Atmosphere lost by oxidation of the surface in the geological history of Mars

Details Atmosphere lost by oxidation of the surface in the geological history of Mars Atmosphere lost by oxidation of the surface in the geological history of Mars

Dec 2004

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2004agufm.p11a0967d&link_type=abstract

American Geophysical Union, Fall Meeting 2004, abstract #P11A-0967

Mathematics

Logic

0325 Evolution Of The Atmosphere, 0343 Planetary Atmospheres (5405, 5407, 5409, 5704, 5705, 5707), 0399 General Or Miscellaneous

Scientific paper

In this work I made an evaluation of the quantity of atmosphere lost by Mars by oxidation of the surface in his geological history. In a previous work I calculate the quantity of igneous rocks generated in the diverse Martian epochs. In this work I use that previous calculus and calculate the quantity of oxygen that reacts with these new rocks. The maximum oxidation of the soil occurred in the middle Noachian and the present rate of oxidation is the minimum.

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