Using planet migration and dust drift to weigh protoplanetary discs

Authors: Yinhao Wu, Clément Baruteau, Sergei Nayakshin

arXiv: 2305.01493v1 - DOI (astro-ph.EP)
15 pages, 9 figures, resubmitted to MNRAS, version addressing referee's comments

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The study by Yinhao Wu, Clément Baruteau, and Sergei Nayakshin explores the use of planet migration and dust drift to accurately weigh protoplanetary discs. The researchers utilized data from the Atacama Large Millimeter/submillimeter Array (ALMA) to spatially resolve over 200 annular structures in protoplanetary discs, many of which suggest the presence of planets. However, determining the mass of these putative planets is difficult due to degeneracies in disc physical properties. To address this issue, the researchers argue against assuming a steady-state model where the planet position is fixed and there is a constant source of dust at the outer edge of the disc. Instead, they demonstrate how planet and dust dynamics can lift degeneracies in such models. Using main disc parameters from HD 163296 with a suspected planet at approximately 86 au as an example, they ran gas and dust hydrodynamical simulations post-processed with dust radiative transfer calculations. They first found steady-state disc and planet parameters that reproduced ALMA continuum observations fairly well. However, when allowing for planet migration in the simulation with the same disc mass, they found that the planet underwent runaway migration and reached the inner disc in approximately 0.2 Myr. Further analysis showed that decreasing the disc mass slowed down planet migration but also increased radial drift of dust particles, leading to faster depletion of disc dust. The opposing constraints of planet migration and dust drift required a maximum disc mass estimate of 0.025 solar masses - much less massive than previously estimated - and for porous rather than compact dust. The authors propose extending similar analyses to other sources with suspected planetary companions to refine our understanding of protoplanetary discs' physical properties accurately. Overall, their findings highlight how considering dynamic processes such as planet migration and dust drift can improve our ability to weigh protoplanetary discs accurately - an essential step towards understanding planetary formation and evolution.
AI-generated keywords: Protoplanetary discs Planet migration Dust drift ALMA Radiative transfer

AI-generated Key Points

  • Yinhao Wu, Clément Baruteau, and Sergei Nayakshin conducted a study on accurately weighing protoplanetary discs using planet migration and dust drift.
  • Data from the Atacama Large Millimeter/submillimeter Array (ALMA) was used to identify over 200 annular structures in protoplanetary discs that suggest the presence of planets.
  • Determining the mass of these putative planets is difficult due to degeneracies in disc physical properties.
  • The researchers argue against assuming a steady-state model and demonstrate how planet and dust dynamics can lift degeneracies in such models.
  • Gas and dust hydrodynamical simulations post-processed with dust radiative transfer calculations were run to determine steady-state disc and planet parameters that reproduced ALMA continuum observations fairly well.
  • Allowing for planet migration in the simulation led to opposing constraints of planet migration and dust drift, requiring a maximum disc mass estimate of 0.025 solar masses - much less massive than previously estimated - and for porous rather than compact dust.
  • The authors propose extending similar analyses to other sources with suspected planetary companions to refine our understanding of protoplanetary discs' physical properties accurately.
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Abstract: ALMA has spatially resolved over 200 annular structures in protoplanetary discs, many of which are suggestive of the presence of planets. Constraining the mass of these putative planets is quite degenerate for it depends on the disc physical properties, and for simplicity a steady-state is often assumed whereby the planet position is kept fixed and there is a constant source of dust at the outer edge of the disc. Here we argue against this approach by demonstrating how the planet and dust dynamics can lift degeneracies of such steady-state models. We take main disc parameters from the well-known protoplanetary disc HD 163296 with a suspected planet at $R\approx 86$~au as an example. By running gas and dust hydrodynamical simulations post-processed with dust radiative transfer calculations, we first find steady-state disc and planet parameters that reproduce ALMA continuum observations fairly well. For the same disc mass, but now allowing the planet to migrate in the simulation, we find that the planet undergoes runaway migration and reaches the inner disc in $\sim 0.2$ Myr. Further, decreasing the disc mass slows down planet migration, but it then also increases the dust's radial drift, thereby depleting the disc dust faster. We find that the opposing constraints of planet migration and dust drift require the disc mass to be at most $0.025~\msun$, must less massive than previously estimated, and for the dust to be porous rather than compact. We propose that similar analysis should be extended to other sources with suspected planetary companions.

Submitted to arXiv on 02 May. 2023

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