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层状和岩盐有序 NaLnMnWO6(Ln = La,Nd,Tb)钙钛矿中不存在铁电极化。

The absence of ferroelectric polarization in layered and rock-salt ordered NaLnMnWO6 (Ln = La, Nd, Tb) perovskites.

机构信息

Chemistry and Physics of Materials Unit, Jawaharlal Nehru Centre for Advanced Scientific Research, Jakkur P.O., Bangalore 560 064, India.

出版信息

Phys Chem Chem Phys. 2014 Mar 21;16(11):5407-11. doi: 10.1039/c3cp54776k.

Abstract

The ordered perovskites, NaLnMnWO6 (Ln = La, Nd, Tb), are reported to exhibit simultaneous ordering of A-site cations (Na and Ln) in layered arrangement and B-site cations (Mn and W) in rock salt structure. They have been shown to crystallize in a monoclinic structure with the polar space group P21. Based on density functional calculations and group theoretical analysis, it has recently been proposed that NaLaMnWO6 should be ferroelectric with a relatively large polarization (16 μC cm(-2)). Contrary to this prediction, our electrical measurements such as conventional P-E loop, Positive-Up and Negative-Down (PUND), piezoelectric response and Second Harmonic Generation (SHG) reveal the absence of ferroelectric polarization in NaLnMnWO6 (Ln = La, Nd, Tb). A dielectric anomaly is observed just below room temperature (∼270 K) for all the three compounds, which is related to the change in conductivity as revealed by temperature dependent ac and dc resistivity. A pyrocurrent peak is also observed at the same temperature. However, its origin cannot be attributed to a ferroelectric transition.

摘要

有序钙钛矿 NaLnMnWO6(Ln = La、Nd、Tb)被报道同时存在 A 位阳离子(Na 和 Ln)层状排列和 B 位阳离子(Mn 和 W)岩盐结构的有序化。它们已被证明结晶为具有极性质点群 P21 的单斜结构。基于密度泛函计算和群论分析,最近有人提出 NaLaMnWO6 应该具有铁电性,具有相对较大的极化(16 μC cm(-2))。与这一预测相反,我们的电测量,如常规 P-E 环、正向上和负向下(PUND)、压电响应和二次谐波产生(SHG),揭示了 NaLnMnWO6(Ln = La、Nd、Tb)中不存在铁电极化。所有三种化合物在室温以下(约 270 K)都观察到介电异常,这与通过温度相关的交流和直流电阻率揭示的电导率变化有关。在相同的温度下也观察到热释电流峰。然而,其起源不能归因于铁电转变。

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