Turbulent Disks are Never Stable: Fragmentation and Turbulence-Promoted Planet Formation
Philip F. Hopkins (Caltech/Berkeley), Jessie L. Christiansen, (SETI/Ames)

TL;DR
This paper demonstrates that turbulence in disks can cause stochastic density fluctuations leading to fragmentation and potential planet formation, even when classical stability criteria suggest the disk should be stable.
Contribution
It develops an analytic framework to predict the probability and mass spectrum of turbulent fragmentation in Keplerian disks, challenging traditional stability assumptions.
Findings
Turbulent disks can produce self-gravitating fragments despite high Toomre Q.
Sub-sonic turbulence can cause fragmentation over Myr timescales.
Cooling times >50 times the dynamical time may suppress fragmentation.
Abstract
A fundamental assumption in our understanding of disks is that when the Toomre Q>>1, the disk is stable against fragmentation into self-gravitating objects (and so cannot form planets via direct collapse). But if disks are turbulent, this neglects a spectrum of stochastic density fluctuations that can produce rare, high-density mass concentrations. Here, we use a recently-developed analytic framework to predict the statistics of these fluctuations, i.e. the rate of fragmentation and mass spectrum of fragments formed in a turbulent Keplerian disk. Turbulent disks are never completely stable: we calculate the (always finite) probability of forming self-gravitating structures via stochastic turbulent density fluctuations in such disks. Modest sub-sonic turbulence above Mach number ~0.1 can produce a few stochastic fragmentation or 'direct collapse' events over ~Myr timescales, even if Q>>1…
Peer Reviews
No public reviews on file for this paper yet. If you reviewed it on a platform where reviews are public (OpenReview, ICLR, NeurIPS, ICML), you can paste yours below so the community can read it here.
Videos
No videos yet. Explain this paper in a talk, walkthrough, or lecture? Add one.
