Thermodynamics of the second order transitions in alpha and epsilon iron

R.A. Howald
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引用次数: 1

Abstract

The presence of a second order transition in epsilon iron, the hexagonal closest packed form, is demonstrated. Two functions of the form T*−1/2 + A + BΘ) are proposed to model the extra heat capacity beyond what can be represented in a polynomial model in the regions 50 K below and 30 K above a lambda point. With A and B chosen so that ΔCp/T is zero with a zero first derivative at the end points, these functions can provide an accurate and convenient representation for the thermodynamic properties of a material at temperatures and pressures near the lambda point for a second order transition. Calculations of the T/P phase diagram of iron provide a good test of the usefulness of this model since two second order transitions are present in the region of interest. This model for the thermodynamic properties of iron reconciles the static and shock wave studies on the melting point of iron at high pressures. Other forms of solid iron may be stable at the melting point above 100 GPa, but the melting point of pure iron at the inner core boundary of the Earth, 328.9 GPa, is probably within 500 K of the calculated melting point for ε′ iron at this pressure, 4 680 K.

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和铁的二阶跃迁热力学
证明了六方最密堆积形式铁的二阶跃迁的存在。提出了两个形式为T*(Θ−1/2 + A + BΘ)的函数来模拟在λ点以下50 K和高于30 K区域的额外热容,这些热容可以用多项式模型表示。选择A和B,使ΔCp/T为零,在端点处一阶导数为零,这些函数可以准确而方便地表示材料在λ点附近的温度和压力下的二阶转变的热力学性质。铁的T/P相图的计算为该模型的有效性提供了一个很好的测试,因为在感兴趣的区域存在两个二阶转变。铁的热力学性质的这个模型调和了铁在高压下熔点的静态和激波研究。其他形式的固体铁在熔点高于100 GPa时可能是稳定的,但地球内核边界的纯铁的熔点为328.9 GPa,可能与ε铁在此压力下的计算熔点(4 680 K)相差不到500 K。
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