Long-Term Evolution of Uranium Mobility within Sulfated Mill Tailings in Arid Regions: A Reactive Transport Study

Management of mill tailings is an important part of mining operations that aims at preventing environmental dispersion of contaminants of concern. To this end, geochemical models and reactive transport modeling provide a quantitative assessment of the mobility of the main contaminants. In arid regio...

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Autores principales: Nicolas Seigneur, Laurent De Windt, Adrien Déjeant, Vincent Lagneau, Michaël Descostes
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Publicado: MDPI AG 2021
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Acceso en línea:https://doaj.org/article/ec3a28efe0e34aca8077434d774fcdd3
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spelling oai:doaj.org-article:ec3a28efe0e34aca8077434d774fcdd32021-11-25T18:26:15ZLong-Term Evolution of Uranium Mobility within Sulfated Mill Tailings in Arid Regions: A Reactive Transport Study10.3390/min111112012075-163Xhttps://doaj.org/article/ec3a28efe0e34aca8077434d774fcdd32021-10-01T00:00:00Zhttps://www.mdpi.com/2075-163X/11/11/1201https://doaj.org/toc/2075-163XManagement of mill tailings is an important part of mining operations that aims at preventing environmental dispersion of contaminants of concern. To this end, geochemical models and reactive transport modeling provide a quantitative assessment of the mobility of the main contaminants. In arid regions with limited rainfall and intense evaporation, solutes transport may significantly differ from the usual gravity-driven vertical flow. In the uranium tailings of the Cominak mine (Niger), these evaporative processes resulted in the crystallization of gypsum, and to a lesser extent jarosite, and in the formation of surface levels of sulfated gypcrete, locally enriched in uranium. We present a fully coupled reactive transport modeling approach using HYTEC, encompassing evaporation, to quantitatively reproduce the complex sequence of observed coupled hydrogeochemical processes. The sulfated gypcrete formation, porosity evolution and solid uranium content were successfully reproduced at the surface and paleosurfaces of the tailing deposit. Simulations confirm that high solubility uranyl-sulfate phase may form at the atmospheric boundary where evaporation takes place, which would then be transformed into uranyl-phosphate phases after being watered or buried under fresh tailings. As these phases usually exhibit a lower solubility, this transition is beneficial for mine operators and tailings management.Nicolas SeigneurLaurent De WindtAdrien DéjeantVincent LagneauMichaël DescostesMDPI AGarticleuranium mill tailingsevaporitic systemsreactive transport modelingHYTECcoupled processesgeochemistryMineralogyQE351-399.2ENMinerals, Vol 11, Iss 1201, p 1201 (2021)
institution DOAJ
collection DOAJ
language EN
topic uranium mill tailings
evaporitic systems
reactive transport modeling
HYTEC
coupled processes
geochemistry
Mineralogy
QE351-399.2
spellingShingle uranium mill tailings
evaporitic systems
reactive transport modeling
HYTEC
coupled processes
geochemistry
Mineralogy
QE351-399.2
Nicolas Seigneur
Laurent De Windt
Adrien Déjeant
Vincent Lagneau
Michaël Descostes
Long-Term Evolution of Uranium Mobility within Sulfated Mill Tailings in Arid Regions: A Reactive Transport Study
description Management of mill tailings is an important part of mining operations that aims at preventing environmental dispersion of contaminants of concern. To this end, geochemical models and reactive transport modeling provide a quantitative assessment of the mobility of the main contaminants. In arid regions with limited rainfall and intense evaporation, solutes transport may significantly differ from the usual gravity-driven vertical flow. In the uranium tailings of the Cominak mine (Niger), these evaporative processes resulted in the crystallization of gypsum, and to a lesser extent jarosite, and in the formation of surface levels of sulfated gypcrete, locally enriched in uranium. We present a fully coupled reactive transport modeling approach using HYTEC, encompassing evaporation, to quantitatively reproduce the complex sequence of observed coupled hydrogeochemical processes. The sulfated gypcrete formation, porosity evolution and solid uranium content were successfully reproduced at the surface and paleosurfaces of the tailing deposit. Simulations confirm that high solubility uranyl-sulfate phase may form at the atmospheric boundary where evaporation takes place, which would then be transformed into uranyl-phosphate phases after being watered or buried under fresh tailings. As these phases usually exhibit a lower solubility, this transition is beneficial for mine operators and tailings management.
format article
author Nicolas Seigneur
Laurent De Windt
Adrien Déjeant
Vincent Lagneau
Michaël Descostes
author_facet Nicolas Seigneur
Laurent De Windt
Adrien Déjeant
Vincent Lagneau
Michaël Descostes
author_sort Nicolas Seigneur
title Long-Term Evolution of Uranium Mobility within Sulfated Mill Tailings in Arid Regions: A Reactive Transport Study
title_short Long-Term Evolution of Uranium Mobility within Sulfated Mill Tailings in Arid Regions: A Reactive Transport Study
title_full Long-Term Evolution of Uranium Mobility within Sulfated Mill Tailings in Arid Regions: A Reactive Transport Study
title_fullStr Long-Term Evolution of Uranium Mobility within Sulfated Mill Tailings in Arid Regions: A Reactive Transport Study
title_full_unstemmed Long-Term Evolution of Uranium Mobility within Sulfated Mill Tailings in Arid Regions: A Reactive Transport Study
title_sort long-term evolution of uranium mobility within sulfated mill tailings in arid regions: a reactive transport study
publisher MDPI AG
publishDate 2021
url https://doaj.org/article/ec3a28efe0e34aca8077434d774fcdd3
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AT vincentlagneau longtermevolutionofuraniummobilitywithinsulfatedmilltailingsinaridregionsareactivetransportstudy
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