Dust rings as a footprint of planet formation in a protoplanetary disk
Kazuhiro D. Kanagawa, Takayuki Muto, Hidekazu Tanaka

TL;DR
This study uses hydrodynamic simulations to explore how dust rings form and evolve around migrating planets in protoplanetary disks, revealing that ring morphology changes can indicate planet formation history.
Contribution
It demonstrates that dust rings do not always follow migrating planets and that their evolving structure can serve as footprints of planet formation and migration.
Findings
Initial dust rings remain stationary at low viscosity.
A new ring forms near the migrating planet from leaking dust.
Asymmetric structures emerge in dust rings with growing planets.
Abstract
Relatively large dust grains (referred to as pebbles) accumulate at the outer edge of the gap induced by a planet in a protoplanetary disk, and a ring structure with a high dust-to-gas ratio can be formed. Such a ring has been thought to be located right outside of the planet orbit. We examined the evolution of the dust ring formed by a migrating planet, by performing two-fluid (gas and dust) hydrodynamic simulations. We found that the initial dust ring does not follow the migrating planet and remains at the initial location of the planet in the cases with a low viscosity of . The initial ring is gradually deformed by viscous diffusion, and a new ring is formed in the vicinity of the migrating planet, which developes from the trap of the dust grains leaking from the initial ring. During this phase, two rings co-exist outside the planet orbit. This phase can continue…
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