Abstract
This paper presents a framework for building anisotropic equations of state for solid solutions. The framework satisfies the connections between elastic and thermodynamic properties required by Maxwell's relations. It builds on a recent anisotropic equation of state for pure phases under small deviatoric stresses, adding a dependence on a vector, whose components contain the molar amounts of independent end-members in the solid solution. These end-members may have distinct chemical compositions, site species occupancies or electronic spin states. The high albite-anorthite (C) plagioclase solid solution is used to illustrate the formulation.
| Original language | English |
|---|---|
| Pages (from-to) | 1900-1909 |
| Number of pages | 10 |
| Journal | Geophysical Journal International |
| Volume | 239 |
| Issue number | 3 |
| Early online date | 14 Oct 2024 |
| DOIs | |
| Publication status | Published - 1 Dec 2024 |
Bibliographical note
Publisher Copyright:© 2024 The Author(s). Published by Oxford University Press on behalf of The Royal Astronomical Society.
Keywords
- Elasticity and anelasticity
- Equations of state
- Seismic anisotropy
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