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首页> 外文期刊>Materials & design >Novel multiferroic (Pb-1 (-) Nd-3x/2(x))(Ti-0.98 (-) yFeyMn0.02)O-3 ceramics with coexisting ferroelectricity and ferromagnetism at ambient temperature
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Novel multiferroic (Pb-1 (-) Nd-3x/2(x))(Ti-0.98 (-) yFeyMn0.02)O-3 ceramics with coexisting ferroelectricity and ferromagnetism at ambient temperature

机译:在环境温度下同时具有铁电和铁磁性的新型多铁(Pb-1(-)Nd-3x / 2(x))(Ti-0.98(-)yFeyMn0.02)O-3陶瓷

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摘要

We report the evolution of structural, dielectric, ferroelectric and ferromagnetic properties in novel (Pb1 - 3x/2Ndx) (Ti0.98 - yFeyMn0.02)O-3 perovskite ceramics (x = 0.08, 0 < y < 0.05). We found room-temperature ferroelectric polarization and ferromagnetism for higher amount of iron ions(y >= 0.04). The paraelectric-ferroelectric phase transition occurred between 650 and 670 K for 0 <= y <= 0.05. Ferromagnetic hysteresis was measured at different temperatures on samples with y >= 0.04. Detailed structural analysis evidenced the variation of unit cell parameters with y increasing, confirming the substitution of the iron element in the lattice. Fe-57 Mtissbauer spectroscopy evidenced that iron ions occupy Ti positions in the perovskite lattice, with the oxidation state Fe3+ and two coordination types. X-ray photoelectron spectroscopy confirmed the presence of iron only as Fe3+ and, moreover, evidenced the presence of a substantial amount of Ti3+ ions in the structure. The presence of both Fe3+ (spin 5/2) in different coordinations as well as Ti3+ (spin 1/2) magnetic ions in B-site positions drives the occurrence of magnetic properties from low temperature to above room temperature, through superexchange Fe3+-O-Fe3+, Fe3+-O-Ti3+ and Ti3+-O-Ti3+ interactions. The finding of coexistent ferroelectric and ferromagnetic properties in these compounds ground the route to facile synthesis of multiferroics by simply doping a classical perovskite ferroelectric material like PbTiO3 with an adequate amount of transition magnetic ions. (C) 2016 Elsevier Ltd. All rights reserved.
机译:我们报告了新型(Pb1-3-2x / 2Ndx)(Ti0.98-yFeyMn0.02)O-3钙钛矿陶瓷(x = 0.08,0 = 0.04)。当0 <= y <= 0.05时,顺电-铁电相变发生在650和670 K之间。在不同的温度下,对y> = 0.04的样品测量铁磁磁滞。详细的结构分析表明,晶胞参数随y的增加而变化,从而确认了晶格中铁元素的替代。 Fe-57 Mtissbauer光谱表明,铁离子占据钙钛矿晶格中的Ti位置,具有氧化态Fe3 +和两种配位类型。 X射线光电子能谱法证实了铁仅以Fe3 +的形式存在,而且证明了结构中存在大量的Ti3 +离子。 B位置的Fe3 +(自旋5/2)和Ti3 +(自旋1/2)磁性离子的存在通过超交换Fe3 + -O促使磁性从低温到高于室温的发生。 -Fe3 +,Fe3 + -O-Ti3 +和Ti3 + -O-Ti3 +相互作用。在这些化合物中共存的铁电和铁磁特性的发现,通过简单地向传统的钙钛矿铁电材料(如PbTiO3)中掺入适量的过渡磁性离子,便为多铁化合物的合成提供了便利。 (C)2016 Elsevier Ltd.保留所有权利。

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  • 来源
    《Materials & design》 |2016年第15期|693-704|共12页
  • 作者单位

    CNR, Ist Sistemi Complessi, Area Ric Roma Tor Vergata, Via Fosso Cavaliere 100, I-00133 Rome, Italy;

    Natl Inst Mat Phys, Str Atomistilor 105 Bis, RO-07125 Magurele, Romania;

    Romanian Acad, Inst Phys Chem, Spl Independentei 202, Bucharest 060021, Romania;

    Romanian Acad, Inst Phys Chem, Spl Independentei 202, Bucharest 060021, Romania;

    Romanian Acad, Inst Phys Chem, Spl Independentei 202, Bucharest 060021, Romania;

    Romanian Acad, Inst Phys Chem, Spl Independentei 202, Bucharest 060021, Romania;

    Natl Inst Mat Phys, Str Atomistilor 105 Bis, RO-07125 Magurele, Romania;

    Natl Inst Mat Phys, Str Atomistilor 105 Bis, RO-07125 Magurele, Romania;

    Natl Inst Mat Phys, Str Atomistilor 105 Bis, RO-07125 Magurele, Romania;

    CNR, ISTEC, Ist Sci & Tecnol Mat Ceramici, Via Granarolo 64, I-48018 Faenza, Italy;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Multiferroics; Dielectric properties; Magnetic properties; Ferroelectric ceramics; Dilute magnetic systems;

    机译:多铁;介电性能;磁性;铁电陶瓷;稀磁系统;

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