Show simple item record

hal.structure.identifierASP 2024
dc.contributor.authorCAVALIÉ, Thibault
hal.structure.identifierCornell University [Ithaca] [CU]
dc.contributor.authorLUNINE, Jonathan
hal.structure.identifierLaboratoire d'Astrophysique de Marseille [LAM]
dc.contributor.authorMOUSIS, Olivier
hal.structure.identifierUniversidad del Pais Vasco / Euskal Herriko Unibertsitatea [Espagne] [UPV/EHU]
dc.contributor.authorHUESO, Ricardo
dc.date.accessioned2024-07-11T02:09:05Z
dc.date.available2024-07-11T02:09:05Z
dc.date.issued2024
dc.identifier.issn0038-6308
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/200828
dc.description.abstractEnDeep elemental composition is a challenging measurement to achieve in the giant planets of the solar system. Yet, knowledge of the deep composition offers important insights in the internal structure of these planets, their evolutionary history and their formation scenarios. A key element whose deep abundance is difficult to obtain is oxygen, because of its propensity for being in condensed phases such as rocks and ices. In the atmospheres of the giant planets, oxygen is largely stored in water molecules that condense below the observable levels. At atmospheric levels that can be investigated with remote sensing, water abundance can modify the observed meteorology, and meteorological phenomena can distribute water through the atmosphere in complex ways that are not well understood and that encompass deeper portions of the atmosphere. The deep oxygen abundance provides constraints on the connection between atmosphere and interior and on the processes by which other elements were trapped, making its determination an important element to understand giant planets. In this paper, we review the current constraints on the deep oxygen abundance of the giant planets, as derived from observations and thermochemical models.
dc.language.isoen
dc.publisherSpringer Verlag
dc.subject.enUranus
dc.subject.enNeptune
dc.subject.enIce giants
dc.subject.enComposition
dc.subject.enFormation
dc.title.enThe Deep Oxygen Abundance in Solar System Giant Planets, with a New Derivation for Saturn
dc.typeArticle de revue
dc.identifier.doi10.1007/s11214-024-01045-6
dc.subject.halPlanète et Univers [physics]/Astrophysique [astro-ph]/Planétologie et astrophysique de la terre [astro-ph.EP]
bordeaux.journalSpace Science Reviews
bordeaux.page8
bordeaux.volume220
bordeaux.hal.laboratoriesLaboratoire d'Astrophysique de Bordeaux (LAB) - UMR 5804*
bordeaux.issue1
bordeaux.institutionUniversité de Bordeaux
bordeaux.institutionCNRS
bordeaux.peerReviewedoui
hal.identifierhal-04643051
hal.version1
hal.popularnon
hal.audienceInternationale
hal.origin.linkhttps://hal.archives-ouvertes.fr//hal-04643051v1
bordeaux.COinSctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=Space%20Science%20Reviews&rft.date=2024&rft.volume=220&rft.issue=1&rft.spage=8&rft.epage=8&rft.eissn=0038-6308&rft.issn=0038-6308&rft.au=CAVALI%C3%89,%20Thibault&LUNINE,%20Jonathan&MOUSIS,%20Olivier&HUESO,%20Ricardo&rft.genre=article


Files in this item

FilesSizeFormatView

There are no files associated with this item.

This item appears in the following Collection(s)

Show simple item record