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The detailed chemical composition of the terrestrial planet host Kepler-10

dc.contributor.authorLiu, Fan
dc.contributor.authorYong, David
dc.contributor.authorAsplund, Martin
dc.contributor.authorRamirez, I
dc.contributor.authorMelendez, Jorge
dc.contributor.authorGustafsson, B
dc.contributor.authorHowes, Louise
dc.contributor.authorRoederer, Ian U.
dc.contributor.authorLambert, D.L.
dc.contributor.authorBensby, T
dc.date.accessioned2018-11-29T22:53:49Z
dc.date.available2018-11-29T22:53:49Z
dc.date.issued2016
dc.date.updated2018-11-29T07:55:26Z
dc.description.abstractChemical abundance studies of the Sun and solar twins have demonstrated that the solar composition of refractory elements is depleted when compared to volatile elements, which could be due to the formation of terrestrial planets. In order to further examine this scenario, we conducted a line-by-line differential chemical abundance analysis of the terrestrial planet host Kepler-10 and 14 of its stellar twins. Stellar parameters and elemental abundances of Kepler-10 and its stellar twins were obtained with very high precision using a strictly differential analysis of high quality Canada–France–Hawaii Telescope, Hobby–Eberly Telescope and Magellan spectra. When compared to the majority of thick disc twins, Kepler-10 shows a depletion in the refractory elements relative to the volatile elements, which could be due to the formation of terrestrial planets in the Kepler-10 system. The average abundance pattern corresponds to ∼13 Earth masses, while the two known planets in Kepler-10 system have a combined ∼20 Earth masses. For two of the eight thick disc twins, however, no depletion patterns are found. Although our results demonstrate that several factors [e.g. planet signature, stellar age, stellar birth location and Galactic chemical evolution (GCE)] could lead to or affect abundance trends with condensation temperature, we find that the trends give further support for the planetary signature hypothesis.
dc.format.mimetypeapplication/pdfen_AU
dc.identifier.issn0035-8711
dc.identifier.urihttp://hdl.handle.net/1885/152582
dc.publisherBlackwell Publishing Ltd
dc.sourceMonthly Notices of the Royal Astronomical Society
dc.titleThe detailed chemical composition of the terrestrial planet host Kepler-10
dc.typeJournal article
dcterms.accessRightsOpen Accessen_AU
local.bibliographicCitation.issue3
local.bibliographicCitation.lastpage2646
local.bibliographicCitation.startpage2636
local.contributor.affiliationLiu, Fan, College of Science, ANU
local.contributor.affiliationYong, David, College of Science, ANU
local.contributor.affiliationAsplund, Martin, College of Science, ANU
local.contributor.affiliationRamirez, I, University of Texas at Austin
local.contributor.affiliationMelendez, Jorge, University of Sao Paulo
local.contributor.affiliationGustafsson, B, Uppsala University
local.contributor.affiliationHowes, Louise, College of Science, ANU
local.contributor.affiliationRoederer, Ian U., University of Michigan
local.contributor.affiliationLambert, D.L., University of Texas
local.contributor.affiliationBensby, T, Lund Observatory
local.contributor.authoruidLiu, Fan, u5217070
local.contributor.authoruidYong, David, u3207952
local.contributor.authoruidAsplund, Martin, u4042723
local.contributor.authoruidHowes, Louise, u5092438
local.description.notesImported from ARIES
local.identifier.absfor020100 - ASTRONOMICAL AND SPACE SCIENCES
local.identifier.absseo970102 - Expanding Knowledge in the Physical Sciences
local.identifier.ariespublicationu4571891xPUB35
local.identifier.citationvolume456
local.identifier.doi10.1093/mnras/stv2821
local.identifier.scopusID2-s2.0-84963786309
local.identifier.thomsonID000372265200026
local.type.statusPublished Version

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