4.7 Article

Low-mass planet migration in magnetically torqued dead zones - II. Flow-locked and runaway migration, and a torque prescription

Journal

MONTHLY NOTICES OF THE ROYAL ASTRONOMICAL SOCIETY
Volume 477, Issue 4, Pages 4596-4614

Publisher

OXFORD UNIV PRESS
DOI: 10.1093/mnras/sty905

Keywords

planets and satellites: dynamical evolution and stability; planet; disc interactions; protoplanetary discs

Funding

  1. STFC [ST/M001202/1, ST/P000592/1]
  2. National Science Foundation [NSF PHY17-48958]
  3. QMUL Research-IT (King, Butcher Zalewski)
  4. DiRAC Data Centric system at Durham University
  5. BIS National E-infrastructure capital grant [ST/K00042X/1]
  6. STFC capital [ST/K00087X/1]
  7. DiRAC Operations [ST/K003267/1]
  8. Durham University
  9. Royal Society University Research Fellowship
  10. STFC [ST/P000592/1, ST/P002293/1, ST/R002363/1, ST/M001202/1, ST/R000832/1, ST/I00162X/1, ST/P002307/1, ST/R002371/1] Funding Source: UKRI

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We examine the migration of low-mass planets in laminar protoplanetary discs, threaded by large-scale magnetic fields in the dead zone that drive radial gas flows. As shown in Paper I, a dynamical corotation torque arises due to the flow-induced asymmetric distortion of the corotation region and the evolving vortensity contrast between the librating horseshoe material and background disc flow. Using simulations of laminar torqued discs containing migrating planets, we demonstrate the existence of the four distinct migration regimes predicted in Paper I. In two regimes, the migration is approximately locked to the inward or outward radial gas flow, and in the other regimes the planet undergoes outward runaway migration that eventually settles to fast steady migration. In addition, we demonstrate torque and migration reversals induced by mid-plane magnetic stresses, with a bifurcation dependent on the disc surface density. We develop a model for fast migration, and show why the outward runaway saturates to a steady speed, and examine phenomenologically its termination due to changing local disc conditions. We also develop an analytical model for the corotation torque at late times that includes viscosity, for application to discs that sustain modest turbulence. Finally, we use the simulation results to develop torque prescriptions for inclusion in population synthesis models of planet formation.

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