Homogeneous SPC/E water nucleation in large molecular dynamics simulations
arXiv:1507.07335 · doi:10.1063/1.4928055
Abstract
We perform direct large molecular dynamics simulations of homogeneous SPC/E water nucleation, using up to molecules. Our large system sizes allow us to measure extremely low and accurate nucleation rates, down to , helping close the gap between experimentally measured rates . We are also able to precisely measure size distributions, sticking efficiencies, cluster temperatures, and cluster internal densities. We introduce a new functional form to implement the Yasuoka-Matsumoto nucleation rate measurement technique (threshold method). Comparison to nucleation models shows that classical nucleation theory over-estimates nucleation rates by a few orders of magnitude. The semi-phenomenological nucleation model does better, under-predicting rates by at worst, a factor of 24. Unlike what has been observed in Lennard-Jones simulations, post-critical clusters have temperatures consistent with the run average temperature. Also, we observe that post-critical clusters have densities very slightly higher, , than bulk liquid. We re-calibrate a Hale-type vs. scaling relation using both experimental and simulation data, finding remarkable consistency in over orders of magnitude in the nucleation rate range, and K in the temperature range.
Accepted for publication in the Journal of Chemical Physics
References in corpus (6)
- Modification of the classical nucleation theory based on molecular simulation data for surface tension, critical nucleus size, and nucleation rate
- Molecular Dynamics Simulations of the Nucleation of Water: Determining the Sticking Probability and Formation Energy of a Cluster
- Properties of Liquid Clusters in Large-scale Molecular Dynamics Nucleation Simulations
- Free energy of cluster formation and a new scaling relation for the nucleation rate
- Steady-State Homogeneous Nucleation and Growth of Water Droplets: Extended Numerical Treatment
- A Method for Analyzing the Non-Stationary Nucleation and Overall Transition Kinetics. A Case of Water