )(y).
643 > \]
644 > The vector filed $f$ has reversing symmetry $h$ if $f = - \tilde f$.
645 > In other words, the flow of this vector field is reversible if and
646 > only if $ h \circ \varphi ^{ - 1}  = \varphi  \circ h $.
647  
648 < \section{\label{introSection:rigidBody}Dynamics of Rigid Bodies}
648 > A \emph{first integral}, or conserved quantity of a general
649 > differential function is a function $ G:R^{2d}  \to R^d $ which is
650 > constant for all solutions of the ODE $\frac{{dx}}{{dt}} = f(x)$ ,
651 > \[
652 > \frac{{dG(x(t))}}{{dt}} = 0.
653 > \]
654 > Using chain rule, one may obtain,
655 > \[
656 > \sum\limits_i {\frac{{dG}}{{dx_i }}} f_i (x) = f \bullet \nabla G,
657 > \]
658 > which is the condition for conserving \emph{first integral}. For a
659 > canonical Hamiltonian system, the time evolution of an arbitrary
660 > smooth function $G$ is given by,
661 > \begin{equation}
662 > \begin{array}{c}
663 > \frac{{dG(x(t))}}{{dt}} = [\nabla _x G(x(t))]^T \dot x(t) \\
664 >  = [\nabla _x G(x(t))]^T J\nabla _x H(x(t)). \\
665 > \end{array}
666 > \label{introEquation:firstIntegral1}
667 > \end{equation}
668 > Using poisson bracket notion, Equation
669 > \ref{introEquation:firstIntegral1} can be rewritten as
670 > \[
671 > \frac{d}{{dt}}G(x(t)) = \left\{ {G,H} \right\}(x(t)).
672 > \]
673 > Therefore, the sufficient condition for $G$ to be the \emph{first
674 > integral} of a Hamiltonian system is
675 > \[
676 > \left\{ {G,H} \right\} = 0.
677 > \]
678 > As well known, the Hamiltonian (or energy) H of a Hamiltonian system
679 > is a \emph{first integral}, which is due to the fact $\{ H,H\}  =
680 > 0$.
681  
329 A rigid body is a body in which the distance between any two given
330 points of a rigid body remains constant regardless of external
331 forces exerted on it. A rigid body therefore conserves its shape
332 during its motion.
682  
683 < Applications of dynamics of rigid bodies.
683 > When designing any numerical methods, one should always try to
684 > preserve the structural properties of the original ODE and its flow.
685  
686 < \subsection{\label{introSection:lieAlgebra}Lie Algebra}
686 > \subsection{\label{introSection:constructionSymplectic}Construction of Symplectic Methods}
687 > A lot of well established and very effective numerical methods have
688 > been successful precisely because of their symplecticities even
689 > though this fact was not recognized when they were first
690 > constructed. The most famous example is leapfrog methods in
691 > molecular dynamics. In general, symplectic integrators can be
692 > constructed using one of four different methods.
693 > \begin{enumerate}
694 > \item Generating functions
695 > \item Variational methods
696 > \item Runge-Kutta methods
697 > \item Splitting methods
698 > \end{enumerate}
699  
700 < \subsection{\label{introSection:DLMMotionEquation}The Euler Equations of Rigid Body Motion}
700 > Generating function tends to lead to methods which are cumbersome
701 > and difficult to use. In dissipative systems, variational methods
702 > can capture the decay of energy accurately. Since their
703 > geometrically unstable nature against non-Hamiltonian perturbations,
704 > ordinary implicit Runge-Kutta methods are not suitable for
705 > Hamiltonian system. Recently, various high-order explicit
706 > Runge--Kutta methods have been developed to overcome this
707 > instability. However, due to computational penalty involved in
708 > implementing the Runge-Kutta methods, they do not attract too much
709 > attention from Molecular Dynamics community. Instead, splitting have
710 > been widely accepted since they exploit natural decompositions of
711 > the system\cite{Tuckerman92}.
712  
713 < \subsection{\label{introSection:otherRBMotionEquation}Other Formulations for Rigid Body Motion}
713 > \subsubsection{\label{introSection:splittingMethod}Splitting Method}
714  
715 < %\subsection{\label{introSection:poissonBrackets}Poisson Brackets}
715 > The main idea behind splitting methods is to decompose the discrete
716 > $\varphi_h$ as a composition of simpler flows,
717 > \begin{equation}
718 > \varphi _h  = \varphi _{h_1 }  \circ \varphi _{h_2 }  \ldots  \circ
719 > \varphi _{h_n }
720 > \label{introEquation:FlowDecomposition}
721 > \end{equation}
722 > where each of the sub-flow is chosen such that each represent a
723 > simpler integration of the system.
724  
725 < \section{\label{introSection:correlationFunctions}Correlation Functions}
725 > Suppose that a Hamiltonian system takes the form,
726 > \[
727 > H = H_1 + H_2.
728 > \]
729 > Here, $H_1$ and $H_2$ may represent different physical processes of
730 > the system. For instance, they may relate to kinetic and potential
731 > energy respectively, which is a natural decomposition of the
732 > problem. If $H_1$ and $H_2$ can be integrated using exact flows
733 > $\varphi_1(t)$ and $\varphi_2(t)$, respectively, a simple first
734 > order is then given by the Lie-Trotter formula
735 > \begin{equation}
736 > \varphi _h  = \varphi _{1,h}  \circ \varphi _{2,h},
737 > \label{introEquation:firstOrderSplitting}
738 > \end{equation}
739 > where $\varphi _h$ is the result of applying the corresponding
740 > continuous $\varphi _i$ over a time $h$. By definition, as
741 > $\varphi_i(t)$ is the exact solution of a Hamiltonian system, it
742 > must follow that each operator $\varphi_i(t)$ is a symplectic map.
743 > It is easy to show that any composition of symplectic flows yields a
744 > symplectic map,
745 > \begin{equation}
746 > (\varphi '\phi ')^T J\varphi '\phi ' = \phi '^T \varphi '^T J\varphi
747 > '\phi ' = \phi '^T J\phi ' = J,
748 > \label{introEquation:SymplecticFlowComposition}
749 > \end{equation}
750 > where $\phi$ and $\psi$ both are symplectic maps. Thus operator
751 > splitting in this context automatically generates a symplectic map.
752  
753 < \section{\label{introSection:langevinDynamics}Langevin Dynamics}
754 <
755 < \subsection{\label{introSection:LDIntroduction}Introduction and application of Langevin Dynamics}
349 <
350 < \subsection{\label{introSection:generalizedLangevinDynamics}Generalized Langevin Dynamics}
351 <
753 > The Lie-Trotter splitting(\ref{introEquation:firstOrderSplitting})
754 > introduces local errors proportional to $h^2$, while Strang
755 > splitting gives a second-order decomposition,
756   \begin{equation}
757 < H = \frac{{p^2 }}{{2m}} + U(x) + H_B  + \Delta U(x,x_1 , \ldots x_N)
758 < \label{introEquation:bathGLE}
757 > \varphi _h  = \varphi _{1,h/2}  \circ \varphi _{2,h}  \circ \varphi
758 > _{1,h/2} , \label{introEquation:secondOrderSplitting}
759   \end{equation}
760 < where $H_B$ is harmonic bath Hamiltonian,
760 > which has a local error proportional to $h^3$. Sprang splitting's
761 > popularity in molecular simulation community attribute to its
762 > symmetric property,
763 > \begin{equation}
764 > \varphi _h^{ - 1} = \varphi _{ - h}.
765 > \label{introEquation:timeReversible}
766 > \end{equation}
767 >
768 > \subsubsection{\label{introSection:exampleSplittingMethod}Example of Splitting Method}
769 > The classical equation for a system consisting of interacting
770 > particles can be written in Hamiltonian form,
771   \[
772 < H_B  =\sum\limits_{\alpha  = 1}^N {\left\{ {\frac{{p_\alpha ^2
359 < }}{{2m_\alpha  }} + \frac{1}{2}m_\alpha  w_\alpha ^2 } \right\}}
772 > H = T + V
773   \]
774 < and $\Delta U$ is bilinear system-bath coupling,
775 < \[
776 < \Delta U =  - \sum\limits_{\alpha  = 1}^N {g_\alpha  x_\alpha  x}
364 < \]
365 < Completing the square,
366 < \[
367 < H_B  + \Delta U = \sum\limits_{\alpha  = 1}^N {\left\{
368 < {\frac{{p_\alpha ^2 }}{{2m_\alpha  }} + \frac{1}{2}m_\alpha
369 < w_\alpha ^2 \left( {x_\alpha   - \frac{{g_\alpha  }}{{m_\alpha
370 < w_\alpha ^2 }}x} \right)^2 } \right\}}  - \sum\limits_{\alpha  =
371 < 1}^N {\frac{{g_\alpha ^2 }}{{2m_\alpha  w_\alpha ^2 }}} x^2
372 < \]
373 < and putting it back into Eq.~\ref{introEquation:bathGLE},
374 < \[
375 < H = \frac{{p^2 }}{{2m}} + W(x) + \sum\limits_{\alpha  = 1}^N
376 < {\left\{ {\frac{{p_\alpha ^2 }}{{2m_\alpha  }} + \frac{1}{2}m_\alpha
377 < w_\alpha ^2 \left( {x_\alpha   - \frac{{g_\alpha  }}{{m_\alpha
378 < w_\alpha ^2 }}x} \right)^2 } \right\}}
379 < \]
380 < where
381 < \[
382 < W(x) = U(x) - \sum\limits_{\alpha  = 1}^N {\frac{{g_\alpha ^2
383 < }}{{2m_\alpha  w_\alpha ^2 }}} x^2
384 < \]
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},
774 > where $T$ is the kinetic energy and $V$ is the potential energy.
