Dissolution of olivine, siderite and basalt at 80°C in 0.1 M H2SO4 in a flow-through process: Insights into acidic weathering on Mars

Authors

D. C. Golden, NASA Johnson Space CenterFollow
D. W. Ming, NASA Johnson Space CenterFollow
Elisabeth M. Hausrath, University of Nevada, Las VegasFollow
R. V. Morris, NASA Johnson Space CenterFollow
P. B. Niles, NASA Johnson Space Center
C. N. Achilles, Engineering and Science Contract Group
D. K. Ross, Engineering and Science Contract Group
B. L. Cooper, Engineering and Science Contract Group
C. P. Gonzalez, Engineering and Science Contract Group
S. A. Mertzman, Franklin and Marshall College, Lancaster

Document Type

Conference Proceeding

Publication Date

1-1-2012

Publication Title

Lunar and Planetary Science Conference XXXXIII

Publisher

Lunar and Planetary Institute

Publisher Location

The Woodlands, TX

First page number:

1

Last page number:

2

Repository Citation

Golden, D. C., Ming, D. W., Hausrath, E. M., Morris, R. V., Niles, P. B., Achilles, C. N., Ross, D. K., Cooper, B. L., Gonzalez, C. P., Mertzman, S. A. (2012). Dissolution of olivine, siderite and basalt at 80°C in 0.1 M H2SO4 in a flow-through process: Insights into acidic weathering on Mars. Lunar and Planetary Science Conference XXXXIII 1-2. The Woodlands, TX: Lunar and Planetary Institute.