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Titan’s smog clears a little
Scientists using NASAs Cassini spacecraft have
unravelled a new piece of the complex chemical processes that take place in the
atmosphere of Titan, in a paper appearing in Science on 11th May 2007.
The atmosphere of Titan is of great interest as it is the only one in the
solar system remotely like that of Earth, containing a nitrogen rich mix of
gases.
Data collected using the Cassini Plasma Spectrometer and the UK-led sensor
on it, the Electron Spectrometer, have revealed an unexpected cloud of very
heavy ions 1000km above Titan's surface.
These ions are complex organic molecules formed from methane and nitrogen
when exposed to intense sunlight, such as polycyclic aromatic hydrocarbons
(PAHs) and similar compounds containing Nitrogen. They gradually form more and
more complex molecules - reaching masses of 8000 times that of a single
Hydrogen atom, possibly up to 40,000 times (more complex than insulin).
These molecules sink towards Titan's surface, forming a group of compounds
named 'tholins' by Carl Sagan. Tholins were observed in the Urey-Miller
experiment in 1953 which demonstrated that organic molecules could be formed
from inorganic precursors. As such, they may provide the building blocks from
which life forms.
Dr Andrew Coates from UCL's Mullard Space Science Laboratory, a co-author
on the paper and lead of the ELS team, said "It's humbling to think that, with
our instrument at Titan, we may be seeing processes which were at work in
Earth's early atmosphere and which eventually led to life on Earth. It turns
out that Titan's atmosphere is an organic chemical factory on a grand scale. To
see such heavy negative ions was a big surprise for us, and is a key finding
linking processes in Titan's atmosphere to the surface of Titan itself - and
perhaps to dark, PAH-related deposits on Saturn's other moons."
"Tholins are very large, complex organic molecules thought to include
chemical precursors to life," said Dr. Hunter Waite, from the Southwest
Research Institute, and leader of Cassini's Ion Neutral Mass Spectrometer
(INMS) team. "Understanding how they form could provide valuable insight into
the origin of life in the solar system."
"The negative ions were a complete surprise," said Dr. David Young, also
an SwRI Institute scientist, and leader of the CAPS investigation. "This
suggests they may play an unexpected role in making tholins from
carbon-nitrogen precursors."
UK participation in the Cassini mission is funded by the Science and
Technology Facilities Council.
Notes for Editors
Cassini-Huygens is a joint mission with NASA, ESA, and ASI, the Italian
Space Agency. It was launched in 1997 to study Saturn and its rings and moons.
ESA contributed the Huygens probe, which was released by the Cassini mothership
in 2004. UK scientists have taken part in the development of eight of the
eighteen instruments on Cassini and Huygens.
Contacts
Julia Maddock
Science and Technology Facilities Council
Press Office
Tel +44 1793 442094
Dr Andrew Coates (at a conference)
UCL MSSL
Mobile +44 7788 448318
Summary
News image:
News Summary:
Scientists using NASA's Cassini
spacecraft have unravelled a new piece of the complex chemical processes that
take place in the atmosphere of Titan, in a paper appearing in Science on
11th May 2007.
Page last updated: 12 January 2009
by Julia Maddock