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Fig. 5

image

Radial distribution (averaged over azimuth) of the dust particles as a function of time for the different planetary masses and for three representative particle sizes. The 10 M planet is able to stop the pebbles efficiently, thus creating a transition disk, suggesting that the pebble isolation mass can be less than 10 M. The Stokes numbers at the planet location from left to right are 0.08, 1.23, and 67.2 after 100 planetary orbits, respectively.

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