CO2-H2O Phase Equilibria: Residual Ice Layers and Basal Melting of the Martian Polar Ice Caps

Details CO2-H2O Phase Equilibria: Residual Ice Layers and Basal Melting of the Martian Polar Ice Caps CO2-H2O Phase Equilibria: Residual Ice Layers and Basal Melting of the Martian Polar Ice Caps

Mar 2004

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2004lpi....35.1857l&link_type=abstract

35th Lunar and Planetary Science Conference, March 15-19, 2004, League City, Texas, abstract no.1857

Physics

Scientific paper

Shifts in saturation surfaces with pressure favor residual layers of
solid CO_2 at the martian south pole. Basal melting of solid-CO_2 layers
within polar ice caps during periods of low obliquity may lead to
storage of liquid CO_2 in the Martian crust.

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