Formation of close in Super-Earths \& Mini-Neptunes: Required Disk Masses \& Their Implications
Hilke E. Schlichting (MIT)

TL;DR
This paper investigates the in situ formation of close-in super-Earths and mini-Neptunes, finding that high disk surface densities are required, which are often gravitationally unstable, implying migration likely played a significant role.
Contribution
It calculates the disk mass requirements for in situ formation of close-in planets, highlighting the necessity of high solid surface densities and the likely importance of migration.
Findings
In situ formation without migration requires highly enhanced disk densities.
Standard gas-to-dust ratios lead to unstable gas disks for many systems.
Formation beyond a few AU aligns with minimum-mass solar nebula models.
Abstract
Recent observations by the {\it Kepler} space telescope have led to the discovery of more than 4000 exoplanet candidates consisting of many systems with Earth- to Neptune-sized objects that reside well inside the orbit of Mercury, around their respective host stars. How and where these close-in planets formed is one of the major unanswered questions in planet formation. Here we calculate the required disk masses for {\it in situ} formation of the {\it Kepler} planets. We find that, if close-in planets formed as {\it isolation masses}, then standard gas-to-dust ratios yield corresponding gas disks that are gravitationally unstable for a significant fraction of systems, ruling out such a scenario. We show that the maximum width of a planet's accretion region in the absence of any migration is , where is the escape velocity of the planet and the…
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