Formation of ultrathin cobalt ferrite films by interdiffusion of Fe3O4/CoO bilayers
Autor(en): | Rodewald, J. Thien, J. Pohlmann, T. Hoppe, M. Timmer, F. Bertram, F. Kuepper, K. Wollschlaeger, J. |
Stichwörter: | ANODE MATERIAL; CATIONIC DISTRIBUTION; COFE2O4; FE; MAGNETIC-PROPERTIES; Materials Science; Materials Science, Multidisciplinary; OXIDE; PHOTOELECTRON ANGULAR-DISTRIBUTION; Physics; Physics, Applied; Physics, Condensed Matter; REFLECTION; THIN-FILMS; X-RAY-ABSORPTION | Erscheinungsdatum: | 2019 | Herausgeber: | AMER PHYSICAL SOC | Journal: | PHYSICAL REVIEW B | Volumen: | 100 | Ausgabe: | 15 | Zusammenfassung: | In this work an alternate pathway is demonstrated to form ultrathin cobalt ferrite (CoxFe3-xO4) films by interdiffusion of Fe3O4/CoO bilayers. Bilayer samples with different Fe3O4/CoO thickness ratios have been prepared by reactive molecular beam epitaxy on Nb-doped SrTiO3(001) substrates to obtain cobalt ferrite films of varied stoichiometry. Subsequently, oxygen-assisted postdeposition annealing experiments for consecutive temperature steps between 300 degrees C and 600 degrees C have been conducted monitoring the interdiffusion process by means of high-resolution x-ray reflectivity, soft and angle-resolved hard x-ray photoelectron, and x-ray absorption spectroscopy. Magnetic properties were characterized using superconducting quantum interference device magnetometry. The interdiffusion process starts from 300 degrees C annealing temperature and is completed for temperatures above 500 degrees C. For completely interdiffused films with Co:Fe ratios larger than 0.84:2 a thin segregated CoO layer on top of the ferrite is formed. This CoO segregation is attributed to surface and interface effects. In addition, multiplet calculations of x-ray absorption spectra are performed to determine the occupancy of different sublattices. These results are correlated with the magnetic properties of the ferrite films. A stoichiometric CoFe2O4 film with partial inversion has been formed exhibiting homogeneously distributed Co2+ and mainly Fe3+ valence states if the initial Co:Fe content is 1.09:2. Thus, for the formation of stoichiometric cobalt ferrite by the proposed postdeposition annealing technique an initial Co excess has to be provided as the formation of a top CoO layer is inevitable. |
ISSN: | 24699950 | DOI: | 10.1103/PhysRevB.100.155418 |
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geprüft am 13.05.2024