Volume 597, January 2017
|Number of page(s)||10|
|Section||Planets and planetary systems|
|Published online||03 January 2017|
Initial mass function of planetesimals formed by the streaming instability
1 Hamburg Observatory, University of
112, 21029 Hamburg, Germany
2 Lund Observatory, Department of Astronomy and Theoretical Physics, Lund University, PO Box 43, 22100 Lund, Sweden
Accepted: 2 November 2016
The streaming instability is a mechanism to concentrate solid particles into overdense filaments that undergo gravitational collapse and form planetesimals. However, it remains unclear how the initial mass function of these planetesimals depends on the box dimensions of numerical simulations. To resolve this, we perform simulations of planetesimal formation with the largest box dimensions to date, allowing planetesimals to form simultaneously in multiple filaments that can only emerge within such large simulation boxes. In our simulations, planetesimals with sizes between 80 km and several hundred kilometers form. We find that a power law with a rather shallow exponential cutoff at the high-mass end represents the cumulative birth mass function better than an integrated power law. The steepness of the exponential cutoff is largely independent of box dimensions and resolution, while the exponent of the power law is not constrained at the resolutions we employ. Moreover, we find that the characteristic mass scale of the exponential cutoff correlates with the mass budget in each filament. Together with previous studies of high-resolution simulations with small box domains, our results therefore imply that the cumulative birth mass function of planetesimals is consistent with an exponentially tapered power law with a power-law exponent of approximately −1.6 and a steepness of the exponential cutoff in the range of 0.3–0.4.
Key words: hydrodynamics / instabilities / methods: numerical / planets and satellites: formation / protoplanetary disks
© ESO 2017
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