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Atomistic and Ab initio modeling of CaAl2O4 high-pressure polymorphs under Earth's mantle conditions

机译:地幔条件下CaAl2O4高压多晶型的原子和从头算模型

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Semi-empirical and ab initio theoretical investigation of crystal structure geometry, interatomic distances, phase densities and elastic properties for some CaAl2O4 phases under pressures up to 200 GPa was performed. Two independent simulation methods predicted the appearance of a still unknown super-dense CaAl2O4 modification. In this structure, the Al coordination polyhedron might be described as distorted one with seven vertices. Ca atoms were situated inside polyhedra with ten vertices and Ca-O distances from 1.96 to 2.49 . It became the densest modification under pressures of 170 GPa (density functional theory prediction) or 150 GPa (semi-empirical prediction). Both approaches indicated that this super-dense CaAl2O4 modification with a "stuffed alpha-PbO2" type structure could be a probable candidate for mutual accumulation of Ca and Al in the lower mantle. The existence of this phase can be verified experimentally using high pressure techniques.
机译:在200 GPa的压力下,对某些CaAl2O4相进行了晶体结构几何,原子间距离,相密度和弹性特性的半经验和从头开始的理论研究。两种独立的模拟方法预测了仍然未知的超稠CaAl2O4修饰的出现。在这种结构中,Al配位多面体可能被描述为具有七个顶点的扭曲多面体。 Ca原子位于多面体内部,具有10个顶点,Ca-O距离为1.96至2.49。在170 GPa(密度泛函理论预测)或150 GPa(半经验预测)的压力下,它成为最稠密的改性。两种方法都表明,这种具有“填充α-PbO2”结构的超稠CaAl2O4修饰可能是Ca和Al在下地幔中相互堆积的一种可能的候选物。此阶段的存在可以使用高压技术通过实验验证。

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