Origin of Martian channels - Clathrates and water

Physics

Scientific paper

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Clathrates, Mars Surface, Surface Water, Water Flow, Carbon Dioxide, Hydrates, Permafrost, Planetology, Tectonics

Scientific paper

Criticism is directed at the suggestion that Martian channels may have been eroded by liquid water produced by the depressurization of CO2 hydrate. The release of pre-existing subsurface liquid water, such as that trapped under a permafrost layer, by meteorite impact or tectonic activity could produce sufficient flow and would not require heat transfer. The presence of water in a CO2 hydrate is shown to be detrimental to its release from an underground reservoir.

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