Formation of Super-Earths by Tidally-Forced Turbulence
Cong Yu (SYSU)

TL;DR
This paper proposes that tidally-forced turbulence inside protoplanets can significantly slow their cooling, allowing super-Earths to form without becoming gas giants, explaining their observed abundance.
Contribution
It introduces a new mechanism involving tidally-forced turbulent diffusion affecting heat transport and planetary evolution, providing a solution to the super-Earth formation puzzle.
Findings
Turbulence generates pseudo-adiabatic regions, reducing cooling efficiency.
A critical turbulent diffusivity threshold determines super-Earth formation.
Inner disk regions favor super-Earths, outer regions favor gas giants.
Abstract
The Kepler observations indicate that many exoplanets are super-Earths, which brings about a puzzle for the core-accretion scenario. Since observed super-Earths are in the range of critical mass, they would accrete gas efficiently and become gas giants. Theoretically, super-Earths are predicted to be rare in the core-accretion framework. To resolve this contradiction, we propose that the tidally-forced turbulent diffusion may affect the heat transport inside the planet. Thermal feedback induced by turbulent diffusion is investigated. We find that the tidally-forced turbulence would generate pseudo-adiabatic regions within radiative zones, which pushes the radiative-convective boundaries (RCBs) inwards. This would decrease the cooling luminosity and enhance the Kelvin-Helmholtz (KH) timescale. For a given lifetime of protoplanetary disks (PPDs), there exists a critical threshold for the…
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