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The P-V-T equation of state and thermodynamic properties of liquid iron

机译:液态铁的P-V-T状态方程和热力学性质

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The equation of state (EoS) and thermodynamic properties of non-magnetic liquid iron were investigated from energy (E)-pressure (P)-volume (V)-temperature (T) relationships calculated by means of ab initio molecular dynamics simulations at 60-420 GPa and 4000-7000 K. Its internally consistent thermodynamic and elastic properties, in particular, density, adiabatic bulk modulus, and P wave velocity, were then analyzed. Compared to the seismological data of the Earth's outer core, pure liquid iron is found to have an 8-10% larger density and 3-10% larger bulk modulus than the Earth's values. Results also show that the P wave velocity of liquid iron has marginal temperature dependence as the bulk sound velocity of solid iron. The new EoS model and thermodynamic properties of liquid iron may serve as fundamental data for the thermochemical modeling of the Earth's core.
机译:从能量(E)-压力(P)-体积(V)-温度(T)的关系,通过从头算分子动力学模拟在60℃下的计算,研究了非磁性液态铁的状态方程(EoS)和热力学性质。 -420 GPa和4000-7000K。然后分析了其内部一致的热力学和弹性特性,特别是密度,绝热体积模量和P波速度。与地球外核的地震数据相比,发现纯铁水的密度比地球值大8-10%,体积模量大3-10%。结果还表明,液态铁的P波速度与固态铁的整体声速具有边际温度依赖性。新的EoS模型和铁水的热力学特性可以作为对地球核心进行热化学建模的基础数据。

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