THE MASS–METALLICITY RELATION FOR GIANT PLANETS
Daniel Thorngren, Jonathan J. Fortney, Ruth Murray‐Clay, Eric Lopez
Abstract
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Daniel Thorngren, Jonathan J. Fortney, Ruth Murray‐Clay, Eric Lopez
Abstract
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ABSTRACT Exoplanet discoveries of recent years have provided a great deal of new data for studying the bulk compositions of giant planets. Here we identify 47 transiting giant planets (20 M ⊕ < M < 20 M J ) whose stellar insolations are low enough ( F * < 2 × 10 8 erg s −1 cm −2 , or roughly T eff < 1000) that they are not affected by the hot-Jupiter radius inflation mechanism(s). We compute a set of new thermal and structural evolution models and use these models in comparison with properties of the 47 transiting planets (mass, radius, age) to determine their heavy element masses. A clear correlation emerges between the planetary heavy element mass M z and the total planet mass, approximately of the form . This finding is consistent with the core-accretion model of planet formation. We also study how stellar metallicity [Fe/H] affects planetary metal-enrichment and find a weaker correlation than has previously been reported from studies with smaller sample sizes. We confirm a strong relationship between the planetary metal-enrichment relative to the parent star Z planet / Z star and the planetary mass, but see no relation in Z planet / Z star with planet orbital properties or stellar mass. The large heavy element masses of many planets (>50 M ⊕ ) suggest significant amounts of heavy elements in H/He envelopes, rather than cores, such that metal-enriched giant planet atmospheres should be the rule. We also discuss a model of core-accretion planet formation in a one-dimensional disk and show that it agrees well with our derived relation between mass and Z planet / Z star .
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ABSTRACT Exoplanet discoveries of recent years have provided a great deal of new data for studying the bulk compositions of giant planets. Here we identify 47 transiting giant planets (20 M ⊕ < M < 20 M J ) whose stellar insolations are low enough ( F * < 2 × 10 8 erg s −1 cm −2 , or roughly T eff < 1000) that they are not affected by the hot-Jupiter radius inflation mechanism(s). We compute a set of new thermal and structural evolution models and use these models in comparison with properties of the 47 transiting planets (mass, radius, age) to determine their heavy element masses. A clear correlation emerges between the planetary heavy element mass M z and the total planet mass, approximately of the form . This finding is consistent with the core-accretion model of planet formation. We also study how stellar metallicity [Fe/H] affects planetary metal-enrichment and find a weaker correlation than has previously been reported from studies with smaller sample sizes. We confirm a strong relationship between the planetary metal-enrichment relative to the parent star Z planet / Z star and the planetary mass, but see no relation in Z planet / Z star with planet orbital properties or stellar mass. The large heavy element masses of many planets (>50 M ⊕ ) suggest significant amounts of heavy elements in H/He envelopes, rather than cores, such that metal-enriched giant planet atmospheres should be the rule. We also discuss a model of core-accretion planet formation in a one-dimensional disk and show that it agrees well with our derived relation between mass and Z planet / Z star .
Key concepts: Physics, Planet, Astrophysics, Metallicity, Exoplanet, Planetary mass, RADIUS, Heavy element