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首页> 外文期刊>The European physical journal, B. Condensed matter physics >Structural transition from marcasite to pyrite phase in FeSe(2)under high pressure: a first-principles study
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Structural transition from marcasite to pyrite phase in FeSe(2)under high pressure: a first-principles study

机译:在高压下,从马赛酯到黄铁矿阶段的结构转变:一项原则研究

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Based on density functional theory, first-principles simulations and calculations are carried out to study the structural stability and electronic properties of FeSe(2)under high pressure. Present theoretical calculations not only reproduce successfully the lattice constants, bulk modulus, and indirect band gap of both the marcasite and pyrite phases at ambient conditions, but also predict a first-order phase transition from the marcasite to pyrite structure at 9 GPa under compression. Based on elastic constants and phonon spectra calculations and detailed analysis of the geometry structures, a possible mechanism of the structural transformation from marcasite to pyrite structure is presented. Furthermore, pressure-induced band gap enlargement is observed in the marcasite phase, which is benefit for the optical applications. By contrast, the band gap of the pyrite phase gradually decreases along with the compression, and finally closes up due to the broadening of bandwidths.
机译:基于密度泛函理论,进行了一原子模拟和计算,以研究在高压下FESE(2)的结构稳定性和电子性质。 目前的理论计算不仅成功再现了马基钛矿和硫铁矿相于环境条件的晶格常数,体积和间接带差异,而且还预测了在压缩下在9GPa下从Marcasite到硫铁矿结构的一阶相转变。 基于弹性常数和声光谱计算及几何结构的详细分析,提出了从马克铁酸盐到硫铁矿结构的结构转化的可能机制。 此外,在Marcasite相中观察到压力诱导的带隙扩大,这对光学应用有益。 相比之下,用压缩逐渐减小硫铁矿相的带隙,并且由于带宽的扩展而最终关闭。

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