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dc.contributor.authorDobrovolskiy, O. V.
dc.contributor.authorVovk, N. R.
dc.contributor.authorBondarenko, A. V.
dc.contributor.authorBunyaev, S. A.
dc.contributor.authorLamb-Camarena, S.
dc.contributor.authorZenbaa, N.
dc.contributor.authorSachser, R.
dc.contributor.authorBarth, S.
dc.contributor.authorGusliyenko, Kostyantyn
dc.contributor.authorChumak, A. V.
dc.contributor.authorHuth, M.
dc.contributor.authorKakazei, G. N.
dc.date.accessioned2021-09-08T11:01:12Z
dc.date.available2021-09-08T11:01:12Z
dc.date.issued2021-03-28
dc.identifier.citationApplied Physics Letters 118(13) : (2021) // Article ID 132405es_ES
dc.identifier.issn0003-6951
dc.identifier.issn1077-3118
dc.identifier.urihttp://hdl.handle.net/10810/52936
dc.description.abstractExtending nanostructures into the third dimension has become a major research avenue in modern magnetism, superconductivity, and spintronics, because of geometry-, curvature-, and topology-induced phenomena. Here, we introduce Co-Fe nanovolcanoes-nanodisks overlaid by nanorings-as purpose-engineered 3D architectures for nanomagnonics, fabricated by focused electron beam-induced deposition. We use both perpendicular spin-wave resonance measurements and micromagnetic simulations to demonstrate that the rings encircling the volcano craters harbor the highest-frequency eigenmodes, while the lower-frequency eigenmodes are concentrated within the volcano crater, due to the non-uniformity of the internal magnetic field. By varying the crater diameter, we demonstrate the deliberate tuning of higher-frequency eigenmodes without affecting the lowest-frequency mode. Thereby, the extension of 2D nanodisks into the third dimension allows one to engineer their lowest eigenfrequency by using 3D nanovolcanoes with 30% smaller footprints. The presented nanovolcanoes can be viewed as multi-mode microwave resonators and 3D building blocks for nanomagnonics.es_ES
dc.description.sponsorshipO.V.D. and S.L.C. acknowledge the Austrian Science Fund (FWF) for support through Grant No. I 4889 (CurviMag). The Portuguese team acknowledges the Network of Extreme Conditions Laboratories-NECL and the Portuguese Foundation of Science and Technology (FCT) support through Project Nos. NORTE-01-0145-FEDER-022096, PTDC/FIS-MAC/31302/2017, POCI-0145-FEDER-030085 (NOVAMAG), and EXPL/IF/00541/2015. N. Z. and A. V. C. acknowledge the Austrian Science Fund (FWF) for support through Grant No. I 4917. S. B. acknowledges funding by the) Deutsche Forschungsgemeinschaft (DFG through Grant Nos. BA 6595/2-1 and BA 6595/1-1. K. G. acknowledges support from IKERBASQUE (the Basque Foundation for Science). The work of K. G. was supported by the Spanish Ministry of Science and Innovation through Grant No. PID2019-108075RB-C33/AEI/10.13039/501100011033. M.H. acknowledges the DFG for support through Grant No. HU 752/16-1. Support through the Frankfurt Center of Electron Microscopy (FCEM) is gratefully acknowledged. Further, support of the European Cooperation in Science and Technology via COST Action No. CA16218 (NANOCOHYBRI) is acknowledged.es_ES
dc.language.isoenges_ES
dc.publisherAmerican Institute of Physicses_ES
dc.relationinfo:eu-repo/grantAgreement/MICINN/PID2019-108075RB-C33/AEI/10es_ES
dc.rightsinfo:eu-repo/semantics/openAccesses_ES
dc.rights.urihttp://creativecommons.org/licenses/by/3.0/es/*
dc.subjectdotes_ES
dc.titleSpin-wave eigenmodes in direct-write 3D nanovolcanoeses_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.rights.holder2021 Author(s). All article content, except where otherwise noted, is licensed under a Creative Commons Attribution (CC BY) license (http://creativecommons.org/licenses/by/4.0/).es_ES
dc.rights.holderAtribución 3.0 España*
dc.relation.publisherversionhttps://aip.scitation.org/doi/10.1063/5.0044325es_ES
dc.identifier.doi10.1063/5.0044325
dc.departamentoesPolímeros y Materiales Avanzados: Física, Química y Tecnologíaes_ES
dc.departamentoeuPolimero eta Material Aurreratuak: Fisika, Kimika eta Teknologiaes_ES


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2021 Author(s). All article content, except where otherwise noted, is licensed under a Creative Commons Attribution (CC BY) license (http://creativecommons.org/licenses/by/4.0/).
Except where otherwise noted, this item's license is described as 2021 Author(s). All article content, except where otherwise noted, is licensed under a Creative Commons Attribution (CC BY) license (http://creativecommons.org/licenses/by/4.0/).