Water on Hot Rocky Exoplanets
Edwin S. Kite, Laura Schaefer

TL;DR
This paper proposes a model where hot rocky exoplanets can develop and retain long-lived, water-rich atmospheres during their evolution from sub-Neptunes, with testable predictions for JWST observations.
Contribution
It introduces a new pathway for rocky exoplanets to acquire and maintain water-dominated atmospheres through magma-atmosphere interactions during their evolution.
Findings
Long-lived H2O atmospheres are possible on 1-1.7 R_Earth planets with 10-100 day orbits.
Water atmospheres form during the transition from sub-Neptunes to rocky planets.
Most planets near the radius valley with specific sizes may still have H2O atmospheres.
Abstract
Data suggest that most rocky exoplanets with orbital period 100 d ("hot" rocky exoplanets) formed as gas-rich sub-Neptunes that subsequently lost most of their envelopes, but whether these rocky exoplanets still have atmospheres is unknown. We identify a pathway by which 1-1.7 (1-10 ) rocky exoplanets with orbital periods of 10-100 days can acquire long-lived 10-2000 bar atmospheres that are HO-dominated, with mean molecular weight 10. These atmospheres form during the planets' evolution from sub-Neptunes into rocky exoplanets. HO that is made by reduction of iron oxides in the silicate magma is highly soluble in the magma, forming a dissolved reservoir that is protected from loss so long as the H-dominated atmosphere persists. The large size of the dissolved reservoir buffers the HO atmosphere against loss after the H has dispersed.…
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