Carbonate complexation enhances hydrothermal transport of rare earth elements in alkaline fluids.


Journal

Nature communications
ISSN: 2041-1723
Titre abrégé: Nat Commun
Pays: England
ID NLM: 101528555

Informations de publication

Date de publication:
18 Mar 2022
Historique:
received: 07 03 2021
accepted: 04 02 2022
entrez: 19 3 2022
pubmed: 20 3 2022
medline: 20 3 2022
Statut: epublish

Résumé

Rare earth elements (REE), essential metals for the transition to a zero-emission economy, are mostly extracted from REE-fluorcarbonate minerals in deposits associated with carbonatitic and/or peralkaline magmatism. While the role of high-temperature fluids (100 < T < 500 °C) in the development of economic concentrations of REE is well-established, the mechanisms of element transport, ore precipitation, and light (L)REE/heavy (H)REE fractionation remain a matter of debate. Here, we provide direct evidence from in-situ X-ray Absorption Spectroscopy (XAS) that the formation of hydroxyl-carbonate complexes in alkaline fluids enhances hydrothermal mobilization of LREE at T ≥ 400 °C and HREE at T ≤ 200 °C, even in the presence of fluorine. These results not only reveal that the modes of REE transport in alkaline fluids differ fundamentally from those in acidic fluids, but further underline that alkaline fluids may be key to the mineralization of hydrothermal REE-fluorcarbonates by promoting the simultaneous transport of (L)REE, fluoride and carbonate, especially in carbonatitic systems.

Identifiants

pubmed: 35304459
doi: 10.1038/s41467-022-28943-z
pii: 10.1038/s41467-022-28943-z
pmc: PMC8933457
doi:

Types de publication

Journal Article

Langues

eng

Sous-ensembles de citation

IM

Pagination

1456

Subventions

Organisme : EC | EU Framework Programme for Research and Innovation H2020 | H2020 Priority Excellent Science | H2020 Marie Skłodowska-Curie Actions (H2020 Excellent Science - Marie Skłodowska-Curie Actions)
ID : 797145

Informations de copyright

© 2022. The Author(s).

Références

Sci Adv. 2020 Oct 9;6(41):
pubmed: 33036966
Inorg Chem. 2000 Mar 20;39(6):1050-1
pubmed: 12526389
Chem Rev. 2002 Jun;102(6):2011-88
pubmed: 12059261
Phys Rev A Gen Phys. 1988 Sep 15;38(6):3098-3100
pubmed: 9900728
J Synchrotron Radiat. 2005 Jul;12(Pt 4):537-41
pubmed: 15968136
J Comput Chem. 2003 Jul 15;24(9):1142-56
pubmed: 12759913
Inorg Chem. 2018 Aug 6;57(15):9020-9027
pubmed: 30004680
Phys Rev B Condens Matter. 1986 Jun 15;33(12):8822-8824
pubmed: 9938299
Contrib Mineral Petrol. 2017;172(11):96
pubmed: 32009662

Auteurs

Marion Louvel (M)

Institute for Mineralogy, WWU Münster, Münster, Germany. marion.louvel@cnrs-orleans.fr.
Institut des Sciences de la Terre d'Orleans CNRS-UMR7327, Orleans, France. marion.louvel@cnrs-orleans.fr.

Barbara Etschmann (B)

School of Earth, Atmosphere & Environment, Monash University, Clayton, Australia. barbara.etschmann@monash.edu.

Qiushi Guan (Q)

School of Earth, Atmosphere & Environment, Monash University, Clayton, Australia. qiushi.guan@monash.edu.

Denis Testemale (D)

University Grenoble Alpes, CNRS, Grenoble INP, Institute Néel, 38000, Grenoble, France. denis.testemale@neel.cnrs.fr.

Joël Brugger (J)

School of Earth, Atmosphere & Environment, Monash University, Clayton, Australia. Joel.Brugger@monash.edu.

Classifications MeSH