Assessment of different formation scenarios for the ring system of (10199) Chariklo

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Campo DCValorIdioma
dc.contributorAstronomía y Astrofísicaes_ES
dc.contributor.authorMelita, Mario Daniel-
dc.contributor.authorDuffard, René-
dc.contributor.authorOrtiz Moreno, José Luis-
dc.contributor.authorCampo Bagatin, Adriano-
dc.contributor.otherUniversidad de Alicante. Departamento de Física, Ingeniería de Sistemas y Teoría de la Señales_ES
dc.contributor.otherUniversidad de Alicante. Instituto Universitario de Física Aplicada a las Ciencias y las Tecnologíases_ES
dc.date.accessioned2017-11-22T12:16:09Z-
dc.date.available2017-11-22T12:16:09Z-
dc.date.issued2017-05-30-
dc.identifier.citationAstronomy & Astrophysics. 2017, 602: A27. doi:10.1051/0004-6361/201629858es_ES
dc.identifier.issn0004-6361 (Print)-
dc.identifier.issn1432-0746 (Online)-
dc.identifier.urihttp://hdl.handle.net/10045/71408-
dc.description.abstractContext. The discovery that the Centaur (10199) Chariklo possesses a ring system opens questions about their origin. Aims. We here asses the plausibility of different scenarios for the origin of the observed ring system. Methods. We first consider the possibility that the material of the ring originated in the disruption of a satellite that had reached a critical distance from the Centaur. We discuss the conditions for the putative satellite to approach the Centaur as a consequence of tidal interaction. A three-body encounter is also considered as a transport mechanism. In addition, we study the case in which the ring is formed by the ejecta of a cratering collision on the Centaur and we constrain the collision parameters and the size of the resulting crater of the event. Finally, we consider that the ring material originates from a catastrophic collision between a background object and a satellite located at a distance corresponding to the current location of the ring. We compute the typical timescales for these scenarios. Results. We estimate that in order to be tidally disrupted a satellite would have had to be larger than approximately 6.5 km at the location of the rings. However the tidal interaction is rather weak for objects of the size of outer solar system bodies at the ring location, therefore we considered other more effective mechanisms by which a satellite might have approached the Centaur. Collisonal scenarios are both physically plausible for the formation, but semianalytical estimations indicate that the probability of the corresponding collisions is low under current conditions.es_ES
dc.description.sponsorshipR.D. acknowledges the support of MINECO for his Ramón y Cajal Contract. Funding from Spanish funding form grant AYA-2014-56637-C2-1-P is acknowledged, as is the Proyecto de Excelencia de la Junta de Andalucía, J. A. 2012-FQM1776. FEDER funds are also acknowledged. R.D. acknowledges the support of MINECO for his Ramon Cajal Contract. Funding from Spanish funding from grant AYA-2014-56637-C2-1-P is acknowledged, as is the Proyecto de Excelencia de la Junta de Andalucía, J. A. 2012- FQM1776. FEDER funds are also acknowledged. M.D.M. acknowledges the support of Min CyT ANPCyt PicT 1144/2013 and the support of the travel grant from CONICET and CSiC.es_ES
dc.languageenges_ES
dc.publisherEDP Scienceses_ES
dc.rights© ESO 2017es_ES
dc.subjectKuiper belt: generales_ES
dc.subjectMinor planets, asteroids: generales_ES
dc.subjectMinor planets, asteroids: individual: (10199) Charikloes_ES
dc.subject.otherFísica Aplicadaes_ES
dc.titleAssessment of different formation scenarios for the ring system of (10199) Charikloes_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.peerreviewedsies_ES
dc.identifier.doi10.1051/0004-6361/201629858-
dc.relation.publisherversionhttp://dx.doi.org/10.1051/0004-6361/201629858es_ES
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses_ES
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