775 > Setting $H_1 = T, H_2 = V$ and applying Strang splitting, one
776 > obtains the following:
777   \begin{align}
778 < \dot p &=  - \frac{{\partial H}}{{\partial x}}
779 <       &= m\ddot x
780 <       &= - \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)}
781 < \label{introEq:Lp5}
778 > q(\Delta t) &= q(0) + \dot{q}(0)\Delta t +
779 >    \frac{F[q(0)]}{m}\frac{\Delta t^2}{2}, %
780 > \label{introEquation:Lp10a} \\%
781 > %
782 > \dot{q}(\Delta t) &= \dot{q}(0) + \frac{\Delta t}{2m}
783 >    \biggl [F[q(0)] + F[q(\Delta t)] \biggr]. %
784 > \label{introEquation:Lp10b}
785   \end{align}
786 < , and
786 > where $F(t)$ is the force at time $t$. This integration scheme is
787 > known as \emph{velocity verlet} which is
788 > symplectic(\ref{introEquation:SymplecticFlowComposition}),
789 > time-reversible(\ref{introEquation:timeReversible}) and
790 > volume-preserving (\ref{introEquation:volumePreserving}). These
791 > geometric properties attribute to its long-time stability and its
792 > popularity in the community. However, the most commonly used
793 > velocity verlet integration scheme is written as below,
794   \begin{align}
795 < \dot p_\alpha   &=  - \frac{{\partial H}}{{\partial x_\alpha  }}
796 <                &= m\ddot x_\alpha
797 <                &= \- m_\alpha  w_\alpha ^2 \left( {x_\alpha   - \frac{{g_\alpha}}{{m_\alpha  w_\alpha ^2 }}x} \right)
795 > \dot{q}\biggl (\frac{\Delta t}{2}\biggr ) &=
796 >    \dot{q}(0) + \frac{\Delta t}{2m}\, F[q(0)], \label{introEquation:Lp9a}\\%
797 > %
798 > q(\Delta t) &= q(0) + \Delta t\, \dot{q}\biggl (\frac{\Delta t}{2}\biggr ),%
799 >    \label{introEquation:Lp9b}\\%
800 > %
801 > \dot{q}(\Delta t) &= \dot{q}\biggl (\frac{\Delta t}{2}\biggr ) +
802 >    \frac{\Delta t}{2m}\, F[q(0)]. \label{introEquation:Lp9c}
803   \end{align}
804 + From the preceding splitting, one can see that the integration of
805 + the equations of motion would follow:
806 + \begin{enumerate}
807 + \item calculate the velocities at the half step, $\frac{\Delta t}{2}$, from the forces calculated at the initial position.
808  
809 < \subsection{\label{introSection:laplaceTransform}The Laplace Transform}
809 > \item Use the half step velocities to move positions one whole step, $\Delta t$.
810  
811 < \[
406 < L(x) = \int_0^\infty  {x(t)e^{ - pt} dt}
407 < \]
811 > \item Evaluate the forces at the new positions, $\mathbf{r}(\Delta t)$, and use the new forces to complete the velocity move.
812  
813 < \[
814 < L(x + y) = L(x) + L(y)
411 < \]
813 > \item Repeat from step 1 with the new position, velocities, and forces assuming the roles of the initial values.
814 > \end{enumerate}
815  
816 < \[
817 < L(ax) = aL(x)
818 < \]
816 > Simply switching the order of splitting and composing, a new
817 > integrator, the \emph{position verlet} integrator, can be generated,
818 > \begin{align}
819 > \dot q(\Delta t) &= \dot q(0) + \Delta tF(q(0))\left[ {q(0) +
820 > \frac{{\Delta t}}{{2m}}\dot q(0)} \right], %
821 > \label{introEquation:positionVerlet1} \\%
822 > %
823 > q(\Delta t) &= q(0) + \frac{{\Delta t}}{2}\left[ {\dot q(0) + \dot
824 > q(\Delta t)} \right]. %
825 > \label{introEquation:positionVerlet2}
826 > \end{align}
827  
828 + \subsubsection{\label{introSection:errorAnalysis}Error Analysis and Higher Order Methods}
829 +
830 + Baker-Campbell-Hausdorff formula can be used to determine the local
831 + error of splitting method in terms of commutator of the
832 + operators(\ref{introEquation:exponentialOperator}) associated with
833 + the sub-flow. For operators $hX$ and $hY$ which are associate to
834 + $\varphi_1(t)$ and $\varphi_2(t$ respectively , we have
835 + \begin{equation}
836 + \exp (hX + hY) = \exp (hZ)
837 + \end{equation}
838 + where
839 + \begin{equation}
840 + hZ = hX + hY + \frac{{h^2 }}{2}[X,Y] + \frac{{h^3 }}{2}\left(
841 + {[X,[X,Y]] + [Y,[Y,X]]} \right) +  \ldots .
842 + \end{equation}
843 + Here, $[X,Y]$ is the commutators of operator $X$ and $Y$ given by
844   \[
845 < L(\dot x) = pL(x) - px(0)
845 > [X,Y] = XY - YX .
846   \]
847 <
847 > Applying Baker-Campbell-Hausdorff formula to Sprang splitting, we
848 > can obtain
849 > \begin{eqnarray*}
850 > \exp (h X/2)\exp (h Y)\exp (h X/2) & = & \exp (h X + h Y + h^2
851 > [X,Y]/4 + h^2 [Y,X]/4 \\ & & \mbox{} + h^2 [X,X]/8 + h^2 [Y,Y]/8 \\
852 > & & \mbox{} + h^3 [Y,[Y,X]]/12 - h^3 [X,[X,Y]]/24 & & \mbox{} +
853 > \ldots )
854 > \end{eqnarray*}
855 > Since \[ [X,Y] + [Y,X] = 0\] and \[ [X,X] = 0\], the dominant local
856 > error of Spring splitting is proportional to $h^3$. The same
857 > procedure can be applied to general splitting,  of the form
858 > \begin{equation}
859 > \varphi _{b_m h}^2  \circ \varphi _{a_m h}^1  \circ \varphi _{b_{m -
860 > 1} h}^2  \circ  \ldots  \circ \varphi _{a_1 h}^1 .
861 > \end{equation}
862 > Careful choice of coefficient $a_1 ,\ldot , b_m$ will lead to higher
863 > order method. Yoshida proposed an elegant way to compose higher
864 > order methods based on symmetric splitting. Given a symmetric second
865 > order base method $ \varphi _h^{(2)} $, a fourth-order symmetric
866 > method can be constructed by composing,
867   \[
868 < L(\ddot x) = p^2 L(x) - px(0) - \dot x(0)
868 > \varphi _h^{(4)}  = \varphi _{\alpha h}^{(2)}  \circ \varphi _{\beta
869 > h}^{(2)}  \circ \varphi _{\alpha h}^{(2)}
870   \]
871 <
871 > where $ \alpha  =  - \frac{{2^{1/3} }}{{2 - 2^{1/3} }}$ and $ \beta
872 > = \frac{{2^{1/3} }}{{2 - 2^{1/3} }}$. Moreover, a symmetric
873 > integrator $ \varphi _h^{(2n + 2)}$ can be composed by
874 > \begin{equation}
875 > \varphi _h^{(2n + 2)}  = \varphi _{\alpha h}^{(2n)}  \circ \varphi
876 > _{\beta h}^{(2n)}  \circ \varphi _{\alpha h}^{(2n)}
877 > \end{equation}
878 > , if the weights are chosen as
879   \[
880 < L\left( {\int_0^t {g(t - \tau )h(\tau )d\tau } } \right) = G(p)H(p)
880 > \alpha  =  - \frac{{2^{1/(2n + 1)} }}{{2 - 2^{1/(2n + 1)} }},\beta =
881 > \frac{{2^{1/(2n + 1)} }}{{2 - 2^{1/(2n + 1)} }} .
882   \]
883  
884 < Some relatively important transformation,
884 > \section{\label{introSection:molecularDynamics}Molecular Dynamics}
885 >
886 > As a special discipline of molecular modeling, Molecular dynamics
887 > has proven to be a powerful tool for studying the functions of
888 > biological systems, providing structural, thermodynamic and
889 > dynamical information.
890 >
891 > One of the principal tools for modeling proteins, nucleic acids and
892 > their complexes. Stability of proteins Folding of proteins.
893 > Molecular recognition by:proteins, DNA, RNA, lipids, hormones STP,
894 > etc. Enzyme reactions Rational design of biologically active
895 > molecules (drug design) Small and large-scale conformational
896 > changes. determination and construction of 3D structures (homology,
897 > Xray diffraction, NMR) Dynamic processes such as ion transport in
898 > biological systems.
899 >
900 > Macroscopic properties are related to microscopic behavior.
901 >
902 > Time dependent (and independent) microscopic behavior of a molecule
903 > can be calculated by molecular dynamics simulations.
