MBE growth and magnetic properties of epitaxial FeMn2O4 film on MgO(100)

  • Duong, Van Thiet (Department of Physics and Energy Harvest Storage Research Center, University of Ulsan) ;
  • Nguyen, Thi Minh Hai (Department of Physics and Energy Harvest Storage Research Center, University of Ulsan) ;
  • Nguyen, Anh Phuong (Department of Physics and Energy Harvest Storage Research Center, University of Ulsan) ;
  • Dang, Duc Dung (Department of Physics and Energy Harvest Storage Research Center, University of Ulsan) ;
  • Duong, Anh Tuan (Department of Physics and Energy Harvest Storage Research Center, University of Ulsan) ;
  • Nguyen, Van Quang (Department of Physics and Energy Harvest Storage Research Center, University of Ulsan) ;
  • Cho, Sunglae (Department of Physics and Energy Harvest Storage Research Center, University of Ulsan)
  • 발행 : 2016.02.17

초록

FeM2X4 spinel structures, where M is a transition metal and X is oxygen or sulfur, are candidate materials for spin filters, one of the key devices in spintronics. Both the Fe and M ions can occupy tetrahedral and octahedral sites; therefore, these types of compounds can display various physical and chemical properties [1]. On the other hand, the electronic and magnetic properties of these spinel structures could be modified via the control of cation distribution [2, 3]. Among the spinel oxides, iron manganese oxide is one of promising materials for applications. FeMn2O4 shows inverse spinel structure above 390 K and ferrimagnetic properties below the temperature [4]. In this work, we report on the structural and magnetic properties of epitaxial FeMn2O4 thin film on MgO(100) substrate. The reflection high energy electron diffraction (RHEED) and X-ray diffraction (XRD) results indicated that films were epitaxially grown on MgO(100) without the impurity phases. The valance states of Fe and Mn in the FeMn2O4 film were carried out using x-ray photoelectron spectrometer (XPS). The magnetic properties were measured by vibrating sample magnetometer (VSM), indicating that the samples are ferromagnetic at room temperature. The structural detail and origin of magnetic ordering in FeMn2O4 will be discussed.

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