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Asteroids were born bigger: An implication of surface mass ablation during gas-assisted implantation into the asteroid belt

dc.contributor.authorRibeiro de Sousa, Rafael [UNESP]
dc.contributor.authorIzidoro, Andre
dc.contributor.authorDeienno, Rogerio
dc.contributor.authorDasgupta, Rajdeep
dc.contributor.institutionUniversidade Estadual Paulista (UNESP)
dc.contributor.institutionRice University
dc.contributor.institutionSouthwest Research Institute
dc.date.accessioned2025-04-29T18:50:09Z
dc.date.issued2024-03-01
dc.description.abstractThe origins of carbonaceous asteroids in the asteroid belt is not fully understood. The leading hypothesis is that they were not born at their current location but instead implanted into the asteroid belt early in the Solar System history. In this study, we investigate how the migration and growth of Jupiter and Saturn in their natal disk impact nearby planetesimals and subsequent planetesimal implantation into the asteroid belt. Unlike traditional studies, we account for the effects of surface ablation of planetesimals caused by thermal and frictional heating between the gas-disk medium and planetesimal surface, when planetesimals travel through the gas disk. We have performed simulations considering planetesimals of different compositions as water-ice rich planetesimals (composed of more than 80% water by mass), water-ice poor planetesimals (relatively dry and enstatite-like), organic-rich planetesimals, and fayalite-rich planetesimals. Our findings indicate that, regardless of the migration history of the giant planets, water-ice rich, organic-rich, and fayalite-rich planetesimals implanted into the asteroid belt generally experience surface ablation during implantation in the asteroid belt, shrinking in size. On the other hand, planetesimals with enstatite-like compositions were inconsequential to surface ablation, preserving their original sizes. By assuming an initial planetesimal size-frequency distribution (SFD), our results show that – under the effects of surface ablation – the planetesimal population implanted into the asteroid belt shows a SFD slope slightly steeper than that of the initial one. This holds true for all migration histories of the giant planets considered in this work, but for the Grand-Tack model where the SFD slope remains broadly unchanged. Altogether, our results suggest that the largest C-type asteroids in the asteroid belt may have been born bigger. High-degree surface ablation during implantation into the asteroid belt may have even exposed the cores of early differentiated C-type planetesimals.en
dc.description.affiliationSão Paulo State University UNESP, Campus of Guaratinguetá, Av. Dr. Ariberto Pereira da Cunha, 333 - Pedregulho
dc.description.affiliationDepartment of Earth Environmental and Planetary Sciences 6100 Main MS 126 Rice University
dc.description.affiliationSouthwest Research Institute, 1050 Walnut St., Suite 300
dc.description.affiliationUnespSão Paulo State University UNESP, Campus of Guaratinguetá, Av. Dr. Ariberto Pereira da Cunha, 333 - Pedregulho
dc.identifierhttp://dx.doi.org/10.1016/j.icarus.2023.115910
dc.identifier.citationIcarus, v. 410.
dc.identifier.doi10.1016/j.icarus.2023.115910
dc.identifier.issn1090-2643
dc.identifier.issn0019-1035
dc.identifier.scopus2-s2.0-85179481774
dc.identifier.urihttps://hdl.handle.net/11449/300630
dc.language.isoeng
dc.relation.ispartofIcarus
dc.sourceScopus
dc.subjectAsteroid belt
dc.subjectAsteroids
dc.subjectProtoplanetary disk interactions
dc.subjectSolar system
dc.subjectSurface mass ablation
dc.titleAsteroids were born bigger: An implication of surface mass ablation during gas-assisted implantation into the asteroid belten
dc.typeArtigopt
dspace.entity.typePublication
relation.isOrgUnitOfPublicationa4071986-4355-47c3-a5a3-bd4d1a966e4f
relation.isOrgUnitOfPublication.latestForDiscoverya4071986-4355-47c3-a5a3-bd4d1a966e4f
unesp.author.orcid0000-0002-1666-5141[1]
unesp.campusUniversidade Estadual Paulista (UNESP), Faculdade de Engenharia e Ciências, Guaratinguetápt

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