904 >
905 > \subsection{\label{introSec:mdInit}Initialization}
906 >
907 > \subsection{\label{introSec:forceEvaluation}Force Evaluation}
908 >
909 > \subsection{\label{introSection:mdIntegration} Integration of the Equations of Motion}
910 >
911 > \section{\label{introSection:rigidBody}Dynamics of Rigid Bodies}
912 >
913 > Rigid bodies are frequently involved in the modeling of different
914 > areas, from engineering, physics, to chemistry. For example,
915 > missiles and vehicle are usually modeled by rigid bodies.  The
916 > movement of the objects in 3D gaming engine or other physics
917 > simulator is governed by the rigid body dynamics. In molecular
918 > simulation, rigid body is used to simplify the model in
919 > protein-protein docking study{\cite{Gray03}}.
920 >
921 > It is very important to develop stable and efficient methods to
922 > integrate the equations of motion of orientational degrees of
923 > freedom. Euler angles are the nature choice to describe the
924 > rotational degrees of freedom. However, due to its singularity, the
925 > numerical integration of corresponding equations of motion is very
926 > inefficient and inaccurate. Although an alternative integrator using
927 > different sets of Euler angles can overcome this difficulty\cite{},
928 > the computational penalty and the lost of angular momentum
929 > conservation still remain. A singularity free representation
930 > utilizing quaternions was developed by Evans in 1977. Unfortunately,
931 > this approach suffer from the nonseparable Hamiltonian resulted from
932 > quaternion representation, which prevents the symplectic algorithm
933 > to be utilized. Another different approach is to apply holonomic
934 > constraints to the atoms belonging to the rigid body. Each atom
935 > moves independently under the normal forces deriving from potential
936 > energy and constraint forces which are used to guarantee the
937 > rigidness. However, due to their iterative nature, SHAKE and Rattle
938 > algorithm converge very slowly when the number of constraint
939 > increases.
940 >
941 > The break through in geometric literature suggests that, in order to
942 > develop a long-term integration scheme, one should preserve the
943 > symplectic structure of the flow. Introducing conjugate momentum to
944 > rotation matrix $Q$ and re-formulating Hamiltonian's equation, a
945 > symplectic integrator, RSHAKE, was proposed to evolve the
946 > Hamiltonian system in a constraint manifold by iteratively
947 > satisfying the orthogonality constraint $Q_T Q = 1$. An alternative
948 > method using quaternion representation was developed by Omelyan.
949 > However, both of these methods are iterative and inefficient. In
950 > this section, we will present a symplectic Lie-Poisson integrator
951 > for rigid body developed by Dullweber and his
952 > coworkers\cite{Dullweber1997} in depth.
953 >
954 > \subsection{\label{introSection:constrainedHamiltonianRB}Constrained Hamiltonian for Rigid Body}
955 > The motion of the rigid body is Hamiltonian with the Hamiltonian
956 > function
957 > \begin{equation}
958 > H = \frac{1}{2}(p^T m^{ - 1} p) + \frac{1}{2}tr(PJ^{ - 1} P) +
959 > V(q,Q) + \frac{1}{2}tr[(QQ^T  - 1)\Lambda ].
960 > \label{introEquation:RBHamiltonian}
961 > \end{equation}
962 > Here, $q$ and $Q$  are the position and rotation matrix for the
963 > rigid-body, $p$ and $P$  are conjugate momenta to $q$  and $Q$ , and
964 > $J$, a diagonal matrix, is defined by
965   \[
966 < L(\cos at) = \frac{p}{{p^2  + a^2 }}
966 > I_{ii}^{ - 1}  = \frac{1}{2}\sum\limits_{i \ne j} {J_{jj}^{ - 1} }
967 > \]
968 > where $I_{ii}$ is the diagonal element of the inertia tensor. This
969 > constrained Hamiltonian equation subjects to a holonomic constraint,
970 > \begin{equation}
971 > Q^T Q = 1$, \label{introEquation:orthogonalConstraint}
972 > \end{equation}
973 > which is used to ensure rotation matrix's orthogonality.
974 > Differentiating \ref{introEquation:orthogonalConstraint} and using
975 > Equation \ref{introEquation:RBMotionMomentum}, one may obtain,
976 > \begin{equation}
977 > Q^T PJ^{ - 1}  + J^{ - 1} P^T Q = 0 . \\
978 > \label{introEquation:RBFirstOrderConstraint}
979 > \end{equation}
980 >
981 > Using Equation (\ref{introEquation:motionHamiltonianCoordinate},
982 > \ref{introEquation:motionHamiltonianMomentum}), one can write down
983 > the equations of motion,
984 > \[
985 > \begin{array}{c}
986 > \frac{{dq}}{{dt}} = \frac{p}{m} \label{introEquation:RBMotionPosition}\\
987 > \frac{{dp}}{{dt}} =  - \nabla _q V(q,Q) \label{introEquation:RBMotionMomentum}\\
988 > \frac{{dQ}}{{dt}} = PJ^{ - 1}  \label{introEquation:RBMotionRotation}\\
989 > \frac{{dP}}{{dt}} =  - \nabla _Q V(q,Q) - 2Q\Lambda . \label{introEquation:RBMotionP}\\
990 > \end{array}
991   \]
992  
993 + In general, there are two ways to satisfy the holonomic constraints.
994 + We can use constraint force provided by lagrange multiplier on the
995 + normal manifold to keep the motion on constraint space. Or we can
996 + simply evolve the system in constraint manifold. The two method are
997 + proved to be equivalent. The holonomic constraint and equations of
998 + motions define a constraint manifold for rigid body
999   \[
1000 < L(\sin at) = \frac{a}{{p^2  + a^2 }}
1000 > M = \left\{ {(Q,P):Q^T Q = 1,Q^T PJ^{ - 1}  + J^{ - 1} P^T Q = 0}
1001 > \right\}.
1002   \]
1003  
1004 + Unfortunately, this constraint manifold is not the cotangent bundle
1005 + $T_{\star}SO(3)$. However, it turns out that under symplectic
1006 + transformation, the cotangent space and the phase space are
1007 + diffeomorphic. Introducing
1008   \[
1009 < L(1) = \frac{1}{p}
1009 > \tilde Q = Q,\tilde P = \frac{1}{2}\left( {P - QP^T Q} \right),
1010   \]
1011 + the mechanical system subject to a holonomic constraint manifold $M$
1012 + can be re-formulated as a Hamiltonian system on the cotangent space
1013 + \[
1014 + T^* SO(3) = \left\{ {(\tilde Q,\tilde P):\tilde Q^T \tilde Q =
1015 + 1,\tilde Q^T \tilde PJ^{ - 1}  + J^{ - 1} P^T \tilde Q = 0} \right\}
1016 + \]
1017  
1018 < First, the bath coordinates,
1018 > For a body fixed vector $X_i$ with respect to the center of mass of
1019 > the rigid body, its corresponding lab fixed vector $X_0^{lab}$  is
1020 > given as
1021 > \begin{equation}
1022 > X_i^{lab} = Q X_i + q.
1023 > \end{equation}
1024 > Therefore, potential energy $V(q,Q)$ is defined by
1025   \[
1026 < p^2 L(x_\alpha  ) - px_\alpha  (0) - \dot x_\alpha  (0) =  - \omega
445 < _\alpha ^2 L(x_\alpha  ) + \frac{{g_\alpha  }}{{\omega _\alpha
446 < }}L(x)
1026 > V(q,Q) = V(Q X_0 + q).
1027   \]
1028 + Hence, the force and torque are given by
1029   \[
1030 < L(x_\alpha  ) = \frac{{\frac{{g_\alpha  }}{{\omega _\alpha  }}L(x) +
450 < px_\alpha  (0) + \dot x_\alpha  (0)}}{{p^2  + \omega _\alpha ^2 }}
1030 > \nabla _q V(q,Q) = F(q,Q) = \sum\limits_i {F_i (q,Q)},
1031   \]
1032 < Then, the system coordinates,
1033 < \begin{align}
1034 < mL(\ddot x) &=  - \frac{1}{p}\frac{{\partial W(x)}}{{\partial x}} -
1035 < \sum\limits_{\alpha  = 1}^N {\left\{ {\frac{{\frac{{g_\alpha
1036 < }}{{\omega _\alpha  }}L(x) + px_\alpha  (0) + \dot x_\alpha
1037 < (0)}}{{p^2  + \omega _\alpha ^2 }} - \frac{{g_\alpha ^2 }}{{m_\alpha
1038 < }}\omega _\alpha ^2 L(x)} \right\}}
1039 < %
1040 < &= - \frac{1}{p}\frac{{\partial W(x)}}{{\partial x}} -
1041 < \sum\limits_{\alpha  = 1}^N {\left\{ { - \frac{{g_\alpha ^2 }}{{m_\alpha  \omega _\alpha ^2 }}\frac{p}{{p^2  + \omega _\alpha ^2 }}pL(x)
1042 < - \frac{p}{{p^2  + \omega _\alpha ^2 }}g_\alpha  x_\alpha  (0)
1043 < - \frac{1}{{p^2  + \omega _\alpha ^2 }}g_\alpha  \dot x_\alpha  (0)} \right\}}
1044 < \end{align}
1045 < Then, the inverse transform,
1032 > and
1033 > \[
1034 > \nabla _Q V(q,Q) = F(q,Q)X_i^t
1035 > \]
1036 > respectively.
