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Trigonal Boracites - A New Type of Ferroelectric and Ferromagnetoelectric that Allows no 180° Electric Polarization Reversal

机译:三角长晶硼铁石-一种新型的铁电和铁磁金属,不允许180°电极化反转

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摘要

The space group of the trigonal phase of the Fe-Cl, Fe-Br, Fe-I, Co-Cl, and Zn-Cl boracites is established as C63v. Ferroelectricity is evidenced by domain switching. High coercive fields at room temp. (up to 8000 kV/cm) are found. Polarization-microscopic studies show that the polarization vector is not reversible by 180°, but can jump only from, e.g., [111] to [111], [111], or [111], etc., in accord with crystal-structure and group-theoretical symmetry considerations. Two twinning "laws" are observed: (a) head-head (tail-tail), domains with {110}cub as compn. plane and (b) head-tail domains with {100}cub as compn. plane. The domain structure and the relevant twinning operations are discussed. The onset of ferromagnetism at low temp. in Fe-Cl, Fe-Br, Fe-I, and Co-Cl boracites leads to ferromagnetoelectricity. In the case of Co-Cl boracite, the ferromagnetoelec. point group is m.
机译:将Fe-Cl,Fe-Br,Fe-I,Co-Cl和Zn-Cl硼铁矿的三角相的空间群建立为C63v。铁电通过域切换来证明。室温下的高矫顽场。 (最高8000 kV / cm)。偏振显微镜研究表明,偏振矢量不可逆180°,而只能根据晶体结构从[111]跳到[111],[111]或[111]等。以及群体理论上的对称性考虑。观察到两个孪生的“律”:(a)头-头(尾),以{110} cub为分量的域。平面和(b)以{100} cub为分量的头尾域。飞机。讨论了域结构和相关的孪生操作。低温下铁磁性的发生。 Fe-Cl,Fe-Br,Fe-I和Co-Cl硼铁矿中的金属导致铁磁电。如果是Co-Cl硼铁矿,则是铁磁锰矿。点组是m。

著录项

  • 作者

    Schmid, Hans;

  • 作者单位
  • 年度 1970
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  • 原文格式 PDF
  • 正文语种 eng
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