Thanatology in protoplanetary discs - The combined influence of Ohmic, Hall, and ambipolar diffusion on dead zones
Abstract
Protoplanetary discs are poorly ionised due to their low temperatures and high column
densities and are therefore subject to three “non-ideal” magnetohydrodynamic (MHD)
effects: Ohmic dissipation, ambipolar diffusion, and the Hall effect. The existence of
magnetically driven turbulence in these discs has been a central question since the
discovery of the magnetorotational instability (MRI). Early models considered Ohmic
diffusion only and led to a scenario of layered accretion, in which a magnetically “dead”
zone in the disc midplane is embedded within magnetically “active” surface layers at
distances of about 1–10 au from the central protostellar object. Recent work has suggested
that a combination of Ohmic dissipation and ambipolar diffusion can render both the
midplane and surface layers of the disc inactive and that torques due to magnetically
driven outflows are required to explain the observed accretion rates. We reassess this
picture by performing three-dimensional numerical simulations that include all three
non-ideal MHD effects for the first time. We find that the Hall effect can generically
“revive” dead zones by producing a dominant azimuthal magnetic field and a large-scale
Maxwell stress throughout the midplane, provided that the angular velocity and magnetic
field satisfy Ω·B > 0. The
attendant large magnetic pressure modifies the vertical density profile and substantially
increases the disc scale height beyond its hydrostatic value. Outflows are produced but
are not necessary to explain accretion rates ≲
10-7 M⊙ yr-1. The flow in the disc midplane
is essentially laminar, suggesting that dust sedimentation may be efficient. These results
demonstrate that if the MRI is relevant for driving mass accretion in protoplanetary
discs, one must include the Hall effect to obtain even qualitatively correct results.
Origin : Publication funded by an institution
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