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A global Mars dust composition refined by the Alpha-Particle X-ray Spectrometer in Gale Crater

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Authors

Berger, Jeff A.
Schmidt, M E
Gellert, R
Campbell, J.L.
King, Penelope
Flemming, R.L.
Ming, Doug
Pradler, I
Thompson, Lucy
Perrett, Glynis

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American Geophysical Union

Abstract

Modern Martian dust is similar in composition to the global soil unit and bulk basaltic Mars crust, but it is enriched in S and Cl. The Alpha Particle X-ray Spectrometer (APXS) on the Mars Science Laboratory Curiosity rover analyzed air fall dust on the science observation tray (o-tray) in Gale Crater to determine dust oxide compositions. The o-tray dust has the highest concentrations of SO3 and Cl measured in Mars dust (SO3 8.3%; Cl 1.1 wt %). The molar S/Cl in the dust (3.35 ± 0.34) is consistent with previous studies of Martian dust and soils (S/Cl = 3.7 ± 0.7). Fe is also elevated ~25% over average Mars soils and the bulk crust. These enrichments link air fall dust with the S-, Cl-, and Fe-rich X-ray amorphous component of Gale Crater soil. Dust and soil have the same S/Cl, constraining the surface concentrations of S and Cl on a global scale.

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Geophysical Research Letters

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Open Access

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