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arXiv 1210.0967cond-mat.mtrl-sci
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硅酸盐四面体链扭曲驱动的铁电性

Ferroelectricity Driven by Twisting of Silicate Tetrahedral Chains

Hiroki Taniguchi, Akihide Kuwabara, Jungeun Kim, Younghun Kim, Hiroki Moriwake, Sungwng Kim, Takuya Hoshiyama, Tsukasa Koyama, Shigeo Mori, Masaki Takata, Hideo… 展开作者

Hiroki Taniguchi, Akihide Kuwabara, Jungeun Kim, Younghun Kim, Hiroki Moriwake, Sungwng Kim, Takuya Hoshiyama, Tsukasa Koyama, Shigeo Mori, Masaki Takata, Hideo Hosono, Yoshiyuki Inaguma, Mitsuru Itoh

摘要:

常规的钙钛矿型铁电体基于氧的八面体单元,并且通常包含有毒的Pb以实现稳健的铁电性。在这里,我们报告的铁电性的硅酸盐基化合物,Bi 2SiO 5(BSO),诱导相应的硅酸盐四面体链的结构不稳定性。低能声子模在~ 673 K时凝聚,引起适当的铁电相变。在BSO单晶中观察到极化开关,矫顽场为30 kV/cm,沿垂直于解理面的方向的自发极化为0.3 microC/cm 2。通过第一性原理计算估计面内偏振为23微C/cm 2。本研究结果为基于SiO 4四面体单元的铁电材料的设计提供了新的指导,SiO 4四面体单元广泛存在于天然矿物中。

英文摘要:

Conventional perovskite-type ferroelectrics are based on octahedral units of oxygen, and often comprise toxic Pb to achieve robust ferroelectricity. Here, we report the ferroelectricity in a silicate-based compound, Bi2SiO5 (BSO), induced by a structural instability of the corresponding silicate tetrahedral chains. A low-energy phonon mode condenses at ~ 673 K to induce the proper ferroelectric phase transition. Polarization switching was observed in a BSO single crystal with a coercive field of 30 kV/cm and a spontaneous polarization of 0.3 microC/cm2 along a direction normal to the cleavage plane. The in-plane polarization was estimated by first principles calculations to be 23 microC/cm2. The present findings provide a new guideline for designing ferroelectric materials based on SiO4 tetrahedral units, which is ubiquitously found in natural minerals.

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