Abstract
A scaled particle-quansilattice model for liquid water, which is based on the ice VII and ice fc structures, is shown to be capable of explaining several anomalous properties of water. The non-Arrhenius temperature dependence of coefficients of self-diffusion and viscosity and nuclear relaxation times are quantitatively interpreted. Negative volumes of activation, which are observed for viscosity and nuclear relaxation, are also computed to be in good agreement with experiment.
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