Forming Planetesimals by Gravitational Instability: I. The Role of the Richardson Number in Triggering the Kelvin-Helmholtz Instability
Aaron T. Lee (UCB), Eugene Chiang (UCB), Xylar Asay-Davis (LANL),, Joseph Barranco (SFSU)

TL;DR
This study investigates how the Richardson number influences the Kelvin-Helmholtz instability in dust-rich disks, revealing conditions that favor planetesimal formation through gravitational instability.
Contribution
It provides the first detailed analysis of the Richardson number's role in triggering Kelvin-Helmholtz instability in dust layers, highlighting its dependence on dust-to-gas ratio.
Findings
Critical Richardson number increases with dust-to-gas ratio.
Solar metallicity disks can resist KHI at Ri ~ 0.2.
Gravitational instability feasible in more massive or metal-rich disks.
Abstract
Gravitational instability (GI) of a dust-rich layer at the midplane of a gaseous circumstellar disk is one proposed mechanism to form planetesimals, the building blocks of rocky planets and gas giant cores. Self-gravity competes against the Kelvin-Helmholtz instability (KHI): gradients in dust content drive a vertical shear which risks overturning the dusty subdisk and forestalling GI. To understand the conditions under which the disk can resist the KHI, we perform 3D simulations of stratified subdisks in the limit that dust particles are small and aerodynamically well coupled to gas. This limit screens out the streaming instability and isolates the KHI. Each subdisk is assumed to have a vertical density profile given by a spatially constant Richardson number Ri. We vary Ri and the midplane dust-to-gas ratio mu and find that the critical Richardson number dividing KH-unstable from…
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