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17/04/2007 Long Timescale Workshop. Outline. Why study crystal nucleation? The timescale problemSimulation methodsBrute force molecular dynamicsUmbrella sampling Monte-Carlo methodsLong timescale methods and metadynamics Application of metadynamics to nucleationLennard-Jones crystallisatio
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1. 17/04/2007
Long Timescale Workshop Metadynamics for Simulating Crystal Nucleation David Quigley
University of Warwick
2. 17/04/2007
Long Timescale Workshop Outline Why study crystal nucleation?
The timescale problem
Simulation methods
Brute force molecular dynamics
Umbrella sampling Monte-Carlo methods
Long timescale methods and metadynamics
Application of metadynamics to nucleation
Lennard-Jones crystallisation revisited
Ice nucleation
Calcium Carbonate
Future Work
3. 17/04/2007
Long Timescale Workshop Why study crystal nucleation? Fundamental Interest
Nucleation mechanisms
Metastability
Industrial
Gas hydrate formation
Limescale
Biomineralisation
Templating
Self Assembly
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Long Timescale Workshop Freezing Questions
Is the structure nucleated consistent with the Ostwald step rule?
Aggregation of crystallites?
What are the free-energy barriers to nucleation of each crystal phase?
How does this vary with temperature/pressure?
System size effects?
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Long Timescale Workshop Nucleation Barrier Assumptions
Nucleus is spherical
Nucleus adopts crystal structure of the bulk solid
Sharp interface between solid and liquid
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Long Timescale Workshop Simulation of freezing Experimental nucleation rates vary from O(101) – O(106) nuclei per cm3 per second.
Consider a simulation cell of 10,000 water molecules.
At best expect 1 nucleation event every 1012 seconds if at freezing temperature.
Can simulate 500 ns at best using molecular simulation.
Approach 1: Heavily supercool to reduce timescale.
Magnitude of ?? increases rapidly below melting temperature.
Lower energy barrier and smaller critical nucleus.
Approach 2: Insertion of a nucleation ‘seed’
Estimate critical nucleus size from bulk free-energy calculations and/or experiment.
Must assume structure of the critical nucleus.
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Long Timescale Workshop Examples
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Long Timescale Workshop Umbrella Sampling Methods Monte-Carlo method first applied to soft spheres by van Duijneveldt and Frenkel.
[J.Chem.Phys 99 4655 – 4668 (1992)]
Crystallisation characterised by one or more reaction co-ordinates or order parameters.
Free-energy profile along the reaction pathway can be reconstructed from the umbrella sampling.
Applied to Lennard-Jones fluid, hard-sphere colloids, water, N2 ,CO2, NaCl and various metals.
9. 17/04/2007
Long Timescale Workshop Metadynamics[Laio & Parrinello P.N.A.S. 99 12562 (2002)] Characterise system by collective variables (order parameters) l = (l1,l2l3….lM) which describe the state of the system.
Derivative of the free-energy w.r.t. l is ;evaluated via MD or MC.
“Thermodynamic force” acting on the order parameters is :
Augment Ftherm with history dependent potential Vaug(l1,l2l3….lM).
Pushes the system away from previously visited l.
Grow a bias potential to overcome energy barriers.
Pushed into rare configurations to overcome entropic barriers.
-Vaug provides a running estimate of the free-energy surface.
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Long Timescale Workshop Lennard-Jones Freezing Simple well studied pair-potential model, often used to benchmark methods.
Phase diagram and free-energy are well known and parameterised.
Stable phase is HCP/FCC, BCC phase closest in free-energy to liquid.
Test of the Ostwald step rule.
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Long Timescale Workshop Order parameter Q6 Steinhardt order parameter[ Steinhardt et al. Phys.Rev.B. 28 784 – 805 (1983) ]
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Long Timescale Workshop Where to look? Aiming to simulate 10% or weaker supercooling.
Understand trends in nucleation across the supercooled region.
Influence of density of structure of crystallites?
Systematic study of system size effects?
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Long Timescale Workshop Cluster Formation
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Long Timescale Workshop Nucleation and Growth
15. 17/04/2007
Long Timescale Workshop Cluster Analysis Define a local vector
whereruns over only the separations between particle i and its nearest neighbours.
Two particles i and j are connected if i.e. if ‘bonds’ align.
A particle with 8 or more connections is part of a cluster.
Clusters can then be identified and subjected to local optimisation.
Crystal structure can then be assigned to each particle based on local order parameters.
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Long Timescale Workshop Aggregation?
17. 17/04/2007
Long Timescale Workshop Cluster Sizes
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Long Timescale Workshop BCC or FCC?
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Long Timescale Workshop Internal structure of nucleus
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Long Timescale Workshop Energy Barriers Refine metadynamics estimate of ? G with umbrella sampling.
Use metadynamics configurations to initialise umbrella sampling in each window.
Expected system size dependence on barrier height.
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Long Timescale Workshop Localising Cluster Growth Biasing Q6 does not prefer growth of one large vs many small clusters – potentially unphysical.
Bias w.r.t. size of largest cluster?
Shown to reduce size of critical nucleus in LJ system.
Identify largest cluster in general system?
[ten Wolde et al Faraday Discuss. 104, 93-110]
Restrict bias to a spatial region?
Used successfully in studiesof N2 and CO2.[Leyssale et al, J.Chem.Phys 122, 104510 (2005)]
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Long Timescale Workshop TIP4P Water Simple rigid-body model of water.
Lennard-Jones site on oxygen
+ three charge sites.
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Long Timescale Workshop Ice Freezing
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Long Timescale Workshop Order Parameters Work of Radhakrishnan and Trout suggests that Q6 combined with a tetrahedral order parameter ? can describe the nucleation of ice I.
j and k run over the four nearest neighbours of i.
? = 0.95 for Ice1h at 200 K
? = 0.63 for water at 300 K
No calculations have yet located an Ice 1 minima, but reach order-parameter values of ices 2 and 3.
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Long Timescale Workshop Relevent Ice Phases
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Long Timescale Workshop Water Progress
Extending cluster analysis to recognise ice 2 and 3.
Parallel tempering options to accelerate sampling.
Localising cluster growth as with Lennard-Jones systems.
Further calculations in progress.
27. 17/04/2007
Long Timescale Workshop Calcium Carbonate Aiming to simulate nucleation of calcite from solution in organic environment.
Using potentials developed within the consortium.
Currently testing metadynamics implementation on nucleation of CaCO3 nanoparticles and bulk.
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Long Timescale Workshop Metastable phases
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Long Timescale Workshop Order Parameters A combination of Q4 order parameters for Ca-Ca and Ca-O bonds describes the orientational order.
Calcite crystallisation simulations are in progress.
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Long Timescale Workshop Future Work Extend metadynamics implementation within DLPOLY code.
Lennard-Jones systems
Nucleation rates.
Bigger systems!
Water
Tuning history dependent potential.
Nucleation of other ice phases.
Gas hydrate nucleation.
Nucleation at surfaces.
Calcium carbonate
Phase boundary calculation.
Nucleation from solution.
Presence of egg-shell proteins?
31. 17/04/2007
Long Timescale Workshop Thanks University of Warwick
Mark Rodger
Mike Allen
University of Sheffield
John Harding
Colin Freeman