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Ethane Production and Release in Comet C/1995 O1 Hale–Bopp
Ethane (C 2H 6) was detected in Comet C/1995 O1 Hale–Bopp on 13 dates between UT 1996 September 20.3 ( R h=3.01 AU pre-perihelion) and 1997 September 25.7 ( R h=2.83 AU post-perihelion) using high-resolution infrared spectroscopy. Production rates and rotational temperatures were measured, and the d...
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Published in: | Icarus (New York, N.Y. 1962) N.Y. 1962), 2001-09, Vol.153 (1), p.162-179 |
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Main Authors: | , , , , |
Format: | Article |
Language: | English |
Citations: | Items that cite this one |
Online Access: | Get full text |
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Summary: | Ethane (C
2H
6) was detected in Comet C/1995 O1 Hale–Bopp on 13 dates between UT 1996 September 20.3 (
R
h=3.01 AU pre-perihelion) and 1997 September 25.7 (
R
h=2.83 AU post-perihelion) using high-resolution infrared spectroscopy. Production rates and rotational temperatures were measured, and the derived heliocentric dependence for ethane production was
Q=(5.52±0.20)×10
28 [
R
h
(−2.43±0.13)] molecules s
−1. The spatial distribution of C
2H
6 molecules in the coma was consistent with all ethane being released directly from the nucleus, although the possibility that a small fraction was released as a distributed source cannot be excluded. When our derived production rates for ethane, water, and acetylene (C
2H
2) are compared, we obtain an average relative abundance of C
2H
6/H
2O=(6.23±0.42)×10
−3, and C
2H
6/C
2H
2=2.4±0.7. The high ethane abundance relative to acetylene in Hale–Bopp suggests its ices were altered by radiation processing and/or hydrogen-atom addition reactions on the surfaces of ice-mantled grains in the natal cloud. These results are not consistent with ices in Hale–Bopp originating in a thermally or chemically equilibrated region of the solar nebula. |
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ISSN: | 0019-1035 1090-2643 |
DOI: | 10.1006/icar.2001.6678 |