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Magnetic field-induced ferroelectric switching in multiferroic aurivillius phase thin films at room temperature

机译:室温下多铁铁相薄膜中的磁场感应铁电转换

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摘要

Single-phase multiferroic materials are of considerable interest for future memory and sensing applications. Thin films of Aurivillius phase Bi 7Ti3Fe3O21 and Bi6Ti 2.8Fe1.52Mn0.68O18 (possessing six and five perovskite units per half-cell, respectively) have been prepared by chemical solution deposition on c-plane sapphire. Superconducting quantum interference device magnetometry reveal Bi7Ti3Fe 3O21 to be antiferromagnetic (TN = 190 K) and weakly ferromagnetic below 35 K, however, Bi6Ti2.8Fe 1.52Mn0.68O18 gives a distinct room-temperature in-plane ferromagnetic signature (Ms = 0.74 emu/g, μ0Hc =7 mT). Microstructural analysis, coupled with the use of a statistical analysis of the data, allows us to conclude that ferromagnetism does not originate from second phase inclusions, with a confidence level of 99.5%. Piezoresponse force microscopy (PFM) demonstrates room-temperature ferroelectricity in both films, whereas PFM observations on Bi6Ti2.8Fe1.52Mn0.68O18 show Aurivillius grains undergo ferroelectric domain polarization switching induced by an applied magnetic field. Here, we show for the first time that Bi6Ti2.8Fe1.52Mn0.68O18 thin films are both ferroelectric and ferromagnetic and, demonstrate magnetic field-induced switching of ferroelectric polarization in individual Aurivillius phase grains at room temperature.
机译:单相多铁性材料对于未来的存储器和传感应用非常感兴趣。通过在c面蓝宝石上化学溶液沉积,制备了Aurivillius相Bi 7Ti3Fe3O21和Bi6Ti 2.8Fe1.52Mn0.68O18相(每个半电池分别具有六个和五个钙钛矿单元)的薄膜。超导量子干涉装置的磁力分析表明Bi7Ti3Fe 3O21具有反铁磁性(TN = 190 K),在35 K以下具有弱铁磁性,但是Bi6Ti2.8Fe 1.52Mn0.68O18具有明显的室温面内铁磁特征(Ms = 0.74 emu / g,μHc= 7 mT)。微观结构分析以及对数据的统计分析的使用使我们可以得出结论,铁磁性不是第二相夹杂物引起的,置信度为99.5%。压电响应显微镜(PFM)在两张膜中均显示出室温铁电性,而Bi6Ti2.8Fe1.52Mn0.68O18上的PFM观察结果表明,Aurivillius晶粒经历了外加磁场引起的铁电畴极化转换。在这里,我们首次显示Bi6Ti2.8Fe1.52Mn0.68O18薄膜既是铁电薄膜又是铁磁薄膜,并展示了室温下磁场诱导的单个Aurivillius相晶粒中铁电极化的转换。

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