Issue |
A&A
Volume 667, November 2022
|
|
---|---|---|
Article Number | L2 | |
Number of page(s) | 10 | |
Section | Letters to the Editor | |
DOI | https://doi.org/10.1051/0004-6361/202244169 | |
Published online | 03 November 2022 |
Letter to the Editor
Evidence of a signature of planet formation processes from solar neutrino fluxes⋆,⋆⋆
1
Department of Physics, Kurume University, 67 Asahimachi, Kurume, Fukuoka, 830-0011, Japan
e-mail: kunitomo.masanobu@gmail.com
2
Université Côte d’Azur, Observatoire de la Côte d’Azur, CNRS, Laboratoire Lagrange, Bd de l’Observatoire, CS 34229, 06304 Nice cedex 4, France
3
Département d’Astronomie, Université de Genève, Chemin Pegasi 51, 1290 Versoix, Switzerland
Received:
2
June
2022
Accepted:
7
October
2022
Solar evolutionary models are thus far unable to reproduce spectroscopic, helioseismic, and neutrino constraints consistently, resulting in the so-called solar modeling problem. In parallel, planet formation models predict that the evolving composition of the protosolar disk and, thus, of the gas accreted by the proto-Sun must have been variable. We show that solar evolutionary models that include a realistic planet formation scenario lead to an increased core metallicity of up to 5%, implying that accurate neutrino flux measurements are sensitive to the initial stages of the formation of the Solar System. Models with homogeneous accretion match neutrino constraints to no better than 2.7σ. In contrast, accretion with a variable composition due to planet formation processes, leading to metal-poor accretion of the last ∼4% of the young Sun’s total mass, yields solar models within 1.3σ of all neutrino constraints. We thus demonstrate that in addition to increased opacities at the base of the convective envelope, the formation history of the Solar System constitutes a key element in resolving the current crisis of solar models.
Key words: neutrinos / Sun: interior / Sun: evolution / accretion, accretion disks / protoplanetary disks / planets and satellites: formation
Supplemental materials are only available at the CDS via anonymous ftp to cdsarc.cds.unistra.fr (130.79.128.5) or via https://cdsarc.cds.unistra.fr/viz-bin/cat/J/A+A/667/L2 or via https://doi.org/10.5281/zenodo.7156794
Animations associated to Figs. 3 and A.1 are available at https://www.aanda.org
© M. Kunitomo et al. 2022
Open Access article, published by EDP Sciences, under the terms of the Creative Commons Attribution License (https://creativecommons.org/licenses/by/4.0), which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.
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