A formation pathway for terrestrial planets with moderate water content involving atmospheric-volatile recycling
Jonas M\"uller, Bertram Bitsch, Aaron David Schneider

TL;DR
This study models the formation of terrestrial planets with moderate water content through pebble accretion and atmospheric-volatile recycling, explaining observed water fractions in TRAPPIST-1 planets.
Contribution
It introduces a semi-analytical model incorporating vapor recycling to explain moderate water fractions in terrestrial exoplanets.
Findings
Decreasing pebble influx leads to moderate water content in planets.
Vapor recycling significantly influences planetary water mass fractions.
Model aligns with water content observed in TRAPPIST-1 planets.
Abstract
Of the many recently discovered terrestrial exoplanets, some are expected to harbor moderate water mass fractions of a few percent. The formation pathways that can produce planets with these water mass fractions are not fully understood. Here, we use the code chemcomp, which consists of a semi-analytical 1D protoplanetary disk model harboring a migrating and accreting planet, to model the growth and composition of planets with moderate water mass fractions by pebble accretion in a protoplanetary disk around a TRAPPIST-1 analog star. This star is accompanied by seven terrestrial planets, of which the outer four planets likely contain water mass fractions of between 1\% and 10\%. We adopt a published model that considers the evaporation of pebbles in the planetary envelope, from where recycling flows can transport the volatile vapor back into the disk. We find that with this model, the…
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