Planet Migration in Nearly Laminar Disks
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If you have a question about this talk, please contact Dr Geoffroy Lesur.
Planet migration occurs as a young proto-planet
moves radially through a gaseous disk. A problem
is that the migration is inward and the timescales are generally
found to be too short for planet formation
in the standard core accretion model. Several
mechanisms have been proposed to slow the planet
migration. One mechanism involves slowing migration
by a feedback effect that is predicted to occur
if the disk turbulent viscosity is low. I describe
recent results of nonlinear simulations of planet migration in a nearly laminar disk.
This talk is part of the DAMTP Astrophysics Seminars series.
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