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

International audience 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 difficul...

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Published in:Communications Earth & Environment
Main Authors: Li, Dongdong, Zhao, Yu-Yan Sara, Meslin, Pierre-Yves, Vals, Margaux, Forget, François, Wu, Zhongchen
Other Authors: Key Laboratory of Comprehensive and Highly Efficient Utilization of Salt Lake Resources, Qinghai Institute of Salt Lakes, Chinese Academy of Sciences, Xining, China, Key Laboratory of Salt Lake Resources Chemistry of Qinghai Province, Xining, China, Center for Lunar and Planetary Sciences, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang, Center for Excellence in Comparative Planetology, Chinese Academy of Sciences Beijing (CAS), Chengdu University of Technology (CDUT), Institut de recherche en astrophysique et planétologie (IRAP), Université Toulouse III - Paul Sabatier (UT3), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP), Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Centre National de la Recherche Scientifique (CNRS), Laboratoire de Météorologie Dynamique (UMR 8539) (LMD), Institut national des sciences de l'Univers (INSU - CNRS)-École polytechnique (X)-École des Ponts ParisTech (ENPC)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Département des Géosciences - ENS Paris, École normale supérieure - Paris (ENS-PSL), Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-École normale supérieure - Paris (ENS-PSL), Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL), Shandong University at Weihai Weihai
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2022
Subjects:
Online Access:https://hal.sorbonne-universite.fr/hal-03561314
https://hal.sorbonne-universite.fr/hal-03561314/document
https://hal.sorbonne-universite.fr/hal-03561314/file/s43247-022-00345-5.pdf
https://doi.org/10.1038/s43247-022-00345-5
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record_format openpolar
institution Open Polar
collection École Polytechnique, Université Paris-Saclay: HAL
op_collection_id ftepunivpsaclay
language English
topic [SDU]Sciences of the Universe [physics]
spellingShingle [SDU]Sciences of the Universe [physics]
Li, Dongdong
Zhao, Yu-Yan Sara
Meslin, Pierre-Yves
Vals, Margaux
Forget, François
Wu, Zhongchen
Cryogenic origin of fractionation between perchlorate and chloride under modern martian climate
topic_facet [SDU]Sciences of the Universe [physics]
description International audience 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.
author2 Key Laboratory of Comprehensive and Highly Efficient Utilization of Salt Lake Resources, Qinghai Institute of Salt Lakes, Chinese Academy of Sciences, Xining, China
Key Laboratory of Salt Lake Resources Chemistry of Qinghai Province, Xining, China
Center for Lunar and Planetary Sciences, Institute of Geochemistry
Chinese Academy of Sciences, Guiyang
Center for Excellence in Comparative Planetology
Chinese Academy of Sciences Beijing (CAS)
Chengdu University of Technology (CDUT)
Institut de recherche en astrophysique et planétologie (IRAP)
Université Toulouse III - Paul Sabatier (UT3)
Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP)
Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3)
Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Centre National de la Recherche Scientifique (CNRS)
Laboratoire de Météorologie Dynamique (UMR 8539) (LMD)
Institut national des sciences de l'Univers (INSU - CNRS)-École polytechnique (X)-École des Ponts ParisTech (ENPC)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Département des Géosciences - ENS Paris
École normale supérieure - Paris (ENS-PSL)
Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-École normale supérieure - Paris (ENS-PSL)
Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)
Shandong University at Weihai Weihai
format Article in Journal/Newspaper
author Li, Dongdong
Zhao, Yu-Yan Sara
Meslin, Pierre-Yves
Vals, Margaux
Forget, François
Wu, Zhongchen
author_facet Li, Dongdong
Zhao, Yu-Yan Sara
Meslin, Pierre-Yves
Vals, Margaux
Forget, François
Wu, Zhongchen
author_sort Li, Dongdong
title Cryogenic origin of fractionation between perchlorate and chloride under modern martian climate
title_short Cryogenic origin of fractionation between perchlorate and chloride under modern martian climate
