The melting temperature of the six site potential of water is calculated using two different methods. The first one combines free energy calculations with Hamiltonian Gibbs-Duhem integration. The second method is based on the evolution (melting or freezing) of an explicit liquid-ice interface. Both methods yield very similar results, so we propose 289K as the melting temperature of the model.
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Abascal et al. (2006) studied this question.
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