The Effect of a Fine-grained Basaltic Layer on the Evaporation of Ice Under Martian Conditions

Details The Effect of a Fine-grained Basaltic Layer on the Evaporation of Ice Under Martian Conditions The Effect of a Fine-grained Basaltic Layer on the Evaporation of Ice Under Martian Conditions

Mar 2007

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2007lpi....38.1246b&link_type=abstract

38th Lunar and Planetary Science Conference, (Lunar and Planetary Science XXXVIII), held March 12-16, 2007 in League City, Texas

Physics

Scientific paper

Diffusion of water vapor through a fine-grained basaltic layer is
experimentally investigated under martian conditions. It is shown to be
similar to that through palagonite, but it is not strongly dependent on
adsorption and/or desorption of water.

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