1037 >
1038 > As a common choice to describe the rotation dynamics of the rigid
1039 > body, angular momentum on body frame $\Pi  = Q^t P$ is introduced to
1040 > rewrite the equations of motion,
1041 > \begin{equation}
1042 > \begin{array}{l}
1043 > \mathop \Pi \limits^ \bullet   = J^{ - 1} \Pi ^T \Pi  + Q^T \sum\limits_i {F_i (q,Q)X_i^T }  - \Lambda  \\
1044 > \mathop Q\limits^{{\rm{   }} \bullet }  = Q\Pi {\rm{ }}J^{ - 1}  \\
1045 > \end{array}
1046 > \label{introEqaution:RBMotionPI}
1047 > \end{equation}
1048 > , as well as holonomic constraints,
1049 > \[
1050 > \begin{array}{l}
1051 > \Pi J^{ - 1}  + J^{ - 1} \Pi ^t  = 0 \\
1052 > Q^T Q = 1 \\
1053 > \end{array}
1054 > \]
1055 >
1056 > For a vector $v(v_1 ,v_2 ,v_3 ) \in R^3$ and a matrix $\hat v \in
1057 > so(3)^ \star$, the hat-map isomorphism,
1058 > \begin{equation}
1059 > v(v_1 ,v_2 ,v_3 ) \Leftrightarrow \hat v = \left(
1060 > {\begin{array}{*{20}c}
1061 >   0 & { - v_3 } & {v_2 }  \\
1062 >   {v_3 } & 0 & { - v_1 }  \\
1063 >   { - v_2 } & {v_1 } & 0  \\
1064 > \end{array}} \right),
1065 > \label{introEquation:hatmapIsomorphism}
1066 > \end{equation}
1067 > will let us associate the matrix products with traditional vector
1068 > operations
1069 > \[
1070 > \hat vu = v \times u
1071 > \]
1072 >
1073 > Using \ref{introEqaution:RBMotionPI}, one can construct a skew
1074 > matrix,
1075 > \begin{equation}
1076 > (\mathop \Pi \limits^ \bullet   - \mathop \Pi \limits^ \bullet  ^T
1077 > ){\rm{ }} = {\rm{ }}(\Pi  - \Pi ^T ){\rm{ }}(J^{ - 1} \Pi  + \Pi J^{
1078 > - 1} ) + \sum\limits_i {[Q^T F_i (r,Q)X_i^T  - X_i F_i (r,Q)^T Q]} -
1079 > (\Lambda  - \Lambda ^T ) . \label{introEquation:skewMatrixPI}
1080 > \end{equation}
1081 > Since $\Lambda$ is symmetric, the last term of Equation
1082 > \ref{introEquation:skewMatrixPI} is zero, which implies the Lagrange
1083 > multiplier $\Lambda$ is absent from the equations of motion. This
1084 > unique property eliminate the requirement of iterations which can
1085 > not be avoided in other methods\cite{}.
1086 >
1087 > Applying hat-map isomorphism, we obtain the equation of motion for
1088 > angular momentum on body frame
1089 > \begin{equation}
1090 > \dot \pi  = \pi  \times I^{ - 1} \pi  + \sum\limits_i {\left( {Q^T
1091 > F_i (r,Q)} \right) \times X_i }.
1092 > \label{introEquation:bodyAngularMotion}
1093 > \end{equation}
1094 > In the same manner, the equation of motion for rotation matrix is
1095 > given by
1096 > \[
1097 > \dot Q = Qskew(I^{ - 1} \pi )
1098 > \]
1099 >
1100 > \subsection{\label{introSection:SymplecticFreeRB}Symplectic
1101 > Lie-Poisson Integrator for Free Rigid Body}
1102 >
1103 > If there is not external forces exerted on the rigid body, the only
1104 > contribution to the rotational is from the kinetic potential (the
1105 > first term of \ref{ introEquation:bodyAngularMotion}). The free
1106 > rigid body is an example of Lie-Poisson system with Hamiltonian
1107 > function
1108 > \begin{equation}
1109 > T^r (\pi ) = T_1 ^r (\pi _1 ) + T_2^r (\pi _2 ) + T_3^r (\pi _3 )
1110 > \label{introEquation:rotationalKineticRB}
1111 > \end{equation}
1112 > where $T_i^r (\pi _i ) = \frac{{\pi _i ^2 }}{{2I_i }}$ and
1113 > Lie-Poisson structure matrix,
1114 > \begin{equation}
1115 > J(\pi ) = \left( {\begin{array}{*{20}c}
1116 >   0 & {\pi _3 } & { - \pi _2 }  \\
1117 >   { - \pi _3 } & 0 & {\pi _1 }  \\
1118 >   {\pi _2 } & { - \pi _1 } & 0  \\
1119 > \end{array}} \right)
1120 > \end{equation}
1121 > Thus, the dynamics of free rigid body is governed by
1122 > \begin{equation}
1123 > \frac{d}{{dt}}\pi  = J(\pi )\nabla _\pi  T^r (\pi )
1124 > \end{equation}
1125 >
1126 > One may notice that each $T_i^r$ in Equation
1127 > \ref{introEquation:rotationalKineticRB} can be solved exactly. For
1128 > instance, the equations of motion due to $T_1^r$ are given by
1129 > \begin{equation}
1130 > \frac{d}{{dt}}\pi  = R_1 \pi ,\frac{d}{{dt}}Q = QR_1
1131 > \label{introEqaution:RBMotionSingleTerm}
1132 > \end{equation}
1133 > where
1134 > \[ R_1  = \left( {\begin{array}{*{20}c}
1135 >   0 & 0 & 0  \\
1136 >   0 & 0 & {\pi _1 }  \\
1137 >   0 & { - \pi _1 } & 0  \\
1138 > \end{array}} \right).
1139 > \]
1140 > The solutions of Equation \ref{introEqaution:RBMotionSingleTerm} is
1141 > \[
1142 > \pi (\Delta t) = e^{\Delta tR_1 } \pi (0),Q(\Delta t) =
1143 > Q(0)e^{\Delta tR_1 }
1144 > \]
1145 > with
1146 > \[
1147 > e^{\Delta tR_1 }  = \left( {\begin{array}{*{20}c}
1148 >   0 & 0 & 0  \\
1149 >   0 & {\cos \theta _1 } & {\sin \theta _1 }  \\
1150 >   0 & { - \sin \theta _1 } & {\cos \theta _1 }  \\
1151 > \end{array}} \right),\theta _1  = \frac{{\pi _1 }}{{I_1 }}\Delta t.
1152 > \]
1153 > To reduce the cost of computing expensive functions in $e^{\Delta
1154 > tR_1 }$, we can use Cayley transformation,
1155 > \[
1156 > e^{\Delta tR_1 }  \approx (1 - \Delta tR_1 )^{ - 1} (1 + \Delta tR_1
1157 > )
1158 > \]
1159 >
1160 > The flow maps for $T_2^r$ and $T_2^r$ can be found in the same
1161 > manner.
1162 >
1163 > In order to construct a second-order symplectic method, we split the
1164 > angular kinetic Hamiltonian function can into five terms
1165 > \[
1166 > T^r (\pi ) = \frac{1}{2}T_1 ^r (\pi _1 ) + \frac{1}{2}T_2^r (\pi _2
1167 > ) + T_3^r (\pi _3 ) + \frac{1}{2}T_2^r (\pi _2 ) + \frac{1}{2}T_1 ^r
1168 > (\pi _1 )
1169 > \].
1170 > Concatenating flows corresponding to these five terms, we can obtain
1171 > an symplectic integrator,
1172 > \[
1173 > \varphi _{\Delta t,T^r }  = \varphi _{\Delta t/2,\pi _1 }  \circ
1174 > \varphi _{\Delta t/2,\pi _2 }  \circ \varphi _{\Delta t,\pi _3 }
1175 > \circ \varphi _{\Delta t/2,\pi _2 }  \circ \varphi _{\Delta t/2,\pi
1176 > _1 }.
1177 > \]
1178 >
1179 > The non-canonical Lie-Poisson bracket ${F, G}$ of two function
1180 > $F(\pi )$ and $G(\pi )$ is defined by
1181 > \[
1182 > \{ F,G\} (\pi ) = [\nabla _\pi  F(\pi )]^T J(\pi )\nabla _\pi  G(\pi
1183 > )
1184 > \]
1185 > If the Poisson bracket of a function $F$ with an arbitrary smooth
1186 > function $G$ is zero, $F$ is a \emph{Casimir}, which is the
1187 > conserved quantity in Poisson system. We can easily verify that the
1188 > norm of the angular momentum, $\parallel \pi
1189 > \parallel$, is a \emph{Casimir}. Let$ F(\pi ) = S(\frac{{\parallel
1190 > \pi \parallel ^2 }}{2})$ for an arbitrary function $ S:R \to R$ ,
1191 > then by the chain rule
1192 > \[
1193 > \nabla _\pi  F(\pi ) = S'(\frac{{\parallel \pi \parallel ^2
1194 > }}{2})\pi
1195 > \]
1196 > Thus $ [\nabla _\pi  F(\pi )]^T J(\pi ) =  - S'(\frac{{\parallel \pi
1197 > \parallel ^2 }}{2})\pi  \times \pi  = 0 $. This explicit
1198 > Lie-Poisson integrator is found to be extremely efficient and stable
1199 > which can be explained by the fact the small angle approximation is
1200 > used and the norm of the angular momentum is conserved.
