How Internal Structure Shapes the Metallicity of Giant Exoplanets

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Hauptverfasser: Peerani, Lorenzo, Howard, Saburo, Helled, Ravit
Format: Preprint
Veröffentlicht: 2025
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author Peerani, Lorenzo
Howard, Saburo
Helled, Ravit
author_facet Peerani, Lorenzo
Howard, Saburo
Helled, Ravit
contents The composition and internal structure of gas giant exoplanets encode key information about their formation and evolution. We investigate how different assumed interior structures affect the inferred bulk metallicity and its correlation with planetary mass. For a sample of 44 giant exoplanets (0.12-5.98 MJ), we computed evolutionary models with CEPAM and retrieved their bulk metallicities under three structural hypotheses: core+envelope (CE), dilute core (DC), and fully mixed (FM). Across all structures, we recover a significant positive correlation between total heavy-element mass (MZ) and planetary mass (M), and a negative correlation between bulk metallicity (Z) and M (also for Z/Zstar vs M). Dilute core structures yield metallicities comparable to CE models, regardless of the assumed extent of the composition gradient. Increasing atmospheric metallicity augments the inferred bulk metallicity, as enhanced opacities slow planetary cooling. Non-adiabatic DC models can further increase the retrieved metallicity by up to 35 percent. We find that the mass-metallicity anti-correlation is primarily driven by low-mass, metal-rich planets (M < 0.2 MJ), and that massive planets (greater than about 1 MJ) can exhibit unexpectedly high metallicities (Z approximately 0.1-0.3). Improved constraints on convective mixing, combined with upcoming accurate measurements of planetary masses, radii, and atmospheric compositions from missions such as PLATO and Ariel, will provide further constraints on interior structure and formation models of gas giant planets.
format Preprint
id arxiv_https___arxiv_org_abs_2510_08280
institution arXiv
publishDate 2025
record_format arxiv
spellingShingle How Internal Structure Shapes the Metallicity of Giant Exoplanets
Peerani, Lorenzo
Howard, Saburo
Helled, Ravit
Earth and Planetary Astrophysics
The composition and internal structure of gas giant exoplanets encode key information about their formation and evolution. We investigate how different assumed interior structures affect the inferred bulk metallicity and its correlation with planetary mass. For a sample of 44 giant exoplanets (0.12-5.98 MJ), we computed evolutionary models with CEPAM and retrieved their bulk metallicities under three structural hypotheses: core+envelope (CE), dilute core (DC), and fully mixed (FM). Across all structures, we recover a significant positive correlation between total heavy-element mass (MZ) and planetary mass (M), and a negative correlation between bulk metallicity (Z) and M (also for Z/Zstar vs M). Dilute core structures yield metallicities comparable to CE models, regardless of the assumed extent of the composition gradient. Increasing atmospheric metallicity augments the inferred bulk metallicity, as enhanced opacities slow planetary cooling. Non-adiabatic DC models can further increase the retrieved metallicity by up to 35 percent. We find that the mass-metallicity anti-correlation is primarily driven by low-mass, metal-rich planets (M < 0.2 MJ), and that massive planets (greater than about 1 MJ) can exhibit unexpectedly high metallicities (Z approximately 0.1-0.3). Improved constraints on convective mixing, combined with upcoming accurate measurements of planetary masses, radii, and atmospheric compositions from missions such as PLATO and Ariel, will provide further constraints on interior structure and formation models of gas giant planets.
title How Internal Structure Shapes the Metallicity of Giant Exoplanets
topic Earth and Planetary Astrophysics
url https://arxiv.org/abs/2510.08280