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Mode coupling between nonpolar and polar phonons as the origin of improper ferroelectricity in hexagonal LuMnO3

机译:非极性和极性声子之间的模式耦合是六角型LuMnO3中铁电不当的起源

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摘要

Currently, the most puzzling problem associated with the hexagonal LuMnO3 (h-LMO) is a large temperature-gap between the structural phase transition to the polar P63cm phase at ~1290 K and the emergence of the spontaneous polarization at a substantially reduced temperature, ~750 K. Interestingly, this large temperature-gap is not limited to h-LMO but is a universal phenomenon valid for other rare-earth manganites. We have examined this important issue by exploiting first-principles calculations. It is shown that the structural phase transition to the polar P63cm phase from the nonpolar P63/mmc phase of h-LMO is mediated by the freezing-in of the zone-boundary K3 phonon. However, the ferroelectric polarization remains at a negligibly small value until the amplitude of the K3 phonon reaches a certain critical value above which the coupling of the polar Γ2~- mode with the nonpolar K3 mode is practically turned on. This coupling-induced polarization explains the observed temperature-gap in h-LMO as well as other rare-earth manganites.
机译:目前,与六方六方锰氧化物(h-LMO)相关的最令人困惑的问题是结构相变在〜1290 K时转变为极性P63cm相与在大幅降低的温度下出现自发极化之间存在较大的温度差。 750K。有趣的是,这种较大的温度差不仅限于h-LMO,而且是普遍现象,适用于其他稀土锰矿。我们已经通过利用第一性原理计算来研究了这个重要问题。结果表明,h-LMO的结构相从非极性P63 / mmc相转变为极性P63cm相是由区域边界K3声子的冻结所介导的。然而,铁电极化保持在可以忽略的较小值,直到K3声子的振幅达到某个临界值为止,在该临界值之上,极性Γ2〜-模式与非极性K3模式的耦合实际上被打开。这种耦合引起的极化解释了在h-LMO和其他稀土锰矿中观察到的温度差。

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