The origin of the high metallicity of close-in giant exoplanets: Combined effect of the resonant and aerodynamic shepherding
arXiv:1911.02292 · doi:10.1051/0004-6361/201936700
Abstract
Context.Recent studies suggest that many giant exoplanets are highly enriched with heavy elements compared to their host star andcontain several tens of Earth masses or more of heavy elements. Such enrichment is considered to have been brought by accretionof planetesimals in late formation stages. Previous dynamical simulations, however, show that planets are unable to collect so muchheavy elements throughin situplanetesimal accretion. Aims.We investigate whether a giant planet migrating inward can capture planetesimals efficiently to significantly increase its metal-licity. Methods.We performed orbital integrations of a migrating giant planet and planetesimals in a protoplanetary gas disc to infer theplanetesimal mass that is accreted by the planet. Results.We find that the two shepherding processes of mean motion resonances trapping and aerodynamic gas drag inhibit plan-etesimal capture of a migrating planet. However, the amplified libration allows the highly-excited planetesimals in the resonances toescape from the resonance trap and be accreted by the planet. Consequently, we show that a migrating giant planet captures planetes-imals with total mass of several tens of Earth masses, if the planet forms at a few tens of AU in a relatively massive disc. We alsofind that planetesimal capture occurs efficiently in a limited range of semi-major axis, and that the total captured planetesimal massincreases with increasing migration distances. Our results have important implications for understanding the relation between giantplanet metallicity and mass, as we suggest that it reflects the formation location of the planet, or more precisely, the location whererunaway gas accretion occurred. We also suggest the observed metal-rich close-in Jupiters migrated to their present locations fromafar, where they formed.
14 pages, 11 figures, accepted for publication in Astronomy and Astrophysics
References in corpus (14)
- Separating gas-giant and ice-giant planets by halting pebble accretion
- Chemical enrichment of giant planets and discs due to pebble drift
- Formation of planetary systems by pebble accretion and migration: Growth of gas giants
- Jupiter's Decisive Role in the Inner Solar System's Early Evolution
- Grain opacity and the bulk composition of extrasolar planets. II. An analytical model for the grain opacity in protoplanetary atmospheres
- On the Origin of HD149026b
- Critical core mass for enriched envelopes: the role of H2O condensation
- Planetesimal Accretion onto Growing Proto-Gas-Giant Planets
- Jupiter's formation and its primordial internal structure
- A Systematic Study of the Final Masses of Gas Giant Planets
- Infall of planetesimals onto growing giant planets: onset of runaway gas accretion and metallicity of their gas envelopes
- Capture of Solids by Growing Proto-gas Giants: Effects of Gap Formation and Supply-limited Growth
- Embryo impacts and gas giant mergers II: Diversity of Hot Jupiters' internal structure
- Breaking mean-motion resonances during Type I planet migration
Cited by in corpus (55)
- Early Release Science of the Exoplanet WASP-39b with JWST NIRSpec G395H
- Early Release Science of the exoplanet WASP-39b with JWST NIRISS
- Tracing the formation history of giant planets in protoplanetary disks with Carbon, Oxygen, Nitrogen and Sulphur
- How drifting and evaporating pebbles shape giant planets I: Heavy element content and atmospheric C/O
- Five key exoplanet questions answered via the analysis of 25 hot Jupiter atmospheres in eclipse
- How drifting and evaporating pebbles shape giant planets II: Volatiles and refractories in atmospheres
- Chemical Diversity in Protoplanetary Disks and Its Impact on the Formation History of Giant Planets
- The Challenge of Forming a Fuzzy Core in Jupiter
- Revelations on Jupiter's Formation, Evolution and Interior: Challenges from Juno Results
- Breaking Degeneracies in Formation Histories by Measuring Refractory Content in Gas Giants
- The Ariel Target List: The Impact of TESS and the Potential for Characterising Multiple Planets Within a System
- Theoretical vs. observational uncertainties: composition of giant exoplanets
- Heavy-metal Jupiters by major mergers: metallicity vs. mass for giant planets
- Exoplanet atmosphere retrievals in 3D using phase curve data with ARCiS: application to WASP-43b
- The TESS-Keck Survey. VIII. Confirmation of a Transiting Giant Planet on an Eccentric 261 day Orbit with the Automated Planet Finder Telescope
- Synthetic Evolution Tracks of Giant Planets
- Setting the Stage: Planet formation and Volatile Delivery
- Is the atmosphere of the ultra-hot Jupiter WASP-121b variable?
