Terrestrial planet formation constrained by mars and the structure of the asteroid belt
Autor(a) principal: | |
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Data de Publicação: | 2015 |
Outros Autores: | , , |
Tipo de documento: | Artigo |
Idioma: | eng |
Título da fonte: | Repositório Institucional da UNESP |
Texto Completo: | http://dx.doi.org/10.1093/mnras/stv1835 http://hdl.handle.net/11449/177633 |
Resumo: | Reproducing the large Earth/Mars mass ratio requires a strong mass depletion in solids within the protoplanetary disc between 1 and 3 au. The Grand Tack model invokes a specific migration history of the giant planets to remove most of themass initially beyond 1 au and to dynamically excite the asteroid belt. However, one could also invoke a steep density gradient created by inward drift and pile-up of small particles induced by gas drag, as has been proposed to explain the formation of close-in super-Earths. Here we show that the asteroid belt's orbital excitation provides a crucial constraint against this scenario for the Solar system. We performed a series of simulations of terrestrial planet formation and asteroid belt evolution starting from discs of planetesimals and planetary embryos with various radial density gradients and including Jupiter and Saturn on nearly circular and coplanar orbits. Discs with shallow density gradients reproduce the dynamical excitation of the asteroid belt by gravitational self-stirring but form Mars analogues significantly more massive than the real planet. In contrast, a disc with a surface density gradient proportional to r-5.5 reproduces the Earth/Mars mass ratio but leaves the asteroid belt in a dynamical state that is far colder than the real belt. We conclude that no disc profile can simultaneously explain the structure of the terrestrial planets and asteroid belt. The asteroid belt must have been depleted and dynamically excited by a different mechanism such as, for instance, in the Grand Tack scenario. |
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Terrestrial planet formation constrained by mars and the structure of the asteroid beltMethods: numericalPlanets and satellites: formationReproducing the large Earth/Mars mass ratio requires a strong mass depletion in solids within the protoplanetary disc between 1 and 3 au. The Grand Tack model invokes a specific migration history of the giant planets to remove most of themass initially beyond 1 au and to dynamically excite the asteroid belt. However, one could also invoke a steep density gradient created by inward drift and pile-up of small particles induced by gas drag, as has been proposed to explain the formation of close-in super-Earths. Here we show that the asteroid belt's orbital excitation provides a crucial constraint against this scenario for the Solar system. We performed a series of simulations of terrestrial planet formation and asteroid belt evolution starting from discs of planetesimals and planetary embryos with various radial density gradients and including Jupiter and Saturn on nearly circular and coplanar orbits. Discs with shallow density gradients reproduce the dynamical excitation of the asteroid belt by gravitational self-stirring but form Mars analogues significantly more massive than the real planet. In contrast, a disc with a surface density gradient proportional to r-5.5 reproduces the Earth/Mars mass ratio but leaves the asteroid belt in a dynamical state that is far colder than the real belt. We conclude that no disc profile can simultaneously explain the structure of the terrestrial planets and asteroid belt. The asteroid belt must have been depleted and dynamically excited by a different mechanism such as, for instance, in the Grand Tack scenario.Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)Laboratoire d'Astrophysique de Bordeaux Université de Bordeaux UMR 5804Capes Foundation Ministry of Education of BrazilUniversity of Nice-Sophia Antipolis CNRS Observatoire de la Côte d'Azur Laboratoire Lagrange, BP 4229CNRS Laboratoire d'Astrophysique de Bordeaux UMR 5804UNESP Univ. Estadual Paulista - Grupo de Dinmica Orbital and Planetologia GuaratinguetáUNESP Univ. Estadual Paulista - Grupo de Dinmica Orbital and Planetologia GuaratinguetáUMR 5804Ministry of Education of BrazilLaboratoire LagrangeUniversidade Estadual Paulista (Unesp)Izidoro, AndréRaymond, Sean N.Morbidelli, AlessandroWinter, Othon C. [UNESP]2018-12-11T17:26:24Z2018-12-11T17:26:24Z2015-01-01info:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/article3619-3634application/pdfhttp://dx.doi.org/10.1093/mnras/stv1835Monthly Notices of the Royal Astronomical Society, v. 453, n. 4, p. 3619-3634, 2015.1365-29660035-8711http://hdl.handle.net/11449/17763310.1093/mnras/stv18352-s2.0-849495294252-s2.0-84949529425.pdfScopusreponame:Repositório Institucional da UNESPinstname:Universidade Estadual Paulista (UNESP)instacron:UNESPengMonthly Notices of the Royal Astronomical Society2,3462,346info:eu-repo/semantics/openAccess2024-07-02T14:29:19Zoai:repositorio.unesp.br:11449/177633Repositório InstitucionalPUBhttp://repositorio.unesp.br/oai/requestopendoar:29462024-08-05T18:06:28.155431Repositório Institucional da UNESP - Universidade Estadual Paulista (UNESP)false |
