论文标题

磁铁矿中的trimeron-phonon耦合

Trimeron-phonon coupling in magnetite

论文作者

Piekarz, P., Legut, D., Baldini, E., Belvin, C. A., Kołodziej, T., Tabiś, W., Kozłowski, A., Kąkol, Z., Tarnawski, Z., Lorenzana, J., Gedik, N., Oleś, A. M., Honig, J. M., Parlinski, K.

论文摘要

使用密度函数理论,我们研究了高温立方和低温单斜层阶段的磁铁矿(Fe $ _3 $ o $ _4 $)的晶格动力学特性。将计算出的声子分散曲线和状态的声子密度与无弹性中子,非弹性X射线和核非弹性散射获得的可用实验数据进行了比较。我们发现单智性$ cc $结构的理论和实验结果之间的一致性非常好,揭示了电荷轨道(Trimeron)订单与特定声子模式之间的强耦合。对于立方阶段,出现明显的差异,可以明显地理解,假设强大的Trimeron-Phonon耦合可以扩展到Verwey过渡的上方,并且受晶格动力学受到短距离Trimeron Order的影响,而不是平均立方体结构。我们的结果确定了Trimerons(和Trimeron-Phonon耦合)在解释磁铁矿的物理学的有效性,这是其原始配方的范围。

Using density functional theory, we study the lattice dynamical properties of magnetite (Fe$_3$O$_4$) in the high-temperature cubic and low-temperature monoclinic phases. The calculated phonon dispersion curves and phonon density of states are compared with the available experimental data obtained by inelastic neutron, inelastic x-ray, and nuclear inelastic scattering. We find a very good agreement between the theoretical and experimental results for the monoclinic $Cc$ structure revealing the strong coupling between charge-orbital (trimeron) order and specific phonon modes. For the cubic phase, clear discrepancies arise which, remarkably, can be understood assuming that the strong trimeron-phonon coupling can be extended above the Verwey transition, with lattice dynamics influenced by the short-range trimeron order instead of the average cubic structure. Our results establish the validity of trimerons (and trimeron-phonon coupling) in explaining the physics of magnetite much beyond their original formulation.

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