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Identifying the spin transition in Fe~(2+)-rich MgSiO_3 perovskite from X-ray diffraction and vibrational spectroscopy

机译:X射线衍射和振动光谱法鉴定富Fe〜(2+)MgSiO_3钙钛矿中的自旋转变

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Based on numerical results from density-functional perturbation theory calculations, we show that the magnetic spin transition in Fe~(2+)-rich MgSiO_3 perovskite can be identified as changes in the powder X?ray diffraction (XRD) pattern and the vibrational spectra. In particular theory predicts how the symmetry breaking and the volume reduction associated with the spin transition affects both structural and vibrational properties. The XRD measurements of (Mg_(0.5)Fe_(0.5))SiO_3 perovskite indeed demonstrated that the new diffraction peaks and the peak broadening formed during the spin transition can be explained by the associated symmetry breaking. We also show computationally that certain vibrational peaks exhibit a shift at the transition; the Grüneisen parameters of certain modes are affected by the transition, thus bearing on the thermodynamical properties. Raman and/or infrared measurements before and after the spin transition could identify these changes
机译:基于密度泛函微扰理论计算的数值结果,我们表明富Fe〜(2+)的MgSiO_3钙钛矿中的磁自旋跃迁可以识别为粉末X射线衍射(XRD)图案和振动光谱的变化。特别地,理论预测了与自旋跃迁相关的对称性破裂和体积减小如何影响结构和振动特性。 (Mg_(0.5)Fe_(0.5))SiO_3钙钛矿的XRD测量确实表明,新的衍射峰和在自旋转变过程中形成的峰展宽可以通过相关的对称破坏来解释。我们还通过计算表明,某些振动峰在跃迁处表现出位移。某些模式的Grüneisen参数受过渡影响,因此影响热力学性质。自旋转变前后的拉曼和/或红外测量可以识别这些变化

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