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arXiv 0907.2456cond-mat.mtrl-scicond-mat.str-el
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磁铁矿:高压和低温效应的拉曼研究

Magnetite: Raman study of the high-pressure and low-temperature effects

L. V. Gasparov, D. Arenas, K. -Y. Choi, G. Guntherodt, H. Berger, L. Forro, G. Margaritondo, V. V. Struzhkin, R. Hemley

摘要:

本文报道了用低温(300 K-15 K)高压(高达22 GPa)Raman光谱研究磁铁矿(Fe_3 O_4)中Verwey相变的结果。我们使用额外的拉曼模式下观察到的Verwey转变,以确定如何转变温度的变化与准流体静压。压力的增加导致Verwey转变温度的线性下降,没有间断。相应的压力系数dTV/dP约为-5.2K/GPa。这样的减少是远远大于平均场库仑相互作用模型的过渡预测。

英文摘要:

We report the results of a low-temperature (300K-15K) high-pressure (up to 22GPa) Raman study of the Verwey transition in magnetite (Fe3O4). We use additional Raman modes observed below the Verwey transition to determine how the transition temperature changes with the quasihydrostatic pressure. Increase of the pressure results in the linear decrease of the Verwey transition temperature, with no discontinuity. The corresponding pressure coefficient dTV/dP is found to be ~ -5.2 K/GPa. Such a decrease is substantially larger than the one predicted by the mean-field Coulomb interaction model of the transition.

机构、总结、中文摘要均由AI分析而来,可能存在错误,请以论文正文为准。

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