The magnetorotational instability in debris-disc gas
Quentin Kral, Henrik Latter

TL;DR
This paper investigates whether the magnetorotational instability (MRI) can occur in debris-disc gas, potentially explaining observed mass transport, and discusses the conditions under which MRI or related MHD processes might influence disc evolution.
Contribution
It explores the viability of MRI in debris-disc gas, considering non-ideal MHD effects and magnetic field constraints, and suggests numerical simulations to clarify MRI's role.
Findings
Linear instability is viable at certain radii.
Outer disc regions may be stabilized by ambient magnetic fields.
Magnetocentrifugal winds could drive transport if MRI is suppressed.
Abstract
Debris discs are commonly swathed in gas which can be observed in UV, in fine structure lines in FIR, and in resolved maps of CO emission. Carbon and oxygen are overabundant in such gas, but it is severely depleted in hydrogen. As a consequence, its ionisation fraction is remarkably high, suggesting magnetohydrodynamic (MHD) processes may be important. In particular, the gas may be subject to the magnetorotational instability (MRI), and indeed recent modelling of Pictoris requires an anomalous viscosity to explain the gas's observed radial structure. In this paper we explore the possibility that the MRI is active in debris-disc gas and responsible for the observed mass transport. We find that non-ideal MHD and dust-gas interactions play a subdominant role, and that linear instability is viable at certain radii. However, owing to low gas densities, the outer parts of the disc…
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