Evolution of Dust In Protoplanetary Disks With Magnetized Winds

Authors: Olcay Goksu, Ralph Pudritz, Timmy Delage

arXiv: 2611.08484v1 (astro-ph.EP)
Submitted to arXiv on 05 Nov. 2026
License: CC BY 4.0
Abstract

Observations and theory increasingly indicate that protoplanetary disks are weakly turbulent, implying that magnetized disk winds may dominate their angular momentum transport and long-term evolution. Yet dust evolution in wind-dominated disks remains poorly understood, despite its importance for planet formation. In particular, whether wind-dominated disk evolution can create regions with enhanced dust-to-gas mass ratios that enable planetesimal formation via the streaming instability is unclear. We build a parametric hybrid disk evolution model that includes turbulent accretion, wind-driven accretion, and wind-driven mass loss to investigate dust evolution in magnetized protoplanetary disks. We employ this model to carry out a parameter study in which the initial total accretion rate, the wind-driven mass loss rate, and the turbulence strength are varied. We find that although wind-dominated disks are more favorable to dust growth and concentration than turbulence-dominated disks, conditions suitable for the streaming instability arise only within the inner few au and only under the most extreme conditions: very weak turbulence ($α_\text{turb} = 10^{-5}$) where magnetized winds drive most of the accretion ($\dot{M}_\text{acc,tot} \simeq \dot{M}_\text{wind,acc}$), and wind-driven mass loss comparable to the accretion rate ($\dot{M}_\text{wind,outflow} \simeq \dot{M}_\text{acc,wind}$). Our results therefore imply that, beyond the inner few au, the parametric wind-driven evolution models considered in the literature do not by themselves produce conditions suitable for planetesimal formation via the streaming instability, motivating more physically complete models in which spontaneous, long-lived dust traps can arise.

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