On the Dust Substructures Triggered by Two Super-Earths Migrating in Low-viscosity Disks
Zijia Cui, Ewa Szuszkiewicz

TL;DR
This study uses hydrodynamic simulations to explore how two migrating super-Earths in a low-viscosity disk create dust substructures, potentially aiding planetesimal formation and influencing planetary system architectures.
Contribution
It reveals specific dust accumulation regions caused by planetary migration and resonance, highlighting their role in planetesimal formation in low-viscosity disks.
Findings
Dust rings form between planetary orbits with high dust-to-gas ratios.
Outer broad dust features evolve into multiple rings over time.
Dust substructures are conducive to planetesimal formation.
Abstract
We investigate dust substructure formation induced by two super-Earths migrating in a low-viscosity disk with single-size dust grains selected from the submillimeter to centimeter range of sizes. The orbital evolution of planets takes place in the vicinity of the 2:1 commensurability, which allows to determine, in addition to the dust substructure properties, the dust impact on the rate of migration, the resonance capture, the libration overstability and the outcome of passage through the commensurability. Using two-dimensional two-fluid hydrodynamic simulations with dust feedback and dust diffusion taken into account, we identify two specific regions in the disk where the accumulation of dust particles is significant, leading to dust substructure formation with the dust-to-gas ratio values close to or even higher than 1 for large grains. The first region, with a narrow dust ring, is…
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