1201 >
1202 > \subsection{\label{introSection:RBHamiltonianSplitting} Hamiltonian
1203 > Splitting for Rigid Body}
1204 >
1205 > The Hamiltonian of rigid body can be separated in terms of kinetic
1206 > energy and potential energy,
1207 > \[
1208 > H = T(p,\pi ) + V(q,Q)
1209 > \]
1210 > The equations of motion corresponding to potential energy and
1211 > kinetic energy are listed in the below table,
1212 > \begin{center}
1213 > \begin{tabular}{|l|l|}
1214 >  \hline
1215 >  % after \\: \hline or \cline{col1-col2} \cline{col3-col4} ...
1216 >  Potential & Kinetic \\
1217 >  $\frac{{dq}}{{dt}} = \frac{p}{m}$ & $\frac{d}{{dt}}q = p$ \\
1218 >  $\frac{d}{{dt}}p =  - \frac{{\partial V}}{{\partial q}}$ & $ \frac{d}{{dt}}p = 0$ \\
1219 >  $\frac{d}{{dt}}Q = 0$ & $ \frac{d}{{dt}}Q = Qskew(I^{ - 1} j)$ \\
1220 >  $ \frac{d}{{dt}}\pi  = \sum\limits_i {\left( {Q^T F_i (r,Q)} \right) \times X_i }$ & $\frac{d}{{dt}}\pi  = \pi  \times I^{ - 1} \pi$\\
1221 >  \hline
1222 > \end{tabular}
1223 > \end{center}
1224 > A second-order symplectic method is now obtained by the composition
1225 > of the flow maps,
1226 > \[
1227 > \varphi _{\Delta t}  = \varphi _{\Delta t/2,V}  \circ \varphi
1228 > _{\Delta t,T}  \circ \varphi _{\Delta t/2,V}.
1229 > \]
1230 > Moreover, $\varphi _{\Delta t/2,V}$ can be divided into two
1231 > sub-flows which corresponding to force and torque respectively,
1232 > \[
1233 > \varphi _{\Delta t/2,V}  = \varphi _{\Delta t/2,F}  \circ \varphi
1234 > _{\Delta t/2,\tau }.
1235 > \]
1236 > Since the associated operators of $\varphi _{\Delta t/2,F} $ and
1237 > $\circ \varphi _{\Delta t/2,\tau }$ are commuted, the composition
1238 > order inside $\varphi _{\Delta t/2,V}$ does not matter.
1239 >
1240 > Furthermore, kinetic potential can be separated to translational
1241 > kinetic term, $T^t (p)$, and rotational kinetic term, $T^r (\pi )$,
1242 > \begin{equation}
1243 > T(p,\pi ) =T^t (p) + T^r (\pi ).
1244 > \end{equation}
1245 > where $ T^t (p) = \frac{1}{2}p^T m^{ - 1} p $ and $T^r (\pi )$ is
1246 > defined by \ref{introEquation:rotationalKineticRB}. Therefore, the
1247 > corresponding flow maps are given by
1248 > \[
1249 > \varphi _{\Delta t,T}  = \varphi _{\Delta t,T^t }  \circ \varphi
1250 > _{\Delta t,T^r }.
1251 > \]
1252 > Finally, we obtain the overall symplectic flow maps for free moving
1253 > rigid body
1254 > \begin{equation}
1255 > \begin{array}{c}
1256 > \varphi _{\Delta t}  = \varphi _{\Delta t/2,F}  \circ \varphi _{\Delta t/2,\tau }  \\
1257 >  \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 }  \\
1258 >  \circ \varphi _{\Delta t/2,\tau }  \circ \varphi _{\Delta t/2,F}  .\\
1259 > \end{array}
1260 > \label{introEquation:overallRBFlowMaps}
1261 > \end{equation}
1262 >
1263 > \section{\label{introSection:langevinDynamics}Langevin Dynamics}
1264 > As an alternative to newtonian dynamics, Langevin dynamics, which
1265 > mimics a simple heat bath with stochastic and dissipative forces,
1266 > has been applied in a variety of studies. This section will review
1267 > the theory of Langevin dynamics simulation. A brief derivation of
1268 > generalized Langevin equation will be given first. Follow that, we
1269 > will discuss the physical meaning of the terms appearing in the
1270 > equation as well as the calculation of friction tensor from
1271 > hydrodynamics theory.
1272 >
1273 > \subsection{\label{introSection:generalizedLangevinDynamics}Derivation of Generalized Langevin Equation}
1274 >
1275 > Harmonic bath model, in which an effective set of harmonic
1276 > oscillators are used to mimic the effect of a linearly responding
1277 > environment, has been widely used in quantum chemistry and
1278 > statistical mechanics. One of the successful applications of
1279 > Harmonic bath model is the derivation of Deriving Generalized
1280 > Langevin Dynamics. Lets consider a system, in which the degree of
1281 > freedom $x$ is assumed to couple to the bath linearly, giving a
1282 > Hamiltonian of the form
1283 > \begin{equation}
1284 > H = \frac{{p^2 }}{{2m}} + U(x) + H_B  + \Delta U(x,x_1 , \ldots x_N)
1285 > \label{introEquation:bathGLE}.
1286 > \end{equation}
1287 > Here $p$ is a momentum conjugate to $q$, $m$ is the mass associated
1288 > with this degree of freedom, $H_B$ is harmonic bath Hamiltonian,
1289 > \[
1290 > H_B  = \sum\limits_{\alpha  = 1}^N {\left\{ {\frac{{p_\alpha ^2
1291 > }}{{2m_\alpha  }} + \frac{1}{2}m_\alpha  \omega _\alpha ^2 }
1292 > \right\}}
1293 > \]
1294 > where the index $\alpha$ runs over all the bath degrees of freedom,
1295 > $\omega _\alpha$ are the harmonic bath frequencies, $m_\alpha$ are
1296 > the harmonic bath masses, and $\Delta U$ is bilinear system-bath
1297 > coupling,
1298 > \[
1299 > \Delta U =  - \sum\limits_{\alpha  = 1}^N {g_\alpha  x_\alpha  x}
1300 > \]
1301 > where $g_\alpha$ are the coupling constants between the bath and the
1302 > coordinate $x$. Introducing
1303 > \[
1304 > W(x) = U(x) - \sum\limits_{\alpha  = 1}^N {\frac{{g_\alpha ^2
1305 > }}{{2m_\alpha  w_\alpha ^2 }}} x^2
1306 > \] and combining the last two terms in Equation
1307 > \ref{introEquation:bathGLE}, we may rewrite the Harmonic bath
1308 > Hamiltonian as
1309 > \[
1310 > H = \frac{{p^2 }}{{2m}} + W(x) + \sum\limits_{\alpha  = 1}^N
1311 > {\left\{ {\frac{{p_\alpha ^2 }}{{2m_\alpha  }} + \frac{1}{2}m_\alpha
1312 > w_\alpha ^2 \left( {x_\alpha   - \frac{{g_\alpha  }}{{m_\alpha
1313 > w_\alpha ^2 }}x} \right)^2 } \right\}}
1314 > \]
1315 > Since the first two terms of the new Hamiltonian depend only on the
1316 > system coordinates, we can get the equations of motion for
1317 > Generalized Langevin Dynamics by Hamilton's equations
1318 > \ref{introEquation:motionHamiltonianCoordinate,
1319 > introEquation:motionHamiltonianMomentum},
1320 > \begin{equation}
1321 > m\ddot x =  - \frac{{\partial W(x)}}{{\partial x}} -
1322 > \sum\limits_{\alpha  = 1}^N {g_\alpha  \left( {x_\alpha   -
1323 > \frac{{g_\alpha  }}{{m_\alpha  w_\alpha ^2 }}x} \right)},
1324 > \label{introEquation:coorMotionGLE}
1325 > \end{equation}
1326 > and
1327 > \begin{equation}
1328 > m\ddot x_\alpha   =  - m_\alpha  w_\alpha ^2 \left( {x_\alpha   -
1329 > \frac{{g_\alpha  }}{{m_\alpha  w_\alpha ^2 }}x} \right).
1330 > \label{introEquation:bathMotionGLE}
1331 > \end{equation}
1332 >
1333 > In order to derive an equation for $x$, the dynamics of the bath
1334 > variables $x_\alpha$ must be solved exactly first. As an integral
1335 > transform which is particularly useful in solving linear ordinary
1336 > differential equations, Laplace transform is the appropriate tool to
1337 > solve this problem. The basic idea is to transform the difficult
1338 > differential equations into simple algebra problems which can be
1339 > solved easily. Then applying inverse Laplace transform, also known
1340 > as the Bromwich integral, we can retrieve the solutions of the
1341 > original problems.
