Dust trapping in protoplanetary discs after stellar flybys
Vasundhara R. Prasad, Cristiano Longarini, Cathie J. Clarke
TL;DR
This study investigates how coplanar stellar flybys perturb protoplanetary discs and influence dust dynamics with 3D SPH simulations. By modeling a two-fluid dust population in a vertically isothermal disc and tracking dust particles within flyby-induced substructures, the work shows that flybys create long-lived dust traps, particularly in prograde encounters, where dust-to-gas ratios rise significantly in dust substructures. The authors connect these overdensities to the streaming instability by converting local dust densities to a surface ratio $Z$ and comparing with the SI threshold $Z_{\rm crit}$ as a function of St; in many cases, the threshold is exceeded for tens of dynamical times after the flyby, implying potential planetesimal formation. Observationally, these results suggest that flyby-induced substructures could be identified via combined dust continuum and gas measurements, providing a mechanism to trigger SI in young discs and influence early planet formation. Overall, the work highlights stellar flybys as a plausible driver of dust trapping and planetesimal formation in dense star-forming environments, with the trapping efficiency depending on encounter geometry, periastron distance, and dust grain size.
Abstract
Stellar flybys are likely to be common in young star-forming regions and could be responsible for substructures observed in protoplanetary discs. Using three-dimensional smoothed particle hydrodynamics simulations, we study dust trapping in discs perturbed by parabolic coplanar flybys. We find that spiral structures are induced in the gas and dust discs for both prograde and retrograde encounters. By tracking individual dust particles within the flyby-induced substructures, we determine that they have a highly enhanced dust to gas ratio compared to particles in an unperturbed disc. We further find that the local dust to gas ratios in flyby-induced substructures are sufficiently high to trigger the streaming instability and hence facilitate planetesimal formation in young discs.
