Planet Migration and Gap Formation by Tidally Induced Shocks

By R. Rafikov. 2001

143 citations recorded by the source corpus.

Gap formation in a gas disk triggered by disk-planet tidal interaction is considered. Density waves launched by the planet are assumed to be damped as a result of their nonlinear evolution leading to shock formation and its subsequent dissipation. As a consequence, wave angular momentum is transferred to the disk, leading to evolution of its surface density. Planetary migration is an important ingredient of the theory; effects of the planet-induced surface density perturbations on the migration speed are considered. A gap is assumed to form when a stationary solution for the surface density profile is no longer possible in the frame of reference migrating with the planet. An analytical limit on the planetary mass necessary to open a gap in an inviscid disk is derived. The critical mass turns out to be smaller than the mass M1 for which the planetary Hill radius equals the disk scale height by a factor of at least Q5/7 (Q is the Toomre stability parameter), depending on the strength of the migration feedback. In viscous disks the critical planetary mass could vary from ~0.2M1 to M1, depending on the disk viscosity. This implies that a gap could be formed by a planet with mass of 2-15 M⊕, depending on the disk aspect ratio, viscosity, and the planet's location in the nebula.

Subfields: Astronomy and Astrophysics, Instrumentation

View Paper: https://www.semanticscholar.org/paper/c76b943ea419f4fc53d6e2b9bdc928eb5415ce89

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In Astronomy and Astrophysics

  1. A. Morbidelli
  2. Anders Johansen
  3. Michiel Lambrechts
  4. B. Bitsch
  5. R. Nelson
  6. A. Crida
  7. W. Kley
  8. K. Kratter

In Instrumentation

  1. A. Morbidelli
  2. Michiel Lambrechts
  3. Anders Johansen
  4. B. Bitsch
  5. W. Kley
  6. R. Nelson
  7. A. Crida
  8. Hidekazu Tanaka

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