Formation of ultrathin cobalt ferrite films by interdiffusion of Fe3O4/CoO bilayers

DC ElementWertSprache
dc.contributor.authorRodewald, J.
dc.contributor.authorThien, J.
dc.contributor.authorPohlmann, T.
dc.contributor.authorHoppe, M.
dc.contributor.authorTimmer, F.
dc.contributor.authorBertram, F.
dc.contributor.authorKuepper, K.
dc.contributor.authorWollschlaeger, J.
dc.date.accessioned2021-12-23T16:13:22Z-
dc.date.available2021-12-23T16:13:22Z-
dc.date.issued2019
dc.identifier.issn24699950
dc.identifier.urihttps://osnascholar.ub.uni-osnabrueck.de/handle/unios/10535-
dc.description.abstractIn 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.
dc.description.sponsorshipDeutsche Forschungsgemeinschaft (DFG)German Research Foundation (DFG) [KU2321/2-1, KU2321/6-1, WO533/20-1]; Financial support from the Deutsche Forschungsgemeinschaft (DFG under Grants No. KU2321/2-1, No. KU2321/6-1, and No. WO533/20-1) is gratefully acknowledged. We thank Diamond Light Source for giving access to beamlines I07 (SI15334-1) and I09 (SI15205-1) and for the great beamline support. Additionally, we would like to acknowledge the assistance at beamline P09 at PETRA III (I-20170258), DESY, where parts of this work were carried out.
dc.language.isoen
dc.publisherAMER PHYSICAL SOC
dc.relation.ispartofPHYSICAL REVIEW B
dc.subjectANODE MATERIAL
dc.subjectCATIONIC DISTRIBUTION
dc.subjectCOFE2O4
dc.subjectFE
dc.subjectMAGNETIC-PROPERTIES
dc.subjectMaterials Science
dc.subjectMaterials Science, Multidisciplinary
dc.subjectOXIDE
dc.subjectPHOTOELECTRON ANGULAR-DISTRIBUTION
dc.subjectPhysics
dc.subjectPhysics, Applied
dc.subjectPhysics, Condensed Matter
dc.subjectREFLECTION
dc.subjectTHIN-FILMS
dc.subjectX-RAY-ABSORPTION
dc.titleFormation of ultrathin cobalt ferrite films by interdiffusion of Fe3O4/CoO bilayers
dc.typejournal article
dc.identifier.doi10.1103/PhysRevB.100.155418
dc.identifier.isiISI:000490467600007
dc.description.volume100
dc.description.issue15
dc.contributor.orcid0000-0002-0426-3591
dc.identifier.eissn24699969
dc.publisher.placeONE PHYSICS ELLIPSE, COLLEGE PK, MD 20740-3844 USA
dcterms.isPartOf.abbreviationPhys. Rev. B
dcterms.oaStatushybrid
crisitem.author.deptFB 04 - Physik-
crisitem.author.deptUniversität Osnabrück-
crisitem.author.deptidfb04-
crisitem.author.orcid0000-0002-0426-3591-
crisitem.author.orcid0000-0001-9002-4118-
crisitem.author.parentorgUniversität Osnabrück-
crisitem.author.netidRoJa644-
crisitem.author.netidBeFl001-
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