论文标题
MGSIO $ _3 $中的植物后酮过渡跨越后的热力学特性和相边界
Anharmonic thermodynamic properties and phase boundary across the post-perovskite transition in MgSiO$_3$
论文作者
论文摘要
为了解决perovskite的晶格非谐度对MGSIO $ _3 $中植物后转变的影响,我们使用Quasiparticle(PHQ)方法进行计算。 PHQ基于\ textIt {ab libio}分子动力学,从原则上讲,它捕获了完全的非谐性。热力学极限($ n \ rightarrow \ infty $)中的自由能是使用声子气体模型中温度依赖性的准粒子分散剂计算的。报道了阿谐热力学特性和相边界的系统结果。进行局部密度近似(LDA)和广义梯度近似(GGA)计算,以提供对这些属性的自信约束。通过将结果与使用准摩尼克近似(QHA)获得的结果进行比较来证明非谐波效应。 QHA的不足是通过对热力学膨胀性和热力学Grüneisen参数的高估以及其在高温极限下的融合等速热容量所表明的。 PHQ相边界具有clapeyron斜率($ dp/dt $),随温度而增加。该结果与QHA相边界的几乎零曲率形成对比。非harm谐性将相边界弯曲到高压下较低的温度。讨论了通过地幔地球热对相边界的双重交叉的影响。
To address the effects of lattice anharmonicity across the perovskite to post-perovskite transition in MgSiO$_3$, we conduct calculations using the phonon quasiparticle (PHQ) approach. The PHQ is based on \textit{ab initio} molecular dynamics and, in principle, captures full anharmonicity. Free energies in the thermodynamic limit ($N \rightarrow \infty$) are computed using temperature-dependent quasiparticle dispersions within the phonon gas model. Systematic results on anharmonic thermodynamic properties and phase boundary are reported. Both the local density approximation (LDA) and the generalized gradient approximation (GGA) calculations are performed to provide confident constraints on these properties. Anharmonic effects are demonstrated by comparing results with those obtained using the quasiharmonic approximation (QHA). The inadequacy of the QHA is indicated by its overestimation of thermal expansivity and thermodynamic Grüneisen parameter and its converged isochoric heat capacity in the high-temperature limit. The PHQ phase boundary has a Clapeyron slope ($dP/dT$) that increases with temperature. This result contrasts with the nearly zero curvature of the QHA phase boundary. Anharmonicity bends the phase boundary to lower temperatures at high pressures. Implications for the double-crossing of the phase boundary by the mantle geotherm are discussed.