Phosphorus sorption by terrestrial basalt and granite and implications for the martian crust

Details Phosphorus sorption by terrestrial basalt and granite and implications for the martian crust Phosphorus sorption by terrestrial basalt and granite and implications for the martian crust

Jan 2004

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2004icar..167..166d&link_type=abstract

Icarus, Volume 167, Issue 1, p. 166-169.

Physics

2

Surface, Geochemistry

Scientific paper

High phosphorus concentrations in the range of 0.5 wt% in rocks and soil have been measured on the martian surface, terrestrial P concentrations are far less uniform and generally lower. Reactions of terrestrial basalt and granite powders with phosphate solution result in an enrichment of phosphorus in both, with basalt having a far better reactivity than granite. The implications of these results for P on Mars are discussed.

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