Abstract

We study the dynamics of a viscous protoplanetary disc hosting a population of dust grains with a range of sizes. We compute steady-state solutions, and show that the radial motion of both the gas and the dust can deviate substantially from those for a single-size dust population. Although the aerodynamic drag from the dust on the gas is weaker than in the case where all grains are optimally coupled to the gas, the cumulative "back-reaction" of the dust particles can still alter the gas dynamics significantly. In typical protoplanetary discs, the net effect of the dust back-reaction decreases the gas accretion flow compared to the dust-free (viscous) case, even for dust-to-gas ratios of order $1\%$. In the outer disc, where dust grains are typically less strongly coupled to the gas and settle towards the midplane, the dust back-reaction can even drive outward gas flow. Moreover, the radial inward drift of large grains is reduced below the gas motion in the inner disc regions, while small dust grains follow the gas dynamics over all the disc extent. The resulting dust and gas dynamics can give rise to observable structures, such as gas and dust cavities. Our results show that the dust back-reaction can play a major role in both the dynamics and observational appearance of protoplanetary discs, and cannot be ignored in models of protoplanetary disc evolution.

Highlights

  • Solids in protoplanetary discs represent the primary building blocks of both rocky planets and cores of gas giants and play an essential role in regulating most of the thermal features of discs (Testi et al 2014)

  • We study the dynamics of a viscous protoplanetary disc hosting a population of dust grains with a range of sizes

  • Our analysis clearly shows that the cumulative interaction between gas and dust grains of different sizes has a non-negligible effect on the evolution of both phases in typical protoplanetary discs

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Summary

Introduction

Solids in protoplanetary discs represent the primary building blocks of both rocky planets and cores of gas giants and play an essential role in regulating most of the thermal features of discs (Testi et al 2014). At the beginning of the star formation process, dust particles are well mixed with the gas and the dust-to-gas ratio is expected to be uniform. Even during the early phases of protostellar collapse, before protoplanetary discs are formed, the solid component is expected to evolve significantly from typical ISM dust to a population of solids characterized by a wider range of sizes (Weidenschilling 1980; Kim, Martin & Hendry 1994). Large dust grains with size 1 μm couple more loosely to the turbulent fluctuations of the gas. As a result, they segregate spatially, concentrate locally, and increase the local dust-to-gas ra-

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