Coagulation Instability in Protoplanetary Disks: A Novel Mechanism Connecting Collisional Growth and Hydrodynamical Clumping of Dust Particles
Ryosuke T. Tominaga, Shu-ichiro Inutsuka, and Hiroshi Kobayashi

TL;DR
This paper introduces coagulation instability, a new mechanism in protoplanetary disks that concentrates dust particles rapidly, potentially facilitating planetesimal formation by linking dust growth and hydrodynamical clumping.
Contribution
The study proposes and analyzes coagulation instability as a novel process that enhances dust concentration in early disk evolution, bridging collisional growth and hydrodynamical effects.
Findings
Growth timescale is a few tens of orbital periods.
Instability persists even in dust-depleted regions.
Dust concentration can trigger further instabilities.
Abstract
We present a new instability driven by a combination of coagulation and radial drift of dust particles. We refer to this instability as ``coagulation instability" and regard it as a promising mechanism to concentrate dust particles and assist planetesimal formation in the very early stages of disk evolution. Because of dust-density dependence of collisional coagulation efficiency, dust particles efficiently (inefficiently) grow in a region of positive (negative) dust density perturbations, which lead to a small radial variation of dust sizes and as a result radial velocity perturbations. The resultant velocity perturbations lead to dust concentration and amplify dust density perturbations. This positive feedback makes a disk unstable. The growth timescale of coagulation instability is a few tens of orbital periods even when dust-to-gas mass ratio is of the order of . In a…
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