Volume 557, September 2013
|Number of page(s)||4|
|Published online||14 August 2013|
Fluffy dust forms icy planetesimals by static compression
1 Department of Astronomical ScienceSchool of Physical Sciences, Graduate University for Advanced Studies (SOKENDAI), Mitaka, 181-8588, Tokyo, Japan
2 National Astronomical Observatory of Japan, Mitaka, 181-8588 Tokyo, Japan
3 Institute of Low Temperature Science, Hokkaido University, Kita, 060-0819 Sapporo, Japan
4 Department of Earth and Planetary Sciences, Tokyo Institute of Technology, Meguro, 152-8551 Tokyo, Japan
5 Planetary Exploration Research Center, Chiba Institute of Technology, Narashino, 275-0016 Chiba, Japan
Received: 26 June 2013
Accepted: 30 July 2013
Context. Several barriers have been proposed in planetesimal formation theory: bouncing, fragmentation, and radial drift problems. Understanding the structure evolution of dust aggregates is a key in planetesimal formation. Dust grains become fluffy by coagulation in protoplanetary disks. However, once they are fluffy, they are not sufficiently compressed by collisional compression to form compact planetesimals.
Aims. We aim to reveal the pathway of dust structure evolution from dust grains to compact planetesimals.
Methods. Using the compressive strength formula, we analytically investigate how fluffy dust aggregates are compressed by static compression due to ram pressure of the disk gas and self-gravity of the aggregates in protoplanetary disks.
Results. We reveal the pathway of the porosity evolution from dust grains via fluffy aggregates to form planetesimals, circumventing the barriers in planetesimal formation. The aggregates are compressed by the disk gas to a density of 10-3 g/cm3 in coagulation, which is more compact than is the case with collisional compression. Then, they are compressed more by self-gravity to 10-1 g/cm3 when the radius is 10 km. Although the gas compression decelerates the growth, the aggregates grow rapidly enough to avoid the radial drift barrier when the orbital radius is ≲6 AU in a typical disk.
Conclusions. We propose a fluffy dust growth scenario from grains to planetesimals. It enables icy planetesimal formation in a wide range beyond the snowline in protoplanetary disks. This result proposes a concrete initial condition of planetesimals for the later stages of the planet formation.
Key words: planets and satellites: formation / methods: analytical / protoplanetary disks
© ESO, 2013
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