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Pesawat luar angkasa Cassini mengungkapkan 101 Geyser lebih pada bulan
Saturnus
Menggunakan
data misi dari pesawat Cassini ilmuwan NASA telah mengidentifikasi 101 Geyser berbeda yang meletus pada
bulan Saturnus es Enceladus. Analisis mereka menunjukkan ini mungkin bagi
air untuk mencapai jalan ke permukaan.
Cassini spacecraft reveals 101 geysers and more on icy Saturn moon
Date:
July 28,
2014
Source:
NASA/Jet Propulsion Laboratory
Summary:
Scientists using mission data from NASA's Cassini
spacecraft have identified 101 distinct geysers erupting on Saturn's icy moon
Enceladus. Their analysis suggests it is possible for liquid water to reach
from the moon's underground sea all the way to its surface.
..................
Scientists using mission data from NASA's Cassini spacecraft
have identified 101 distinct geysers erupting on Saturn's icy moon Enceladus.
Their analysis suggests it is possible for liquid water to reach from the
moon's underground sea all the way to its surface.
These
findings, and clues to what powers the geyser eruptions, are presented in two
articles published in the current online edition of the Astronomical Journal.
Over a
period of almost seven years, Cassini's cameras surveyed the south polar
terrain of the small moon, a unique geological basin renowned for its four
prominent "tiger stripe" fractures and the geysers of tiny icy
particles and water vapor first sighted there nearly 10 years ago. The result
of the survey is a map of 101 geysers, each erupting from one of the tiger
stripe fractures, and the discovery that individual geysers are coincident with
small hot spots. These relationships pointed the way to the geysers' origin.
After the
first sighting of the geysers in 2005, scientists suspected that repeated
flexing of Enceladus by Saturn's tides as the moon orbits the planet had something
to do with their behavior. One suggestion included the back-and-forth rubbing
of opposing walls of the fractures generating frictional heat that turned ice
into geyser-forming vapor and liquid.
Alternate
views held that the opening and closing of the fractures allowed water vapor
from below to reach the surface. Before this new study, it was not clear which
process was the dominating influence. Nor was it certain whether excess heat
emitted by Enceladus was everywhere correlated with geyser activity.
To determine
the surface locations of the geysers, researchers employed the same process of
triangulation used historically to survey geological features on Earth, such as
mountains. When the researchers compared the geysers' locations with
low-resolution maps of thermal emission, it became apparent the greatest geyser
activity coincided with the greatest thermal radiation. Comparisons between the
geysers and tidal stresses revealed similar connections. However, these
correlations alone were insufficient to answer the question, "What
produces what?"
The answer
to this mystery came from comparison of the survey results with high-resolution
data collected in 2010 by Cassini's heat-sensing instruments. Individual
geysers were found to coincide with small-scale hot spots, only a few dozen
feet (or tens of meters) across, which were too small to be produced by
frictional heating, but the right size to be the result of condensation of
vapor on the near-surface walls of the fractures. This immediately implicated the
hot spots as the signature of the geysering process.
"Once
we had these results in hand, we knew right away heat was not causing the
geysers, but vice versa," said Carolyn Porco, leader of the Cassini
imaging team from the Space Science Institute in Boulder, Colorado, and lead
author of the first paper. "It also told us the geysers are not a
near-surface phenomenon, but have much deeper roots."
Thanks to
recent analysis of Cassini gravity data, the researchers concluded the only
plausible source of the material forming the geysers is the sea now known to
exist beneath the ice shell. They also found that narrow pathways through the
ice shell can remain open from the sea all the way to the surface, if filled
with liquid water.
In the
companion paper, the authors report the brightness of the plume formed by all
the geysers, as seen with Cassini's high-resolution cameras, changes
periodically as Enceladus orbits Saturn. Armed with the conclusion that the
opening and closing of the fractures modulates the venting, the authors
compared the observations with the expected venting schedule due to tides.
They found
the simplest model of tidal flexing provides a good match for the brightness
variations Cassini observes, but it does not predict the time when the plume begins
to brighten. Some other important effect is present and the authors considered
several in the course of their work.
The
Cassini-Huygens mission is a cooperative project of NASA, the European Space
Agency and the Italian Space Agency. The Jet Propulsion Laboratory (JPL) in
Pasadena, California, manages the mission for NASA's Science Mission
Directorate in Washington. The Cassini orbiter and its two onboard cameras were
designed, developed and assembled at JPL. The imaging team consists of
scientists from the United States, England, France and Germany. The imaging
team is based at the Space Science Institute.
Additional
details, images and an animation are available at: http://www.ciclops.org/view_event/202
More
information about Cassini is available at:
Story
Source:
The above
story is based on materials provided by NASA/Jet Propulsion Laboratory. Note: Materials may be edited
for content and length.