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首页> 外文期刊>EPL >Magnetic transition and spin rotation in a new multiferroic Ba 3 TaFe 3 Si 2 O 14 observed by the M?ssbauer spectroscopy
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Magnetic transition and spin rotation in a new multiferroic Ba 3 TaFe 3 Si 2 O 14 observed by the M?ssbauer spectroscopy

机译:Msssbauer光谱法观察到新型多铁性Ba 3 TaFe 3 Si 2 O 14中的磁跃迁和自旋旋转

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摘要

The long-range 3D magnetic ordering in the Fe ~(3+) -containing langasite family compound Ba _3 TaFe_3 Si _2 O _(14) was observed below 27 K with the iron lattice split into two nonequivalent magnetic sublattices. The appearance of the nonequivalent Fe sites is associated with the structural phase transition P 321→ P 3 induced by the magnetic ordering. At this transition, the presence of the polar threefold axis creates the conditions for the ferroelectric state and Ba _3 TaFe_3 Si_2 O_(14) may be considered as a magnetically induced multiferroic. The Fe~(3+) magnetic moments in the two sublattices are oriented at different angles to the local crystal axes with a mean value ~45°. At temperatures between 4.2 and 25 K, iron spins in two sublattices rotate in opposite directions which can be related to the magnetic chirality in the helicoidal magnetic structure.
机译:在27 K以下观察到了含Fe〜(3+)的镧铁矿族化合物Ba _3 TaFe_3 Si _2 O _(14)中的长距离3D磁性排序,其中铁晶格分裂为两个非等价的亚晶格。 Fe等价位点的出现与磁有序诱导的结构相变P 321→P 3有关。在此跃迁中,极性三重轴的存在为铁电态创造了条件,Ba _3 TaFe_3 Si_2 O_(14)可以被认为是磁感应多铁性体。两个亚晶格中的Fe〜(3+)磁矩与局部晶轴的夹角不同,平均值为〜45°。在4.2到25 K之间的温度下,两个亚晶格中的铁自旋沿相反的方向旋转,这可能与螺旋磁性结构中的磁性手性有关。

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