CO2: Adsorption on palagonite and the Martian regolith

Details CO2: Adsorption on palagonite and the Martian regolith CO2: Adsorption on palagonite and the Martian regolith

May 1987

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1987pggp.rept..181z&link_type=abstract

In NASA, Washington, Reports of Planetary Geology and Geophysics Program, 1986 p 181-183 (SEE N87-23341 16-91)

Physics

Geophysics

Adsorption, Carbon Dioxide, Climate, Greenhouse Effect, Mars Atmosphere, Mars Surface, Mathematical Models, Regolith, Soils, Brines, Carbonates, Deposition, Erosion, Minerals, Water

Scientific paper

Possible scenarios for the evolution of the Martian climate are discussed. In the interest of determining an upper limit on the absorptive capacity of the Martian regolith, researchers examined the results of Fanale and Cannon (1971, 1974) for CO2 adsorption on nontronite and basalt. There appeared to be a strong proportionality between the capacity of the absorbent and its specific surface area. A model of the Martian climate is given that allows the researchers to make some estimates of exchangeable CO2 abundances.

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