Abundances in Comet Halley at the time of the spacecraft encounters

Spectrophotometric observations of Comet Halley obtained in March 1986 at the time of the spacecraft encounters with the comet are described, and the column densities derived from the integrated emission band fluxes are presented. The scale lengths are determined from the spatial profiles of the obs...

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Veröffentlicht in:Astrophys. J.; (United States) 1988-02, Vol.325 (2), p.927-938
Hauptverfasser: Wyckoff, Susan, Tegler, Stephen, Wehinger, Peter A., Spinard, Hyron, Belton, Michael J. S.
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container_issue 2
container_start_page 927
container_title Astrophys. J.; (United States)
container_volume 325
creator Wyckoff, Susan
Tegler, Stephen
Wehinger, Peter A.
Spinard, Hyron
Belton, Michael J. S.
description Spectrophotometric observations of Comet Halley obtained in March 1986 at the time of the spacecraft encounters with the comet are described, and the column densities derived from the integrated emission band fluxes are presented. The scale lengths are determined from the spatial profiles of the observed species. Production rates are derived and the parent identities and abundance ratios of the studied species are discussed. The data indicate that the abundance of the primordial condensate NH3 comprises about 0.2 percent of the total volatile fraction of the comet nucleus. The ratio of production rates Q(NH2)/Q(H2O) = 0.003 indicates that Q(NH3)/Q(H2O) is roughly 0.3 percent, which is nearly 10 times lower than the value determined from Giotto ion mass spectrometer data. The production rate Q(CH)/Q(H2O) of 0.007 and the CH spatial profile indicate that CH cannot derive entirely from direct photodissociation of CH4.
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Production rates are derived and the parent identities and abundance ratios of the studied species are discussed. The data indicate that the abundance of the primordial condensate NH3 comprises about 0.2 percent of the total volatile fraction of the comet nucleus. The ratio of production rates Q(NH2)/Q(H2O) = 0.003 indicates that Q(NH3)/Q(H2O) is roughly 0.3 percent, which is nearly 10 times lower than the value determined from Giotto ion mass spectrometer data. The production rate Q(CH)/Q(H2O) of 0.007 and the CH spatial profile indicate that CH cannot derive entirely from direct photodissociation of CH4.</abstract><cop>Legacy CDMS</cop><pub>University of Chicago Press</pub><doi>10.1086/166064</doi><tpages>12</tpages></addata></record>
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source NASA Technical Reports Server; Alma/SFX Local Collection
subjects 640107 - Astrophysics & Cosmology- Planetary Phenomena
ABUNDANCE
ACCRETION DISKS
ALKANES
AMMONIA
Astronomy
Astrophysics
CHEMICAL COMPOSITION
CLASSICAL AND QUANTUM MECHANICS, GENERAL PHYSICS
COMETS
DISTRIBUTION
Earth, ocean, space
Exact sciences and technology
HALLEY COMET
HYDRIDES
HYDROCARBONS
HYDROGEN COMPOUNDS
Interplanetary space
METHANE
NITROGEN COMPOUNDS
NITROGEN HYDRIDES
ORGANIC COMPOUNDS
OXYGEN COMPOUNDS
Solar system
SPATIAL DISTRIBUTION
SPECTROPHOTOMETRY
WATER
title Abundances in Comet Halley at the time of the spacecraft encounters
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