磁铁矿中的三介子-声子耦合

P. Piekarz, D. Legut, E. Baldini, Carina A. Belvin, T. Kolodziej, W. Tabiś, A. Kozłowski, Z. Kąkol, Z. Tarnawski, J. Lorenzana, N. Gedik, A. Oleś, J. Honig, K. Parlinski
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引用次数: 6

摘要

利用密度泛函理论研究了Fe$_3$O$_4$磁铁矿在高温立方相和低温单斜相中的晶格动力学性质。计算得到的声子色散曲线和声子态密度与非弹性中子、非弹性x射线和核非弹性散射得到的实验数据进行了比较。我们发现单斜$Cc$结构的理论和实验结果非常吻合,揭示了电荷-轨道(三聚子)序和特定声子模式之间的强耦合。对于立方相,明显的差异出现了,值得注意的是,可以理解假设强三聚子-声子耦合可以扩展到Verwey跃迁之上,晶格动力学受近程三聚子顺序而不是平均立方结构的影响。我们的结果确立了三聚子(以及三聚子-声子耦合)在解释磁铁矿物理方面的有效性,远远超出了它们最初的表述。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Trimeron-phonon coupling in magnetite
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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