The origin and evolution of comet nuclei and Comet Halley results

Mathematics – Logic

Scientific paper

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Comet Nuclei, Cosmic Dust, Evolution (Development), Halley'S Comet, Refractory Materials, Albedo, Density Distribution, Mass Spectroscopy, Oort Cloud, Particle Size Distribution, Solar Heating

Scientific paper

The chemistry and morphological structure of a comet nucleus as an aggregate of interstellar dust is used to provide comparisons with comet Halley results: the density of the nucleus and of the dust; the dust cloud model and its consequences on the production of C(+) and CN in the coma by small organic grains; the surface albedo and the nucleus heat conductivity and high surface temperature; the appearance of 10 to the minus 14th to minus 17th power g dust particles along with higher masses; the mass spectra of dust and infrared spectroscopy as evidence for complex organic grain mantles (0.15 microns) and of very small (0.01 micron) carbonaceous and silicate grains; and the appearance of small grains resulting from breakup of larger grains. The cosmic ray dosage of a comet nucleus during its 4 1/2 billion yr in the Oort cloud appears to be many orders of magnitude less than the dosage of the pre-aggregated interstellar dust by ultraviolet photons except perhaps in the outer few meters of the nucleus of a new comet. It is shown that solar heating of the interior of a nucleus is lower than previously estimated.

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