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Titan, Saturn's
largest natural satellite, is located 1300 million kilometres from
Earth. It is a fascinating object and a real challenge to
scientists. Indeed, Titan resembles the very young Earth before the appearance
of life, when oxygen probably existed in the form of carbon dioxide
and supplies of methane were abundant. Titan lacks the input from intense
meteoritic bombardment
which occurred on Earth during its accretion phase and delivered the
water and organics into the atmosphere. As temperatures on Titan are quite low, the chemical reactions
leading to complex prebiotic molecular chains are very slow. There is
also a deficiency of the main catalyst, liquid water. In addition,
there is very little oxygen on Titan and until very recently it was
detected exclusively in the form of traces of carbon monoxide and
dioxide. But recently we have discovered water vapour in the
atmosphere, see below. Titan's surface may be partly covered with organic deposits falling like
rain through the atmosphere. The liquid lakes would be mostly
hydrocarbons. The rest of the surface could be composed of ices and rocks. Nevertheless, within the Solar System Titan resembles our planet
most closely and it is the best possible natural laboratory to study
conditions on the primordial (very young) Earth. In 1997, ESA's artificial satellite ISO, the Infrared Space
Observatory, in geostationary orbit around the Earth since 1995,
offered a wonderful opportunity to study Titan. ISO performed
beautifully for two years and gave us fantastic new results on both
astronomical and planetary objects allowing astronomers to study the
Universe without having to worry about the interference from the
Earth's atmosphere. The ISO observations of Titan showed two narrow emission lines at
wavelengths around 40 µm (1 µm = 0.001 mm) which were due
to water vapour. This provides an explanation for the existence of
oxygen compounds on Titan. The water vapour enters Titan's atmosphere
in the form of water ice particles sputtered from the near-by
Saturnian rings and satellites, which then vaporise and combine with
hydrocarbons to produce the CO and CO2 we see today. Yet
another similarity was discovered between Titan and our home
planet! Titan's atmosphere is indeed an enigma, because no other
satellite has such characteristics. Just as for terrestrial planet
atmospheres, there are two controversial theories for the origin of
Titan's nitrogen gas envelope. Some scientists believe that the
primary atmosphere was created from outgassing from the satellite's
interior during its formation. Others say it resulted from cometary
impacts on the surface. Recent measurements of the isotopic
composition of some elements in comets show differences with those of
Titan. So the first theory is probably correct. The mystery will
perhaps not be solved before the vital clues that will be provided by
the Cassini/Hyugens
mission. But what about the surface of this fascinating object? We do not
know much about Titan's surface. It lies hidden under thick layers of
methane clouds. For a long time, it was thought that with all these organics
falling on the surface, and with ethane being the major product
in liquid form, Titan's surface must be covered entirely with
ethane-methane oceans. It has been shown since that this is not
the case. From spectroscopic measurements over almost ten years, we have
discovered that the surface of Titan is not the same when you look at
different longitudes or latitudes. The leading hemisphere is brighter
than the trailing one. We would like to know if Titan's surface is
mostly liquid (not water, but liquid hydrocarbon, also known as fuel,
falling down through the atmosphere in some sort of rain), or if is it
mostly solid, with ices and rocks sharing the landscape. From images that have been made with the Hubble Space Telescope and other
advanced techniques (like "adaptive optics") using Earth's biggest
telescopes, such as the Canada-France-Hawaii Telescope
(CFHT) and the European Southern Observatory (ESO), it has been found that both bright and dark terrain
are present on Titan's surface, an indication that it may be covered
with combinations of frozen continents and hydrocarbon
lakes. Based on observations, it would seem that water ice
covers most of Titan, but rocks, in the form of silicates and some
minor lake formations can also exist. Starting this year, a group of astronomers plans to use the ESO Very Large
Telescope (VLT) in Chile to study Titan's surface more
extensively. A fabulous landscape should appear in future images of Titan:
snow-covered mountains, dark brown soft-edged lakes and a lot of
rocks. However, the reality of this landscape will probably only be
fully revealed to us by the Huygens probe, in 2004.
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Life in the Universe
Exploring the Solar System
Space Missions to the Outer Planets and their Moons
Titan - Saturn's Largest Moon
Titan's Atmosphere and Surface
The Cassini/Huygens Mission
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Last updated July 30, 2001