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Updated: Mar 29, 2026

Ice Generation and the Heat and Mass Transfer Phenomena of Introducing Water to a Cold Bath of Brine
Published on: March 13, 2017
Water Freezing and Ice Melting.
1Department of Chemistry, Boston University , Boston, Massachusetts 02215-2521, United States.
The generalized replica exchange method (gREM) effectively samples coexisting phases for strong first-order phase transitions. This simulation approach accurately models water freezing and ice melting, yielding key thermodynamic properties.
Area of Science:
- Physical Chemistry
- Computational Materials Science
- Thermodynamics
Background:
- First-order phase transitions, such as freezing and melting, are critical phenomena in materials science.
- Accurately simulating coexisting phases and phase transitions remains a computational challenge.
- Understanding the thermodynamics of water's phase transitions is essential for various scientific disciplines.
Purpose of the Study:
- To present and validate the isobaric molecular dynamics (MD) version of the generalized replica exchange method (gREM).
- To apply gREM to the phase transitions of water, specifically freezing and melting of hexagonal and cubic ice.
- To obtain thermodynamic properties and analyze phase transition pathways.
Main Methods:
- Implementation of the isobaric molecular dynamics version of the generalized replica exchange method (gREM).
- Simulation of liquid water freezing and hexagonal/cubic ice melting processes.
- Application of entropic analysis to determine equilibrium transition temperatures, latent heats, and surface tensions.
Main Results:
- gREM successfully sampled coexisting liquid-water and ice phases.
- Hysteresis between freezing and melting processes was observed and analyzed.
- Accurate thermodynamic properties (transition temperatures, latent heats, surface tensions) were obtained for hexagonal and cubic ice transitions.
- A novel method for assigning water molecules to symmetry types was developed.
- Freezing pathways revealed intermediate layered structures composed of hexagonal and cubic ice.
Conclusions:
- The generalized replica exchange method (gREM) is a powerful tool for simulating first-order phase transitions and coexisting phases.
- The study provides accurate thermodynamic data for water's phase transitions, validating the gREM approach.
- Observed freezing pathways offer new insights into the molecular mechanisms of ice formation.
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