The role of density perturbation on planet formation by pebble accretion
Geoffrey Andama, Nelson Ndugu, Simon .K. Anguma, Edward Jurua

TL;DR
This study investigates how density perturbations in protoplanetary discs influence dust evolution and planet formation via pebble accretion, revealing that pressure bumps can both hinder and promote core growth depending on their location.
Contribution
It introduces global disc simulations with pressure perturbations to analyze their impact on dust dynamics and core formation, highlighting the dual role of pressure bumps in planet formation.
Findings
Pressure bumps can confine dust for millions of years.
Core formation varies with pressure profile, enabling massive cores at pressure maxima.
Inner disc regions are less conducive to planet formation in perturbed discs.
Abstract
Protoplanetary discs exhibit a diversity of gaps and rings of dust material, believed to be a manifestation of pressure maxima commonly associated with an ongoing planet formation and several other physical processes. Hydrodynamic disc simulations further suggest that multiple dust ring-like structures may be ubiquitous in discs. In the recent past, it has been shown that dust rings may provide a suitable avenue for planet formation. We study how a globally perturbed disc affects dust evolution and core growth by pebble accretion. We performed global disc simulations featuring a Gaussian pressure profile, in tandem with global perturbations of the gas density, mimicking wave-like structures, and simulated planetary core formation at pressure minima and maxima. With Gaussian pressure profiles, grains in the inside disc regions were extremely depleted in the first 0.1 Myrs of disc…
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.
