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dc.contributor.authorMartins, Luiz Gustavo Pimenta
dc.contributor.authorMatos, Matheus J. S.
dc.contributor.authorPaschoal, Alexandre R.
dc.contributor.authorFreire, Paulo T. C.
dc.contributor.authorAndrade, Nadia F.
dc.contributor.authorAguiar, Acrísio L.
dc.contributor.authorKong, Jing
dc.contributor.authorNeves, Bernardo R. A.
dc.contributor.authorde Oliveira, Alan B.
dc.contributor.authorMazzoni, Mário S.C.
dc.contributor.authorFilho, Antonio G. Souza
dc.contributor.authorCançado, Luiz Gustavo
dc.date.accessioned2018-02-13T20:32:41Z
dc.date.available2018-02-13T20:32:41Z
dc.date.issued2017-07
dc.date.submitted2016-11
dc.identifier.issn2041-1723
dc.identifier.urihttp://hdl.handle.net/1721.1/113640
dc.description.abstractDespite the advanced stage of diamond thin-film technology, with applications ranging from superconductivity to biosensing, the realization of a stable and atomically thick two-dimensional diamond material, named here as diamondene, is still forthcoming. Adding to the outstanding properties of its bulk and thin-film counterparts, diamondene is predicted to be a ferromagnetic semiconductor with spin polarized bands. Here, we provide spectroscopic evidence for the formation of diamondene by performing Raman spectroscopy of double-layer graphene under high pressure. The results are explained in terms of a breakdown in the Kohn anomaly associated with the finite size of the remaining graphene sites surrounded by the diamondene matrix. Ab initio calculations and molecular dynamics simulations are employed to clarify the mechanism of diamondene formation, which requires two or more layers of graphene subjected to high pressures in the presence of specific chemical groups such as hydroxyl groups or hydrogens.en_US
dc.publisherNature Publishing Groupen_US
dc.relation.isversionofhttp://dx.doi.org/10.1038/S41467-017-00149-8en_US
dc.rightsCreative Commons Attribution 4.0 International Licenseen_US
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/en_US
dc.titleRaman evidence for pressure-induced formation of diamondeneen_US
dc.typeArticleen_US
dc.identifier.citationMartins, Luiz Gustavo Pimenta et al. “Raman Evidence for Pressure-Induced Formation of Diamondene.” Nature Communications 8, 1 (July 2017) © 2017 The Author(s)en_US
dc.contributor.departmentMassachusetts Institute of Technology. Department of Electrical Engineering and Computer Scienceen_US
dc.contributor.mitauthorKong, Jing
dc.relation.journalNature Communicationsen_US
dc.eprint.versionFinal published versionen_US
dc.type.urihttp://purl.org/eprint/type/JournalArticleen_US
eprint.statushttp://purl.org/eprint/status/PeerRevieweden_US
dc.date.updated2018-02-09T15:29:49Z
dspace.orderedauthorsMartins, Luiz Gustavo Pimenta; Matos, Matheus J. S.; Paschoal, Alexandre R.; Freire, Paulo T. C.; Andrade, Nadia F.; Aguiar, Acrísio L.; Kong, Jing; Neves, Bernardo R. A.; de Oliveira, Alan B.; Mazzoni, Mário S.C.; Filho, Antonio G. Souza; Cançado, Luiz Gustavoen_US
dspace.embargo.termsNen_US
dc.identifier.orcidhttps://orcid.org/0000-0003-0551-1208
mit.licensePUBLISHER_POLICYen_US


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