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      Gravito-turbulence and the excitation of small-scale parametric instability in astrophysical discs

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          Abstract

          Young protoplanetary discs and the outer radii of active galactic nucleii may be subject to gravitational instability and, as a consequence, fall into a `gravitoturbulent' state. While in this state, appreciable angular momentum can be transported. Alternatively, the gas may collapse into bound clumps, the progenitors of planets or stars. In this paper, we numerically characterize the properties of 3D gravitoturbulence, focussing especially on its dependence on numerical parameters (resolution, domain size) and its excitation of small-scale dynamics. Via a survey of vertically stratified shearing box simulations with PLUTO and RODEO, we find (a) evidence that certain gravitoturbulent properties are independent of horizontal box size only when the box is larger than \(\simeq 40 H_0\), where \(H_0\) is the height scale, (b) at high resolution, small-scale isotropic turbulence appears off the midplane around \(z\simeq 0.5 -1 H_0\), and (c) this small-scale dynamics results from a parametric instability, involving the coupling of inertial waves with a large-scale axisymmetric epicyclic mode. This mode oscillates at a frequency close to \(\Omega\) and is naturally excited by gravito-turbulence, via a nonlinear process to be determined. The small-scale turbulence we uncover has potential implications for a wide range of disc physics, e.g. turbulent saturation levels, fragmentation, turbulent mixing, and dust settling.

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          Gravito-turbulence in irradiated protoplanetary discs

          Using radiation hydrodynamics simulations in a local stratified shearing box with realistic equations of state and opacities, we explored the outcome of self-gravity at 50 AU in a protoplanetary disc irradiated by the central star. We found that gravito-turbulence is sustained for a finite range of the surface density, from \(\sim 80\) to \(\sim\) 250 gcm\(^{-2}\). The disk is laminar below the range while fragments above it. In the range of gravito-turbulence, the Toomre parameter decreases monotonically from \(\sim 1\) to \(\sim 0.7\) as the surface density increases while an effective cooling time is almost constant at \(\sim 4\) in terms of the inverse of the orbital frequency. The turbulent motions are supersonic at all heights, which dissipates through both shock waves and compressional heating. The compressional motions, occurring near the midplane, create upward flows, which not only contribute to supporting the disc but also to transporting the dissipated energy to the disc surfaces. The irradiation does not affect much the gravito-turbulence near the midplane unless the grazing angle is larger than 0.32. We also show that a simple cooling function with a constant cooling time does not approximate the realistic cooling.
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            Author and article information

            Journal
            2017-06-20
            Article
            1706.06537
            a188761e-d9c1-4d6c-984d-96bc5cc1c527

            http://arxiv.org/licenses/nonexclusive-distrib/1.0/

            History
            Custom metadata
            22 pages, 19 figures, accepted for publication in MNRAS
            astro-ph.EP astro-ph.HE

            Planetary astrophysics,High energy astrophysical phenomena
            Planetary astrophysics, High energy astrophysical phenomena

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