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	<id>https://biomolmd.org/mw/index.php?action=history&amp;feed=atom&amp;title=AMMM%3AMetadynamics</id>
	<title>AMMM:Metadynamics - Revision history</title>
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	<updated>2026-04-04T08:54:47Z</updated>
	<subtitle>Revision history for this page on the wiki</subtitle>
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	<entry>
		<id>https://biomolmd.org/mw/index.php?title=AMMM:Metadynamics&amp;diff=1892&amp;oldid=prev</id>
		<title>Cda923: Recreation of correctly named page</title>
		<link rel="alternate" type="text/html" href="https://biomolmd.org/mw/index.php?title=AMMM:Metadynamics&amp;diff=1892&amp;oldid=prev"/>
		<updated>2022-08-31T17:27:24Z</updated>

		<summary type="html">&lt;p&gt;Recreation of correctly named page&lt;/p&gt;
&lt;p&gt;&lt;b&gt;New page&lt;/b&gt;&lt;/p&gt;&lt;div&gt;&lt;br /&gt;
==What is Metadynamics?==&lt;br /&gt;
•A simulation method normally applied as part of molecular dynamics&lt;br /&gt;
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•Used to estimate free energy and state functions of systems where ergodicity (given enough time simulation will explore all possible configurations/areas of phase space) is hindered by energy landscape&lt;br /&gt;
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•Similar to: Adaptively biased MD, Adaptive reaction coordinate forces, Local elevation umbrella sampling&lt;br /&gt;
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•Suggested and developed by Alessandro Laio and Michele Parrinello&lt;br /&gt;
==How does Metadynamics work?==&lt;br /&gt;
•Filling free energy wells with computational sand&lt;br /&gt;
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•Tracking grains of sand placed along collective variables&lt;br /&gt;
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•Eventually the wells are completely full and you add sand to sand (known as convergence)&lt;br /&gt;
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•The landscape is opposite of sum of all sand&lt;br /&gt;
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Movie: https://www.youtube.com/watch?v=IzEBpQ0c8TA&lt;br /&gt;
==How Metadynamics Really Work!==&lt;br /&gt;
•Collective variables (s): set of variables which accurately describe the system&lt;br /&gt;
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•CV Examples: Dihedral angle for cis to trans butane, Distance for cation and anion&lt;br /&gt;
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•Limitations: 3CV or 8CV with multiple replicas coupled together&lt;br /&gt;
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•Exponential cost increase with each CV&lt;br /&gt;
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•Grains of sand are bias potentials&lt;br /&gt;
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•Hamiltonian is augmented with bias potential Vbias shown in Equation 1[[File:Hamiltonian With Bias Potential.png|thumb|Equation 1|link=https://biomolmd.org/mw/index.php/File:Hamiltonian_With_Bias_Potential.png]]&lt;br /&gt;
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•Bias potential Vbias is continuously updated by adding bias (more grains of sand) visualized in Figure 1[[File:Energy Landscape Filled With Gaussians.png|thumb|Figure 1|link=https://biomolmd.org/mw/index.php/File:Energy_Landscape_Filled_With_Gaussians.png]]&lt;br /&gt;
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[[File:Bias Potential Equation and Integral.png|thumb|Equation 2|link=https://biomolmd.org/mw/index.php/File:Bias_Potential_Equation_and_Integral.png]]&lt;br /&gt;
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Defined Variables for Equation 2:&lt;br /&gt;
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•Vbias: bias potential&lt;br /&gt;
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•tsim: simulation time&lt;br /&gt;
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•s: collective variable&lt;br /&gt;
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•st: instantaneous collective variable at time t&lt;br /&gt;
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•ω: bias deposition rate&lt;br /&gt;
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•F: free energy&lt;br /&gt;
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•C: constant (irrelevant)&lt;br /&gt;
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•Evaluating the integral of bias potential over the time duration of the simulation returns free energy F with a negative sign given enough time&lt;br /&gt;
==How to make Metadynamics efficient and computationally viable?==&lt;br /&gt;
[[File:Efficient Bias Potential Equation.png|thumb|Equation 3|link=https://biomolmd.org/mw/index.php/File:Efficient_Bias_Potential_Equation.png]]•Time is discretized into T time intervals&lt;br /&gt;
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•The Dirac delta function is replaced with a Gaussian function&lt;br /&gt;
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•Time intervals (T), bias deposition rate (ω), and width of Gaussian functions (σ) are constants determined as inputs&lt;br /&gt;
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•Vbias equation for efficient implementation shown in Equation 3&lt;br /&gt;
==Two types of Metadynamics==&lt;br /&gt;
•Everything so far has been “original” or “plain” metadynamics&lt;br /&gt;
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•Well-tempered metadynamics scales Gaussian height down as wells are filled[[File:Gaussian Height Scaling Equation.png|thumb|Equation 4|link=https://biomolmd.org/mw/index.php/File:Gaussian_Height_Scaling_Equation.png]]Defined Variables for Equation 4 and 5:&lt;br /&gt;
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•w: Gaussian height&lt;br /&gt;
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•ω: bias deposition rate&lt;br /&gt;
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•Vb: estimate of free energy at current CV position and time step&lt;br /&gt;
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•ΔT: tunable parameter controls how quickly Gaussian height reduces as wells are filled[[File:Free Energy Equation Using Well-Tempered Metadynamics.png|thumb|Equation 5|link=https://biomolmd.org/mw/index.php/File:Free_Energy_Equation_Using_Well-Tempered_Metadynamics.png]]•F: free energy&lt;br /&gt;
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•Final value of biasing potential is a scaled approximation of free energy as shown in Equation 5&lt;br /&gt;
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• Well-tempered metadynamics allows for rapid exploration of phase space as the wells are filled quickly (at Vbias=0 the amount of bias deposited is relatively large, at Vbias=infinity the amount of bias deposited is infinitely small)&lt;br /&gt;
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•As wells fill progressively smaller perturbations to bias potential lead to &amp;quot;smooth convergence&amp;quot; (less excess bias potential or sand deposited on &amp;#039;top&amp;#039;)&lt;br /&gt;
&lt;br /&gt;
•Suggested and developed by Alessandro Barducci, Giovanni Bussi, and Michele Parrinello&lt;br /&gt;
&lt;br /&gt;
Movie Comparing MD, MTD, and WTMTD: https://www.youtube.com/watch?v=IzEBpQ0c8TA&lt;br /&gt;
==Applications of Metadynamics==&lt;br /&gt;
•Able to sample free energy curve even when ergodicity is limited by energy landscape&lt;br /&gt;
&lt;br /&gt;
•Keys to successful metadynamics simulation are choice and definition of CVs&lt;br /&gt;
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•Applicable systems: Protein folding, Molecular docking, Phase transitions, Chemical reactions, Simple to complex systems as long as CVs are sufficient to describe system&lt;br /&gt;
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•Widely integrated as PLUMED and Collective Variable Module:&lt;br /&gt;
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•PLUMED: AMBER, GROMACS, LAMMPS, NAMD, Q ESPRESSO, CP2K, OpenMM&lt;br /&gt;
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•Collective Variable Module: LAMMPS, NAMD, GROMACS, ORAC, CP2K, Desmond&lt;/div&gt;</summary>
		<author><name>Cda923</name></author>
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