Exoplanet interior retrievals: core masses and metallicities from atmospheric abundances

Author:

Bloot S123ORCID,Miguel Y14ORCID,Bazot M56ORCID,Howard S7ORCID

Affiliation:

1. Leiden Observatory, Leiden University ,  Niels Bohrweg 2, 2333 CA , Leiden, the Netherlands

2. ASTRON, Netherlands Institute for Radio Astronomy , Oude Hoogeveensedijk 4, 7991 PD , Dwingeloo, the Netherlands

3. Kapteyn Astronomical Institute, University of Groningen , Landleven 12, 9747 AD , Groningen, the Netherlands

4. SRON Netherlands Institute for Space Research , Niels Bohrweg 4, 2333 CA , Leiden, the Netherlands

5. Heidelberg Institute for Theoretical Studies (HITS gGmbH) , Schloss-Wolfsbrunnenweg 35, 69118 Heidelberg, Germany

6. CITIES, NYUAD Institute, New York University Abu Dhabi , Saadiyat Island , Abu Dhabi, United Arab Emirates

7. Université Côte d’Azur, Observatoire de la Côte d’Azur, CNRS, Laboratoire Lagrange, , Boulevard de l’Observatoire, CS 34229, 06304 Nice Cedex 4, France

Abstract

ABSTRACT The mass and distribution of metals in the interiors of exoplanets are essential for constraining their formation and evolution processes. Never the less, with only masses and radii measured, the determination of exoplanet interior structures is degenerate, and so far simplified assumptions have mostly been used to derive planetary metallicities. In this work, we present a method based on a state-of-the-art interior code, recently used for Jupiter, and a Bayesian framework, to explore the possibility of retrieving the interior structure of exoplanets. We use masses, radii, equilibrium temperatures, and measured atmospheric metallicities to retrieve planetary bulk metallicities and core masses. Following results on the giant planets in the Solar system and recent development in planet formation, we implement two interior structure models: one with a homogeneous envelope and one with an inhomogeneous one. Our method is first evaluated using a test planet and then applied to a sample of 37 giant exoplanets with observed atmospheric metallicities from the pre-JWST era. Although neither internal structure model is preferred with the current data, it is possible to obtain information on the interior properties of the planets, such as the core mass, through atmospheric measurements in both cases. We present updated metal mass fractions, in agreement with recent results on giant planets in the Solar system.

Publisher

Oxford University Press (OUP)

Subject

Space and Planetary Science,Astronomy and Astrophysics

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