Superabundance of Exoplanet Sub-Neptunes Explained by Fugacity Crisis

Transiting planets with radii 2-3 R_\bigoplus are much more numerous than larger planets. We propose that this drop-off is so abrupt because at $R$ $\sim$ 3 R_\bigoplus, base-of-atmosphere pressure is high enough for the atmosphere to readily dissolve into magma, and this sequestration acts as a strong brake on further growth. The viability of this idea is demonstrated using a simple model. Our results support extensive magma-atmosphere equilibration on sub-Neptunes, with numerous implications for sub-Neptune formation and atmospheric chemistry.