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The random phase approximation applied to ice.

M Macher1, J Klimeš1, C Franchini1

  • 1Faculty of Physics and Center for Computational Materials Science, University of Vienna, Sensengasse 8/12, A-1090 Vienna, Austria.

The Journal of Chemical Physics
|March 5, 2014
PubMed
Summary
This summary is machine-generated.

Standard density functionals inadequately describe ice phases. The random phase approximation (RPA) offers a balanced description of water ice, approaching diffusion Monte Carlo accuracy for energies and volumes.

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Area of Science:

  • Computational physics
  • Materials science
  • Quantum chemistry

Background:

  • Standard density functionals struggle to accurately model ice phases, particularly high-pressure forms, often predicting them as too unstable.
  • While van der Waals interactions improve descriptions, significant errors in relative volumes persist.

Purpose of the Study:

  • To evaluate the random phase approximation (RPA) for calculating correlation energy in ice phases.
  • To compare RPA results with experimental data and diffusion Monte Carlo (DMC) simulations for ice.

Main Methods:

  • Utilizing the random phase approximation (RPA) to compute correlation energy for various ice phases.
  • Comparing RPA predictions for relative energies and volumes against experimental measurements and high-accuracy DMC data.

Main Results:

  • The RPA provides a highly balanced and accurate description across different ice phases.
  • RPA results for relative energies and volumes closely approach the accuracy of diffusion Monte Carlo.
  • This method significantly improves upon standard density functionals and those including van der Waals interactions.

Conclusions:

  • The random phase approximation (RPA) offers a promising and accurate approach for describing molecular water phases.
  • This method shows potential for accurate modeling of water ice on surfaces and within cavities.
  • RPA presents a viable alternative for precise simulations of condensed matter systems.