Giant Impact: An Efficient Mechanism for the Devolatilization of Super-Earths
arXiv:1509.05772 · doi:10.1088/0004-637X/812/2/164
Abstract
Mini-Neptunes and volatile-poor super-Earths coexist on adjacent orbits in proximity to host stars such as Kepler-36 and Kepler-11. Several post-formation processes have been proposed for explaining the origin of the compositional diversity: the mass loss via stellar XUV irradiation, degassing of accreted material, and in-situ accumulation of the disk gas. Close-in planets are also likely to experience giant impacts during the advanced stage of planet formation. This study examines the possibility of transforming volatile-rich super-Earths / mini-Neptunes into volatile-depleted super-Earths through giant impacts. We present the results of three-dimensional giant impact simulations in the accretionary and disruptive regimes. Target planets are modeled with a three-layered structure composed of an iron core, silicate mantle and hydrogen/helium envelope. In the disruptive case, the giant impact can remove most of the H/He atmosphere immediately and homogenize the refractory material in the planetary interior. In the accretionary case, the planet can retain more than half of the gaseous envelope, while a compositional gradient suppresses efficient heat transfer as its interior undergoes double-diffusive convection. After the giant impact, a hot and inflated planet cools and contracts slowly. The extended atmosphere enhances the mass loss via both a Parker wind induced by thermal pressure and hydrodynamic escape driven by the stellar XUV irradiation. As a result, the entire gaseous envelope is expected to be lost due to the combination of those processes in both cases. We propose that Kepler-36b may have been significantly devolatilized by giant impacts, while a substantial fraction of Kepler-36c's atmosphere may remain intact. Furthermore, the stochastic nature of giant impacts may account for the large dispersion in the mass--radius relationship of close-in super-Earths and mini-Neptunes.
8 pages, 8 figures, 1 table, to be published in ApJ, readability improved according to the proof
References in corpus (8)
- Modules for Experiments in Stellar Astrophysics (MESA)
- Line and Mean Opacities for Ultracool Dwarfs and Extrasolar Planets
- The Mass of Kepler-93b and The Composition of Terrestrial Planets
- Ranges of Atmospheric Mass and Composition of Super Earth Exoplanets
- A test suite for quantitative comparison of hydrodynamics codes in astrophysics
- Formation of close in Super-Earths \& Mini-Neptunes: Required Disk Masses \& Their Implications
- Collisional Stripping and Disruption of Super-Earths
- Embryo impacts and gas giant mergers II: Diversity of Hot Jupiters' internal structure
Cited by in corpus (72)
- The California-Kepler Survey. III. A Gap in the Radius Distribution of Small Planets
- The California Kepler Survey VII. Precise Planet Radii Leveraging Gaia DR2 Reveal the Stellar Mass Dependence of the Planet Radius Gap
- An asteroseismic view of the radius valley: stripped cores, not born rocky
- Formation of planetary systems by pebble accretion and migration: How the radial pebble flux determines a terrestrial-planet or super-Earth growth mode
- Born Dry in the Photo-Evaporation Desert: Kepler's Ultra-Short-Period Planets Formed Water-Poor
- How formation time-scales affect the period dependence of the transition between rocky super-Earths and gaseous sub-Neptunes and implications for
- Secure TTV Mass Measurements: Ten Kepler Exoplanets between 3 and 8 Earth Masses with Diverse Densities and Incident Fluxes
- A giant impact as the likely origin of different twins in the Kepler-107 exoplanet system
- Habitability of Terrestrial-Mass Planets in the HZ of M Dwarfs. I. H/He-Dominated Atmospheres
- Stealing the Gas: Giant Impacts and the Large Diversity in Exoplanet Densities
- The Formation of Jupiter's Diluted Core by a Giant Impact
- The Exoplanet Radius Valley from Gas-driven Planet Migration and Breaking of Resonant Chains
- Giant planet formation in radially structured protoplanetary discs
- Planetary Magnetic Field Control of Ion Escape from Weakly Magnetized Planets
- Atmospheric mass loss due to giant impacts: the importance of the thermal component for hydrogen-helium envelopes
- Consequences of Giant Impacts on Early Uranus for Rotation, Internal Structure, Debris, and Atmospheric Erosion
- A Tale of Planet Formation: From Dust to Planets
