What is it about?
This is a first principles calculation of both thermal expansion and compressibility of diamond as functions of temperature and pressure, by using one of the best computational approaches available for crystalline solids. Results are useful for the estimation of confinement pressure of mineral inclusions within diamond, which in turn, is a crucial datum for the understanding of processes of diamond formation within the Earth's mantle.
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Why is it important?
The use of hybrid HF/DFT functionals assures a reliable estimation of thermoelastic properties of crystals as functions of temperature and pressure. In this case, the calculated bulk modulus of diamond at room temperature equals the best available experimental datum within the limit of the experimental error (less than 1GPa); the same is true for thermal expansion. High reliability is assured even at higher temperatures and pressures where accuracies of experimental data could be lower.
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This page is a summary of: Toward an accurate ab initio estimation of compressibility and thermal expansion of diamond in the [0, 3000 K] temperature and [0, 30 GPa] pressures ranges, at the hybrid HF/DFT theoretical level, American Mineralogist, May 2014, GeoScienceWorld,
DOI: 10.2138/am.2014.4772.
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Academy of Science (Torino, Italy)
Presentation given at the Academy of Science of Torino (Italy), concerning the state of the art of ab initio calculations of compressibility and thermal expansion of minerals, in view of applications in the Earth Sciences field. The presentation was one of the contributions to the meeting "Impact of Crystallography on Modern Science". Academy of Science, Torino, 25/06/2014.
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