H2O-Silicate Microphysics in Ascending Volcanic Plumes on Mars

Details H2O-Silicate Microphysics in Ascending Volcanic Plumes on Mars H2O-Silicate Microphysics in Ascending Volcanic Plumes on Mars

Jul 2003

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2003mars.conf.3136z&link_type=abstract

Sixth International Conference on Mars, July 20-25 2003, Pasadena, California, abstract no.3136

Physics

Scientific paper

Physical adsorption of water vapor plays a much more significant role in
eruptive plume energetics on Mars than on Earth. Release of latent heat
of condensation and the onset of moist convection are diminished,
delayed, or even prevented by adsorptive interaction.

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