Terrestrial planet formation constrained by mars and the structure of the asteroid belt

Detalhes bibliográficos
Autor(a) principal: Izidoro, André
Data de Publicação: 2015
Outros Autores: Raymond, Sean N., Morbidelli, Alessandro, Winter, Othon C. [UNESP]
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.
id UNSP_8e672f1bc3d4cce8b77b96daa522a209
oai_identifier_str oai:repositorio.unesp.br:11449/177633
network_acronym_str UNSP
network_name_str Repositório Institucional da UNESP
repository_id_str 2946
spelling 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