Dehydration of Na-Jarosite, Ferricopiapite, and Rhomboclase at High T and Implications on Martian Ferric Sulfates

Details Dehydration of Na-Jarosite, Ferricopiapite, and Rhomboclase at High T and Implications on Martian Ferric Sulfates Dehydration of Na-Jarosite, Ferricopiapite, and Rhomboclase at High T and Implications on Martian Ferric Sulfates

Mar 2012

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2012lpi....43.2791l&link_type=abstract

43rd Lunar and Planetary Science Conference, held March 19–23, 2012 at The Woodlands, Texas. LPI Contribution No. 1659, id.2791

Physics

1

Scientific paper

Our dehydration experiments of ferric sulfates show that OH-bearing
Na-jarosite is relatively stable at 95°C and RH ≤ 11%, while
H_2O/OH-bearing ferricopiapite and rhomboclase have converted entirely
to anhydrous phases.

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