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arXiv 1607.02601cond-mat.mtrl-sci
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多铁性材料BiFeO3中电场梯度和磁旋轮线椭圆率的取向

Orientation of the electric field gradient and ellipticity of the magnetic cycloid in multiferroic BiFeO3

A. Pierzga, A. Blachowski, K. Komedera, K. Ruebenbauer, A. Kalvane, R. Bujakiewicz-Koronska

摘要:

本文利用57 Fe的14.41keV共振跃迁,研究了多铁性BiFeO_3中57 Fe核上的超精细相互作用,并将透射几何应用于随机粉末样品。在80 K,190 K和室温下获得光谱。发现铁以高自旋三价态存在。超精细磁场的分布是由于磁旋轮线的类椭圆畸变引起的。椭圆的长轴沿着<111>菱面体晶胞的方向定向。在室温下,该方向的超精细磁场约为垂直方向磁场的1.013。在80 K时,该比值减小到1.010。铁原子上的轴对称电场梯度(EFG)具有相同方向的主轴,且EFG的主分量为正。我们的结果与铁的磁矩局限于[1-21]晶面的发现是一致的。

英文摘要:

The paper deals with the hyperfine interactions observed on the 57Fe nucleus in multiferroic BiFeO3 by means of the 14.41-keV resonant transition in 57Fe, and for transmission geometry applied to the random powder sample. Spectra were obtained at 80 K, 190 K and at room temperature. It was found that iron occurs in the high spin trivalent state. Hyperfine magnetic field follows distribution due to the elliptic-like distortion of the magnetic cycloid. The long axis of the ellipse is oriented along <111> direction of the rhombohedral unit cell. The hyperfine magnetic field in this direction is about 1.013 of the field in the perpendicular direction at room temperature. This ratio diminishes to 1.010 at 80 K. Axially symmetric electric field gradient (EFG) on the iron atoms has the principal axis oriented in the same direction and the main component of the EFG is positive. Our results are consistent with the finding that iron magnetic moments are confined to the [1-21] crystal plane.

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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