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Embargoed until 1:00 p.m. U.S. EST, Wednesday, November 26, 2003

Pushing out the Kuiper belt

Boulder, Colorado -- A new study by researchers at Southwest Research Institute 
(SwRI) and the Observatoire de la Côte d'Azur provides an explanation for one of 
the more mysterious aspects of the population of objects beyond Neptune. In 
doing so, it provides a unique glimpse into the proto-planetary disk from which 
the Solar System's planets formed. Results will be published in the November 27 
issue of Nature.

The Kuiper belt is a region of the Solar System that extends outward from 
Neptune's orbit, containing billions of icy objects from kilometers to thousands 
of kilometers across. It was discovered in 1992 and, since that time nearly 
1,000 objects have been cataloged. Some of these objects are very large -- the 
largest having a diameter of more than 1,000 kilometers.

As astronomers have studied this structure, a mystery has unfolded. Like most of 
the planets in the Solar System, the large Kuiper belt objects are believed to 
have been formed from smaller objects that stuck together when they collided. 
For this process to have worked in the distant regions beyond Neptune, the 
Kuiper belt would have to contain more than 10 times the amount of material than 
is in the Earth. However, telescopic surveys of this region show that it 
currently contains roughly one-tenth the mass of the Earth, or less.

To solve the puzzle, researchers have been searching for several years for a way 
to remove more than 99 percent of the Kuiper belt's material. However, Dr. 
Harold Levison (SwRI) and Dr. Alessandro Morbidelli (Observatoire de la Côte 
d'Azur of Nice, France) describe in their article, "Forming the Kuiper Belt by 
the Outerward Transport of Objects During Neptune's Migration," that the Kuiper 
belt may not have lost much mass at all.

"The mass depletion problem has been sticking in our throat for some time," says 
Levison, a staff scientist in the SwRI Space Studies Department. "It looks like 
we may finally have a possible answer."

Levison and Morbidelli argue that the proto-planetary disk from which the 
planets, asteroids and comets all formed had a heretofore unanticipated edge at 
the current location of Neptune, which is at 30 astronomical units (AU, the 
average distance between the Sun and Earth), and that the region now occupied by 
the Kuiper belt was empty. All the Kuiper belt objects we see beyond Neptune 
formed much closer to the Sun and were transported outward during the final 
stages of planet formation.

Researchers have known for 20 years that the orbits of the giant planets moved 
around as they formed. In particular, Uranus and Neptune formed closer to the 
Sun and migrated outward. Levison and Morbidelli show that Neptune could have 
pushed all the observed Kuiper belt objects outward as it migrated.

"We really didn't solve the mass depletion problem, we circumvented it," says 
Levison. "According to our work, the void beyond Neptune was probably devoid of 
objects."

However, in this model, the region interior to 30 AU contained enough material 
for the Kuiper belt objects to form. The mechanisms employed by Neptune to push 
out the Kuiper belt only affected a small fraction of the objects. These became 
the objects seen by astronomers; the rest were scattered out of the Solar System 
by Neptune. This new theory explains many of the observable features of the 
outer Solar System, including the characteristics of the orbits of the Kuiper 
belt objects and the location of Neptune.

"One of the puzzling aspects of Neptune's migration is why it stopped where it 
did," says Morbidelli. "Our new model explains this as well. Neptune migrated 
until it hit the edge of the proto-planetary disk, at which point it abruptly 
stopped."

NASA, the National Science Foundation and the Centre National de la Recherche 
Scientifique in Paris funded this research.

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