Boss' model disk after 205 years of evolution, courtesy of Alan Boss.
Credit: Alan Boss
New work from Carnegie's Alan Boss offers a
potential solution to a longstanding problem in the prevailing theory of
how rocky planets formed in our own Solar System, as well as in others.
The snag he's untangling: how dust grains in the matter orbiting a
young protostar avoid getting dragged into the star before they
accumulate into bodies large enough that their own gravity allows them
to rapidly attract enough material to grow into planets. The study is
published by The Astrophysical Journal.
In the early stages of their formation, stars are surrounded by
rotating disks of gas and dust. The dust grains in the disk collide and
aggregate to form pebbles, which grow into boulders, and so on
increasing in size through planetesimals, planetary embryos, and finally
rocky terrestrial planets. But there are some difficult outstanding
questions raised by this theory. One of these is that the pressure
gradient of the gas in the disk would create a headwind that would
spiral the pebbles and boulders inward toward the young protostar, where
they would be destroyed.
The problem is most acute in bodies that are between 1 and 10 meters
in radius, because they would be most susceptible to the gas drag. If
too many particles in this size range were lost, there wouldn't be
enough remaining to collide with each other and accumulate into
planetesimals and, eventually, planets.
Observations of young stars that are still surrounded by their gas
disks demonstrate that those similar in size to our own Sun often
undergo periodic explosive bursts, about 100 years in duration, during
which the star's luminosity increases. More importantly, these events
can be linked to a period of gravitational instability in the disk.
Boss's new work shows that such a phase can scatter the at-risk 1- to
10-meter bodies outward away from the developing star, rather than
inward toward it.
Recent work has shown the presence of spiral arms around young stars,
similar to those thought to be involved in the short-term disruptions
in the disk. The gravitational forces of these spiral arms could scatter
outward the problematic boulder-sized bodies, allowing them to
accumulate rapidly to form planetesimals large enough that gas drag is
no longer a problem. Boss's modeling techniques hone in on the idea that
spiral arms might be able to answer the question of how a developing
solar system avoids losing too many larger bodies before the boulders
have a chance to grow into something bigger.
"This work shows that boulder-sized particles could, indeed, be
scattered around the disk by the formation of spiral arms and then avoid
getting dragged into the protostar at the center of the developing
system," Boss explained. "Once these bodies are in the disk's outer
regions, they are safe and able to grow into planetesimals."
Smaller particles, however, ranging between 1 and 10 centimeters, are
much more likely to be accreted back into the protostar and lost,
regardless of spiral arm formation, Boss' models show.
"While not every developing protostar may experience this kind of
short-term gravitational disruption phase, it is looking increasingly
likely that they may be much more important for the early phases of
terrestrial planet formation than we thought," Boss added.
This work was partially supported by NASA.
Story Source:
The above post is reprinted from
materials provided by
Carnegie Institution.
Note: Materials may be edited for content and length.
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