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Date: Thu, 03 May 2007 13:34:04 -0700
From: NASA Jet Propulsion Laboratory <[EMAIL PROTECTED]>
To: "[EMAIL PROTECTED]" <[EMAIL PROTECTED]>
Subject: NASA Antenna Cuts Mercury to Core, Solves 30 Year Mystery

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Dwayne Brown/Tabatha Thompson 202-358-1726/3895
NASA Headquarters, Washington

News Release: 2007-050                                               May 3, 2007

NASA Antenna Cuts Mercury to Core, Solves 30 Year Mystery

Researchers working with high-precision planetary radars, including the 
Goldstone Solar System Radar of NASA's Jet Propulsion Laboratory, Pasadena, 
Calif., have discovered strong evidence that the planet Mercury has a molten 
core. The finding explains a more than three-decade old planetary mystery that 
began with the flight of JPL's Mariner 10 spacecraft. The research appears in 
this week's issue of the journal Science.

Launched in Nov. 1973, Mariner 10 made three close approaches to Mercury in 
1974 and 75.  Among its discoveries was that Mercury had its own weak magnetic 
field -- about one percent as strong as that found on Earth.

"Scientists had not expected to find a magnetic field at Mercury," said Professor 
Jean-Luc Margot of Cornell University, Ithaca, N.Y., leader of the research team.  "Planetary 
magnetic fields are associated with molten cores, and the prevailing theory was the planet was too 
small to have a molten core."

Scientists theorized that Mercury consisted of a silicate mantle surrounding a 
solid iron core. This iron was considered solid -- or so the theory went -- 
because small planets like Mercury cool off rapidly after their formation. If 
Mercury followed this pattern, then its core should have frozen long ago.

Many believed the Mercury mystery would only be resolved if and when a 
spacecraft landed on its aggressively toasty surface. Then, in 2002, scientists 
began pointing some of the most powerful antennas on our planet at Mercury in 
an attempt to find the answer.

"On 18 separate occasions over the past five years, we used JPL's Goldstone 70-meter 
[230-foot] antenna to fire a strong radar signal at Mercury," said Planetary Radar Group 
Supervisor Martin Slade of JPL, a co-author of the paper. "Each time, the radar echoes from 
the planet were received about 10 minutes later at Goldstone and another antenna in West 
Virginia."

Measuring the echo of particular surface patterns from the surface of Mercury 
and how long they took to reproduce at both Goldstone and the Robert C. Byrd 
Green Bank Telescope in West Virginia allowed scientists to calculate Mercury's 
spin rate to an accuracy of one-thousandth of a percent.  The effect was also 
verified with three more independent radar observations of Mercury transmitted 
from the National Science Foundation's Arecibo Observatory in Puerto Rico.

With these data the science team was able to detect tiny twists in Mercury's 
spin as it orbited the sun. These small variations were double what would be 
expected for a completely solid body. This finding ruled out a solid core, so 
the only logical explanation remaining was that the core -- or at the very 
least the outer core -- is molten and not forced to rotate along with its shell.

Maintaining a molten core over billions of years requires that it also contain 
a lighter element, such as sulfur, to lower the melting temperature of the core 
material. The presence of sulfur supports the idea that radial mixing, or the 
combining of elements both close to the sun and farther away, was involved in 
Mercury's formation process.

"The chemical composition of Mercury's core can provide important clues about the processes 
involved in planet formation," said Margot. "It is fundamental to our understanding of 
how habitable worlds -- planets like our own -- form and evolve."

Mercury still has its share of mysteries. Some may be solved with the NASA spacecraft 
Messenger, launched in 2004 and expected to make its first Mercury flyby in 2008. The 
spacecraft will then begin orbiting the planet in 2011. "It is our hope that 
Messenger will address the remaining questions that we cannot address from the 
ground," said Margot.

The study's other co-authors include Stan Peale of the University of Santa 
Barbara in California; Raymond Jurgens, a JPL engineer, and Igor Holin of the 
Space Research Institute in Moscow, Russia.

The Goldstone antenna is part of NASA's Deep Space Network Goldstone station in 
Southern California's Mojave Desert.  Goldstone's 70-meter diameter antenna is 
capable of tracking a spacecraft traveling more than 16 billion kilometers (10 
billion miles) from Earth. The surface of the 70-meter reflector must remain 
accurate within a fraction of the signal wavelength, meaning that the precision 
across the 3,850-square-meter (41,400-square-foot) surface is maintained within 
one centimeter (0.4 inch).

For more information about NASA and agency programs on the Internet, visit:

http://www.nasa.gov


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