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Comet reservoir gets more real.


Comets may make a spectacle of themselves when they near the sun, but it's tricky to determine exactly where any of them was born. Simulations tracing the orbits of comets back in time suggest that the solar system solar system, the sun and the surrounding planets, natural satellites, dwarf planets, asteroids, meteoroids, and comets that are bound by its gravity. The sun is by far the most massive part of the solar system, containing almost 99.9% of the system's total mass. The principal members of the sun's retinue are the eight major planets; other parts of the solar system are discussed in separate articles: see comet, asteroid, and meteor. harbors two reservoirs of these icy bodies. A disk-shaped storehouse, known as the Kuiper belt Kuiper belt: see comet; Kuiper, Gerard Peter., lies just beyond the orbits of Pluto and Neptune. A vast spherical region called the Oort cloud Oort cloud: see comet. originated even closer to the sun, between the orbits of Uranus Uranus - Hideyuki Nakashima , 1993. A logic-based knowledge representation language. An extension of Prolog written in Common Lisp, with Lisp-like syntax. Extends Prolog with a multiple world mechanism, plus term descriptions to provide functional programming.

ftp://etlport.etl.go.jp/pub/uranus/ftp.
 and Neptune, but was kicked out about 1,000 times farther than the belt.

Over the past 5 years, as astronomers have imaged more than 30 residents of the Kuiper belt, this proposed storehouse has become accepted as a source of cornets cornet, brass wind musical instrument, created in France about 1830 by adding valves to the post horn. It is usually in B flat and is the same size as the B flat trumpet, but has a more conical bore. The cornet, a transposing instrument, has a less brilliant tone but greater agility than the trumpet. It has long been a standard instrument in bands. In the orchestra, the cornet is used with the trumpet. It was used extensively in jazz in the early 20th cent.. Astronomers have little hope of detecting the present-day members of the more remote Oort cloud, however. Now, ultraviolet Studies of Comet Hale-Bopp provide support for the existence of the cloud.

Using the Extreme Ultraviolet Explorer Extreme Ultraviolet Explorer: see ultraviolet astronomy. satellite, Michael J. Mumma and Vladimir A. Krasnopolsky of NASA's Goddard Space Flight Center in Greenbelt, Md., and their colleagues recently searched for emissions from neon in the spectra of Hale-Bopp. They discovered that the abundance of neon relative to oxygen in the comet, thought to be an emigre from the Oort cloud, is at most one-twenty-fifth the abundance in the sun and could well be zero. The team had previously found that another Oort cloud comet, Hyakutake, also contains little or no neon.

Neon ice turns to vapor at 25 kelvins, readily escaping the nucleus of a cornet. The absence of neon suggests that the grains of interstellar ice that built Hale-Bopp and Hyakutake must have done so in a part of the solar system where temperatures are above 25 kelvins. The region between Uranus and Neptune meets this temperature criterion without being hot enough to boil off other ices found in the comet.

The match in temperature adds to the evidence that the Oort cloud did indeed assemble between these two planets and only later migrated to the fringes of the solar system. The team reported the neon measurement in an April 14 circular of the International Astronomical Union.
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Title Annotation:simulation tracing back of comets suggests that they come from two storage areas, one just beyond Pluto and Neptune, and one between the orbits of Uranus and Neptune
Author:Cowen, Ron
Publication:Science News
Article Type:Brief Article
Date:Jun 7, 1997
Words:359
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