Comparative analysis of vertical metal zonation in Ginigalpelessa and Indikolapelessa serpentinite complex

dc.contributor.authorMahendran, M
dc.contributor.authorMaduranga, U.K.D.
dc.contributor.authorAmarasinghe, A.A.Y.D.T.
dc.contributor.authorAbeysinghe, A.M.K.B.
dc.contributor.authorRatnayake, N.P.
dc.contributor.authorPremasiri, H.M.R.
dc.contributor.authorDushyantha, N.P.
dc.contributor.authorBatapola, N.M.
dc.contributor.authorDilshara, R.M.P.
dc.contributor.editorIresha, H.
dc.contributor.editorElakneswaran, Y.
dc.contributor.editorDassanayake, A.
dc.contributor.editorJayawardena, C.
dc.date.accessioned2025-01-08T04:32:30Z
dc.date.available2025-01-08T04:32:30Z
dc.date.issued2024
dc.description.abstractSerpentinite deposits in Ginigalpelessa and Indikolapelessa Sri Lanka, are known to exhibit a high supergene enrichment of Ni, Cr, and Co in the regolith due to the prolonged weathering of the underlying serpentinite bedrock. However, no detailed studies have been conducted to determine the vertical zonation of these critical metals in these deposits. The vertical metal distribution of a deposit is significant to delineate its vertical metal enrichment patterns and mobilization which may lead to the identification of efficient exploration and extraction methods. Therefore, this study assessed the vertical zonation of Ni, Cr, and Co in both Ginigalpelessa and Indikolapelessa serpentinite deposits. Twenty-four soil (n=12) and weathered rock (n=12) samples from 4 soil horizons (O, A, B, C) in soil profile were collected and analyzed for Ni, Co, Cr, and Cu by ICP-MS. Our findings revealed high metal concentrations in the soil or highly weathered rock samples over the partially weathered rock samples. The Ginigalpelessa deposit demonstrated4 a higher concentration of Ni, Co, Cr, and Cu compared to the Indikolapelessa deposit. It observed that the concentrations of Ni, Co, Cr and Cu in the topsoil were lower compared to deeper horizons (A, B, and C) in some locations. This may have occurred due to the bioavailability of some metals like Ni, which accumulates in the plants and reduce the concentration in the soil. Conversely, the low bioavailability of Cr compared to the other metals have resulted high Cr concentrations in the surface horizon. In addition, previous studies found that Cr is immobile, whereas Ni and Co are scarcely mobile under the moderate acidic conditions in the serpentine soil. During the weathering process, the slightly acidic rainwater leaches these Ni-like metals from the O and A horizons, resulting their enrichment in the B horizon. However, further studies are necessary to identify the suitable leaching or extraction method to recover these metals from serpentine soil. Therefore, this research contributes to a deeper understanding of vertical metal zonation in serpentinite deposits to facilitate more efficient and sustainable exploration of valuable metals like Ni in serpentinite deposits.en_US
dc.identifier.citationMahendran, M, Maduranga, UKD Amarasinghe, AAYDT Abeysinghe, AMKB, Ratnayake, NP , Premasiri, HMR, Dushyantha, NP,Batapola, NM & Dilshara, RMP, (2024). Comparative analysis of vertical metal zonation in Ginigalpelessa and Indikolapelessa serpentinite complex. In H. Iresha, Y. Elakneswaran, A. Dassanayake, & C. Jayawardena (Ed.), Eight International Symposium on Earth Resources Management & Environment – ISERME 2024: Proceedings of the international Symposium on Earth Resources Management & Environment (pp. 105-112). Department of Earth Resources Engineering, University of Moratuwa. https://doi.org/10.31705/ISERME.2024.18
dc.identifier.conferenceEight International Symposium on Earth Resources Management & Environment - ISERME 2024en_US
dc.identifier.departmentDepartment of Earth Resources Engineeringen_US
dc.identifier.doihttps://doi.org/10.31705/ISERME.2024.18
dc.identifier.emailamkb@uom.lk,en_US
dc.identifier.facultyEngineeringen_US
dc.identifier.pgnospp. 105-112en_US
dc.identifier.placeHokkaido University, Japanen_US
dc.identifier.proceedingProceedings of International Symposium on Earth Resources Management and Environmenten_US
dc.identifier.urihttp://dl.lib.uom.lk/handle/123/23104
dc.identifier.year2024en_US
dc.language.isoenen_US
dc.publisherDivision of Sustainable Resources Engineering, Hokkaido University, Japanen_US
dc.subjectWeathering processesen_US
dc.subjectNickelen_US
dc.subjectInductively Coupled Plasma Mass Spectrometryen_US
dc.subjectMetal distributionen_US
dc.subjectSri Lanka.en_US
dc.titleComparative analysis of vertical metal zonation in Ginigalpelessa and Indikolapelessa serpentinite complexen_US
dc.typeConference-Full-texten_US

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Serpentinite deposits in Ginigalpelessa and Indikolapelessa Sri Lanka, are known to exhibit a high supergene enrichment of Ni, Cr, and Co in the regolith due to the prolonged weathering of the underlying serpentinite bedrock. However, no detailed studies have been conducted to determine the vertical zonation of these critical metals in these deposits. The vertical metal distribution of a deposit is significant to delineate its vertical metal enrichment patterns and mobilization which may lead to the identification of efficient exploration and extraction methods. Therefore, this study assessed the vertical zonation of Ni, Cr, and Co in both Ginigalpelessa and Indikolapelessa serpentinite deposits. Twenty-four soil (n=12) and weathered rock (n=12) samples from 4 soil horizons (O, A, B, C) in soil profile were collected and analyzed for Ni, Co, Cr, and Cu by ICP-MS. Our findings revealed high metal concentrations in the soil or highly weathered rock samples over the partially weathered rock samples. The Ginigalpelessa deposit demonstrated4 a higher concentration of Ni, Co, Cr, and Cu compared to the Indikolapelessa deposit. It observed that the concentrations of Ni, Co, Cr and Cu in the topsoil were lower compared to deeper horizons (A, B, and C) in some locations. This may have occurred due to the bioavailability of some metals like Ni, which accumulates in the plants and reduce the concentration in the soil. Conversely, the low bioavailability of Cr compared to the other metals have resulted high Cr concentrations in the surface horizon. In addition, previous studies found that Cr is immobile, whereas Ni and Co are scarcely mobile under the moderate acidic conditions in the serpentine soil. During the weathering process, the slightly acidic rainwater leaches these Ni-like metals from the O and A horizons, resulting their enrichment in the B horizon. However, further studies are necessary to identify the suitable leaching or extraction method to recover these metals from serpentine soil. Therefore, this research contributes to a deeper understanding of vertical metal zonation in serpentinite deposits to facilitate more efficient and sustainable exploration of valuable metals like Ni in serpentinite deposits.

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