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Deep Impact Turns Up Cometary Ice [science news item]

samoth

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Deep Impact Turns Up Cometary Ice

Summary - (Thu, 02 Feb 2006) When NASA's Deep Impact spacecraft smashed into Comet Tempel 1 last summer, it helped reveal just what's inside a comet. The spacecraft also photographed three distinct patches of water ice on the surface of the comet. While Tempel 1 has a surface area of about 116 square kilometres (45 square miles), these patches of ice only cover about 6% of the comet's surface. It appears that the comet's jets were once inside, but slowly became uncovered over time.

Full Story - Comet Tempel 1, which created a flamboyant Fourth of July fireworks display in space last year, is covered with a small amount of water ice. These results, reported by members of NASA's Deep Impact team in an advanced online edition of Science, offer the first definitive evidence of surface ice on any comet.

deep_cometry-1.jpg


"We have known for a long time that water ice exists in comets, but this is the first evidence of water ice on comets," said Jessica Sunshine, Deep Impact co-investigator and lead author of the Science article.
Tempel I

A chief scientist with Science Applications International Corporation who holds three Brown University degrees, Sunshine said the discovery offers important insight into the composition of comets - small, Sun-orbiting space travelers that are believed to be leftovers from the formation of the solar system.

"Understanding a comet's water cycle and supply is critical to understanding these bodies as a system and as a possible source that delivered water to Earth," she said. "Add the large organic component in comets and you have two of the key ingredients for life."

The findings help satisfy one of the major goals of the Deep Impact mission: Find out what is on the inside - and outside - of a comet.

To that end, NASA's Jet Propulsion Laboratory teamed with the University of Maryland to slam a space probe into Tempel 1, then analyze materials from the comet's surface and interior. On July 4, 2005, mission members hit their mark when the copper-tipped probe collided with Tempel 1 and created a spectacular extraterrestrial explosion 83 million miles from Earth.

Since then, the Deep Impact team has reported a few key findings. These include an abundance of organic matter in Tempel 1's interior as well as its likely origins - the region of the solar system now occupied by Uranus and Neptune.

According to the new research in Science, the comet's surface features three pockets of thin ice. The area the ice covers is small. The surface area of Tempel 1 is roughly 45 square miles or 1.2 billion square feet. The ice, however, covers roughly 300,000 square feet. And only 6 percent of that area consists of pure water ice. The rest is dust.

"It's like a seven-acre skating rink of snowy dirt," said Peter Schultz, professor of geological sciences at Brown, Deep Impact co-investigator and co-author on the Science paper.

Sunshine, Schultz and the rest of the team arrived at their findings by analyzing data captured by an infrared spectrometer, an optical instrument that uses light to determine the composition of matter.

Based on this spectral data, it appears that the surface ice used to be inside Tempel 1 but became exposed over time. The team reports that jets - occasional blasts of dust and vapor - may send this surface ice, as well as interior ice, to the coma, or tail, of Tempel 1.

"So we know we're looking at a geologically active body whose surface is changing over time," Schultz said. "Now we can begin to understand how and why these jets erupt."

NASA funded the work. For more information on Deep Impact, visit the JPL Web site.

Original Source: Brown University



:cow:
 
Excuse my limited knowledge in this but when they say water ice, do they mean oxygenated water? Also when they stated they found organic material, are they talking about methane type material from previous lifeforms albeit plant, animal, or bacterial?
 
Here is the full text of Dr. A'Hearn's first refereed paper of the results of Deep Impact's collision with Tempel 1.

http://www.sciencemag.org/cgi/rapidpdf/1118923v1?ijkey=I4kys.nPb.1lE&keytype=ref&siteid=sci

Abstract:

Deep Impact: Excavating Comet Tempel 1
M. F. A'Hearn,1* M. J. S. Belton,2 W. A. Delamere,3 J. Kissel,4 K. P. Klaasen,5 L. A. McFadden,1 K. J. Meech,6 H. J. Melosh,7 P. H. Schultz,8 J. M. Sunshine,9 P. C. Thomas,10 J. Veverka,10 D. K. Yeomans,5 M. W. Baca,9 I. Busko,11 C. J. Crockett,1 S. M. Collins,5 M. Desnoyer,10 C. A. Eberhardy,8 C. M. Ernst,8 T. L. Farnham,1 L. Feaga,1 O. Groussin,1 D. Hampton,12 S. I. Ipatov,1 J.-Y. Li,1 D. Lindler,13 C. M. Lisse,1,14 N. Mastrodemos,5 W. M. Owen, Jr.,5 J. E. Richardson,7,10 D. D. Wellnitz,1 R. L. White11

Deep Impact collided with comet Tempel 1, excavating a crater controlled by gravity. The comet's outer layer is composed of 1- to 100-micrometer fine particles with negligible strength (<65 pascals). Local gravitational field and average nucleus density (600 kilograms per cubic meter) are estimated from ejecta fallback. Initial ejecta were hot (>1000 kelvins). A large increase in organic material occurred during and after the event, with smaller changes in carbon dioxide relative to water. On approach, the spacecraft observed frequent natural outbursts, a mean radius of 3.0 ± 0.1 kilometers, smooth and rough terrain, scarps, and impact craters. A thermal map indicates a surface in equilibrium with sunlight.

1 University of Maryland, College Park, MD 20742, USA.
2 Belton Space Exploration Initiatives, Tucson, AZ 85716, USA.
3 Delamere Support Services, Boulder, CO 80301, USA.
4 Max-Planck-Institute for Solar System Research, Katlenburg-Lindau, D37191 Germany.
5 Jet Propulsion Laboratory, Pasadena, CA 91109, USA.
6 University of Hawaii, Honolulu, HI 96822, USA.
7 University of Arizona, Tucson, AZ 85721, USA.
8 Brown University, Providence, RI 02412, USA.
9 SAIC, Chantilly, VA 20151, USA.
10 Cornell University, Ithaca, NY 14853, USA.
11 Space Telescope Science Institute, Baltimore, MD 21218, USA.
12 Ball Aerospace and Technology Corporation, Boulder, CO 80301, USA.
13 Sigma Scientific, Greenbelt, MD 20771, USA.
14 Applied Physics Laboratory, Johns Hopkins University, Laurel, MD 20723, USA.

* To whom correspondence should be addressed. E-mail: [email protected]
 
Delinquent said:
Excuse my limited knowledge in this but when they say water ice, do they mean oxygenated water? Also when they stated they found organic material, are they talking about methane type material from previous lifeforms albeit plant, animal, or bacterial?

In deep space most things freeze. By saying water ice, they mean actual H2O and not some other molecule.
 
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