1342 >
1343 > Let $f(t)$ be a function defined on $ [0,\infty ) $. The Laplace
1344 > transform of f(t) is a new function defined as
1345 > \[
1346 > L(f(t)) \equiv F(p) = \int_0^\infty  {f(t)e^{ - pt} dt}
1347 > \]
1348 > where  $p$ is real and  $L$ is called the Laplace Transform
1349 > Operator. Below are some important properties of Laplace transform
1350 > \begin{equation}
1351 > \begin{array}{c}
1352 > L(x + y) = L(x) + L(y) \\
1353 > L(ax) = aL(x) \\
1354 > L(\dot x) = pL(x) - px(0) \\
1355 > L(\ddot x) = p^2 L(x) - px(0) - \dot x(0) \\
1356 > L\left( {\int_0^t {g(t - \tau )h(\tau )d\tau } } \right) = G(p)H(p) \\
1357 > \end{array}
1358 > \end{equation}
1359 >
1360 > Applying Laplace transform to the bath coordinates, we obtain
1361 > \[
1362 > \begin{array}{c}
1363 > p^2 L(x_\alpha  ) - px_\alpha  (0) - \dot x_\alpha  (0) =  - \omega _\alpha ^2 L(x_\alpha  ) + \frac{{g_\alpha  }}{{\omega _\alpha  }}L(x) \\
1364 > L(x_\alpha  ) = \frac{{\frac{{g_\alpha  }}{{\omega _\alpha  }}L(x) + px_\alpha  (0) + \dot x_\alpha  (0)}}{{p^2  + \omega _\alpha ^2 }} \\
1365 > \end{array}
1366 > \]
1367 > By the same way, the system coordinates become
1368 > \[
1369 > \begin{array}{c}
1370 > mL(\ddot x) =  - \frac{1}{p}\frac{{\partial W(x)}}{{\partial x}} \\
1371 >  - \sum\limits_{\alpha  = 1}^N {\left\{ { - \frac{{g_\alpha ^2 }}{{m_\alpha  \omega _\alpha ^2 }}\frac{p}{{p^2  + \omega _\alpha ^2 }}pL(x) - \frac{p}{{p^2  + \omega _\alpha ^2 }}g_\alpha  x_\alpha  (0) - \frac{1}{{p^2  + \omega _\alpha ^2 }}g_\alpha  \dot x_\alpha  (0)} \right\}}  \\
1372 > \end{array}
1373 > \]
1374  
1375 + With the help of some relatively important inverse Laplace
1376 + transformations:
1377 + \[
1378 + \begin{array}{c}
1379 + L(\cos at) = \frac{p}{{p^2  + a^2 }} \\
1380 + L(\sin at) = \frac{a}{{p^2  + a^2 }} \\
1381 + L(1) = \frac{1}{p} \\
1382 + \end{array}
1383 + \]
1384 + , we obtain
1385   \begin{align}
1386   m\ddot x &=  - \frac{{\partial W(x)}}{{\partial x}} -
1387   \sum\limits_{\alpha  = 1}^N {\left\{ {\left( { - \frac{{g_\alpha ^2
# Line 483 | Line 1401 | t)\dot x(t - \tau )d} \tau }  + \sum\limits_{\alpha  =
1401   (\omega _\alpha  t)} \right\}}
1402   \end{align}
1403  
1404 + Introducing a \emph{dynamic friction kernel}
1405   \begin{equation}
1406 + \xi (t) = \sum\limits_{\alpha  = 1}^N {\left( { - \frac{{g_\alpha ^2
1407 + }}{{m_\alpha  \omega _\alpha ^2 }}} \right)\cos (\omega _\alpha  t)}
1408 + \label{introEquation:dynamicFrictionKernelDefinition}
1409 + \end{equation}
1410 + and \emph{a random force}
1411 + \begin{equation}
1412 + R(t) = \sum\limits_{\alpha  = 1}^N {\left( {g_\alpha  x_\alpha  (0)
1413 + - \frac{{g_\alpha ^2 }}{{m_\alpha  \omega _\alpha ^2 }}x(0)}
1414 + \right)\cos (\omega _\alpha  t)}  + \frac{{\dot x_\alpha
1415 + (0)}}{{\omega _\alpha  }}\sin (\omega _\alpha  t),
1416 + \label{introEquation:randomForceDefinition}
1417 + \end{equation}
1418 + the equation of motion can be rewritten as
1419 + \begin{equation}
1420   m\ddot x =  - \frac{{\partial W}}{{\partial x}} - \int_0^t {\xi
1421   (t)\dot x(t - \tau )d\tau }  + R(t)
1422   \label{introEuqation:GeneralizedLangevinDynamics}
1423   \end{equation}
1424 < %where $ {\xi (t)}$ is friction kernel, $R(t)$ is random force and
1425 < %$W$ is the potential of mean force. $W(x) =  - kT\ln p(x)$
1424 > which is known as the \emph{generalized Langevin equation}.
1425 >
1426 > \subsubsection{\label{introSection:randomForceDynamicFrictionKernel}Random Force and Dynamic Friction Kernel}
1427 >
1428 > One may notice that $R(t)$ depends only on initial conditions, which
1429 > implies it is completely deterministic within the context of a
1430 > harmonic bath. However, it is easy to verify that $R(t)$ is totally
1431 > uncorrelated to $x$ and $\dot x$,
1432   \[
1433 < \xi (t) = \sum\limits_{\alpha  = 1}^N {\left( { - \frac{{g_\alpha ^2
1434 < }}{{m_\alpha  \omega _\alpha ^2 }}} \right)\cos (\omega _\alpha  t)}
1433 > \begin{array}{l}
1434 > \left\langle {x(t)R(t)} \right\rangle  = 0, \\
1435 > \left\langle {\dot x(t)R(t)} \right\rangle  = 0. \\
1436 > \end{array}
1437   \]
1438 < For an infinite harmonic bath, we can use the spectral density and
1439 < an integral over frequencies.
1438 > This property is what we expect from a truly random process. As long
1439 > as the model, which is gaussian distribution in general, chosen for
1440 > $R(t)$ is a truly random process, the stochastic nature of the GLE
1441 > still remains.
1442  
1443 + %dynamic friction kernel
1444 + The convolution integral
1445   \[
1446 < R(t) = \sum\limits_{\alpha  = 1}^N {\left( {g_\alpha  x_\alpha  (0)
502 < - \frac{{g_\alpha ^2 }}{{m_\alpha  \omega _\alpha ^2 }}x(0)}
503 < \right)\cos (\omega _\alpha  t)}  + \frac{{\dot x_\alpha
504 < (0)}}{{\omega _\alpha  }}\sin (\omega _\alpha  t)
1446 > \int_0^t {\xi (t)\dot x(t - \tau )d\tau }
1447   \]
1448 < The random forces depend only on initial conditions.
1448 > depends on the entire history of the evolution of $x$, which implies
1449 > that the bath retains memory of previous motions. In other words,
1450 > the bath requires a finite time to respond to change in the motion
1451 > of the system. For a sluggish bath which responds slowly to changes
1452 > in the system coordinate, we may regard $\xi(t)$ as a constant
1453 > $\xi(t) = \Xi_0$. Hence, the convolution integral becomes
1454 > \[
1455 > \int_0^t {\xi (t)\dot x(t - \tau )d\tau }  = \xi _0 (x(t) - x(0))
1456 > \]
1457 > and Equation \ref{introEuqation:GeneralizedLangevinDynamics} becomes
1458 > \[
1459 > m\ddot x =  - \frac{\partial }{{\partial x}}\left( {W(x) +
1460 > \frac{1}{2}\xi _0 (x - x_0 )^2 } \right) + R(t),
1461 > \]
1462 > which can be used to describe dynamic caging effect. The other
1463 > extreme is the bath that responds infinitely quickly to motions in
1464 > the system. Thus, $\xi (t)$ can be taken as a $delta$ function in
1465 > time:
1466 > \[
1467 > \xi (t) = 2\xi _0 \delta (t)
1468 > \]
1469 > Hence, the convolution integral becomes
1470 > \[
1471 > \int_0^t {\xi (t)\dot x(t - \tau )d\tau }  = 2\xi _0 \int_0^t
1472 > {\delta (t)\dot x(t - \tau )d\tau }  = \xi _0 \dot x(t),
1473 > \]
1474 > and Equation \ref{introEuqation:GeneralizedLangevinDynamics} becomes
1475 > \begin{equation}
1476 > m\ddot x =  - \frac{{\partial W(x)}}{{\partial x}} - \xi _0 \dot
1477 > x(t) + R(t) \label{introEquation:LangevinEquation}
1478 > \end{equation}
1479 > which is known as the Langevin equation. The static friction
1480 > coefficient $\xi _0$ can either be calculated from spectral density
1481 > or be determined by Stokes' law for regular shaped particles.A
1482 > briefly review on calculating friction tensor for arbitrary shaped
1483 > particles is given in section \ref{introSection:frictionTensor}.
1484  
1485   \subsubsection{\label{introSection:secondFluctuationDissipation}The Second Fluctuation Dissipation Theorem}
1486 < So we can define a new set of coordinates,
1486 >
1487 > Defining a new set of coordinates,
1488   \[
1489   q_\alpha  (t) = x_\alpha  (t) - \frac{1}{{m_\alpha  \omega _\alpha
1490   ^2 }}x(0)
1491 < \]
1492 < This makes
1491 > \],
1492 > we can rewrite $R(T)$ as
1493   \[
1494 < R(t) = \sum\limits_{\alpha  = 1}^N {g_\alpha  q_\alpha  (t)}
1494 > R(t) = \sum\limits_{\alpha  = 1}^N {g_\alpha  q_\alpha  (t)}.
