The Dynamical Interaction between Low-mass Planets and Dust Coagulation
Qiang Hou, Cong Yu, Shu-ichiro Inutsuka
TL;DR
This work analyzes how a low-mass planet embedded in a protoplanetary disk affects dust coagulation and, in turn, planetary migration. It employs a local 2D linear framework with coupled dust–gas dynamics and a single-size coagulation model to identify a planet-induced coagulation mode (CM) that can suppress dust growth in the co-orbital region and modify the dust-driven torque. A key finding is that outward migration requires a threshold stopping time $\tau$ of about $0.3$ under typical turbulence $\alpha$ and sticking efficiency, due to the phase-shifted interactions between dust density, stopping time, and radial velocity. This work links coagulation physics to pebble-driven migration, offering new insights into early planet formation and disk evolution, while noting limitations from the linear, 2D, single-size approximation that motivate future nonlinear, 3D, and full-size-distribution treatments.
Abstract
We investigate the impact of a low-mass planet on dust coagulation, and its consequent feedback on planetary migration, using a linear analysis of the coupled dust-gas hydrodynamic equations. Dust coagulation is incorporated via a single-size approximation. In the co-orbital region of the planet, we find that the growth of dust size is significantly suppressed by planet-induced coagulation modes (CMs). This effect are less pronounced with smaller stopping times, stronger gaseous turbulence or imperfect sticking. Regarding planetary migration, we find that CMs make outward migration require $τ\gtrsim 0.3$ ($τ$ is dimensionless stopping time) with typical turbulent strength and dust coagulation efficiency. We demonstrate that the torque variations are reasonable and arise from phase shifts between the density and stopping time perturbations in the coagulation modes.
