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arXiv 1102.2756cond-mat.mes-hallcond-mat.other
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天然石墨的高场磁透射研究

High field magneto-transmission investigation of natural graphite

N. Ubrig, P. Plochocka, P. Kossacki, M. Orlita, D. K. Maude, O. Portugall, G. L. J. A. Rikken

摘要:

在B=20- 60 T的磁场中,用磁透射法测量了天然石墨的H点和K点朗道能级跃迁。在H点处,观察到两个系列的跃迁,其能量演化为$\sqrt{B}$。一个简化的Slonczewski,Weiss和McClure(SWM)模型,只有两个参数来描述层内(gamma 0)和层间(gamma 1)耦合正确地描述了所有观察到的过渡。极化分辨的测量证实,所观察到的明显分裂的H点跃迁在高磁场不能归因于狄拉克锥的不对称性。

英文摘要:

Magneto-transmission measurements in magnetic fields in the range B=20-60T have been performed to probe the H and K-point Landau level transitions in natural graphite. At the H-point, two series of transitions, whose energy evolves as $\sqrt{B}$ are observed. A reduced Slonczewski, Weiss and McClure (SWM) model with only two parameters to describe the intra-layer (gamma0) and inter-layer (gamma1) coupling correctly describes all observed transitions. Polarization resolved measurements confirm that the observed apparent splitting of the H-point transitions at high magnetic field cannot be attributed to an asymmetry of the Dirac cone.

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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