Evaluation of Sc Concentrations in Ni-Co Laterites Using Al as a Geochemical Proxy

Scandium (Sc) is used in several modern industrial applications. Recently, significant Sc concentrations (~100 ppm) were reported in some nickel-cobalt lateritic ores, where Sc may be valuably co-produced. However, Sc is typically not included in routine analyses of Ni-Co ores. This contribution exa...

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Main Authors: Yoram Teitler, Sylvain Favier, Jean-Paul Ambrosi, Brice Sevin, Fabrice Golfier, Michel Cathelineau
Format: Article
Language:English
Published: MDPI AG 2022-05-01
Series:Minerals
Subjects:
Online Access:https://www.mdpi.com/2075-163X/12/5/615
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author Yoram Teitler
Sylvain Favier
Jean-Paul Ambrosi
Brice Sevin
Fabrice Golfier
Michel Cathelineau
author_facet Yoram Teitler
Sylvain Favier
Jean-Paul Ambrosi
Brice Sevin
Fabrice Golfier
Michel Cathelineau
author_sort Yoram Teitler
collection DOAJ
description Scandium (Sc) is used in several modern industrial applications. Recently, significant Sc concentrations (~100 ppm) were reported in some nickel-cobalt lateritic ores, where Sc may be valuably co-produced. However, Sc is typically not included in routine analyses of Ni-Co ores. This contribution examines the relevance of using routinely analysed elements as geochemical proxies for estimating Sc concentration and distribution. Three Ni-Co lateritic deposits from New Caledonia were investigated. In each deposit, Sc is well correlated with Al<sub>2</sub>O<sub>3</sub>. The slopes of deposit-scale Sc-Al<sub>2</sub>O<sub>3</sub> regression lines are remarkably controlled by the composition of enstatite from the parent peridotite. In all deposits, maximum Sc enrichment occurs in the yellow limonite, above the highest Ni and Co enrichment zones. Sc- and Al-bearing crystalline goethite is predominant in the oxide-rich zones, though Sc shows a higher affinity for amorphous iron oxides than Al. We propose that, in already assayed Ni-Co lateritic ores, the concentration and distribution of Sc can be estimated from that of Al. Deposit-scale Sc-Al<sub>2</sub>O<sub>3</sub> correlations may be determined after analysing a limited number of spatially and chemically representative samples. Therefore, mining operators may get a first-order evaluation of the Sc potential resource in Ni-Co lateritic deposits at low additional costs.
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spelling doaj.art-bc9c42695ab041e28281d3cd3ddcbf732023-11-23T12:19:28ZengMDPI AGMinerals2075-163X2022-05-0112561510.3390/min12050615Evaluation of Sc Concentrations in Ni-Co Laterites Using Al as a Geochemical ProxyYoram Teitler0Sylvain Favier1Jean-Paul Ambrosi2Brice Sevin3Fabrice Golfier4Michel Cathelineau5Université de Lorraine, CNRS, GeoRessources, 54506 Vandoeuvre-lès-Nancy, FranceUniversité de Lorraine, CNRS, GeoRessources, 54506 Vandoeuvre-lès-Nancy, FranceAix-Marseille Université, CNRS, IRD, INRAE, CEREGE, CEDEX 4, 13545 Aix-en-Provence, FranceService de la Géologie de Nouvelle-Calédonie, Direction de l’Industrie, des Mines et de l’Énergie, 1ter Rue Unger, BP 465, CEDEX, 98845 Nouméa, New CaledoniaUniversité de Lorraine, CNRS, GeoRessources, 54506 Vandoeuvre-lès-Nancy, FranceUniversité de Lorraine, CNRS, GeoRessources, 54506 Vandoeuvre-lès-Nancy, FranceScandium (Sc) is used in several modern industrial applications. Recently, significant Sc concentrations (~100 ppm) were reported in some nickel-cobalt lateritic ores, where Sc may be valuably co-produced. However, Sc is typically not included in routine analyses of Ni-Co ores. This contribution examines the relevance of using routinely analysed elements as geochemical proxies for estimating Sc concentration and distribution. Three Ni-Co lateritic deposits from New Caledonia were investigated. In each deposit, Sc is well correlated with Al<sub>2</sub>O<sub>3</sub>. The slopes of deposit-scale Sc-Al<sub>2</sub>O<sub>3</sub> regression lines are remarkably controlled by the composition of enstatite from the parent peridotite. In all deposits, maximum Sc enrichment occurs in the yellow limonite, above the highest Ni and Co enrichment zones. Sc- and Al-bearing crystalline goethite is predominant in the oxide-rich zones, though Sc shows a higher affinity for amorphous iron oxides than Al. We propose that, in already assayed Ni-Co lateritic ores, the concentration and distribution of Sc can be estimated from that of Al. Deposit-scale Sc-Al<sub>2</sub>O<sub>3</sub> correlations may be determined after analysing a limited number of spatially and chemically representative samples. Therefore, mining operators may get a first-order evaluation of the Sc potential resource in Ni-Co lateritic deposits at low additional costs.https://www.mdpi.com/2075-163X/12/5/615scandiumlateriteNi-lateritesequential extractionNew Caledonia
spellingShingle Yoram Teitler
Sylvain Favier
Jean-Paul Ambrosi
Brice Sevin
Fabrice Golfier
Michel Cathelineau
Evaluation of Sc Concentrations in Ni-Co Laterites Using Al as a Geochemical Proxy
Minerals
scandium
laterite
Ni-laterite
sequential extraction
New Caledonia
title Evaluation of Sc Concentrations in Ni-Co Laterites Using Al as a Geochemical Proxy
title_full Evaluation of Sc Concentrations in Ni-Co Laterites Using Al as a Geochemical Proxy
title_fullStr Evaluation of Sc Concentrations in Ni-Co Laterites Using Al as a Geochemical Proxy
title_full_unstemmed Evaluation of Sc Concentrations in Ni-Co Laterites Using Al as a Geochemical Proxy
title_short Evaluation of Sc Concentrations in Ni-Co Laterites Using Al as a Geochemical Proxy
title_sort evaluation of sc concentrations in ni co laterites using al as a geochemical proxy
topic scandium
laterite
Ni-laterite
sequential extraction
New Caledonia
url https://www.mdpi.com/2075-163X/12/5/615
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AT bricesevin evaluationofscconcentrationsinnicolateritesusingalasageochemicalproxy
AT fabricegolfier evaluationofscconcentrationsinnicolateritesusingalasageochemicalproxy
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