Volume 555, July 2013
|Number of page(s)||5|
|Section||Planets and planetary systems|
|Published online||08 July 2013|
Photophoresis boosts giant planet formation
Faculty of Physics, University of Duisburg-Essen,
2 The University of Texas at Austin, Department of Astronomy, 2515 Speedway Dr. Stop 1400, Austin, TX 78712, USA
Accepted: 17 June 2013
In the core accretion model of giant planet formation, a solid protoplanetary core begins to accrete gas directly from the nebula when its mass reaches ~5 M⊕. The protoplanet has at most a few million years to reach runaway gas accretion, as young stars lose their gas disks after 10 million years at the latest. Yet gas accretion also brings small dust grains entrained in the gas into the planetary atmosphere. Dust accretion creates an optically thick protoplanetary atmosphere that cannot efficiently radiate away the kinetic energy deposited by incoming planetesimals. A dust-rich atmosphere severely slows down atmospheric cooling, contraction, and inflow of new gas, in contradiction to the observed timescales of planet formation. Here we show that photophoresis is a strong mechanism for pushing dust out of the planetary atmosphere due to the momentum exchange between gas and dust grains. The thermal radiation from the heated inner atmosphere and core is sufficient to levitate dust grains and to push them outward. Photophoresis can significantly accelerate the formation of giant planets.
Key words: planets and satellites: formation / protoplanetary disks / methods: numerical
© ESO, 2013
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