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A&A 441, 1-8 (2005)
DOI: 10.1051/0004-6361:20053080
The effect of MHD turbulence on massive protoplanetary disk fragmentation
S. Fromang1, 21 Astronomy Unit, Queen Mary, University of London, Mile End Road, London E1 4NS, UK
2 Institut d'Astrophysique de Paris, 98bis Bd. Arago, 75014 Paris, France
e-mail: s.fromang@qmul.ac.uk
(Received 17 March 2005 / Accepted 6 June 2005 )
Abstract
Massive disk fragmentation has been suggested to be one of the
mechanisms leading to the formation of giant planets. While it has been
heavily studied in quiescent hydrodynamic disks, the effect of MHD turbulence arising from the magnetorotational instability (MRI) has never
been investigated. This paper fills this gap and presents 3D numerical
simulations of the evolution of locally isothermal, massive and
magnetized disks. In the absence of magnetic fields, a laminar disk
fragments and clumps are formed due to the effect of self-gravity. Although
they disapear in less than a dynamical timescale in the simulations because of
the limited numerical resolution, various diagnostics suggest that they should
survive and form giant planets in real disks. When the disk is magnetized, it
becomes turbulent at the same time as gravitational instabilities develop.
At intermediate resolution, no fragmentation is observed in these turbulent
models, while a large number of fragments appear in the equivalent
hydrodynamical runs. This is because MHD turbulence reduces the strength of
the gravitational instability. As the resolution is increased, the most
unstable wavelengths of the MRI are better resolved and small scale
angular momentum transport starts to play a role: fragments are found to form
in massive and turbulent disks in that case. All of these results indicate
that there is a complicated interaction between gravitational instabilities
and MHD turbulence that influences disk fragmentation processes.
Key words: accretion, accretion disks -- magnetohydrodynamics (MHD) -- methods: numerical -- stars: planetary system: formation
© ESO 2005
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