Authors: Graeme Lufkin and Tom Quinn
Abstract: We present the results of a suite of giant planet migration simulations using Smoothed Particle Hydrodynamics (SPH). These simulations take a disk model with an embedded planet and evolve the system for several dynamical times, measuring the rates of migration and accretion. The simulations are global, three-dimensional, include the self-gravify of the disk, have free boundary conditions, and do not prescribe a model for accretion onto the planet. These are the first simulations to include these features simultaneously. The suite covers variation in the initial planet and disk masses and numerical parameters. The disk mass varied from 0.005 to 0.09 Solar masses, and initial planet mass from 0.25 to 2 Jupiter masses. During the first few hundred years, most of the systems exhibited a constant rate of inward migration. A 1 Jupiter mass planet initially on a circular orbit at 5.2 AU in a 0.01 Solar mass disk moved inward at 10-3 AU/yr. The dependence of migration rate on disk mass was linear, as predicted by the theory of type I migration. We found no dependence on planet mass, contrary to linear theory. This is because the disk response to the planet is non-linear. The process of accretion is a more complicated function of disk and planet mass, and can depend sensitively on numerical parameters.
You can get my typeset copy here (1.1M) or in gzipped Postscript (2.1M).
Note: This paper was originally a chapter in my thesis. It has been significantly edited; see the original for even more detail.
All figures are included in the paper, and are available here in independent high-resolution bitmap form as PNGs.
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