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Magnetic characterization and electrical field-induced switching of magnetite thin films synthesized by atomic layer deposition and subsequent thermal reduction

机译:通过原子层沉积和随后的热还原合成的磁铁矿薄膜的磁性表征和电场感应转换

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Magnetite (Fe3O4) of high quality was prepared by combining atomic layer deposition (ALD) with a subsequent thermal reduction process. The reduction process in hydrogen atmosphere was investigated by in situ x-ray diffraction studies as a function of temperature. A complete reduction to Fe3O4 was confirmed within a narrow temperature window during the thermal treatment. Magnetic characterization of magnetite thin films as a function of temperature, applied magnetic field and magnetic field orientation were performed. The highly stoichiometry-and impurity-sensitive Verwey transition was observed in magnetic and electrical measurements. Moreover, the isotropic point at which the magnetocrystalline anisotropy of magnetite vanishes was unveiled. Both findings prove, first, the formation of the magnetite phase against the undesired maghemite and, second, the quality of the ALD thin films to be comparable with samples grown by molecular beam epitaxy. The magnetic easy and hard axis could be found to be in-plane and out-of-plane, respectively. Consistent with angular-dependent studies of the coercive field, additionally performed first-order reversal curve measurements revealed a complex micromagnetic structure with different magnetization reversal paths for both configurations. Finally, electric field-induced resistive switching was studied in detail being in perfect agreement with results of single-crystalline samples. The presented data and its analysis support the assumption of previous works of the magnetization reversal in magnetite nanotubes, suggest improvement for future magnetization studies of nanostructures by exploiting the isotropic point and might open new paths for low-cost resistive switching devices.
机译:通过将原子层沉积(ALD)与随后的热还原工艺相结合,可以制备出高质量的磁铁矿(Fe3O4)。通过原位x射线衍射研究了氢气氛中还原过程与温度的关系。在热处理过程中,在狭窄的温度范围内证实了Fe3O4的完全还原。磁铁矿薄膜的磁特性随温度,外加磁场和磁场取向而变化。在磁和电测量中观察到高度化学计量和杂质敏感的Verwey跃迁。此外,揭示了磁铁矿的磁晶各向异性消失的各向同性点。两项发现都证明,首先,磁铁矿相相对于不需要的磁赤铁矿形成,其次,ALD薄膜的质量可与分子束外延生长的样品相媲美。磁易轴和硬轴分别位于平面内和平面外。与矫顽场的角度相关研究一致,另外执行的一阶反转曲线测量显示了两种配置都具有不同磁化反转路径的复杂微磁结构。最后,详细研究了与单晶样品结果完全一致的电场感应电阻开关。提出的数据及其分析支持了磁铁矿纳米管中磁化反转先前工作的假设,建议通过利用各向同性点来改进纳米结构的未来磁化研究,并可能为低成本电阻式开关器件开辟新的道路。

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