Dissolution of Olivine, Siderite, and Basalt at 80°C in 0.1M H_2SO_4 in a Flow Through Process: Insights into Acidic Weathering on Mars

Details Dissolution of Olivine, Siderite, and Basalt at 80°C in 0.1M H_2SO_4 in a Flow Through Process: Insights into Acidic Weathering on Mars Dissolution of Olivine, Siderite, and Basalt at 80°C in 0.1M H_2SO_4 in a Flow Through Process: Insights into Acidic Weathering on Mars

Mar 2012

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2012lpi....43.2521g&link_type=abstract

43rd Lunar and Planetary Science Conference, held March 19–23, 2012 at The Woodlands, Texas. LPI Contribution No. 1659, id.2521

Physics

Scientific paper

The object of this research is to determine acidic dissolution rates of
olivine, siderite, and basaltic materials at 80°C using a flow-thru
reactor and to characterize the weathering products.

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