Planet formation via pebble accretion in externally photoevaporating discs
Lin Qiao, Gavin A. L. Coleman, Thomas J. Haworth

TL;DR
This paper shows that external photoevaporation of protoplanetary discs significantly influences planet formation via pebble accretion, with shielding duration critically affecting planetary growth and final characteristics.
Contribution
It introduces the impact of external photoevaporation and shielding duration on pebble accretion-driven planet formation, highlighting environmental effects on planetary architectures.
Findings
Photoevaporation truncates outer discs, limiting pebble flux.
Shielding can preserve pebble reservoirs, enabling planet growth.
Planetary outcomes are highly sensitive to environmental shielding duration.
Abstract
We demonstrate that planet formation via pebble accretion is sensitive to external photoevaporation of the outer disc. In pebble accretion, planets grow by accreting from a flux of solids (pebbles) that radially drift inwards from the pebble production front. If external photoevaporation truncates the outer disc fast enough, it can shorten the time before the pebble production front reaches the disc outer edge, cutting off the supply of pebble flux for accretion, hence limiting the pebble mass reservoir for planet growth. Conversely, cloud shielding can protect the disc from strong external photoevaporation and preserve the pebble reservoir. Because grain growth and drift can occur quickly, shielding even on a short time-scale (<1 Myr) can have a non-linear impact on the properties of planets growing by pebble accretion. For example a planetary seed at 25 au stays at…
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Taxonomy
TopicsAstrophysics and Star Formation Studies · Phase Equilibria and Thermodynamics · Stellar, planetary, and galactic studies
