Sulfate Mineral Phase Equilibria as a Function of Relative Humidity. Intermediate Compositions in the (Mg,Fe,Cu)SO4-H2O System at 1 atm

Details Sulfate Mineral Phase Equilibria as a Function of Relative Humidity. Intermediate Compositions in the (Mg,Fe,Cu)SO4-H2O System at 1 atm Sulfate Mineral Phase Equilibria as a Function of Relative Humidity. Intermediate Compositions in the (Mg,Fe,Cu)SO4-H2O System at 1 atm

Jul 2007

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2007lpico1353.3316a&link_type=abstract

Seventh International Conference on Mars, held July 9-13, 2007 in Pasadena, California, LPI Contribution No. 1353, p.3316

Physics

Scientific paper

Careful characterization of minerals present at the martian surface
requires a detailed understanding of hydrous sulfate phase
relationships. This study explores the effect of metal substitution on
the hydration behaviour of hydrous metal sulfates.

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