TY - JOUR
T1 - Jarosite stability on Mars
AU - Navrotsky, Alexandra
AU - Forray, Ferenc Lázár
AU - Drouet, Christophe
N1 - Funding Information:
This work was supported by the U.S. Department of Energy Grant DEFG0397SF14749. We thank to S. McLennan and anonymous reviewers for their helpful comments and suggestions, which improve the quality of this paper.
PY - 2005/7
Y1 - 2005/7
N2 - Jarosite, a potassium (sodium) iron sulphate hydrated mineral, has recently been identified on the martian surface by the Opportunity rover. Using recent thermochemical data [Drouet and Navrotsky, 2003, Geochim. Cosmochim. Acta 67, 2063-2076; Forray et al., 2005, Geochim. Cosmochim. Acta, in press], we calculate the equilibrium decomposition curve of jarosite and show that it is thermodynamically stable under most present martian pressures and temperatures. Its stability makes jarosite potentially useful to retain textural, chemical, and isotopic evidence of past history, including possible biological activity, on Mars.
AB - Jarosite, a potassium (sodium) iron sulphate hydrated mineral, has recently been identified on the martian surface by the Opportunity rover. Using recent thermochemical data [Drouet and Navrotsky, 2003, Geochim. Cosmochim. Acta 67, 2063-2076; Forray et al., 2005, Geochim. Cosmochim. Acta, in press], we calculate the equilibrium decomposition curve of jarosite and show that it is thermodynamically stable under most present martian pressures and temperatures. Its stability makes jarosite potentially useful to retain textural, chemical, and isotopic evidence of past history, including possible biological activity, on Mars.
KW - Jarosite
KW - Mars climate
KW - Mineral stability
KW - Mineralogy
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U2 - 10.1016/j.icarus.2005.02.003
DO - 10.1016/j.icarus.2005.02.003
M3 - Article
AN - SCOPUS:18844377441
SN - 0019-1035
VL - 176
SP - 250
EP - 253
JO - Icarus
JF - Icarus
IS - 1
ER -