Cryogenic origin of fractionation between perchlorate and chloride under modern martian climate - Sorbonne Université
Article Dans Une Revue Communications Earth & Environment Année : 2022

Cryogenic origin of fractionation between perchlorate and chloride under modern martian climate

Résumé

The high perchlorate (ClO 4 −) to chloride (Cl −) ratios observed at the Phoenix landing site, northern polar region of Mars, have been puzzling since detection. However, a lack of understanding of perchlorate-chloride-water systems under cryogenic conditions makes it difficult to assess ClO 4 − /Cl − ratios during deliquescence-related processes. Here we quantitatively evaluate ClO 4 − /Cl − fractionation in deliquescence-induced brines of magnesium-and calcium-perchlorate-chloride salt mixtures under subzero conditions, by measuring solubility data and constructing temperature-dependent thermodynamic models. We find that under specific relative humidity (RH) and temperature (T) conditions, deliquescence of perchlorate-chloride mixtures may form brines with fractionated ClO 4 − /Cl − signatures. Appropriate RH-T, water-limited conditions, and aeolian processes are required to produce and preserve the elevated ClO 4 − /Cl − signatures in soils. Under the present climate, the north polar region can support ClO 4 − /Cl − fractionation and potentially enrich perchlorate for longer periods on global Mars. This highlights the uniqueness of Mars' arctic environment and its implications for modern habitability.
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hal-03561314 , version 1 (08-02-2022)

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Dongdong Li, Yu-Yan Sara Zhao, Pierre-Yves Meslin, Margaux Vals, François Forget, et al.. Cryogenic origin of fractionation between perchlorate and chloride under modern martian climate. Communications Earth & Environment, 2022, 3 (1), pp.15. ⟨10.1038/s43247-022-00345-5⟩. ⟨hal-03561314⟩
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