Issue |
A&A
Volume 644, December 2020
|
|
---|---|---|
Article Number | A20 | |
Number of page(s) | 5 | |
Section | Planets and planetary systems | |
DOI | https://doi.org/10.1051/0004-6361/202039312 | |
Published online | 24 November 2020 |
Destruction of eccentric planetesimals by ram pressure and erosion
University of Duisburg-Essen, Faculty of Physics,
Lotharstr. 1,
47057
Duisburg,
Germany
e-mail: tunahan.demirci@uni-due.de
Received:
1
September
2020
Accepted:
22
October
2020
Small, pebble-sized objects and large bodies of planetesimal size both play important roles in planet formation. They form the evolutionary steps of dust growth in their own respect. However, at later times, they are also thought to provide background populations of mass that larger bodies might feed upon. What we suggest in this work is that starting at times of viscous stirring, planetesimals on eccentric orbits could simply explode as they become supersonic in comparison to small, porous planetary bodies entering Earth’s atmosphere. We present a toy model of planetesimal motion and destruction to show the key aspects of this process. The consequences are quite severe. At all times, it is shown that only planetesimals on more or less circular orbits exist in the inner disk. After the destruction of a planetesimal, the remaining matter is continuously redistributed to the pebble reservoir of the protoplanetary disk. Since destruction typically occurs at small stellar distances due to supersonic speeds, it is expected to boost pebble accretion in the inner protoplanetary disk as one of its main effects.
Key words: protoplanetary disks / planet–disk interactions / planets and satellites: dynamical evolution and stability
© ESO 2020
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