Optically Thin Core Accretion: How Planets Get Their Gas in Nearly Gas-Free Disks
Eve J. Lee, Eugene Chiang, and Jason W. Ferguson

TL;DR
This paper develops models of planetary atmospheres in optically thin environments, showing that super-Earths and sub-Neptunes can accrete their gas envelopes efficiently without the need for dense, opaque disks, challenging traditional assumptions.
Contribution
It introduces time-dependent models of optically thin planetary atmospheres, demonstrating gas accretion processes in gas-poor disks that align with observed exoplanet characteristics.
Findings
Super-Earths can accrete ~1% gas envelopes in gas-poor environments.
Envelope growth rate is similar to traditional radiative diffusion models.
Atmospheric temperature inversions can occur but do not significantly affect accretion rates.
Abstract
Models of core accretion assume that in the radiative zones of accreting gas envelopes, radiation diffuses. But super-Earths/sub-Neptunes (1-4, 2-20) point to formation conditions that are optically thin: their modest gas masses are accreted from short-lived and gas-poor nebulae reminiscent of the transparent cavities of transitional disks. Planetary atmospheres born in such environments can be optically thin to both incident starlight and internally generated thermal radiation. We construct time-dependent models of such atmospheres, showing that super-Earths/sub-Neptunes can accrete their 1%-by-mass gas envelopes, and super-puffs/sub-Saturns their 20%-by-mass envelopes, over a wide range of nebular depletion histories requiring no fine tuning. Although nascent atmospheres can exhibit stratospheric temperature inversions effected by atomic Fe and various…
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