|
Two
More Active Moons Around Saturn
06/13/07
This
is a compound image made from separate images of Saturn's
two moons, Tethys (to the left) and Dione (to the right),
taken by Cassini.
The
two moons are flinging great streams of particles into
space, according to data from the NASA/ESA/ASI Cassini
mission to Saturn. The discovery suggests the possibility of
some sort of geological activity, perhaps even volcanic, on
these icy worlds.
The
particles were traced to the two moons because of the
dramatic movement of electrically charged gas in the
magnetic environs of Saturn. Known as plasma, the gas is
composed of negatively charged electrons and positively
charged ions, which are atoms with one or more electrons
missing. Because they are charged, the electrons and ions
can get trapped inside a magnetic field.
Credits:
NASA/ JPL
|
Saturn’s moons Tethys
and Dione are flinging great streams of particles into space,
according to data from the NASA/ESA/ASI Cassini mission to
Saturn. The discovery suggests the possibility of some sort of
geological activity, perhaps even volcanic, on these icy
worlds. The particles were traced to the two moons
because of the dramatic movement of electrically charged gas in
the magnetic environs of Saturn. Known as plasma, the gas is
composed of negatively charged electrons and positively charged
ions, which are atoms with one or more electrons missing. Because
they are charged, the electrons and ions can get trapped inside a
magnetic field.
Saturn rotates around itself in
just 10 hours and 46 minutes. This sweeps the magnetic field and
the trapped plasma through space. Just like a child on a
fast-spinning merry-go-round, the trapped gas feels a force
trying to throw it outwards, away from the center of rotation.
Soon after Cassini reached
Saturn, in June 2004, it revealed that the planet’s hurried
rotation squashes the plasma into a disc and that great fingers
of gas are indeed being thrown out into space from the disc’s
outer edges. Hotter, more tenuous plasma then rushes in to fill
the gaps.
Now, Jim Burch of the Southwest
Research Institute, USA, and colleagues have made a careful study
of these events using the Cassini Plasma Spectrometer (CAPS).
They have shown that the direction of the ejected electrons
points back towards Tethys and Dione. “It establishes
Tethys and Dione as important sources of plasma in Saturn’s
magnetosphere,” says Burch.
Until this result, among
Saturn’s inner moons only Enceladus was known to be an
active world, with huge geysers spraying gases hundreds of
kilometers above the moon’s surface. “This new result
seems to be a strong indication that there is activity on Tethys
and Dione as well,” says Andrew Coates from the Mullard
Space Science Laboratory, University College London, and a
collaborator on this latest work.
Activity is a draw for
planetary scientists as it means that the planet has yet to reach
equilibrium, or is perhaps being supplied with energy. The
activity on Enceladus was detected first by Cassini's Dual
Technique Magnetometer (MAG). This led the flight team to
schedule a particularly close pass of Enceladus, which revealed a
wealth of data about Enceladus’ alien geysers – and
spectacular pictures, too.
“The best results arise
when we combine a variety of data sets to understand the
observations,” says Michele Dougherty, Imperial College,
London, and Principal Investigator of MAG.
In the case of Dione and
Tethys, more fly-bys are scheduled in the future, which will
allow the team and the other instruments a close-up look at the
moons. Before that happens, the team has to go back and search
for further signs of activity in the data already collected
during the Tethys and Dione flybys of 2005.
In addition, Burch says that,
having detected the electrons, they will now be on the lookout
for the ions, so that the composition of the Tethys and Dione
plasmas can be determined.
Source:
ESA

|
Scientific
Frontline®
The
Comm Center
Space
Weather Alerts
Stellar
Nights®
Imagineers
The
E.A.R.®
World
News Report
Photo,
Sketches, & Video Gallery
|