A model of elastic softening and displacive phase transitions in anisotropic phases, with application to stishovite and post-stishovite

SUMMARY This paper introduces a comprehensive framework for modelling both instantaneous and time-dependent elastic softening in anisotropic materials at high pressure and temperature. This framework employs Landau Theory, minimizing the Helmholtz energy by varying isochemical parameters ($\boldsymbol {q}$) that capture structural changes, atomic ordering and/or electronic spin states. This allows for internally consistent predictions of volume, unit cell parameters, the elastic tensor, and other thermodynamic properties, while allowing large symmetry-breaking strains. The formulation is validated using the stishovite-to-post-stishovite transition. It is demonstrated that, near this transition, both stishovite and post-stishovite exhibit auxetic behaviour in several directions, with post-stishovite also displaying negative linear compressibility along the long axis of its unit cell (either the a- or b-axis). The new formulation is implemented in the open-source BurnMan software package.

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Publication Details

Journal
Geophysical Journal International
Published
2025-02-04
DOI
https://doi.org/10.1093/gji/ggaf043
Primary Topic
Geotechnical and Geomechanical Engineering
Type
article
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article

A model of elastic softening and displacive phase transitions in anisotropic phases, with application to stishovite and post-stishovite

Robert Myhill
Geophysical Journal International
Geotechnical and Geomechanical Engineering
article

A model of elastic softening and displacive phase transitions in anisotropic phases, with application to stishovite and post-stishovite

Robert Myhill
article en

Abstract

SUMMARY This paper introduces a comprehensive framework for modelling both instantaneous and time-dependent elastic softening in anisotropic materials at high pressure and temperature. This framework employs Landau Theory, minimizing the Helmholtz energy by varying isochemical parameters ($\boldsymbol {q}$) that capture structural changes, atomic ordering and/or electronic spin states. This allows for internally consistent predictions of volume, unit cell parameters, the elastic tensor, and other thermodynamic properties, while allowing large symmetry-breaking strains. The formulation is validated using the stishovite-to-post-stishovite transition. It is demonstrated that, near this transition, both stishovite and post-stishovite exhibit auxetic behaviour in several directions, with post-stishovite also displaying negative linear compressibility along the long axis of its unit cell (either the a- or b-axis). The new formulation is implemented in the open-source BurnMan software package.

Geophysical Journal InternationalVol. 241(2)
University of Bristol (GB)
Openalex Percentile: Top 98%
Geotechnical and Geomechanical Engineering
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A model of elastic softening and displacive phase transitions in anisotropic phases, with application to stishovite and post-stishovite — Robert Myhill · Geophysical Journal International (2025) | TGRS Research Map | TGRS