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Pressure-induced polymorphism and piezochromism in Mn_2FeSbO_6

机译:Mn_2FeSbO_6的压力诱导多态性和压致变色

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摘要

In the last decade, major efforts have been devoted to searching for polar magnets due to their vast potential applications in spintronic devices. However, the polar magnets are rare because of conflicting electronic configuration requirements of ferromagnetism and electric polarization. Double-perovskite oxides with a polar structure containing transition metal elements represent excellent candidates for the polar magnet design. Herein, the crystal structure evolution of Mn2FeSbO6 (MFSO) was investigated at pressures reaching similar to 50 GPa by in situ synchrotron X-ray diffraction (XRD), Raman scattering, and ab initio calculation techniques. The XRD results reveal ilmenite-to perovskite-type phase transition at around 35 GPa. An additional intermediate phase, observed in the range of 31-36 GPa by Raman spectroscopy, but not the XRD technique, is proposed to represent the polar LiNbO3 phase. It is argued that this phase emerged due to the heating effect of the Raman-excitation laser. The LiNbO3-type MFSO compounds, displaying an intrinsic dipole ordering, represent a promising candidate for multiferroic materials. The detected phase transitions were found to be reversible although a significant hysteresis was noticeable between compression and decompression runs. Moreover, a pressure-induced piezochromism, signifying a bandgap change, was discovered by the direct visual observations and corroborated by ab initio calculations. The present study benefits an efficient high-pressure synthesis of polar magnetic double-perovskite oxides in the future. Published under license by AIP Publishing.
机译:在过去的十年中,由于极性磁体在自旋电子设备中的巨大潜在应用,人们已经做出了巨大的努力来寻找极性磁体。但是,由于铁磁性和极化的电子配置要求相互矛盾,因此极磁体很少见。具有包含过渡金属元素的极性结构的双钙钛矿氧化物是极性磁体设计的极佳候选材料。本文中,通过原位同步加速器X射线衍射(XRD),拉曼散射和从头算技术,研究了Mn2FeSbO6(MFSO)在接近50 GPa压力下的晶体结构演变。 XRD结果显示钛铁矿到钙钛矿型相变在35 GPa左右。建议用拉曼光谱法在31-36 GPa的范围内观察到另一中间相,而不是XRD技术,以表示极性LiNbO3相。据认为,该阶段是由于拉曼激发激光器的加热作用而出现的。 LiNbO3型MFSO化合物显示出固有的偶极有序性,是多铁材料的有希望的候选者。尽管在压缩和减压运行之间存在明显的磁滞现象,但发现检测到的相变是可逆的。此外,通过直接的视觉观察发现了压力引起的压致变色,其表示带隙变化,并且通过从头算来得到证实。本研究有益于将来高效地高压合成极性磁性双钙钛矿氧化物。由AIP Publishing授权发布。

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  • 来源
    《Applied Physics Letters》 |2019年第16期|162903.1-162903.5|共5页
  • 作者单位

    Uppsala Univ, Dept Earth Sci, S-75236 Uppsala, Sweden;

    CAEP, Natl Key Lab Shock Wave & Detonat Phys, Inst Fluid Phys, Mianyang 621900, Sichuan, Peoples R China|NYU, Dept Chem, New York, NY 10003 USA;

    Chinese Acad Sci, Beijing Synchrotron Radiat Facil, Inst High Energy Phys, Beijing 100049, Peoples R China;

    Univ Hawaii Manoa, Partnership Extreme Crystallog, Honolulu, HI 96822 USA;

    Uppsala Univ, Dept Engn Sci, S-75121 Uppsala, Sweden;

    Uppsala Univ, Dept Engn Sci, S-75121 Uppsala, Sweden|Karpovs Inst Phys Chem, Dept Inorgan Mat, Moscow 105046, Russia;

    Swedish Museum Nat Hist, Dept Geosci, S-10405 Stockholm, Sweden;

    Uppsala Univ, Dept Earth Sci, S-75236 Uppsala, Sweden;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《生物学医学文摘》(MEDLINE);
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  • 正文语种 eng
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  • 入库时间 2022-08-18 04:18:11

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