Salt Finding from NASA's Cassini Hints at Ocean within Saturn Moon

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June 24, 2009

Dwayne Brown 
Headquarters, Washington 
202-358-1726 
dwayne.c.brown@xxxxxxxx 

DC Agle 
Jet Propulsion Laboratory, Pasadena, Calif. 
818-393-9011 
agle@xxxxxxxxxxxx 

RELEASE: 09-147

SALT FINDING FROM NASA'S CASSINI HINTS AT OCEAN WITHIN SATURN MOON

PASADENA, Calif. -- For the first time, scientists working on NASA's 
Cassini mission have detected sodium salts in ice grains of Saturn's 
outermost ring. Detecting salty ice indicates that Saturn's moon 
Enceladus, which primarily replenishes the ring with material from 
discharging jets, could harbor a reservoir of liquid water -- perhaps 
an ocean -- beneath its surface. 

Cassini discovered the water-ice jets in 2005 on Enceladus. These jets 
expel tiny ice grains and vapor, some of which escape the moon's 
gravity and form Saturn's outermost ring. Cassini's cosmic dust 
analyzer has examined the composition of those grains and found salt 
within them. 

"We believe that the salty minerals deep inside Enceladus washed out 
from rock at the bottom of a liquid layer," said Frank Postberg, 
Cassini scientist for the cosmic dust analyzer at the Max Planck 
Institute for Nuclear Physics in Heidelberg, Germany. Postberg is 
lead author of a study that appears in the June 25 issue of the 
journal Nature. 

Scientists on Cassini's cosmic dust detector team conclude that liquid 
water must be present because it is the only way to dissolve the 
significant amounts of minerals that would account for the levels of 
salt detected. The process of sublimation, the mechanism by which 
vapor is released directly from solid ice in the crust, cannot 
account for the presence of salt. 

"Potential plume sources on Enceladus are an active area of research 
with evidence continuing to converge on a possible salt water ocean," 
said Linda Spilker, Cassini deputy project scientist at NASA's Jet 
Propulsion Laboratory in Pasadena, Calif. "Our next opportunity to 
gather data on Enceladus will come during two flybys in November." 

The makeup of the outermost ring grains, determined when thousands of 
high-speed particle hits were registered by Cassini, provides 
indirect information about the composition of the plume material and 
what is inside Enceladus. The outermost ring particles are almost 
pure water ice, but nearly every time the dust analyzer has checked 
for the composition, it has found at least some sodium within the 
particles. 

"Our measurements imply that besides table salt, the grains also 
contain carbonates like soda. Both components are in concentrations 
that match the predicted composition of an Enceladus ocean," Postberg 
said. "The carbonates also provide a slightly alkaline pH value. If 
the liquid source is an ocean, it could provide a suitable 
environment on Enceladus for the formation of life precursors when 
coupled with the heat measured near the moon's south pole and the 
organic compounds found within the plumes." 

However, in another study published in Nature, researchers doing 
ground-based observations did not see sodium, an important salt 
component. That team notes that the amount of sodium being expelled 
from Enceladus is actually less than observed around many other 
planetary bodies. These scientists were looking for sodium in the 
plume vapor and could not see it in the expelled ice grains. They 
argue that if the plume vapor does come from ocean water the 
evaporation must happen slowly deep underground rather than as a 
violent geyser erupting into space. 

"Finding salt in the plume gives evidence for liquid water below the 
surface," said Sascha Kempf, also a Cassini scientist for the cosmic 
dust analyzer from the Max Planck Institute for Nuclear Physics. "The 
lack of detection of sodium vapor in the plume gives hints about what 
the water reservoir might look like." 

Determining the nature and origin of the plume material is a top 
priority for Cassini during its extended tour, called the Cassini 
Equinox Mission. 

"The original picture of the plumes as violently erupting 
Yellowstone-like geysers is changing," said Postberg."They seem more 
like steady jets of vapor and ice fed by a large water reservoir. 
However, we cannot decide yet if the water is currently 'trapped' 
within huge pockets in Enceladus' thick ice crust or still connected 
to a large ocean in contact with the rocky core." 

The Cassini-Huygens mission is a cooperative project of NASA, the 
European Space Agency and the Italian Space Agency. The Cassini 
cosmic dust analyzer was provided by the German Aerospace Center. The 
Cassini orbiter was designed, developed and assembled at JPL. JPL 
manages the mission for the Science Mission Directorate at NASA 
Headquarters in Washington. 

More information about the Cassini mission is available at: 



http://www.nasa.gov/cassini 

	
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