Oxidation of the Martian surface - Constraints due to chemical processes in the atmosphere

Astronomy and Astrophysics – Astronomy

Scientific paper

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Atmospheric Chemistry, Mars Atmosphere, Mars Surface, Oxygen Atoms, Planetary Composition, Abundance, Astronomical Spectroscopy, Atmospheric Models, Carbon Dioxide, Gas Dissociation, Molecular Gases, Oxidation, Photodissociation

Scientific paper

Dissociation of water in the Martian atmosphere may supply oxygen to the surface and may result in the formation of minerals such as goethite, as proposed by Huguenin. The supply rate is limited by chemical processes in the atmosphere which regulate the abundance of O2. The net surface sink for atmospheric oxygen can be as large as 33 million atoms per sq cm per sec which compares to the escape rate of 60 million atoms per sq cm per sec.

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