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Morphological, structural and magnetic evolution of sputtered Fe70Ga30 thin films upon annealing in oxygen atmosphere

dc.contributor.authorBisero, D.
dc.contributor.authorFin, S.
dc.contributor.authorRanchal Sánchez, Rocío
dc.date.accessioned2023-06-17T22:05:57Z
dc.date.available2023-06-17T22:05:57Z
dc.date.issued2017
dc.description©2017 Elsevier B.V. All rights reserved. This work has been financially supported through the project MAT2015-66888-C3-3-R of the Spanish Ministry of Economy and Competitiveness (MINECO/FEDER). We thank “CAI Difracción de rayos-X” of UCM for the X-ray diffractometry measurements, “Centro Nacional de Microscopía” of UCM for EDS measuresuments and Instituto of Sistemas Optoelectrónicos y Microtecnología (ISOM) for using its facilities for the growth and magnetic characterization of the samples. We also want to thank BM25-Spline, the Spanish CRG at ESRF for providing beamtime.
dc.description.abstractWe report on the evolution of uncapped Fe_(70)Ga_(30) layers deposited by sputtering and post-growth annealed in oxygen atmosphere in a temperature range from 500 °C to 800 °C. We have investigated the morphology, structure and magnetic properties of films with a thickness of 200 nm deposited on Mo buffer layers on glass substrates. X-ray diffractometry shows a decrease of the lattice parameter up to 600 °C whereas a further increase of the temperature up to 800 °C promotes the transformation to Fe_2O_3. We have observed by x-ray absorption fine structure the partial oxidation of Ga and the formation of Ga aggregates at 600 °C. These aggregates form Ga-rich bubbles that can be observed on the sample surface from which Ga evaporates leaving a Ga-poor layer that is later oxidized into Fe_2O_3. The thermal treatment on oxygen atmosphere has also a clear impact on the magnetic properties of the layers. The uniaxial in-plane magnetic anisotropy of the as-grown film evolves to magnetic isotropy when annealed at 600 °C probably due to the segregation and formation of Ga-rich areas. After Ga evaporates from the sample, Fe is fully oxidized and only a weak ferromagnetism related to Fe_2O_3 is detected.
dc.description.departmentDepto. de Física de Materiales
dc.description.facultyFac. de Ciencias Físicas
dc.description.refereedTRUE
dc.description.sponsorshipMinisterio de Economía y Competitividad (MINECO)/FEDER
dc.description.statuspub
dc.eprint.idhttps://eprints.ucm.es/id/eprint/44594
dc.identifier.doi10.1016/j.jallcom.2017.04.158
dc.identifier.issn0925-8388
dc.identifier.officialurlhttp://dx.doi.org/10.1016/j.jallcom.2017.04.158
dc.identifier.relatedurlhttp://www.sciencedirect.com
dc.identifier.urihttps://hdl.handle.net/20.500.14352/18060
dc.journal.titleJournal of alloys and compounds
dc.language.isoeng
dc.page.final135
dc.page.initial129
dc.publisherElsevier Science SA
dc.relation.projectIDMAT2015-66888-C3-3-R
dc.rights.accessRightsopen access
dc.subject.cdu538.9
dc.subject.keywordSol-gel
dc.subject.keywordGaFeO_3
dc.subject.ucmFísica de materiales
dc.subject.ucmFísica del estado sólido
dc.subject.unesco2211 Física del Estado Sólido
dc.titleMorphological, structural and magnetic evolution of sputtered Fe70Ga30 thin films upon annealing in oxygen atmosphere
dc.typejournal article
dc.volume.number713
dspace.entity.typePublication
relation.isAuthorOfPublicationeca2c0e4-9357-4a13-a15b-35493ec315af
relation.isAuthorOfPublication.latestForDiscoveryeca2c0e4-9357-4a13-a15b-35493ec315af

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