1495   \]
1496   And since the $q$ coordinates are harmonic oscillators,
1497   \[
1498 < \begin{array}{l}
1498 > \begin{array}{c}
1499 > \left\langle {q_\alpha ^2 } \right\rangle  = \frac{{kT}}{{m_\alpha  \omega _\alpha ^2 }} \\
1500   \left\langle {q_\alpha  (t)q_\alpha  (0)} \right\rangle  = \left\langle {q_\alpha ^2 (0)} \right\rangle \cos (\omega _\alpha  t) \\
1501   \left\langle {q_\alpha  (t)q_\beta  (0)} \right\rangle  = \delta _{\alpha \beta } \left\langle {q_\alpha  (t)q_\alpha  (0)} \right\rangle  \\
1502 + \left\langle {R(t)R(0)} \right\rangle  = \sum\limits_\alpha  {\sum\limits_\beta  {g_\alpha  g_\beta  \left\langle {q_\alpha  (t)q_\beta  (0)} \right\rangle } }  \\
1503 +  = \sum\limits_\alpha  {g_\alpha ^2 \left\langle {q_\alpha ^2 (0)} \right\rangle \cos (\omega _\alpha  t)}  \\
1504 +  = kT\xi (t) \\
1505   \end{array}
1506   \]
1507 + Thus, we recover the \emph{second fluctuation dissipation theorem}
1508 + \begin{equation}
1509 + \xi (t) = \left\langle {R(t)R(0)} \right\rangle
1510 + \label{introEquation:secondFluctuationDissipation}.
1511 + \end{equation}
1512 + In effect, it acts as a constraint on the possible ways in which one
1513 + can model the random force and friction kernel.
1514  
1515 < \begin{align}
1516 < \left\langle {R(t)R(0)} \right\rangle  &= \sum\limits_\alpha
1517 < {\sum\limits_\beta  {g_\alpha  g_\beta  \left\langle {q_\alpha
1518 < (t)q_\beta  (0)} \right\rangle } }
1519 < %
1520 < &= \sum\limits_\alpha  {g_\alpha ^2 \left\langle {q_\alpha ^2 (0)}
1521 < \right\rangle \cos (\omega _\alpha  t)}
1522 < %
1523 < &= kT\xi (t)
1524 < \end{align}
1515 > \subsection{\label{introSection:frictionTensor} Friction Tensor}
1516 > Theoretically, the friction kernel can be determined using velocity
1517 > autocorrelation function. However, this approach become impractical
1518 > when the system become more and more complicate. Instead, various
1519 > approaches based on hydrodynamics have been developed to calculate
1520 > the friction coefficients. The friction effect is isotropic in
1521 > Equation, \zeta can be taken as a scalar. In general, friction
1522 > tensor \Xi is a $6\times 6$ matrix given by
1523 > \[
1524 > \Xi  = \left( {\begin{array}{*{20}c}
1525 >   {\Xi _{}^{tt} } & {\Xi _{}^{rt} }  \\
1526 >   {\Xi _{}^{tr} } & {\Xi _{}^{rr} }  \\
1527 > \end{array}} \right).
1528 > \]
1529 > Here, $ {\Xi^{tt} }$ and $ {\Xi^{rr} }$ are translational friction
1530 > tensor and rotational resistance (friction) tensor respectively,
1531 > while ${\Xi^{tr} }$ is translation-rotation coupling tensor and $
1532 > {\Xi^{rt} }$ is rotation-translation coupling tensor. When a
1533 > particle moves in a fluid, it may experience friction force or
1534 > torque along the opposite direction of the velocity or angular
1535 > velocity,
1536 > \[
1537 > \left( \begin{array}{l}
1538 > F_R  \\
1539 > \tau _R  \\
1540 > \end{array} \right) =  - \left( {\begin{array}{*{20}c}
1541 >   {\Xi ^{tt} } & {\Xi ^{rt} }  \\
1542 >   {\Xi ^{tr} } & {\Xi ^{rr} }  \\
1543 > \end{array}} \right)\left( \begin{array}{l}
1544 > v \\
1545 > w \\
1546 > \end{array} \right)
1547 > \]
1548 > where $F_r$ is the friction force and $\tau _R$ is the friction
1549 > toque.
1550  
1551 + \subsubsection{\label{introSection:resistanceTensorRegular}The Resistance Tensor for Regular Shape}
1552 +
1553 + For a spherical particle, the translational and rotational friction
1554 + constant can be calculated from Stoke's law,
1555 + \[
1556 + \Xi ^{tt}  = \left( {\begin{array}{*{20}c}
1557 +   {6\pi \eta R} & 0 & 0  \\
1558 +   0 & {6\pi \eta R} & 0  \\
1559 +   0 & 0 & {6\pi \eta R}  \\
1560 + \end{array}} \right)
1561 + \]
1562 + and
1563 + \[
1564 + \Xi ^{rr}  = \left( {\begin{array}{*{20}c}
1565 +   {8\pi \eta R^3 } & 0 & 0  \\
1566 +   0 & {8\pi \eta R^3 } & 0  \\
1567 +   0 & 0 & {8\pi \eta R^3 }  \\
1568 + \end{array}} \right)
1569 + \]
1570 + where $\eta$ is the viscosity of the solvent and $R$ is the
1571 + hydrodynamics radius.
1572 +
1573 + Other non-spherical shape, such as cylinder and ellipsoid
1574 + \textit{etc}, are widely used as reference for developing new
1575 + hydrodynamics theory, because their properties can be calculated
1576 + exactly. In 1936, Perrin extended Stokes's law to general ellipsoid,
1577 + also called a triaxial ellipsoid, which is given in Cartesian
1578 + coordinates by
1579 + \[
1580 + \frac{{x^2 }}{{a^2 }} + \frac{{y^2 }}{{b^2 }} + \frac{{z^2 }}{{c^2
1581 + }} = 1
1582 + \]
1583 + where the semi-axes are of lengths $a$, $b$, and $c$. Unfortunately,
1584 + due to the complexity of the elliptic integral, only the ellipsoid
1585 + with the restriction of two axes having to be equal, \textit{i.e.}
1586 + prolate($ a \ge b = c$) and oblate ($ a < b = c $), can be solved
1587 + exactly. Introducing an elliptic integral parameter $S$ for prolate,
1588 + \[
1589 + S = \frac{2}{{\sqrt {a^2  - b^2 } }}\ln \frac{{a + \sqrt {a^2  - b^2
1590 + } }}{b},
1591 + \]
1592 + and oblate,
1593 + \[
1594 + S = \frac{2}{{\sqrt {b^2  - a^2 } }}arctg\frac{{\sqrt {b^2  - a^2 }
1595 + }}{a}
1596 + \],
1597 + one can write down the translational and rotational resistance
1598 + tensors
1599 + \[
1600 + \begin{array}{l}
1601 + \Xi _a^{tt}  = 16\pi \eta \frac{{a^2  - b^2 }}{{(2a^2  - b^2 )S - 2a}} \\
1602 + \Xi _b^{tt}  = \Xi _c^{tt}  = 32\pi \eta \frac{{a^2  - b^2 }}{{(2a^2  - 3b^2 )S + 2a}} \\
1603 + \end{array},
1604 + \]
1605 + and
1606 + \[
1607 + \begin{array}{l}
1608 + \Xi _a^{rr}  = \frac{{32\pi }}{3}\eta \frac{{(a^2  - b^2 )b^2 }}{{2a - b^2 S}} \\
1609 + \Xi _b^{rr}  = \Xi _c^{rr}  = \frac{{32\pi }}{3}\eta \frac{{(a^4  - b^4 )}}{{(2a^2  - b^2 )S - 2a}} \\
1610 + \end{array}.
1611 + \]
1612 +
1613 + \subsubsection{\label{introSection:resistanceTensorRegularArbitrary}The Resistance Tensor for Arbitrary Shape}
1614 +
1615 + Unlike spherical and other regular shaped molecules, there is not
1616 + analytical solution for friction tensor of any arbitrary shaped
1617 + rigid molecules. The ellipsoid of revolution model and general
1618 + triaxial ellipsoid model have been used to approximate the
1619 + hydrodynamic properties of rigid bodies. However, since the mapping
1620 + from all possible ellipsoidal space, $r$-space, to all possible
1621 + combination of rotational diffusion coefficients, $D$-space is not
1622 + unique\cite{Wegener79} as well as the intrinsic coupling between
1623 + translational and rotational motion of rigid body\cite{}, general
1624 + ellipsoid is not always suitable for modeling arbitrarily shaped
1625 + rigid molecule. A number of studies have been devoted to determine
1626 + the friction tensor for irregularly shaped rigid bodies using more
1627 + advanced method\cite{} where the molecule of interest was modeled by
1628 + combinations of spheres(beads)\cite{} and the hydrodynamics
1629 + properties of the molecule can be calculated using the hydrodynamic
1630 + interaction tensor. Let us consider a rigid assembly of $N$ beads
1631 + immersed in a continuous medium. Due to hydrodynamics interaction,
1632 + the ``net'' velocity of $i$th bead, $v'_i$ is different than its
1633 + unperturbed velocity $v_i$,
1634 + \[
1635 + v'_i  = v_i  - \sum\limits_{j \ne i} {T_{ij} F_j }
1636 + \]
1637 + where $F_i$ is the frictional force, and $T_{ij}$ is the
1638 + hydrodynamic interaction tensor. The friction force of $i$th bead is
1639 + proportional to its ``net'' velocity
1640   \begin{equation}
1641 < \xi (t) = \left\langle {R(t)R(0)} \right\rangle
1642 < \label{introEquation:secondFluctuationDissipation}
1641 > F_i  = \zeta _i v_i  - \zeta _i \sum\limits_{j \ne i} {T_{ij} F_j }.
