Epitaxially stabilized thin films of ε-Fe2O3 (001) grown on YSZ (100)

• Published in: Scientific reports Vol. 7; no. 1; pp. 1 - 9
• Main Authors: Corbellini, Luca, Lacroix, Christian, Harnagea, Catalin, Korinek, Andreas, Botton, Gianluigi A., Ménard, David, Pignolet, Alain
• Format: Journal Article
• Language: English
• Published: London Nature Publishing Group UK 16.06.2017; Nature Publishing Group; Nature Portfolio
• Subjects: 639/301/1005/1008; 639/301/119/997; 639/301/357/537; 639/301/357/997; 639/925/357/997; Anisotropy; Crystal structure; Electron microscopy; Humanities and Social Sciences; Magnetic properties; Magnetism; Magnetite; multidisciplinary; Nanoparticles; Science; Science (multidisciplinary); Thin films; Transmission electron microscopy; Yttrium; Zirconia
• ISSN: 2045-2322; 2045-2322
• DOI: 10.1038/s41598-017-02742-9

Epsilon ferrite (ε-Fe 2 O 3 ) is a metastable phase of iron(III) oxide, intermediate between maghemite and hematite. It has recently attracted interest because of its magnetocrystalline anisotropy, which distinguishes it from the other polymorphs, and results in a gigantic coercive field and a natural ferromagnetic resonance frequency in the THz range. Moreover, it possesses a polar crystal structure, making it a potential ferroelectric, hence a potential multiferroic. Due to the need of size confinement to stabilize the metastable phase, ε-Fe 2 O 3 has been synthesized mainly as nanoparticles. However, to favor integration in devices, and take advantage of its unique functional properties, synthesis as epitaxial thin films is desirable. In this paper, we report the growth of ε-Fe 2 O 3 as epitaxial thin films on (100)-oriented yttrium-stabilized zirconia substrates. Structural characterization outlined the formation of multiple in-plane twins, with two different epitaxial relations to the substrate. Transmission electron microscopy showed how such twins develop in a pillar-like structure from the interface to the surface. Magnetic characterization confirmed the high magnetocrystalline anisotropy of our film and revealed the presence of a secondary phase which was identified as the well-known magnetite. Finally, angular analysis of the magnetic properties revealed how the presence of twins impacts their azimuthal dependence.