Abstract
Significance Glassy water is abundant, occurring in such varied circumstances as thin films condensed on interstellar dust particles and as hosts to hyperquenched protein crystals. Yet quantitative understanding of this class of materials is limited, hampered by lack of formalism needed to systematically treat long time scales and far-from-equilibrium behaviors. Here, we describe a theory to overcome some of this difficulty and apply the theory with simulation to establish the existence of distinct amorphous ices and coexistence between them. This advance allows systematic treatment of dynamics interconverting and melting these nonequilibrium solids, and thereby provides principled explanations of experiments that have probed these processes.
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Dates
Type | When |
---|---|
Created | 11 years, 3 months ago (May 23, 2014, 10:40 p.m.) |
Deposited | 3 years, 4 months ago (April 12, 2022, 11:31 p.m.) |
Indexed | 2 weeks, 6 days ago (Aug. 6, 2025, 9:16 a.m.) |
Issued | 11 years, 3 months ago (May 23, 2014) |
Published | 11 years, 3 months ago (May 23, 2014) |
Published Online | 11 years, 3 months ago (May 23, 2014) |
Published Print | 11 years, 1 month ago (July 1, 2014) |
@article{Limmer_2014, title={Theory of amorphous ices}, volume={111}, ISSN={1091-6490}, url={http://dx.doi.org/10.1073/pnas.1407277111}, DOI={10.1073/pnas.1407277111}, number={26}, journal={Proceedings of the National Academy of Sciences}, publisher={Proceedings of the National Academy of Sciences}, author={Limmer, David T. and Chandler, David}, year={2014}, month=may, pages={9413–9418} }