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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Autores principales: 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
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Publicado: Nature Portfolio 2020
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Acceso en línea:https://doaj.org/article/4b3ca714b3774544b4e3898c804eaf7a
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spelling oai:doaj.org-article:4b3ca714b3774544b4e3898c804eaf7a2021-12-02T19:09:20ZAdsorption of rare earth elements in regolith-hosted clay deposits10.1038/s41467-020-17801-52041-1723https://doaj.org/article/4b3ca714b3774544b4e3898c804eaf7a2020-09-01T00:00:00Zhttps://doi.org/10.1038/s41467-020-17801-5https://doaj.org/toc/2041-1723Global 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.Anouk M. BorstMartin P. SmithAdrian A. FinchGuillaume EstradeCristina Villanova-de-BenaventPeter NasonEva MarquisNicola J. HorsburghKathryn M. GoodenoughCheng XuJindřich KynickýKalotina GerakiNature PortfolioarticleScienceQENNature Communications, Vol 11, Iss 1, Pp 1-15 (2020)
institution DOAJ
collection DOAJ
language EN
topic Science
Q
spellingShingle Science
Q
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
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.
format article
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
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 Portfolio
publishDate 2020
url https://doaj.org/article/4b3ca714b3774544b4e3898c804eaf7a
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