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arXiv 0907.1424cond-mat.mtrl-scicond-mat.str-el
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磁铁矿中的电子喇曼散射,自旋与电荷隙

Electronic Raman scattering in Magnetite, Spin vs. Charge gap

L. Gasparov, A. Rush, G. Guntherodt, H. Berger

摘要:

本文报道了Fe_3O_4单晶的拉曼散射数据,其Verwey转变温度(Tv)分别为123和117 K。这两种单晶显示了广泛的电子背景延伸到900波数(~110 meV)。当样品冷却到低于Tv时,观察到该背景的再分布。特别是,低温相的光谱显示出低于300波数的背景减弱,随后是300和400波数之间的电子背景增强。为了增强这种背景重新分布的效果,我们将跃迁正下方的光谱除以跃迁正上方的光谱。由此产生的宽峰状功能进行观察,集中在370波数(45毫电子伏)。该特征的峰位置不与转变温度成比例。我们讨论了两种替代的分配这一功能的自旋或电荷的差距磁铁矿。

英文摘要:

We report Raman scattering data of single crystals of magnetite (Fe3O4) with Verwey transition temperatures (Tv) of 123 and 117K, respectively. Both single crystals reveal broad electronic background extending up to 900 wavenumbers (~110 meV). Redistribution of this background is observed when samples are cooled below Tv. In particular, spectra of the low temperature phase show diminished background below 300 wavenumbers followed by an enhancement of the electronic background between 300 and 400 wavenumbers. To enhance the effect of this background redistribution we divide the spectra just below the transition by the spectra just above the transition. A resultant broad peak-like feature is observed, centered at 370 wavenumbers (45 meV). The peak position of this feature does not scale with the transition temperature. We discuss two alternative assignments of this feature to a spin or charge gap in magnetite.

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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