- Exploring the link between star and planet formation with Ariel
- SimAb: A simple, fast and flexible model to assess the effects of planet formation on the atmospheric composition of gas giants
- Enriching inner discs and giant planets with heavy elements
- Towards a new era in giant exoplanet characterisation
- Ariel stellar characterisation: I -- homogeneous stellar parameters of 187 FGK planet host stars Description and validation of the method
- Measuring Elemental Abundances of JWST Target Stars for Exoplanet Characterization I. FGK Stars
- Constraining the origin of giant exoplanets via elemental abundance measurements
- On spectroscopic phase-curve retrievals: H2 dissociation and thermal inversion in the atmosphere of the ultra-hot Jupiter WASP-103 b
- Revising the Giant Planet Mass-Metallicity Relation: Deciphering the Formation Sequence of Giant Planets
- Ariel Planetary Interiors White Paper
- Formation of giant planets with large metal masses and metal fractions via giant impacts in a rapidly dissipating disk
- Super stellar abundances of alkali metals suggest significant migration for Hot Jupiters
- Enrichment of Jupiter's atmosphere by late planetesimal bombardment
- The origin of the high metallicity of close-in giant exoplanets II The nature of the sweet spot for accretion
- The GAPS program at TNG XLVII: The unusual formation history of V1298 Tau
- Measuring Tracers of Planet Formation in the Atmosphere of WASP-77A b: Sub-stellar O/H and C/H ratios, with a stellar C/O ratio and a potentially Super-stellar Ti/H ratio
- Giant Outer Transiting Exoplanet Mass (GOT 'EM) Survey. II. Discovery of a Failed Hot Jupiter on a 2.7 Year, Highly Eccentric Orbit
- In-situ enrichment in heavy elements of hot Jupiters
- A strong H- opacity signal in the near-infrared emission spectrum of the ultra-hot Jupiter KELT-9b
- Planetary core formation via multi-species pebble accretion
- A low accretion efficiency of planetesimals formed at planetary gap edges
- Inferring Late Stage Enrichment of Exoplanet Atmospheres from Observed Interstellar Comets
- Heavy-element Accretion by Proto-Jupiter in a Massive Planetesimal Disk, Revisited
- TOI-837 b: characterisation, formation and evolutionary history of an infant warm Saturn-mass planet
- An Approximation for the Capture Radius of Gaseous Protoplanets
- Ariel stellar characterisation III. Fast rotators and new FGK stars in the Ariel Mission Candidate Sample
- Strong NUV Refractory Absorption and Dissociated Water in the Hubble Transmission Spectrum of the Ultra Hot Jupiter KELT-20 b
- GEMS JWST: Transmission spectroscopy of TOI-5205b reveals significant stellar contamination and a metal-poor atmosphere
- Accretion of aerodynamically large pebbles
- Coupled Thermal-Chemical Evolution Models of Sub-Neptunes Reveal Atmospheric Signatures of Their Formation Location
- The New Generation Planetary Population Synthesis (NGPPS) VIII. Impact of host star metallicity on planet occurrence rates, orbital periods, eccentricities, and radius valley morphology
- The Compositional Dimension of Planet Formation
- The Effect of Accretion Rate and Composition on the Structure of Ice-rich Super-Earths
- Detailed Calculations of the Efficiency of Planetesimal Accretion in the Core-Accretion Model -II: The effect of Saturn
- Mercury-Ares: a high-performance n-body code for planet formation studies
- A sub-Saturn Mass-Radius Desert for Planets with Equilibrium Temperature Less than 600 K
- Possible in situ formation of Uranus and Neptune via Pebble Accretion