Host-star and exoplanet compositions: A pilot study using a wide binary with a polluted white dwarf

Autor: Paula Jofre, Amy Bonsor, Carl Melis, Oliver Shorttle, Siyi Xu, Laura K. Rogers
Přispěvatelé: Bonsor-Matthews, Amy [0000-0002-8070-1901], Shorttle, Oliver [0000-0002-8713-1446], Apollo - University of Cambridge Repository
Rok vydání: 2021
Předmět:
Solar System
010504 meteorology & atmospheric sciences
stars: abundances
FOS: Physical sciences
Astrophysics::Cosmology and Extragalactic Astrophysics
01 natural sciences
Astrobiology
Chondrite
Planet
0103 physical sciences
Astrophysics::Solar and Stellar Astrophysics
planets and satellites: formation
010303 astronomy & astrophysics
planetary systems
Solar and Stellar Astrophysics (astro-ph.SR)
Refractory (planetary science)
Astrophysics::Galaxy Astrophysics
0105 earth and related environmental sciences
Earth and Planetary Astrophysics (astro-ph.EP)
Physics
sub-99
planets and satellites: composition
White dwarf
Astronomy and Astrophysics
Planetary system
Exoplanet
planets and satellites: interiors
Stars
Astrophysics - Solar and Stellar Astrophysics
13. Climate action
Space and Planetary Science
Physics::Space Physics
Astrophysics::Earth and Planetary Astrophysics
techniques: spectroscopic
Astrophysics - Earth and Planetary Astrophysics
ISSN: 0035-8711
Popis: Planets and stars ultimately form out of the collapse of the same cloud of gas. Whilst planets, and planetary bodies, readily loose volatiles, a common hypothesis is that they retain the same refractory composition as their host star. This is true within the Solar System. The refractory composition of chondritic meteorites, Earth and other rocky planetary bodies are consistent with solar, within the observational errors. This work aims to investigate whether this hypothesis holds for exoplanetary systems. If true, the internal structure of observed rocky exoplanets can be better constrained using their host star abundances. In this paper, we analyse the abundances of the K-dwarf, G200-40, and compare them to its polluted white dwarf companion, WD 1425+540. The white dwarf has accreted planetary material, most probably a Kuiper belt-like object, from an outer planetary system surviving the star's evolution to the white dwarf phase. Given that binary pairs are chemically homogeneous, we use the binary companion, G200-40, as a proxy for the composition of the progenitor to WD 1425+540. We show that the elemental abundances of the companion star and the planetary material accreted by WD 1425+540 are consistent with the hypothesis that planet and host-stars have the same true abundances, taking into account the observational errors.
8 pages, MNRAS in press, mistake in star names corrected
Databáze: OpenAIRE