Infrared emission by organic grains in the coma of comet Halley

Christopher Chyba, Carl Sagan

Research output: Contribution to journalArticle

27 Scopus citations

Abstract

Spacecraft1 and ground-based2-5 observations of comet Halley in the near-infrared reveal a triple-peaked emission feature near 3.4 μm, characteristic of C-H stretching in hydrocarbons (-CH3 and -CH2- alkanes). Here we discuss transmission spectra of organic residues produced by laboratory irradiation of candidate cometary ices, which serve as the basis for a model of emitting cometary dust. The laboratory synthesis of solid organic residue from irradiated low-occupancy methane ice clathrate simulates the radiation processing experienced by comet Halley. The transmission spectrum of this residue, convolved with a simple two-component thermal emission model based on the spacecraft-determined dust distribution in the Halley coma, fits the 3.4 μm feature, provides optical depths in excellent agreement with those observationally determined, and accounts for the absence of features at longer wavelengths (despite their presence in transmission spectra of typical ice irradiation residues).

Original languageEnglish (US)
Pages (from-to)350-353
Number of pages4
JournalNature
Volume330
Issue number6146
DOIs
StatePublished - Jan 1 1987
Externally publishedYes

All Science Journal Classification (ASJC) codes

  • General

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