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Magnesium sulphate salts and the history of water on Mars

Abstract

Recent reports of 30 wt% of sulphate within saline sediments on Mars1,2—probably occurring in hydrated form3—suggest a role for sulphates in accounting for equatorial H2O observed in a global survey by the Odyssey spacecraft4. Among salt hydrates likely to be present3, those of the MgSO4·nH2O series have many hydration states. Here we report the exposure of several of these phases to varied temperature, pressure and humidity to constrain their possible H2O contents under martian surface conditions. We found that crystalline structure and H2O content are dependent on temperature–pressure history, that an amorphous hydrated phase with slow dehydration kinetics forms at <1% relative humidity, and that equilibrium calculations may not reflect the true H2O-bearing potential of martian soils. Mg sulphate salts can retain sufficient H2O to explain a portion of the Odyssey observations5. Because phases in the MgSO4·nH2O system are sensitive to temperature and humidity, they can reveal much about the history of water on Mars. However, their ease of transformation implies that salt hydrates collected on Mars will not be returned to Earth unmodified, and that accurate in situ analysis is imperative.

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Acknowledgements

This research was supported by Los Alamos National Laboratory – Directed Research and Development Funding and by a NASA Mars Fundamental Research Program grant. Comments and suggestions by J. F. Bell and B. C. Clark helped to improve this Letter.

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Correspondence to David T. Vaniman.

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The authors declare that they have no competing financial interests.

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Figure 1: Dehydration experiment in an environmental cell.
Figure 2: Rehydration experiment in an environmental cell.
Figure 3: Results of controlled-humidity XRD experiments at 298 K plotted against stability fields for epsomite, hexahydrite and kieserite, modified from ref. 19.

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