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Magnon self-energy in the correlated ferromagnetic Kondo lattice model: Spin-charge coupling effects on magnon excitations in manganites

机译:相关铁磁近藤晶格模型中的磁振子自能:自旋电荷耦合对锰矿中磁振子激发的影响

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摘要

Magnon self-energy due to spin-charge coupling is calculated for the correlated ferromagnetic Kondo lattice model (FKLM) including the intraorbital Coulomb repulsion term U for the band electrons using a diagrammatic expansion scheme. By systematically incorporating correlation effects in the form of self-energy and vertex corrections, the expansion scheme explicitly preserves the continuous spin-rotation symmetry and hence the Goldstone mode. Due to a near cancellation of the correlation-induced quantum correction terms at intermediate coupling and optimal band filling relevant for ferromagnetic manganites, the renormalized magnon energies for the correlated FKLM are nearly independent of correlation term. Even at higher-band fillings, despite exhibiting overall non-Heisenberg behavior, magnon dispersion in the T-X direction retains nearly Heisenberg form. Therefore, the experimentally observed doping-dependent zone-boundary magnon softening must be ascribed to spin-orbital coupling effects.
机译:使用图解扩展方案,针对带电子的包括轨道内库仑排斥项U在内的相关铁磁近藤晶格模型(FKLM),计算了由于自旋电荷耦合而产生的磁振子自能。通过以自能和顶点校正的形式系统地整合相关效应,扩展方案明确保留了连续的自旋旋转对称性,从而保留了Goldstone模式。由于在中间耦合时相关感应的量子校正项几乎被抵消,并且与铁磁锰矿有关的最佳能带填充,相关FKLM的重新归一化的磁振子能量几乎与相关项无关。即使在较高频带的填充物中,尽管表现出整体非海森堡行为,但在T-X方向上的磁振子色散仍保留了几乎海森堡形式。因此,实验观察到的与掺杂有关的区域边界磁振子软化必须归因于自旋-轨道耦合效应。

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