{"title":"The Sun's Birth Environment: Context for Meteoritics","authors":"Steve Desch, Núria Miret-Roig","doi":"arxiv-2409.10638","DOIUrl":null,"url":null,"abstract":"Meteorites trace planet formation in the Sun's protoplanetary disk, but they\nalso record the influence of the Sun's birth environment. Whether the Sun\nformed in a region like Taurus-Auriga with ~10^2 stars, or a region like the\nCarina Nebula with ~10^6 stars, matters for how large the Sun's disk was, for\nhow long and from how far away it accreted gas from the molecular cloud, and\nhow it acquired radionuclides like 26Al. To provide context for the\ninterpretation of meteoritic data, we review what is known about the Sun's\nbirth environment. Based on an inferred gas disk outer radius ~50-90 AU, radial\ntransport in the disk, and the abundances of noble gases in Jupiter's\natmosphere, the Sun's molecular cloud and protoplanetary disk were exposed to\nan ultraviolet flux G0 ~30-3000 during its birth and first ~10 Myr of\nevolution. Based on the orbits of Kuiper Belt objects, the Solar System was\nsubsequently exposed to a stellar density ~100 Msol/pc^3 for ~100 Myr, strongly\nimplying formation in a bound cluster. These facts suggest formation in a\nregion like the outskirts of the Orion Nebula, perhaps 2 pc from the center.\nThe protoplanetary disk might have accreted gas for many Myr, but a few x10^5\nyr seems more likely. It probably inherited radionuclides from its molecular\ncloud, enriched by inputs from supernovae and especially Wolf-Rayet star winds,\nand acquired a typical amount of 26Al.","PeriodicalId":501270,"journal":{"name":"arXiv - PHYS - Geophysics","volume":"187 1","pages":""},"PeriodicalIF":0.0000,"publicationDate":"2024-09-16","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"arXiv - PHYS - Geophysics","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/arxiv-2409.10638","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0
Abstract
Meteorites trace planet formation in the Sun's protoplanetary disk, but they
also record the influence of the Sun's birth environment. Whether the Sun
formed in a region like Taurus-Auriga with ~10^2 stars, or a region like the
Carina Nebula with ~10^6 stars, matters for how large the Sun's disk was, for
how long and from how far away it accreted gas from the molecular cloud, and
how it acquired radionuclides like 26Al. To provide context for the
interpretation of meteoritic data, we review what is known about the Sun's
birth environment. Based on an inferred gas disk outer radius ~50-90 AU, radial
transport in the disk, and the abundances of noble gases in Jupiter's
atmosphere, the Sun's molecular cloud and protoplanetary disk were exposed to
an ultraviolet flux G0 ~30-3000 during its birth and first ~10 Myr of
evolution. Based on the orbits of Kuiper Belt objects, the Solar System was
subsequently exposed to a stellar density ~100 Msol/pc^3 for ~100 Myr, strongly
implying formation in a bound cluster. These facts suggest formation in a
region like the outskirts of the Orion Nebula, perhaps 2 pc from the center.
The protoplanetary disk might have accreted gas for many Myr, but a few x10^5
yr seems more likely. It probably inherited radionuclides from its molecular
cloud, enriched by inputs from supernovae and especially Wolf-Rayet star winds,
and acquired a typical amount of 26Al.