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Institute of Astronomy webpage
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Discs06 Scientific Highlights
Last Updated: 2006-07-05
The purpose of this page is to showcase some of the most exciting
results to be presented at the conference, with a particular emphasis
on those which may be of interest to the general public as well as the
scientific community. It will be updated regularly before and during
the event, as news of new results come in. If you think a story should
be added to this page, please contact Suzanne Aigrain.
Recently discovered planets should harbour fluid water
A few weeks ago, a team of scientists led by Christophe Lovis from
Geneva observatory announced the discovery of a system containing
three Neptune-mass planets (see ESO
press release from 18/05). This system is particularly interesting
because it shares many properties with out own, most notably the fact
that it has three planets of similar size close to the central star, one of
which is near the inner edge of the "habitable zone" (where liquid
water can exist at the surface of rocky or icy bodies), and an
asteroid belt.
Now, a team led by Yann Alibert at the University of Bern have
finished a detailed investigation into the past history of this
system. As illustrated schematically in the diagrams below, they have
been able to show that the inner planet, initially composed of a rocky
core with a thick gaseous enveloppe, should have had most of its
enveloppe evaporated off by radiation from the central star as it
migrated closer in. But, most interestingly, the outer two planets
should have accreted a significant amount of water ice early on, then
moved into warmer regions of the system. Some of the water is now
expected to be in the form of a fluid at very high pressure, buried
under a thick enveloppe of gas. This is the first time that
extra-solar planets have been shown to contain fluid water, albeit in
a form that is probably very different from the water oceans of our
own world.
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Schematic representation of the formation of the system,
showing the inital and present day positions of the planets (numbers
indicate distances from the star in astronomical units) together width
the material they accreted as they migrated through the system (blue:
ice, brown: rock, grey: gas) and their present day composition. The
asteroid belt is also shown.
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Present day state of the system, showing asteroid belt and
the positions and inner composition of the planets.
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Yann Alibert will give a talk entitled Extended core accretion
models of planet formation on Wednesday 19th July at
12.05 pm. For more information, he can be contacted by email.
References:
- An extrasloar planetary system with three Neptune-mass planets
Lovis, C., Mayor, M., Pepe, F., Alibert, Y. et al., Nature, Vol. 441, p. 305 (2006)
- Formation and structure of the three Neptune-mass planets system around HD69830
Alibert, Y., Baraffe, I., Benz, W. Chabrier, G. et al., to appear in Astronomy and Astrophysics
Tracing giant planets during their formation
Planets are thought to form in circumstellar disks, the disks of
gas and dust which naturally form around emerging young stars, and
from which the latter acquire the material they are made from. While
we now have a detailed picture of the evolution of these disks,
exactly how planets form within them is still under discussion. To
verify or rule out the various theoretical scenarios, observations of
planetary systems in the process of forming are needed.
Over the next few years, a number of new large interfermoetric
facilities (for example the Atacama
Large Millimeter Array or ALMA) will become available. By
combining the light of many separate telescopes pointing at the same
object (such as a young star surroundered by a disk), they will enable
us to resolve its close environment within more intricate detail
than was ever possible before. Using numerical simulations, Sebastian
Wolf from the Max Planck Institute for Astronomy in Heidleberg and
Gennaro D'Angelo of the NASA Ames Research Center have shown that ALMA
will enable us to trace young, still accreting giant planets in nearby
protoplanetary disks. Because different scenarios of planet formation
make very different predictions for what planetary systems should look
like in their early stages, these observations will provide clues as
to the mechanism(s) which actually govern planet formation.
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Simulated image of a face-on circumstellar disk situated 50
parsec away from the Earth, as it would be seen by ALMA. The most
readily observable signatures of the presence of a planet (whose orbit
is indicated by the dhaed line) are the gap it creates in the disk and
the clumb of bright, hot material near the planet itself.
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Artist's impression of ALMA.
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Sebastian Wolf will give a review talk entitled Prospects for the
detection of protoplanets on Thursday 20th July at
2.00 pm. For more information, he can be contacted by email.
References:
- On the Observability of Giant Protoplanets in Circumstellar Disks
Wolf, S., D.Angelo, G., The Astrophysical Journal, Vol. 619, p. 1114 (2005)
Gas and dust stratification in young circumstellar disks
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In the standard picture of star formation, stars form in giant
clouds of gas and dust called molecular clouds. Under the influence of
their own gravitiy, slightlly denser clumps in thes clouds collapse to
form a stellar embryo, or protostar, surrounded by an spinning
enveloppe of gas and dust which gradually settles into a thin
circumstellar disk. The heavier materials (small rocks and dust)
quickly fall to the mid-plane of the disk, while the light gaseous
material remains more diffuse above and below. It is in these
circumstellar disks that planets form, and the details of the settling
down, or stratification process are crucial in determining excatly
what type of planets can form where in the disk and how quickly.
Using the world's largest optical telescope (Keck II), a team of
astronomers led by Terence Rettig of the University of Notre
Dame were able to measure exactly how much gas and dust lies along the
line of sight to four young stars surronded by circmustellar disks,
which are very likely to be in the midst of forming planetesimals
(comets), and perhaps protoplanets and planets. By comparing the
relative amounts of gas and dust in the four objects, whise disks lie
at different inclinations, they can tell how much dust has settled
down.
These measurements allow them to deduce important information on
the conditions in the disk midplane, most importantly the degree of
turbulence. For a simple analogy closer to home, we can compare how
bright the Sun appears at noon and at Sunset. The difference in
apparent brightness is due to the number of dust particles along the
line of sight through our own atmosphere, which is much larger at
sunset because the Sun's rays have to cross more of the atmosphere to
reach us. We would be able to tell if the earth's atmosphere were
extremely turbulent (as happens in a dust storm), because then there
would be far less difference between the Sun's brightness at noon and
sunset.
Rettig and collaborators expect their results to be used by
theorists in the ongoing efforts to understand planet formation. If
the midplane of circumstellar disks is very turbulent, it is unlikely
that sufficient numbers of particles can settle and stick together to
form planetesimals. In the long run, understanding the degree of
turbulence will enable us to constrain the rate at which dust
particles of all sizes can coagulate to spur on planet growth.
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Density dust grains (10 microns, top), small dust particles (0.1 micron, middle) and gas (bottom) as a function of height above the midplane and distance from the central star, in the model proposed by Rettig and collaborators.
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Terrence Rettig will present a poster entitled Dust
stratification in young circumstellar disks which will be
displayed between Monday 17th July and Thursday
20th July. For more information, he can be contacted by email.
References:
- Dust Stratification in Young Circumstellar Disks
Rettig, T., Brittain, S., Simon, T., Gibb, E. et al., to appear in the July 20th 2006 issue of the Astrophysical Journal
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