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Homogeneous ice nucleation rate at negative pressures: The role of the density anomaly

  • Elise Rosky
  • , Will Cantrell
  • , Tianshu Li
  • , Raymond A. Shaw
  • Michigan Technological University
  • The George Washington University School of Engineering and Applied Science

Research output: Contribution to journalArticlepeer-review

8 Scopus citations

Abstract

Recent experiments suggest a role for pressure fluctuations in nucleation. Homogeneous ice nucleation rates for the ML-mW and mW water models are evaluated at pressures ranging from atmospheric to -1000 atm, using forward flux sampling and constant cooling simulations. Results indicate that the density difference Δνls between water and ice exhibited by these models plays a central role in controlling the change in nucleation rate with pressure. A linear function is found to be a reasonable approximation for lines of constant nucleation rate, which can be useful in making experimental predictions to advance the study of ice nucleation mechanisms.

Original languageEnglish
Article number139289
JournalChemical Physics Letters
Volume789
DOIs
StatePublished - Feb 2022
Externally publishedYes

Keywords

  • Homogeneous nucleation
  • Ice nucleation
  • Molecular dynamics
  • Pressure dependence of nucleation

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