The influence of CO ice on the activity and the near-surface differentiation of comet nuclei

Mathematics

Scientific paper

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Carbon Monoxide, Comet Nuclei, Ice, Chemical Composition, Computer Programs, Interplanetary Dust, Mathematical Models, Water Temperature, Comets, Comet Nuclei, Carbon Monoxide, Ice, Surface, Differentiation, Computer Methods, Water Ice, Dust, Models, Volatility, Porosity, Gases, Temperature, Flux, Parameters, Pressure, Permeability, Mantle, Distance

Scientific paper

A comet nucleus model whose composition is a homogeneous mixture of water ice, CO ice, and dust, in a Halley-type orbit, is presently used to investigate the role of unclathrated CO ice in the activity and near-surface differentiation of comet nuclei. Temperatures of water and CO ice surfaces, CO gas and water steam fluxes, and depths of CO ice, are presented as functions of orbital position. It is determined that CO ice should always exist within 3 m of the surface; CO gas production exceeds water steam production beyond 2.5 AU, with consequences for the planned in situ elemental analysis of nuclei.

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