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Heating a crystalline solid increases the average energy of its atoms, molecules, or ions, and the solid gets hotter. At some point, the added energy becomes large enough to partially overcome the forces holding the molecules or ions of the solid in their fixed positions, and the solid begins the process of transitioning to the liquid state or melting. At this point, the temperature of the solid stops rising, despite the continual input of heat, and it remains constant until all of the solid is...
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Some solids can transition directly into the gaseous state, bypassing the liquid state, via a process known as sublimation. At room temperature and standard pressure, a piece of dry ice (solid CO2) sublimes, appearing to gradually disappear without ever forming any liquid. Snow and ice sublimate at temperatures below the melting point of water, a slow process that may be accelerated by winds and the reduced atmospheric pressures at high altitudes. When solid iodine is warmed, the solid sublimes...
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A phase transition is the process in which a substance changes from one state of matter to another, like from a solid to a liquid, liquid to gas, or vice versa, at a specific temperature and under given pressure conditions. This change is spontaneous and is affected by alterations in temperature and pressure. These parameters impact the strength of the forces between molecules (intermolecular forces) in the substance.During a phase transition, both the initial and final phases of the substance...
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A phase diagram combines plots of pressure versus temperature for the liquid-gas, solid-liquid, and solid-gas phase-transition equilibria of a substance. These diagrams indicate the physical states that exist under specific conditions of pressure and temperature and also provide the pressure dependence of the phase-transition temperatures (melting points, sublimation points, boiling points). Regions or areas labeled solid, liquid, and gas represent single phases, while lines or curves represent...
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Superionic-Superionic Phase Transitions in Body-Centered Cubic H_{2}O Ice.

Jean-Alexis Hernandez1, Razvan Caracas1

  • 1Laboratoire de Géologie de Lyon, UMR CNRS 5276 (CNRS, ENS, Université Lyon1), École Normale Supérieure de Lyon, 69364 Lyon Cedex 07, France.

Physical Review Letters
|October 8, 2016
PubMed
Summary
This summary is machine-generated.

This study reveals three distinct superionic phases in body-centered-cubic (bcc) H2O ice under extreme conditions. These phases involve unique proton delocalization and bonding behaviors, crucial for understanding high-pressure ice properties.

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Area of Science:

  • Condensed Matter Physics
  • Materials Science
  • Geophysics

Background:

  • Superionic proton conduction in ice is critical for understanding planetary interiors.
  • The behavior of O─H⋯O bonds influences ice phase transitions under extreme conditions.

Purpose of the Study:

  • To investigate the relationship between superionic proton conduction and O─H⋯O bond behavior in bcc H2O ice.
  • To identify distinct phases within the superionic bcc stability field.

Main Methods:

  • First-principles molecular dynamics simulations.
  • Analysis of structural, energetic, and elastic properties.
  • Simulations conducted between 1300-2000 K and up to 300 GPa.

Main Results:

  • Evidence for three distinct superionic phases in bcc H2O ice.
  • Phase VII'' exhibits highly delocalized protons and fast diffusion at lower pressures.
  • Phase VII' shows partial proton localization, separated by a first-order transition.
  • Phase X features symmetric O─H─O bonds, reached via a second-order transition upon compression.

Conclusions:

  • The study elucidates the phase diagram of superionic bcc H2O ice.
  • Proton delocalization and O─H⋯O bond symmetry evolve distinctly across the identified phases.
  • Findings provide insights into the behavior of water ice under extreme pressures and temperatures.