Modelling the secular evolution of proto-planetary disc dust sizes -- A comparison between the viscous and magnetic wind case
Francesco Zagaria, Giovanni P. Rosotti, Cathie J. Clarke, Beno\^it, Tabone

TL;DR
This study compares viscous and magnetic wind models for proto-planetary disc evolution, predicting distinct dust size evolution patterns that can be tested with future high-resolution observations.
Contribution
It provides the first detailed comparison of dust disc size evolution in viscous versus magnetic wind models using one-dimensional simulations.
Findings
Magnetic wind models produce compact discs with sizes remaining constant or decreasing over time.
Viscous models predict discs that grow larger with time, especially for α ≥ 10^{-3}.
Both models can fit current ALMA observations, but future data could distinguish them.
Abstract
For many years proto-planetary discs have been thought to evolve viscously: angular momentum redistribution leads to accretion and outward disc spreading. Recently, the hypothesis that accretion is due, instead, to angular momentum removal by magnetic winds gained new popularity: no disc spreading is expected in this case. In this paper, we run several one-dimensional gas and dust simulations to make predictions on the time-evolution of disc sizes \textit{in the dust} and to assess whether they can be used to understand how discs evolve. We show that viscous and magnetic wind models have very different dust disc radii. In particular, MHD wind models are compact and their sizes either remain constant or decrease with time. On the contrary, discs become larger with time in the viscous case (when ). Although current observations lack enough sensitivity to discriminate…
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