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Copy file name to clipboardExpand all lines: paper/basic_training.tex
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@@ -202,14 +202,14 @@ \subsection{Thermodynamics}
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\subsubsection{Key concepts}
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A variety of thermodynamic concepts are particularly important for molecular simulations:
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\begin{itemize}
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\item Temperature, pressure, stress
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\item Internal energy, enthalpy
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\item Temperature and pressure% removed stress; seems out of place
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\item Internal energy and enthalpy
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\item Gibbs and Helmholtz free energy
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\item Entropy
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\end{itemize}
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One of the main objectives of molecular simulations is to estimate/predict thermodynamic behavior of real systems as observed in the laboratory.
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Typically this means we are interested in macroscopic systems, consisting of $10^{23}$ particles or more (i.e. at least several moles of particles).
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Typically this means we are interested in macroscopic systems, consisting of $10^{23}$ particles or more (i.e. at least a mole of particles).
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But properties of interest include not only macroscopic, bulk thermodynamic properties, such as density or heat capacity,
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but also microscopic properties like specific free energy differences associated with, say, changes in the conformation of a molecule.
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For this reason, it is important to understand key concepts in thermodynamics, such as temperature, pressure, entropy, internal energy, various forms of free energy, and the relationships between them.
\caption{Energy landscapes. (a) A highly simplified landscape used to illustrate rate concepts and (b) a schematic of a complex landscape with numerous minima and ambiguous state boundaries.}
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\caption{Energy landscapes. (a) A highly simplified landscape used to illustrate rate concepts and (b) a schematic of a more complex landscape with numerous minima and ambiguous state boundaries.}
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\label{landscapes}
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\end{figure}
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The key dynamical concept to understand is embodied in the twin characteristics of timescales and rates.
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The two are literally reciprocals of one another.
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In Fig.\ \ref{landscapes}(a), assume you have started an MD simulation in basin A.
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The trajectory is likely to remain in that basin for a period of time -- the ``dwell'' timescale -- which increases exponentially with the barrier height according to the (reciprocal) Arrhenius factor as $\exp[(U^\ddagger - U_A)/k_B T]$; barriers many times the thermal energy $k_BT$ imply long dwells.
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The rate $k_{AB}$, which is the transition probability per unit time, exhibits reciprocal behavior -- i.e., $k_{AB} \sim\exp[-(U^\ddagger - U_A)/k_B T]$ according to the traditional Arrhenius factor.
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Note that all transitions occur in a random, \emph{stochastic} fashion and are not predictable except in terms of average behavior.
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More detailed discussions of rate constants can be found in numerous textbooks (e.g.,~\cite{DillBook, Zuckerman:2010:}).
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The trajectory is likely to remain in that basin for a period of time -- the ``dwell'' timescale -- which increases exponentially with the barrier height, $(U^\ddagger - U_A)$.
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Barriers many times the thermal energy $k_BT$ imply long dwell timescales, approximated as the reciprocal of $\exp[(U^\ddagger - U_A)/(k_B T)]$.
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The rate coefficient $k_{AB}$, which relates to the transition probability per unit time per amount of reactant(s).
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All transitions occur in a random, \emph{stochastic} fashion and are predictable only in terms of average behavior.
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More detailed discussions of rates and rate coefficients can be found in numerous textbooks (e.g.,~\cite{DillBook, Zuckerman:2010:}).
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Once you have understood that MD behavior reflects system timescales, you must set this behavior in the context of an \emph{extremely} complex energy landscape consisting of almost innumerable minima and barriers, as schematized in Fig.\ \ref{landscapes}(b).
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Each small basin represents something like a different rotameric state of a protein side chain or perhaps a tiny part of the Ramachandran spaces (backbone phi-psi angles) for one or a few residues.
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There is a closely related connection for on- and off-rates with the binding equilibrium constant.
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For a \emph{continuous} coordinate (e.g., the distance between two residues in a protein), the probability-determining free energy is called the ``potential of mean force'' (PMF); the Boltzmann factor of a PMF gives the relative probability of a given coordinate.
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Any kind of free energy implicitly includes \emph{entropic} effects; in terms of an energy landscape (Fig.\ \ref{landscapes}), the entropy quantifies the \emph{width} of a basin.
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These points are discussed in textbooks, as are the differences between free energies for different thermodynamic ensembles -- e.g.., $F$, the Helmholtz free energy, when $T$ is constant, and $G$, the Gibbs free energy, when both $T$ and pressure are constant -- which are not essential to our introduction~\cite{DillBook, Zuckerman:2010:}.
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These points are discussed in textbooks, as are the differences between free energies for different thermodynamic ensembles -- e.g.., $F$, the Helmholtz free energy, when $T$ is constant, and $G$, the Gibbs free energy, when both $T$ and pressure are constant -- which are not essential to our introduction~\cite{DillBook, Zuckerman:2010:}.
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A final essential topic is the difference between equilibrium and non-equilibrium systems.
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We noted above that an MD trajectory is not likely to represent the equilibrium ensemble because the trajectory is probably too short.
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Books which we recommend as particularly helpful in this area include:
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\begin{itemize}
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\item Reif's ``Fundamentals of Statistical and Thermal Physics''~\cite{Reif:2009:}
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