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Phonon spectrum, thermodynamic properties, and pressure-temperature phase diagram of uranium dioxide

机译:声子谱,热力学性质和压力 - 温度   二氧化铀相图

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摘要

We present a study of the structural phase transition, mechanical andthermodynamic properties of UO$_{2}$ by means of the local densityapproximation (LDA)$+U$ approach. A phase transition pressure of 40 GPa, whichagrees well with the experimental value of 42 GPa, is obtained from theory at 0K. Pressure-induced enhancements of elastic constants, elastic moduli, elasticwave velosities, and Debye temperature of the fluorite phase are observed.Phonon spectrums of both the ground state fluorite structure and high pressurecotunnite structure calculated by the supercell approach show that thecotunnite structure is dynamically unstable under ambient pressure. Based onthe imaginary mode along the $\Gamma$$-$$X$ direction and soft phonon modealong the $\Gamma$$-$$Z$ direction, a transition path from cotunnite tofluorite has been identified. We calculate the lattice vibrational energy inthe quasiharmonic approximation using both first-principles phonon density ofstate and the Debye model. Calculated temperature dependence of latticeparameter, entropy, and specific heat agree well with experimental observationsin the low temperature domain. The difference of Gibbs free energy between thetwo phases of UO$_{2}$ has predicted a boundary in the pressure-temperaturephase diagram. The solid-liquid boundary is approximated by an empiricalequation using our calculated elastic constants.
机译:我们通过局部密度近似(LDA)$ + U $方法研究了UO $ _ {2} $的结构相变,力学和热力学性质。从0K的理论值可以得出40 GPa的相变压力与42 GPa的实验值非常吻合。观察到了压力引起的萤石相的弹性常数,弹性模量,弹性波速度和德拜温度的增强。通过超晶胞方法计算的基态萤石结构和高压共生辉石结构的声子光谱表明,该共融结构在动态条件下是动态不稳定的。环境压力。基于沿$ \ Gamma $$-$$ X $方向的虚模和沿$ \ Gamma $$-$ Z $方向的软声子模态,确定了从辉石到萤石的过渡路径。我们使用状态的第一性原理声子密度和德拜模型,以准谐波近似计算晶格振动能。计算得到的晶格参数,熵和比热的温度依赖性与低温领域的实验观测结果非常吻合。 UO $ _ {2} $的两个相之间的吉布斯自由能的差异已经预测了压力-温度相图中的边界。使用我们计算的弹性常数,通过经验方程式近似固液边界。

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