The relationship of active comets, ``extinct'' comets, and dark asteroids
Abstract
Spectrophotometric data on groups of asteroids in different types of orbits reveal different distributions of spectral properties, depending on whether the orbits are cometary or noncometary. In a list of 10 asteroids frequently suggested on purely dynamical grounds to be extinct or dormant comets, all have properties suggestive of spectral classes D, P, or C. Preliminary IRAS albedo results support this. Objects in these classes are very dark, reddish-black to neutral-black, and prevalent among the Trojans and outer belt. Two comets observed at low activity (visible nuclei) also have properties more consistent with D asteroids than any other class (very low reported geometric albedos of 0.02 and red colors). Consistent with these results are very low albedos reported for materials in more than a dozen comets; they average 0.05. Also, sampled cometary dust particles appear to consist of dark carbonaceous materials. Dramatically different are a control group of 13 Aten/Apollo/Amor objects selected from noncometary orbits. Most are in moderate-albedo classes: 8 or 9 appear to be of class S, and only 1 is in a low-albedo class (C). These are probably mostly objects perturbed out of the inner asteroid belt. The preponderence of S's in the noncometary group, together with the preponderence of ordinary chondrites among meteorites, may be evidence that such meteorites came from S asteroids. The data indicate that extinct, dormant, inactive, and minimally active comet nuclei have low albedos ( pv=a few percent) and very red to moderately red colors. As a group, their spectra are more similar to those of outer Solar System asteroids of classes D, P, and C, than to those of inner belt classes, though the observations are frequently not yet complete enough to assign definitively a spectral class. The results, taken together, support the view that dynamically identified "extinct comet candidates" are indeed outer Solar System objects probably of cometary origin. The results also support a scenario of Solar System formation in which dark carbonaceous dust dominated the spectrophotometric properties of planetesimals formed from about 2.7 AU out to at least the Trojan region at 5.2 AU. From 2.7 to at least 5.2 AU, and from class C to class D, the color of this dust reddens, apparently due to increasing amounts of red organic condensates. Comets are probably also colored to different degrees, by dust of this type, and may in some cases be even redder than D asteroids.
- Publication:
-
Icarus
- Pub Date:
- January 1987
- DOI:
- 10.1016/0019-1035(87)90005-4
- Bibcode:
- 1987Icar...69...33H
- Keywords:
-
- Asteroids;
- Comets;
- Interplanetary Dust;
- Solar System;
- Activity;
- Albedo;
- Ice;
- Nebulae;
- Stratosphere;
- COMETS;
- ASTEROIDS;
- SPECTROPHOTOMETRY;
- OPTICAL PROPERTIES;
- SPECTRA;
- ORBITS;
- CLASSIFICATION;
- COLOR;
- TROJAN ASTEROIDS;
- D ASTEROIDS;
- P ASTEROIDS;
- DUST;
- C ASTEROIDS;
- ALBEDO;
- COMPOSITION;
- CARBONACEOUS MATERIAL;
- AMOR ASTEORIDS;
- ATEN ASTEROIDS;
- APOLLO ASTEROIDS;
- S ASTEROIDS;
- COMET NUCLEI;
- ORIGIN;
- INTERPLANETARY DUST;
- CATALOG;
- REFLECTANCE