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Structural domain walls in polar hexagonalmanganites

机译:极性六方锰矿中的结构畴壁

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The domain structure in the multiferroic hexagonal manganites, h-RMnO3 (R Sc, Y, Dy-Lu),is currently intensely investigated, motivated by the observation of nanoscale electricalconductivity at the domain walls and intriguing sixfold topological defects at their meetingpoints, as well as reports of coupling between ferroelectricity, magnetism and structuralantiphase domains. The detailed structure of the domain walls, as well as the origin of suchcouplings, however, was previously unknown. Here we use first-principles electronic structurecalculations to elucidate the structure and properties of the structural domain walls inthe hexagonal manganites. Our results allow us to explain why ferroelectric domain wallsare always simultaneously antiphase walls, propose a mechanism for ferroelectric switchingthrough domain-wall motion, suggest a structure for the observed sixfold topological defectsand predict a topological protection of experimentally observed stripe domains in hexagonalmanganites.
机译:目前,由于在畴壁处观察到纳米级电导率并在其汇合点产生了六倍的拓扑缺陷,因此对六方锰铁矿h-RMnO3(R Sc,Y,Dy-Lu)中的畴结构进行了深入研究。作为铁电,磁性和结构反相域之间耦合的报告。但是,畴壁的详细结构以及这种耦合的起源以前是未知的。在这里,我们使用第一性原理电子结构计算来阐明六角锰矿中结构域壁的结构和性质。我们的结果使我们能够解释为什么铁电畴壁总是同时为反相壁,提出了通过畴壁运动进行铁电转换的机制,提出了所观察到的六重拓扑缺陷的结构,并预测了实验观察到的六方锰矿中的条形畴的拓扑保护。

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