The Role of Core Mass in Controlling Evaporation: the Kepler Radius Distribution and the Kepler-36 Density Dichotomy
Eric Lopez, Jonathan Fortney

TL;DR
This study models how planetary core mass influences atmospheric evaporation, explaining the Kepler-36 density contrast and predicting the distribution of sub-Neptune planets based on photo-evaporation effects.
Contribution
It introduces coupled thermal evolution and mass loss models that highlight core mass as a key factor in planetary evaporation and radius distribution, providing analytic fits for threshold XUV fluxes.
Findings
Density contrast explained by core mass differences, not irradiation.
Predicted decline of 1.8-4.0 R_earth planets within 10 days orbit.
Inner planets tend to be smaller due to photo-evaporation.
Abstract
We use models of coupled thermal evolution and photo-evaporative mass loss to understand the formation and evolution of the Kepler-36 system. We show that the large contrast in mean planetary density observed by Carter et al. (2012) can be explained as a natural consequence of photo-evaporation from planets that formed with similar initial compositions. However, rather than being due to differences in XUV irradiation between the planets, we find that this contrast is due to the difference in the masses of the planets' rock/iron cores and the impact that this has on mass loss evolution. We explore in detail how our coupled models depend on irradiation, mass, age, composition, and the efficiency of mass loss. Based on fits to large numbers of coupled evolution and mass loss runs, we provide analytic fits to understand threshold XUV fluxes for significant atmospheric loss, as a function of…
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