Pebble trapping in vortices: three-dimensional simulations
Natalie Raettig, Wladimir Lyra, Hubert Klahr

TL;DR
This study uses 3D simulations to explore how vortices in protoplanetary disks trap pebbles, revealing conditions that lead to planetesimal formation through streaming instability and potential gravitational collapse.
Contribution
First 3D simulations of pebble trapping in vortices generated by convective overstability, highlighting stability conditions and implications for planetesimal formation.
Findings
Vortex columns are perturbed at certain pebble sizes and dust ratios.
Streaming instability occurs even at very low dust-to-gas ratios.
Pebble concentrations can exceed Roche density, suggesting possible gravitational collapse.
Abstract
Disk vortices have been heralded as promising routes for planet formation due to their ability to trap significant amounts of pebbles. While the gas motions and trapping properties of two-dimensional vortices have been studied in enough detail in the literature, pebble trapping in three dimensions has received less attention, due to the higher computational demand. Here we use the Pencil Code to study 3D vortices generated by convective overstability and the trapping of solids within them. The gas is unstratified whereas the pebbles settle to the midplane due to vertical gravity. We find that for pebbles of normalized friction times of St = 0.05 and St = 1, and dust-to-gas ratio , the vortex column in the midplane is strongly perturbed. Yet, when the initial dust-to-gas ratio is decreased the vortices remain stable and function as efficient pebble traps. Streaming…
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