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首页> 外文期刊>Physics and Chemistry of Minerals >Calculation of infrared and Raman vibration modes of magnesite at high pressure by density-functional perturbation theory and comparison with experiments
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Calculation of infrared and Raman vibration modes of magnesite at high pressure by density-functional perturbation theory and comparison with experiments

机译:用密度泛函微扰理论计算高压菱镁矿的红外和拉曼振动模态并与实验比较

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摘要

We predict the IR-TO, IR-LO and Raman modes (wave numbers and intensities) of magnesite (MgCO3) up to 50 GPa, at T = 0 K, using the density-functional perturbation theory up to a third order perturbation, under the harmonic assumption. The predicted IR-TO and Raman mode wave numbers, the mode Grüneisen parameters and the Davydov splittings are systematically compared with experimental data for all modes up to the pressures of 10–30 GPa and for some modes up to 50 GPa. Existing experiments allow extending this comparison only to IR-LO wave numbers of the E u3) asymmetric-stretch mode, confirming the odd experimental behavior of this mode at very high pressures. Predicted IR-TO, IR-LO and Raman intensities up to 50 GPa are just tabulated, but data are missing for their comparison with precise experiments. However, the generally good agreement observed between numerical results and experimental data, when their comparison is possible, suggests that first-principles methods are a major help to predict the entire spectrum up to very high pressures.
机译:我们使用密度泛函微扰理论预测了在T = 0 K时,镁砂(MgCO 3 )的IR-TO,IR-LO和拉曼模式(波数和强度)高达50 GPa。在谐波假设下,直至三阶扰动。系统将预测的IR-TO和拉曼模式波数,模式Grüneisen参数和Davydov分裂与实验数据进行了比较,所有实验压力高达10–30 GPa,某些模式高达50 GPa。现有的实验仅允许将此比较扩展到E u (ν 3 )不对称拉伸模式的IR-LO波数,从而证实了该模式在非常高的实验性能高压。仅列出了高达50 GPa的预测IR-TO,IR-LO和拉曼强度,但缺少与精确实验进行比较的数据。但是,如果可以进行比较,则数值结果和实验数据之间通常会观察到良好的一致性,这表明第一原理方法是预测非常高压力下的整个光谱的主要帮助。

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