title_full Cryogenic origin of fractionation between perchlorate and chloride under modern martian climate
title_fullStr Cryogenic origin of fractionation between perchlorate and chloride under modern martian climate
title_full_unstemmed Cryogenic origin of fractionation between perchlorate and chloride under modern martian climate
title_sort cryogenic origin of fractionation between perchlorate and chloride under modern martian climate
publisher HAL CCSD
publishDate 2022
url https://hal.sorbonne-universite.fr/hal-03561314
https://hal.sorbonne-universite.fr/hal-03561314/document
https://hal.sorbonne-universite.fr/hal-03561314/file/s43247-022-00345-5.pdf
https://doi.org/10.1038/s43247-022-00345-5
geographic Arctic
geographic_facet Arctic
genre Arctic
genre_facet Arctic
op_source ISSN: 2662-4435
Communications Earth & Environment
https://hal.sorbonne-universite.fr/hal-03561314
Communications Earth & Environment, 2022, 3 (1), pp.15. ⟨10.1038/s43247-022-00345-5⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1038/s43247-022-00345-5
hal-03561314
https://hal.sorbonne-universite.fr/hal-03561314
https://hal.sorbonne-universite.fr/hal-03561314/document
https://hal.sorbonne-universite.fr/hal-03561314/file/s43247-022-00345-5.pdf
doi:10.1038/s43247-022-00345-5
op_rights http://creativecommons.org/licenses/by/
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op_doi https://doi.org/10.1038/s43247-022-00345-5
container_title Communications Earth & Environment
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spelling ftepunivpsaclay:oai:HAL:hal-03561314v1 2024-06-09T07:44:09+00:00 Cryogenic origin of fractionation between perchlorate and chloride under modern martian climate Li, Dongdong Zhao, Yu-Yan Sara Meslin, Pierre-Yves Vals, Margaux Forget, François Wu, Zhongchen Key Laboratory of Comprehensive and Highly Efficient Utilization of Salt Lake Resources, Qinghai Institute of Salt Lakes, Chinese Academy of Sciences, Xining, China Key Laboratory of Salt Lake Resources Chemistry of Qinghai Province, Xining, China Center for Lunar and Planetary Sciences, Institute of Geochemistry Chinese Academy of Sciences, Guiyang Center for Excellence in Comparative Planetology Chinese Academy of Sciences Beijing (CAS) Chengdu University of Technology (CDUT) Institut de recherche en astrophysique et planétologie (IRAP) Université Toulouse III - Paul Sabatier (UT3) Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP) Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3) Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Centre National de la Recherche Scientifique (CNRS) Laboratoire de Météorologie Dynamique (UMR 8539) (LMD) Institut national des sciences de l'Univers (INSU - CNRS)-École polytechnique (X)-École des Ponts ParisTech (ENPC)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Département des Géosciences - ENS Paris École normale supérieure - Paris (ENS-PSL) Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-École normale supérieure - Paris (ENS-PSL) Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL) Shandong University at Weihai Weihai 2022-02-01 https://hal.sorbonne-universite.fr/hal-03561314 https://hal.sorbonne-universite.fr/hal-03561314/document https://hal.sorbonne-universite.fr/hal-03561314/file/s43247-022-00345-5.pdf https://doi.org/10.1038/s43247-022-00345-5 en eng HAL CCSD Springer Nature info:eu-repo/semantics/altIdentifier/doi/10.1038/s43247-022-00345-5 hal-03561314 https://hal.sorbonne-universite.fr/hal-03561314 https://hal.sorbonne-universite.fr/hal-03561314/document https://hal.sorbonne-universite.fr/hal-03561314/file/s43247-022-00345-5.pdf doi:10.1038/s43247-022-00345-5 http://creativecommons.org/licenses/by/ info:eu-repo/semantics/OpenAccess ISSN: 2662-4435 Communications Earth & Environment https://hal.sorbonne-universite.fr/hal-03561314 Communications Earth & Environment, 2022, 3 (1), pp.15. ⟨10.1038/s43247-022-00345-5⟩ [SDU]Sciences of the Universe [physics] info:eu-repo/semantics/article Journal articles 2022 ftepunivpsaclay https://doi.org/10.1038/s43247-022-00345-5 2024-05-16T12:01:35Z International audience 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. Article in Journal/Newspaper Arctic École Polytechnique, Université Paris-Saclay: HAL Arctic Communications Earth & Environment 3 1