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Local order parameters for use in driving homogeneous ice nucleation with all-atom models of water
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10.1063/1.4766362
/content/aip/journal/jcp/137/19/10.1063/1.4766362
http://aip.metastore.ingenta.com/content/aip/journal/jcp/137/19/10.1063/1.4766362
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Figures

Image of FIG. 1.
FIG. 1.

A typical probability density distribution for all pairs of , where the centres of mass of molecules i and j are within 3.5 Å of each other. The three states depicted were equilibrated at 200 K (using the TIP4P/2005 water model) and the ice structures are not, therefore, “perfect”. This figure is analogous to those in Refs. 25,36,52.

Image of FIG. 2.
FIG. 2.

An example of non-ice-like chain growth in TIP4P/2005 umbrella sampling simulations when using the order parameter without chain removal as described in the text. The system has 1000 molecules at 240 K, starting from a 24-molecule cluster. Molecules classified as being part of the largest crystalline cluster are shown in red and violet; there are 45 molecules in this cluster. Molecules whose centres of mass are within 3.5 Å are connected with lines. Molecules shown in violet would be removed from the largest crystalline cluster on application of the chain removal algorithm described in the text.

Image of FIG. 3.
FIG. 3.

Neighbour-averaged order parameters for systems of ices Ih and Ic and liquid water. All systems were equilibrated at 200 K using the TIP4P/2005 water model, and they contain different numbers of molecules. The neighbour cutoff distance was 3.5 Å.

Image of FIG. 4.
FIG. 4.

Representative nucleation snapshots from umbrella sampling simulations of TIP4P/2005 water. In each case, two pictures depict the same cluster from different perspectives; one within the liquid framework (in cyan) and one showing solely the largest crystalline cluster. In the former, spheres represent centres of mass of molecules classified as ice: red spheres correspond to cubic ice, orange spheres correspond to hexagonal ice and pink spheres correspond to ice molecules not within the largest crystalline cluster. Pictures representing solely the largest cluster depict both the oxygen (red) and the hydrogens (white) of each molecule. In (a), an 82-molecule ice cluster grown from the supercooled liquid at 240 K is shown; in (b), a 73-molecule ice cluster grown from a small cluster of Ih ice at 240 K is shown; and in (c), a series of ice clusters of increasing size (comprising 23, 60, 77, 107, and 145 molecules from left to right) grown from a small cluster of Ic ice at 200 K is depicted. There are 1900 molecules in the system in (a) and the first three configurations of (c), and 2500 molecules in (b) and the last two configurations of (c). Simulations of nucleation from a hexagonal seed (shown in (b)) were undertaken using the hybrid Monte Carlo approach, and the rest by a standard Metropolis Monte Carlo approach. p = 1 bar.

Image of FIG. 5.
FIG. 5.

The global order parameters Q 6 and ζ calculated as a function of the size of the largest crystalline cluster, the order parameter used to drive nucleation in this work, for the system seeded with a cubic ice nucleus. Error bars show the standard deviation for the population of configurations at each cluster size. The results depicted here refer to the nearest 576 particles from the centre of mass of the ice nucleus. T = 200 K, p = 1 bar.

Image of FIG. 6.
FIG. 6.

MD simulations of melting. The starting point is a crystalline cluster comprising approximately 220 molecules embedded in supercooled liquid water. The curves exhibiting melting were simulated at 240 K, whilst the remaining ones were simulated at 200 K. These simulations entailed 2500 TIP4P/2005 water molecules. Note that the melting point of TIP4P/2005 ice is 252 K.61 p = 1 bar.

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/content/aip/journal/jcp/137/19/10.1063/1.4766362
2012-11-21
2014-04-20
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752b84549af89a08dbdd7fdb8b9568b5 journal.articlezxybnytfddd
Scitation: Local order parameters for use in driving homogeneous ice nucleation with all-atom models of water
http://aip.metastore.ingenta.com/content/aip/journal/jcp/137/19/10.1063/1.4766362
10.1063/1.4766362
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