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dc.contributor.authorRodríguez-Mendoza, Ulises Ruymán
dc.contributor.authorLeón-Luís, Sergio Fabián
dc.contributor.authorMuñoz-Santiuste, Juan E Muñoz
dc.contributor.authorJaque García, Daniel 
dc.contributor.authorLavín, Víctor
dc.contributor.otherUAM. Departamento de Física de Materialeses_ES
dc.date.accessioned2014-10-06T07:42:12Z
dc.date.available2014-10-06T07:42:12Z
dc.date.issued2013-06-07
dc.identifier.citationJournal of Applied Physics 113.21 (2013): 213517en_US
dc.identifier.issn0021-8979 (print)es_ES
dc.identifier.issn1089-7550 (online)es_ES
dc.identifier.urihttp://hdl.handle.net/10486/662051
dc.descriptionThe following article appeared in Journal of Applied Physics 113.21 (2013): 213517 and may be found at http://scitation.aip.org/content/aip/journal/jap/113/21/10.1063/1.4809217en_US
dc.description.abstractA pressure-induced shift of the emission spectrum corresponding to the near infrared 4F3/2 → 4I9/2 transition of Nd3+ ions in a calcium gadolinium germanium garnet was obtained in the interval from ambient conditions up to 23 GPa in order to test its suitability as an optical pressure sensor. Although several Nd3+ non-equivalent centers are present in this garnet, which complicates the assignation of the optical transitions, the R1,R2 → Z5 transitions are unequivocally characterised and fit the requirements of an ideal optical pressure sensor. Results obtained for these emission peaks indicate large pressure coefficients of -8.8 and -10.8 cm -1 GPa-1; meanwhile, the rest of the R1,R 2 → Z1-4 emissions remain almost unchanged under pressure. This behaviour is ascribed to the influence of the crystal-field at high pressure on the Z5 Stark level of the ground state and can be easily reproduced exclusively by varying the cubic term of fourth rank of the crystal-field Hamiltonian, which accounts for the Nd3+ ions and is related to medium Nd3+-oxygen distances. These coefficients are larger than those found for the R-lines of Cr3+ in ruby, -7.56 cm-1 GPa-1, suggesting that this system may be a good candidate for a luminescence pressure sensor.en_US
dc.description.sponsorshipThis work has been partially supported by MICINN (MAT2010-21270-C04-02, The MALTA Consolider CSD2007-0045 and the National Program of Infrastructure), and by EU-FEDER funds. S. F. León-Luis also wishes to thank MICINN for the FPI Grant (BES-2008-003353).en_US
dc.format.extent8 pag.en
dc.format.mimetypeapplication/pdfen
dc.language.isoenges_ES
dc.publisherAmerican Institute of Physics.en_US
dc.relation.ispartofJournal of Applied Physicsen_US
dc.rights© 2013 AIP Publishing LLCen_US
dc.subject.otherGarneten_US
dc.subject.otherHigh pressureen_US
dc.subject.otherRare earth ionsen_US
dc.subject.otherLuminescenceen_US
dc.subject.otherPressure measurementen_US
dc.titleNd3+-doped Ca3Ga2Ge3O12 garnet: A new optical pressure sensoren_US
dc.typearticleen
dc.subject.ecienciaFísicaes_ES
dc.relation.publisherversionhttp://dx.doi.org/10.1063/1.4809217es_ES
dc.identifier.doi10.1063/1.4809217es_ES
dc.identifier.publicationfirstpage213517es_ES
dc.identifier.publicationissue21es_ES
dc.identifier.publicationlastpageundefinedes_ES
dc.identifier.publicationvolume113es_ES
dc.type.versioninfo:eu-repo/semantics/publishedVersiones_ES
dc.rights.accessRightsopenAccessen
dc.facultadUAMFacultad de Ciencias


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