4.2 Article

Low-density liquid water is the mother of ice: on the relation between mesostructure, thermodynamics and ice crystallization in solutions

Journal

FARADAY DISCUSSIONS
Volume 167, Issue -, Pages 371-388

Publisher

ROYAL SOC CHEMISTRY
DOI: 10.1039/c3fd00085k

Keywords

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Funding

  1. National Science Foundation [CHE-1012651, CHE-1125235]
  2. Arnold and Mabel Beckman Foundation through a Young Investigator Award
  3. Camille and Henry Dreyfus Foundation through a Teacher-Scholar Award
  4. Direct For Mathematical & Physical Scien
  5. Division Of Chemistry [1012651] Funding Source: National Science Foundation
  6. Division Of Chemistry
  7. Direct For Mathematical & Physical Scien [1125235] Funding Source: National Science Foundation

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Predicting the temperature and extent of ice freezing in aqueous solutions is crucial for areas as diverse as cryobiology and materials design. It has long been recognized that the thermodynamics of liquid water controls the temperature and kinetics of ice crystallization. Parameterizations of the freezing temperatures in terms of the water activity of the solution have been successfully established, but the fundamental origin of the thermodynamic control of the non-equilibrium crystallization of ice has remained elusive. Here we use large-scale molecular simulations to elucidate the relationship between the structure, thermodynamics, and ice crystallization temperatures for solutions of mW water and a strongly hydrophilic solute that mimics LiCl ions. Fast cooling of solutions with up to 20 mol% ions results in the formation of nanosegregated glasses with domains of low-density amorphous ice and an ion-rich vitrified solution. Slow cooling of the mixtures results in nucleation and growth of ice within the domains of four-coordinated liquid water. The temperature of crystallization T-X coincides with the temperature of appearance of nanoscopic domains of four-coordinated liquid water in the mixture, T-L. We use the insight provided by the simulations to derive a thermodynamic expression for the crystallization temperature as a function of the water activity, T-X(a(W)), analogous to the dependence of the melting temperature, T-m(a(W)). The simple expression derived in this work provides a good account of the experimental freezing temperatures of water and the well-known steepest dependence of T-X on solute concentration compared to that of T-m.

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