- The New Generation Planetary Population Synthesis (NGPPS). V. Predetermination of planet types in global core accretion models
- Evolution of the Exoplanet Size Distribution: Forming Large Super-Earths Over Billions of Years
- One year of AU Mic with HARPS: I -- measuring the masses of the two transiting planets
- Influence of the water content in protoplanetary discs on planet migration and formation
- Growth and evolution of secondary volcanic atmospheres: I. Identifying the geological character of hot rocky planets
- Two Transiting Low Density Sub-Saturns from K2
- The Magellan-TESS Survey I: Survey Description and Mid-Survey Results
- Atmospheric Erosion by Giant Impacts onto Terrestrial Planets
- Super-Earths and Earth-like Exoplanets
- Atmospheric Erosion by Giant Impacts onto Terrestrial Planets: A Scaling Law for any Speed, Angle, Mass, and Density
- Atmosphere loss in planet-planet collisions
- Realistic On-The-Fly Outcomes of Planetary Collisions: Machine Learning Applied to Simulations of Giant Impacts
- Shallower radius valley around low-mass hosts: Evidence for icy planets, collisions or high-energy radiation scatter
- Discovery and Validation of a High-Density sub-Neptune from the K2 Mission
- The initial physical conditions of Kepler-36 b & c
- Enhanced mixing in giant impact simulations with a new Lagrangian method
- K2-110 b - a massive mini-Neptune exoplanet
- K2-265 b: A Transiting Rocky Super-Earth
- Potential long-term habitable conditions on planets with primordial H-He atmospheres
- Examining the Radius Valley: a Machine Learning Approach
- Kepler-1656b: a Dense Sub-Saturn With an Extreme Eccentricity
- Losing Oceans: The Effects of Composition on the Thermal Component of Impact-driven Atmospheric Loss
- The Role of Giant Impacts in Planet Formation
- HATS-43b, HATS-44b, HATS-45b, and HATS-46b: Four Short Period Transiting Giant Planets in the Neptune-Jupiter Mass Range
- Close-in Super-Earths: The first and the last stages of planet formation in an MRI-accreting disc
- Non-Trivial Oblique Spin Equilibria of Super-Earths in Multi-planetary Systems
- Atmosphere Loss in Oblique Super-Earth Impacts
- TOI-1075 b: A Dense, Massive, Ultra-Short Period Hot Super-Earth Straddling the Radius Gap
- Outcomes of Grazing Impacts Between Sub-Neptunes in Kepler Multis
- Dynamics and Collisional Evolution of Closely Packed Planetary Systems
- Exoplanet atmosphere evolution: emulation with neural networks
- Size evolution of close-in super-Earths through giant impacts and photoevaporation
- Atmospheric Mass Loss from High Velocity Giant Impacts
- Formation of Super-Earths by Tidally-Forced Turbulence
- Collisional formation of massive exomoons of super-terrestrial exoplanets
- Characterizing K2 Candidate Planetary Systems Orbiting Low-Mass Stars III: A High Mass & Low Envelope Fraction for the Warm Neptune K2-55b
- Effects of Planetesimal Accretion on the Thermal and Structural Evolution of Sub-Neptunes
- Unveiling the Planet Population at Birth
- A primordial radius valley as a consequence of planet formation
- Formation of super-Earths and mini-Neptunes from rings of planetesimals
- In-depth characterization of the Kepler-10 three-planet system with HARPS-N radial velocities and Kepler transit timing variations
- Precise characterisation of HD 15337 with CHEOPS: a laboratory for planet formation and evolution
- Can Rocky Exoplanets with Rings Pose as Sub-Neptunes?
- Discovery and characterization of a dense sub-Saturn TOI-6651b
- Diversity of disc viscosities can explain the period ratios of resonant and non-resonant systems of hot super-Earths and mini-Neptunes
- Formation of Super-Earths
- Constraining the formation history of the HAT-P-11 system by atmospheric abundances
- Three young planets around the K-dwarf K2-198: High-energy environment, evaporation history and expected future
- No dilute core produced in simulations of giant impacts on to Jupiter
- Super-earths and mini-neptunes follow different orbital period-eccentricity relations
- Effects of Self-gravity on Mass-loss of the Post-impact Super-Earths
- Ohmic dissipation during the formation of super-Earth
- The effect of late giant collisions on the atmospheres of protoplanets and the formation of cold sub-Saturns
- Revisiting the exoplanet radius valley with host stars from SWEET-Cat
- Re-accretion of Giant Impact Ejecta Can Drive Significant Atmospheric Erosion on Terrestrial Planets