1642 > \label{introEquation:tensorExpression}
1643   \end{equation}
1644 + This equation is the basis for deriving the hydrodynamic tensor. In
1645 + 1930, Oseen and Burgers gave a simple solution to Equation
1646 + \ref{introEquation:tensorExpression}
1647 + \begin{equation}
1648 + T_{ij}  = \frac{1}{{8\pi \eta r_{ij} }}\left( {I + \frac{{R_{ij}
1649 + R_{ij}^T }}{{R_{ij}^2 }}} \right).
1650 + \label{introEquation:oseenTensor}
1651 + \end{equation}
1652 + Here $R_{ij}$ is the distance vector between bead $i$ and bead $j$.
1653 + A second order expression for element of different size was
1654 + introduced by Rotne and Prager\cite{} and improved by Garc\'{i}a de
1655 + la Torre and Bloomfield,
1656 + \begin{equation}
1657 + T_{ij}  = \frac{1}{{8\pi \eta R_{ij} }}\left[ {\left( {I +
1658 + \frac{{R_{ij} R_{ij}^T }}{{R_{ij}^2 }}} \right) + R\frac{{\sigma
1659 + _i^2  + \sigma _j^2 }}{{r_{ij}^2 }}\left( {\frac{I}{3} -
1660 + \frac{{R_{ij} R_{ij}^T }}{{R_{ij}^2 }}} \right)} \right].
1661 + \label{introEquation:RPTensorNonOverlapped}
1662 + \end{equation}
1663 + Both of the Equation \ref{introEquation:oseenTensor} and Equation
1664 + \ref{introEquation:RPTensorNonOverlapped} have an assumption $R_{ij}
1665 + \ge \sigma _i  + \sigma _j$. An alternative expression for
1666 + overlapping beads with the same radius, $\sigma$, is given by
1667 + \begin{equation}
1668 + T_{ij}  = \frac{1}{{6\pi \eta R_{ij} }}\left[ {\left( {1 -
1669 + \frac{2}{{32}}\frac{{R_{ij} }}{\sigma }} \right)I +
1670 + \frac{2}{{32}}\frac{{R_{ij} R_{ij}^T }}{{R_{ij} \sigma }}} \right]
1671 + \label{introEquation:RPTensorOverlapped}
1672 + \end{equation}
1673  
1674 < \section{\label{introSection:hydroynamics}Hydrodynamics}
1674 > To calculate the resistance tensor at an arbitrary origin $O$, we
1675 > construct a $3N \times 3N$ matrix consisting of $N \times N$
1676 > $B_{ij}$ blocks
1677 > \begin{equation}
1678 > B = \left( {\begin{array}{*{20}c}
1679 >   {B_{11} } &  \ldots  & {B_{1N} }  \\
1680 >    \vdots  &  \ddots  &  \vdots   \\
1681 >   {B_{N1} } &  \cdots  & {B_{NN} }  \\
1682 > \end{array}} \right),
1683 > \end{equation}
1684 > where $B_{ij}$ is given by
1685 > \[
1686 > B_{ij}  = \delta _{ij} \frac{I}{{6\pi \eta R}} + (1 - \delta _{ij}
1687 > )T_{ij}
1688 > \]
1689 > where $\delta _{ij}$ is Kronecker delta function. Inverting matrix
1690 > $B$, we obtain
1691  
1692 < \subsection{\label{introSection:frictionTensor} Friction Tensor}
1693 < \subsection{\label{introSection:analyticalApproach}Analytical
1694 < Approach}
1692 > \[
1693 > C = B^{ - 1}  = \left( {\begin{array}{*{20}c}
1694 >   {C_{11} } &  \ldots  & {C_{1N} }  \\
1695 >    \vdots  &  \ddots  &  \vdots   \\
1696 >   {C_{N1} } &  \cdots  & {C_{NN} }  \\
1697 > \end{array}} \right)
1698 > \]
1699 > , which can be partitioned into $N \times N$ $3 \times 3$ block
1700 > $C_{ij}$. With the help of $C_{ij}$ and skew matrix $U_i$
1701 > \[
1702 > U_i  = \left( {\begin{array}{*{20}c}
1703 >   0 & { - z_i } & {y_i }  \\
1704 >   {z_i } & 0 & { - x_i }  \\
1705 >   { - y_i } & {x_i } & 0  \\
1706 > \end{array}} \right)
1707 > \]
1708 > where $x_i$, $y_i$, $z_i$ are the components of the vector joining
1709 > bead $i$ and origin $O$. Hence, the elements of resistance tensor at
1710 > arbitrary origin $O$ can be written as
1711 > \begin{equation}
1712 > \begin{array}{l}
1713 > \Xi _{}^{tt}  = \sum\limits_i {\sum\limits_j {C_{ij} } } , \\
1714 > \Xi _{}^{tr}  = \Xi _{}^{rt}  = \sum\limits_i {\sum\limits_j {U_i C_{ij} } } , \\
1715 > \Xi _{}^{rr}  =  - \sum\limits_i {\sum\limits_j {U_i C_{ij} } } U_j  \\
1716 > \end{array}
1717 > \label{introEquation:ResistanceTensorArbitraryOrigin}
1718 > \end{equation}
1719  
1720 < \subsection{\label{introSection:approximationApproach}Approximation
1721 < Approach}
1720 > The resistance tensor depends on the origin to which they refer. The
1721 > proper location for applying friction force is the center of
1722 > resistance (reaction), at which the trace of rotational resistance
1723 > tensor, $ \Xi ^{rr}$ reaches minimum. Mathematically, the center of
1724 > resistance is defined as an unique point of the rigid body at which
1725 > the translation-rotation coupling tensor are symmetric,
1726 > \begin{equation}
1727 > \Xi^{tr}  = \left( {\Xi^{tr} } \right)^T
1728 > \label{introEquation:definitionCR}
1729 > \end{equation}
1730 > Form Equation \ref{introEquation:ResistanceTensorArbitraryOrigin},
1731 > we can easily find out that the translational resistance tensor is
1732 > origin independent, while the rotational resistance tensor and
1733 > translation-rotation coupling resistance tensor depend on the
1734 > origin. Given resistance tensor at an arbitrary origin $O$, and a
1735 > vector ,$r_{OP}(x_{OP}, y_{OP}, z_{OP})$, from $O$ to $P$, we can
1736 > obtain the resistance tensor at $P$ by
1737 > \begin{equation}
1738 > \begin{array}{l}
1739 > \Xi _P^{tt}  = \Xi _O^{tt}  \\
1740 > \Xi _P^{tr}  = \Xi _P^{rt}  = \Xi _O^{tr}  - U_{OP} \Xi _O^{tt}  \\
1741 > \Xi _P^{rr}  = \Xi _O^{rr}  - U_{OP} \Xi _O^{tt} U_{OP}  + \Xi _O^{tr} U_{OP}  - U_{OP} \Xi _O^{tr} ^{^T }  \\
1742 > \end{array}
1743 > \label{introEquation:resistanceTensorTransformation}
1744 > \end{equation}
1745 > where
1746 > \[
1747 > U_{OP}  = \left( {\begin{array}{*{20}c}
1748 >   0 & { - z_{OP} } & {y_{OP} }  \\
1749 >   {z_i } & 0 & { - x_{OP} }  \\
1750 >   { - y_{OP} } & {x_{OP} } & 0  \\
1751 > \end{array}} \right)
1752 > \]
1753 > Using Equations \ref{introEquation:definitionCR} and
1754 > \ref{introEquation:resistanceTensorTransformation}, one can locate
1755 > the position of center of resistance,
1756 > \[
1757 > \left( \begin{array}{l}
1758 > x_{OR}  \\
1759 > y_{OR}  \\
1760 > z_{OR}  \\
1761 > \end{array} \right) = \left( {\begin{array}{*{20}c}
1762 >   {(\Xi _O^{rr} )_{yy}  + (\Xi _O^{rr} )_{zz} } & { - (\Xi _O^{rr} )_{xy} } & { - (\Xi _O^{rr} )_{xz} }  \\
1763 >   { - (\Xi _O^{rr} )_{xy} } & {(\Xi _O^{rr} )_{zz}  + (\Xi _O^{rr} )_{xx} } & { - (\Xi _O^{rr} )_{yz} }  \\
1764 >   { - (\Xi _O^{rr} )_{xz} } & { - (\Xi _O^{rr} )_{yz} } & {(\Xi _O^{rr} )_{xx}  + (\Xi _O^{rr} )_{yy} }  \\
1765 > \end{array}} \right)^{ - 1} \left( \begin{array}{l}
1766 > (\Xi _O^{tr} )_{yz}  - (\Xi _O^{tr} )_{zy}  \\
1767 > (\Xi _O^{tr} )_{zx}  - (\Xi _O^{tr} )_{xz}  \\
1768 > (\Xi _O^{tr} )_{xy}  - (\Xi _O^{tr} )_{yx}  \\
1769 > \end{array} \right).
1770 > \]
1771 > where $x_OR$, $y_OR$, $z_OR$ are the components of the vector
1772 > joining center of resistance $R$ and origin $O$.
1773  
1774 < \subsection{\label{introSection:centersRigidBody}Centers of Rigid
552 < Body}
1774 > %\section{\label{introSection:correlationFunctions}Correlation Functions}

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