Adsorption of rare earth elements in regolith-hosted clay deposits

Global resources of heavy Rare Earth Elements (REE) are dominantly sourced from Chinese regolith-hosted ion-adsorption deposits, yet the adsorption mechanisms remain unclear. Here, the authors find that heavy REE are adsorbed as easily leachable 8-coordinated outer-sphere hydrated complexes, dominan...

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Main Authors: Anouk M. Borst, Martin P. Smith, Adrian A. Finch, Guillaume Estrade, Cristina Villanova-de-Benavent, Peter Nason, Eva Marquis, Nicola J. Horsburgh, Kathryn M. Goodenough, Cheng Xu, Jindřich Kynický, Kalotina Geraki
Format: Article
Language:English
Published: Nature Publishing Group 2020-09-01
Series:Nature Communications
Online Access:https://doi.org/10.1038/s41467-020-17801-5
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spelling doaj-4b3ca714b3774544b4e3898c804eaf7a2021-09-05T11:44:44ZengNature Publishing GroupNature Communications2041-17232020-09-0111111510.1038/s41467-020-17801-5Adsorption of rare earth elements in regolith-hosted clay depositsAnouk M. Borst0Martin P. Smith1Adrian A. Finch2Guillaume Estrade3Cristina Villanova-de-Benavent4Peter Nason5Eva Marquis6Nicola J. Horsburgh7Kathryn M. Goodenough8Cheng Xu9Jindřich Kynický10Kalotina Geraki11School of Earth and Environmental Sciences, University of St. AndrewsSchool of Environment and Technology, University of BrightonSchool of Earth and Environmental Sciences, University of St. AndrewsGET, CNRS, IRD, UPS, University of ToulouseSchool of Environment and Technology, University of BrightonSchool of Environment and Technology, University of BrightonSchool of Environment and Technology, University of BrightonSchool of Earth and Environmental Sciences, University of St. AndrewsBritish Geological Survey, The Lyell CentreCollege of Earth Sciences, Guilin University of TechnologyDepartment of Geology and Pedology, Mendel UniversityDiamond Light Source, Physical ScienceGlobal resources of heavy Rare Earth Elements (REE) are dominantly sourced from Chinese regolith-hosted ion-adsorption deposits, yet the adsorption mechanisms remain unclear. Here, the authors find that heavy REE are adsorbed as easily leachable 8-coordinated outer-sphere hydrated complexes, dominantly onto kaolinite, in clays from both China and Madagascar.https://doi.org/10.1038/s41467-020-17801-5
collection DOAJ
language English
format Article
sources DOAJ
author Anouk M. Borst
Martin P. Smith
Adrian A. Finch
Guillaume Estrade
Cristina Villanova-de-Benavent
Peter Nason
Eva Marquis
Nicola J. Horsburgh
Kathryn M. Goodenough
Cheng Xu
Jindřich Kynický
Kalotina Geraki
spellingShingle Anouk M. Borst
Martin P. Smith
Adrian A. Finch
Guillaume Estrade
Cristina Villanova-de-Benavent
Peter Nason
Eva Marquis
Nicola J. Horsburgh
Kathryn M. Goodenough
Cheng Xu
Jindřich Kynický
Kalotina Geraki
Adsorption of rare earth elements in regolith-hosted clay deposits
Nature Communications
author_facet Anouk M. Borst
Martin P. Smith
Adrian A. Finch
Guillaume Estrade
Cristina Villanova-de-Benavent
Peter Nason
Eva Marquis
Nicola J. Horsburgh
Kathryn M. Goodenough
Cheng Xu
Jindřich Kynický
Kalotina Geraki
author_sort Anouk M. Borst
title Adsorption of rare earth elements in regolith-hosted clay deposits
title_short Adsorption of rare earth elements in regolith-hosted clay deposits
title_full Adsorption of rare earth elements in regolith-hosted clay deposits
title_fullStr Adsorption of rare earth elements in regolith-hosted clay deposits
title_full_unstemmed Adsorption of rare earth elements in regolith-hosted clay deposits
title_sort adsorption of rare earth elements in regolith-hosted clay deposits
publisher Nature Publishing Group
series Nature Communications
issn 2041-1723
publishDate 2020-09-01
description Global resources of heavy Rare Earth Elements (REE) are dominantly sourced from Chinese regolith-hosted ion-adsorption deposits, yet the adsorption mechanisms remain unclear. Here, the authors find that heavy REE are adsorbed as easily leachable 8-coordinated outer-sphere hydrated complexes, dominantly onto kaolinite, in clays from both China and Madagascar.
url https://doi.org/10.1038/s41467-020-17801-5
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