Origin of Critical Metals in Fe–Ni Laterites from the Balkan Peninsula: Opportunities and Environmental Risk

As the global energy sector is expected to experience a gradual shift towards renewable energy sources, access to special metals in known resources is of growing concern within the EU and at a worldwide scale. This is a review on the Fe–Ni ± Co-laterite deposits in the Balkan Peninsula, which are ch...

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Main Authors: Maria Economou-Eliopoulos, Magdalena Laskou, Demetrios G. Eliopoulos, Ifigeneia Megremi, Sofia Kalatha, George D. Eliopoulos
Format: Article
Language:English
Published: MDPI AG 2021-09-01
Series:Minerals
Subjects:
REE
PGE
Online Access:https://www.mdpi.com/2075-163X/11/9/1009
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spelling doaj-fdc39e7131e3417aafab55ca88c180912021-09-26T00:45:06ZengMDPI AGMinerals2075-163X2021-09-01111009100910.3390/min11091009Origin of Critical Metals in Fe–Ni Laterites from the Balkan Peninsula: Opportunities and Environmental RiskMaria Economou-Eliopoulos0Magdalena Laskou1Demetrios G. Eliopoulos2Ifigeneia Megremi3Sofia Kalatha4George D. Eliopoulos5Department of Geology and Geoenvironment, National and Kapodistrian University of Athens, 15784 Athens, GreeceDepartment of Geology and Geoenvironment, National and Kapodistrian University of Athens, 15784 Athens, GreeceInstitute of Geology and Mineral Exploration (IGME), Olympic Village, 13677 Acharnae, GreeceDepartment of Geology and Geoenvironment, National and Kapodistrian University of Athens, 15784 Athens, GreeceDepartment of Geology and Geoenvironment, National and Kapodistrian University of Athens, 15784 Athens, GreeceDepartment of Chemistry, University of Crete, 70013 Heraklion, GreeceAs the global energy sector is expected to experience a gradual shift towards renewable energy sources, access to special metals in known resources is of growing concern within the EU and at a worldwide scale. This is a review on the Fe–Ni ± Co-laterite deposits in the Balkan Peninsula, which are characterized by multistage weathering/redeposition and intense tectonic activities. The ICP-MS analyses of those laterites indicated that they are major natural sources of Ni and Co, with ore grading from 0.21 to 3.5 wt% Ni and 0.03 to 0.31 wt% Co, as well as a significant Sc content (average 55 mg/kg). The SEM-EDS analyses revealed that fine Fe-, Ni-, Co-, and Mn-(hydr)oxides are dominant host minerals and that the enrichment in these elements is probably controlled by the post-formation evolution of initial ore redeposition. The paucity of rare earth element (REE) within the typical Fe–Ni laterite ore and the preferential occurrence of Co (up to 0.31 wt%), REE content (up to 6000 mg/kg ΣREE), and REE-minerals along with Ni, Co, and Mn (asbolane and silicates) towards the lowermost part of the Lokris (C. Greece) laterite ore suggest that their deposition is controlled by epigenetic processes. The platinum-group element (PGE) content in those Fe–Ni laterites, reaching up to 88 μg/kg Pt and 26 μg/kg Pd (up to 186 μg/kg Pd in one sample), which is higher than those in the majority of chromite deposits associated with ophiolites, may indicate important weathering and PGE supergene accumulation. Therefore, the mineralogical and geochemical features of Fe–Ni laterites from the Balkan Peninsula provide evidence for potential sources of certain critical metals and insights to suitable processing and metallurgical methods. In addition, the contamination of soil by heavy metals and irrigation groundwater by toxic Cr(VI), coupled with relatively high Cr(VI) concentrations in water leachates for laterite samples, altered ultramafic rocks and soils neighboring the mining areas and point to a potential human health risk and call for integrated water–soil–plant investigations in the basins surrounding laterite mines.https://www.mdpi.com/2075-163X/11/9/1009Fe–Ni–Co lateritescritical metalsREEPGECr(VI) contamination
