Structural Order in Glassy Water

TL;DR

This study uses molecular dynamics simulations to analyze the structural order of glassy water, revealing how different preparation methods influence the order parameters and structural differences among various amorphous ice forms.

Contribution

It introduces a detailed analysis of structural order in glassy water using order parameters and maps, comparing cooling and compression methods and their impact on structure.

Findings

Order parameters increase upon cooling into the glassy state.

Glasses fall on a line in the order map at T=0 K, depending only on density.

Structural differences between glasses from cooling and compression are weakly reflected in pair correlation functions.

Abstract

We investigate structural order in glassy water by performing classical molecular dynamics simulations using the extended simple point charge (SPC/E) model of water. We perform isochoric cooling simulations across the glass transition temperature at different cooling rates and densities. We quantify structural order by orientational and translational order metrics. Upon cooling the liquid into the glassy state, both the orientational order parameter $Q$ and translational order parameter $\tau$ increase. At T=0 K, the glasses fall on a line in the $Q$-$\tau$ plane or {\it order map}. The position of this line depends only on density and coincides with the location in the order map of the inherent structures (IS) sampled upon cooling. We evaluate the energy of the IS, $e_{IS}(T)$, and find that both order parameters for the IS are proportional to $e_{IS}$. We also study the structural order during the transformation of low-density amorphous ice (LDA) to high-density amorphous ice (HDA) upon isothermal compression and are able to identify distinct regions in the order map corresponding to these glasses. Comparison of the order parameters for LDA and HDA with those obtained upon isochoric cooling indicates major structural differences between glasses obtained by cooling and glasses obtained by compression. These structural differences are only weakly reflected in the pair correlation function. We also characterize the evolution of structural order upon isobaric annealing, leading at high pressure to very-high density amorphous ice (VHDA).