dc.title.none.fl_str_mv |
Terrestrial planet formation constrained by mars and the structure of the asteroid belt |
title |
Terrestrial planet formation constrained by mars and the structure of the asteroid belt |
spellingShingle |
Terrestrial planet formation constrained by mars and the structure of the asteroid belt Izidoro, André Methods: numerical Planets and satellites: formation |
title_short |
Terrestrial planet formation constrained by mars and the structure of the asteroid belt |
title_full |
Terrestrial planet formation constrained by mars and the structure of the asteroid belt |
title_fullStr |
Terrestrial planet formation constrained by mars and the structure of the asteroid belt |
title_full_unstemmed |
Terrestrial planet formation constrained by mars and the structure of the asteroid belt |
title_sort |
Terrestrial planet formation constrained by mars and the structure of the asteroid belt |
author |
Izidoro, André |
author_facet |
Izidoro, André Raymond, Sean N. Morbidelli, Alessandro Winter, Othon C. [UNESP] |
author_role |
author |
author2 |
Raymond, Sean N. Morbidelli, Alessandro Winter, Othon C. [UNESP] |
author2_role |
author author author |
dc.contributor.none.fl_str_mv |
UMR 5804 Ministry of Education of Brazil Laboratoire Lagrange Universidade Estadual Paulista (Unesp) |
dc.contributor.author.fl_str_mv |
Izidoro, André Raymond, Sean N. Morbidelli, Alessandro Winter, Othon C. [UNESP] |
dc.subject.por.fl_str_mv |
Methods: numerical Planets and satellites: formation |
topic |
Methods: numerical Planets and satellites: formation |
description |
Reproducing the large Earth/Mars mass ratio requires a strong mass depletion in solids within the protoplanetary disc between 1 and 3 au. The Grand Tack model invokes a specific migration history of the giant planets to remove most of themass initially beyond 1 au and to dynamically excite the asteroid belt. However, one could also invoke a steep density gradient created by inward drift and pile-up of small particles induced by gas drag, as has been proposed to explain the formation of close-in super-Earths. Here we show that the asteroid belt's orbital excitation provides a crucial constraint against this scenario for the Solar system. We performed a series of simulations of terrestrial planet formation and asteroid belt evolution starting from discs of planetesimals and planetary embryos with various radial density gradients and including Jupiter and Saturn on nearly circular and coplanar orbits. Discs with shallow density gradients reproduce the dynamical excitation of the asteroid belt by gravitational self-stirring but form Mars analogues significantly more massive than the real planet. In contrast, a disc with a surface density gradient proportional to r-5.5 reproduces the Earth/Mars mass ratio but leaves the asteroid belt in a dynamical state that is far colder than the real belt. We conclude that no disc profile can simultaneously explain the structure of the terrestrial planets and asteroid belt. The asteroid belt must have been depleted and dynamically excited by a different mechanism such as, for instance, in the Grand Tack scenario. |
publishDate |
2015 |
dc.date.none.fl_str_mv |
2015-01-01 2018-12-11T17:26:24Z 2018-12-11T17:26:24Z |
dc.type.status.fl_str_mv |
info:eu-repo/semantics/publishedVersion |
dc.type.driver.fl_str_mv |
info:eu-repo/semantics/article |
format |
article |
status_str |
publishedVersion |
dc.identifier.uri.fl_str_mv |
http://dx.doi.org/10.1093/mnras/stv1835 Monthly Notices of the Royal Astronomical Society, v. 453, n. 4, p. 3619-3634, 2015. 1365-2966 0035-8711 http://hdl.handle.net/11449/177633 10.1093/mnras/stv1835 2-s2.0-84949529425 2-s2.0-84949529425.pdf |
url |
http://dx.doi.org/10.1093/mnras/stv1835 http://hdl.handle.net/11449/177633 |
identifier_str_mv |
Monthly Notices of the Royal Astronomical Society, v. 453, n. 4, p. 3619-3634, 2015. 1365-2966 0035-8711 10.1093/mnras/stv1835 2-s2.0-84949529425 2-s2.0-84949529425.pdf |
dc.language.iso.fl_str_mv |
eng |
language |
eng |
dc.relation.none.fl_str_mv |
Monthly Notices of the Royal Astronomical Society 2,346 2,346 |
dc.rights.driver.fl_str_mv |
info:eu-repo/semantics/openAccess |
eu_rights_str_mv |
openAccess |
dc.format.none.fl_str_mv |
3619-3634 application/pdf |
dc.source.none.fl_str_mv |
Scopus reponame:Repositório Institucional da UNESP instname:Universidade Estadual Paulista (UNESP) instacron:UNESP |
instname_str |
Universidade Estadual Paulista (UNESP) |
instacron_str |
UNESP |
institution |
UNESP |
reponame_str |
Repositório Institucional da UNESP |
collection |
Repositório Institucional da UNESP |
repository.name.fl_str_mv |
Repositório Institucional da UNESP - Universidade Estadual Paulista (UNESP) |
repository.mail.fl_str_mv |
|
_version_ |
1808128895787991040 |