Magnetorotational instability in stratified, weakly ionised accretion discs

Details Magnetorotational instability in stratified, weakly ionised accretion discs Magnetorotational instability in stratified, weakly ionised accretion discs

2003-07-14

arxiv.org/abs/astro-ph/0307272v1

Mon.Not.Roy.Astron.Soc.345:992,2003

Astronomy and Astrophysics

Astrophysics

19 pages, 13 figures, 3 tables. To appear in MNRAS

Scientific paper

10.1046/j.1365-8711.2003.07024.x

We present a linear analysis of the vertical structure and growth of the magnetorotational instability in stratified, weakly ionised accretion discs, such as protostellar and quiescent dwarf novae systems. The method includes the effects of the magnetic coupling, the conductivity regime of the fluid and the strength of the magnetic field, which is initially vertical. The conductivity is treated as a tensor and assumed constant with height. We obtained solutions for the structure and growth rate of global unstable modes for different conductivity regimes, strengths of the initial magnetic field and coupling between ionised and neutral components of the fluid. The envelopes of short-wavelenght perturbations are determined by the action of competing local growth rates at different heights, driven by the vertical stratification of the disc. Ambipolar diffusion perturbations peak consistently higher above the midplane than modes including Hall conductivity. For weak coupling, perturbations including the Hall effect grow faster and act over a more extended cross-section of the disc than those obtained using the ambipolar diffusion approximation. Finally, we derived an approximate criterion for when Hall diffusion determines the growth of the magnetorotational instability. This is satisfied over a wide range of radii in protostellar discs, reducing the extent of the magnetic `dead zone'. Even if the magnetic coupling is weak, significant accretion may occur close to the midplane, rather than in the surface regions of weakly-ionised discs.

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