Issue |
A&A
Volume 660, April 2022
|
|
---|---|---|
Article Number | A85 | |
Number of page(s) | 17 | |
Section | Planets and planetary systems | |
DOI | https://doi.org/10.1051/0004-6361/202142738 | |
Published online | 20 April 2022 |
Forming Planets Around Stars With Non-Solar Elemental Composition
1
Kapteyn Astronomical Institute, University of Groningen,
PO Box 800, 9700AV
Groningen,
The Netherlands
e-mail: jorge@astro.rug.nl
2
Department of Astrophysics/IMAPP, Radboud University,
PO Box 9010, 6500
GL Nijmegen,
The Netherlands
3
SRON Netherlands Institute for Space Research,
Niels Bohrweg 4,
2333
CA Leiden,
the Netherlands
4
Space Research Institute, Austrian Academy of Sciences,
Schmiedlstrasse 6,
8042
Graz,
Austria
5
SUPA, School of Physics & Astronomy, St Andrews University,
North Haugh,
St Andrews
KY16 9SS,
UK
6
Centre for Exoplanet Science, University of St Andrews,
North Haugh,
St Andrews
KY16 9SS,
UK
7
Institute of Geophysics, ETH Zurich,
Sonneggstrasse 5,
8092
Zurich,
Switzerland
Received:
24
November
2021
Accepted:
23
February
2022
Context. Stars in the solar neighbourhood have refractory element ratios slightly different from that of the Sun. It is unclear how much the condensation of solids and thus the composition of planets forming around these stars is affected.
Aims. We aim to understand the impact of changing the ratios of the refractory elements Mg, Si, and Fe within the range observed in solar-type stars within 150 pc of the Sun on the composition of planets forming around them.
Methods. We use the GGchem code to simulate the condensation of solids in protoplanetary disks with a minimum mass solar nebula around main sequence G-type stars in the solar neighbourhood. We extract the stellar elemental composition from the Hypatia Database.
Results. We find that a lower Mg/Si ratio shifts the condensation sequence from forsterite (Mg2SiO4) and SiO to enstatite (MgSiO3) and quartz (SiO2); a lower Fe/S ratio leads to the formation of FeS and FeS2 and few or no Fe-bearing silicates. Ratios of refractory elements translate directly from the gas phase to the condensed phase for T < 1000 K. However, ratios with respect to volatile elements (e.g. oxygen and sulphur) in the condensates – the building blocks of planets – differ from the original stellar composition.
Conclusions. Our study shows that the composition of planets crucially depends on the abundances of the stellar system under investigation. Our results can have important implications for planet interiors, which depend strongly on the degree of oxidation and the sulphur abundance.
Key words: stars: abundances / protoplanetary disks / planets and satellites: composition / astrochemistry
© ESO 2022
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