Semi-empirical pressure-volume-temperature equation of state; MgSiO3 perovskite is an example
Jozsef Garai

TL;DR
This paper introduces a semi-empirical p-V-T equation of state for elastic solids, tested on MgSiO3 perovskite, showing it accurately models experimental data and outperforms traditional models across temperature ranges.
Contribution
A new semi-empirical p-V-T equation of state derived and validated for perovskite, demonstrating superior performance over conventional isothermal equations.
Findings
Accurately fits experimental p-V-T data of perovskite.
Outperforms traditional EoSs in temperature-dependent modeling.
Parameters are within experimental uncertainties.
Abstract
Simple general formula describing the p-V-T relationships of elastic solids is derived from theoretical considerations. The new EoS was tested to experiments of perovskite 0-109 GPa and 293-2000 K. The parameters providing the best fit are: Ko = 267.5 GPa, Vo = 24.284 cm3, alpha_o = 2.079x10^-5 K^-1, the pressure derivative of Ko is 1.556 and the pressure derivative of alpha_o is -1.098x10^-7 K^-1GPa^-1 . The root-mean-square-deviations (RMSD) of the residuals are 0.043 cm3, 0.79 GPa, and 125 K for the molar volume, pressure, and temperature respectively. These RMSD values are in the range of the uncertainty of the experiments, indicating that the five parameters semi-empirical EoS correctly describes the p-V-T relationships of perovskite. Separating the experiments into 200 K ranges the semi-empirical EoS was compared to the most widely used finite strain, interatomic potential, and…
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