collection DOAJ
language English
format Article
sources DOAJ
author Maria Economou-Eliopoulos
Magdalena Laskou
Demetrios G. Eliopoulos
Ifigeneia Megremi
Sofia Kalatha
George D. Eliopoulos
spellingShingle Maria Economou-Eliopoulos
Magdalena Laskou
Demetrios G. Eliopoulos
Ifigeneia Megremi
Sofia Kalatha
George D. Eliopoulos
Origin of Critical Metals in Fe–Ni Laterites from the Balkan Peninsula: Opportunities and Environmental Risk
Minerals
Fe–Ni–Co laterites
critical metals
REE
PGE
Cr(VI) contamination
author_facet Maria Economou-Eliopoulos
Magdalena Laskou
Demetrios G. Eliopoulos
Ifigeneia Megremi
Sofia Kalatha
George D. Eliopoulos
author_sort Maria Economou-Eliopoulos
title Origin of Critical Metals in Fe–Ni Laterites from the Balkan Peninsula: Opportunities and Environmental Risk
title_short Origin of Critical Metals in Fe–Ni Laterites from the Balkan Peninsula: Opportunities and Environmental Risk
title_full Origin of Critical Metals in Fe–Ni Laterites from the Balkan Peninsula: Opportunities and Environmental Risk
title_fullStr Origin of Critical Metals in Fe–Ni Laterites from the Balkan Peninsula: Opportunities and Environmental Risk
title_full_unstemmed Origin of Critical Metals in Fe–Ni Laterites from the Balkan Peninsula: Opportunities and Environmental Risk
title_sort origin of critical metals in fe–ni laterites from the balkan peninsula: opportunities and environmental risk
publisher MDPI AG
series Minerals
issn 2075-163X
publishDate 2021-09-01
description As the global energy sector is expected to experience a gradual shift towards renewable energy sources, access to special metals in known resources is of growing concern within the EU and at a worldwide scale. This is a review on the Fe–Ni ± Co-laterite deposits in the Balkan Peninsula, which are characterized by multistage weathering/redeposition and intense tectonic activities. The ICP-MS analyses of those laterites indicated that they are major natural sources of Ni and Co, with ore grading from 0.21 to 3.5 wt% Ni and 0.03 to 0.31 wt% Co, as well as a significant Sc content (average 55 mg/kg). The SEM-EDS analyses revealed that fine Fe-, Ni-, Co-, and Mn-(hydr)oxides are dominant host minerals and that the enrichment in these elements is probably controlled by the post-formation evolution of initial ore redeposition. The paucity of rare earth element (REE) within the typical Fe–Ni laterite ore and the preferential occurrence of Co (up to 0.31 wt%), REE content (up to 6000 mg/kg ΣREE), and REE-minerals along with Ni, Co, and Mn (asbolane and silicates) towards the lowermost part of the Lokris (C. Greece) laterite ore suggest that their deposition is controlled by epigenetic processes. The platinum-group element (PGE) content in those Fe–Ni laterites, reaching up to 88 μg/kg Pt and 26 μg/kg Pd (up to 186 μg/kg Pd in one sample), which is higher than those in the majority of chromite deposits associated with ophiolites, may indicate important weathering and PGE supergene accumulation. Therefore, the mineralogical and geochemical features of Fe–Ni laterites from the Balkan Peninsula provide evidence for potential sources of certain critical metals and insights to suitable processing and metallurgical methods. In addition, the contamination of soil by heavy metals and irrigation groundwater by toxic Cr(VI), coupled with relatively high Cr(VI) concentrations in water leachates for laterite samples, altered ultramafic rocks and soils neighboring the mining areas and point to a potential human health risk and call for integrated water–soil–plant investigations in the basins surrounding laterite mines.
topic Fe–Ni–Co laterites
critical metals
REE
PGE
Cr(VI) contamination
url https://www.mdpi.com/2075-163X/11/9/1009
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