We derive a phase diagram for amorphous solids and liquid supercooled water and explain why the amorphous solids of water exist in several different forms. Application of large-deviation theory allows us to prepare such phases in computer simulations. Along with nonequilibrium transitions between the ergodic liquid and two distinct amorphous solids, we establish coexistence between these two amorphous solids. The phase diagram we predict includes a nonequilibrium triple point where two amorphous phases and the liquid coexist. Whereas the amorphous solids are long-lived and slowly aging glasses, their melting can lead quickly to the formation of crystalline ice. Further, melting of the higher density amorphous solid at low pressures takes place in steps, transitioning to the lower-density glass before accessing a nonequilibrium liquid from which ice coarsens.glass transition | putative liquid-liquid transition A morphous ices are nonequilibrium, low-temperature phases of water (1-3). These phases lack long-range order and their properties are fundamentally dependent on the protocols by which they are prepared (4, 5). They are molecular glasses that exhibit a variety of reproducible behaviors, including transitions between different amorphous states. This paper provides quantitative analysis and numerical simulation of this polyamorphism and predicts a nonequilibrium phase diagram, offering explanations of previous experimental observations (1, 3, 6-9) and possibly guiding future experiments on supercooled water.Our treatment can be applied generally in many cases where there is interest in comparing phase behaviors of nonequilibrium glasses with those of equilibrium liquids and crystals. For water in particular, however, our results bear on whether observed nonequilibrium polyamorphism can be interpreted as evidence of more than one distinct liquid phase of water. It is a topic of current interest and controversy. There are no direct measurements of twoliquid behavior in water, but the low-temperature critical point that would accompany such behavior has been offered as an explanation for unusual properties of liquid water, such as maxima in various response functions (4, 10), and molecular simulation results are often cited as supporting this theoretical idea, e.g., refs. 11-14. However, water anomalies can be explained with models for which there is demonstrably only one liquid phase (15), and seemingly rigorous equilibrium analysis of various simulation models argues against cold water exhibiting the existence of two distinct liquids (16,17). Rather, it seems that an illusion of two-liquid behavior in simulation coincides with coarsening of ice, and this paper shows how arresting those fluctuations yields a multitude of nonequilibrium amorphous solids.
PhenomenologyA phase diagram is drawn in Fig. 1A. It is partitioned with the onset temperature, T o (p), which is the crossover temperature below which liquid-phase dynamics is spatially heterogeneous. This temperature is an equilibrium material property. The pr...