The first study was an overview of the four exoplanet candidates, covered by John Timmer. The
second set of observations focused on one of the four planet
candidates, HR 8799c. Quinn Konopacky, Travis Barman, Bruce Macintosh,
and Christian Marois performed a detailed spectral analysis of the
atmosphere of the possible exoplanet. They compared their findings to
the known properties of a brown dwarf and concluded that they don't
match—it is indeed a young planet. Chemical differences between HR 8799c
and its host star led the researchers to conclude the system likely
formed in the same way the Solar System did.
The HR 8799 system was one of the first where direct imaging of the
exoplanets was possible; in most cases, the evidence for a planet's
presence is indirect. (See the Ars overview of exoplanet science
for more.) This serendipity is possible for two major reasons: the
system is very young, and the planet candidates orbit far from their
host star.
The young age means the bodies orbiting the system still retain heat
from their formation and so are glowing in the infrared; older planets
emit much less light. That makes it possible to image these planets at
these wavelengths. (We mostly image planets in the Solar System using
reflected sunlight, but that's not a viable detection strategy at these
distances). A large planet-star separation means that the star's light
doesn't overwhelm the planets' warm glow. Astronomers are also assisted
by HR 8799's relative closeness to us—it's only about 130 light-years
away.
However, the brightness of the exoplanet candidates also obscures
their identity. They are all much larger than Jupiter—each is more than 5
times Jupiter's mass, and the largest could be 35 times greater. That,
combined with their large infrared emission, could mean that they are
not planets but brown dwarfs: star-like objects with insufficient mass
to engage in hydrogen fusion. Since brown dwarfs can overlap in size and
mass with the largest planets, we haven't been certain that the objects
observed in the HR 8799 system are planets.
For this reason, the two recent studies aimed at measuring the
chemistry of these bodies using their spectral emissions. The Palomar
study described yesterday provided a broad, big-picture view of the
whole HR 8799 system. By contrast, the second study used one of the
10-meter Keck telescopes for a focused, in-depth view of one object:
HR 8799c, the second-farthest out of the four.
The researchers measured relatively high levels of carbon monoxide (CO) and water (H2O,
just in case you forgot the formula), which were present at levels well
above the abundance measured in the spectrum of the host star.
According to the researchers, this difference in chemical composition
indicated that the planet likely formed via "core accretion"— the
gradual, bottom-up accumulation of materials to make a planet—rather
than a top-down fragmentation of the disk surrounding the newborn star.
The original disk in this scenario would have contained a lot of ice
fragments, which merged to make a world relatively high in water
content.
In many respects, HR 8799c seemed to have properties between brown
dwarfs and other exoplanets, but the chemical and gravitational analyses
pushed the object more toward the planet side. In particular, the size
and chemistry of HR 8799c placed its surface gravity lower than expected
for a brown dwarf, especially when considered with the estimated age of
the star system. While this analysis says nothing about whether the
other bodies in the system are planets, it does provide further hints
about the way the system formed.
One final surprise was the lack of methane (CH4) in
HR 8799c's atmosphere. Methane is a chemical component present in all
the Jupiter-like planets in our Solar System. The authors argued that
this could be due to vigorous mixing of the atmosphere, which is
expected because the exoplanet has higher temperatures and pressures
than seen on Jupiter or Neptune. This mixing could enable reactions that
limit methane formation. Since the HR 8799 system is much younger than
the Solar System—roughly 30 million years compared with 4.5 billion
years—it's uncertain how much this chemical balance may change over
time.
These new observations of HR 8799 could help reveal a lot about
planet formation in general. In particular, the core-accretion model is
widely thought to be the path the Solar System followed, but that may
not be the case in other exosolar systems. Measuring the atmospheric
composition of a young, large, hot exoplanet such as HR 8799c is a
significant step in learning about the possible ways planets form, and
it could help us understand much about the assumptions—correct and
incorrect—that go into our models.
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9 years ago
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