Recycling of the first atmospheres of embedded planets: Dependence on core mass and optical depth
arXiv:2202.11422 · doi:10.1051/0004-6361/202141955
Abstract
Recent observations found close-in planets with significant atmospheres of hydrogen and helium in great abundance. These are the so-called super-Earths and mini-Neptunes. Their atmospheric composition suggests that they formed early during the gas-rich phase of the circumstellar disk and were able to avoid becoming hot Jupiters. As a possible explanation, recent studies explored the recycling hypothesis and showed that atmosphere-disk recycling is able to fully compensate for radiative cooling and thereby halt Kelvin-Helmholtz contraction to prevent runaway gas accretion. To understand the parameters that determine the efficiency of atmospheric recycling, we extend our earlier studies by exploring the effects of the core mass, the effect of circumstellar gas on sub-Keplerian orbits (headwind), and the optical depth of the surrounding gas on the recycling timescale. Additionally, we analyze their effects on the size and mass of the forming atmosphere. For the explored parameter space, all simulations eventually reach an equilibrium where heating due to hydrodynamic recycling fully compensates radiative cooling. In this equilibrium, the atmosphere-to-core mass ratio stays well below , preventing the atmosphere from becoming self-gravitating and entering runaway gas accretion. Higher core masses cause the atmosphere to become turbulent, which further enhances recycling. Even for our highest core mass of , atmosphere-disk recycling is efficient enough to fully compensate for radiative cooling and prevent the atmosphere from becoming self-gravitating. Hence, in-situ formation of hot Jupiters is very unlikely, and migration of gas giants is a key process required to explain their existence. Our findings imply that atmosphere-disk recycling is the most natural explanation for the prevalence of close-in super-Earths and mini-Neptunes.
18 pages, 13 figures, Accepted for publication by A&A on 2/7/2022
References in corpus (15)
- PLUTO: a Numerical Code for Computational Astrophysics
- Separating gas-giant and ice-giant planets by halting pebble accretion
- Make Super-Earths, Not Jupiters: Accreting Nebular Gas onto Solid Cores at 0.1 AU and Beyond
- Hydrodynamics of Embedded Planets' First Atmospheres. II. A Rapid Recycling of Atmospheric Gas
- An Atmospheric Structure Equation for Grain Growth
- Hydrodynamics of embedded planets' first atmospheres - III. The role of radiation transport for super-Earth planets
- Grain opacity and the bulk composition of extrasolar planets. II. An analytical model for the grain opacity in protoplanetary atmospheres
- Angular Momentum Accretion onto a Gas Giant Planet
- Hydrodynamics of Embedded Planets' First Atmospheres. I. A Centrifugal Growth Barrier for 2D Flows
- The End of Runaway: How Gap Opening Limits the Final Masses of Gas Giants
- Envelopes of embedded super-Earths II. Three-dimensional isothermal simulations
- Steady State by Recycling prevents Premature Collapse of Protoplanetary Atmospheres
- Makemake + Sedna: A Continuum Radiation Transport and Photoionization Framework for Astrophysical Newtonian Fluid Dynamics
- Radial Gradients in Dust-to-Gas Ratio Lead to Preferred Region for Giant Planet Formation
- ALMA observations require slower Core Accretion runaway growth
Cited by in corpus (16)
- The Exoplanet Radius Valley from Gas-driven Planet Migration and Breaking of Resonant Chains
- Efficient planet formation by pebble accretion in ALMA rings
- A fading radius valley towards M-dwarfs, a persistent density valley across stellar types
- Giants are bullies: how their growth influences systems of inner sub-Neptunes and super-Earths
- Super-Earths and Earth-like Exoplanets
- The maximum accretion rate of a protoplanet: how fast can runaway be?
- Atmospheric Recyling of Volatiles by Pebble-Accreting Planets
- The Planetary Accretion Shock. III. Smoothing-free 2.5D simulations and calculation of H alpha emission
- Spin of protoplanets generated by pebble accretion: Influences of protoplanet-induced gas flow
- Gas accretion onto Jupiter mass planets in discs with laminar accretion flows
- A formation pathway for terrestrial planets with moderate water content involving atmospheric-volatile recycling
- An impact-free mechanism to deliver water to terrestrial planets and exoplanets
- Constraining the formation history of the HAT-P-11 system by atmospheric abundances
- Late gas released in the young Kuiper belt could have significantly contributed to the carbon enrichment of the atmospheres of Neptune and Uranus
- Interior dynamics of envelopes around disk-embedded planets
- Evolution and Observable Properties of Rocky Planet Atmospheres