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Geochemical assessment and speciation of metals in sediments of Osun and Erinle Rivers, Southwestern Nigeria

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Abstract

Fifty sediment samples were collected from Osun (urban) and Erinle (suburban) rivers in addition to ten samples of the underlying rock types (schist and gneiss) and analyzed for elemental constituents while speciation of metals was determined by sequential analysis. Data were geochemically evaluated and ArcGIS was used to generate geochemical maps. Metal concentrations (ppm) in sub-urban and urban areas were Cd (0.2–0.2, 0.2–1.1), Cu (37.0–272.0, 49.0–970.0), Ni (6.0–27.0, 3.0–43.0), Pb (16.0–67.0, 15.0–2650.0), Zn (32.0–170.0, 50.0–987.0), Co (8.0–60.0, 2.0–86.0), Cr (26.0–153.0, 9.0–128.0), V (30.0–142.0, 9.0–135.0), and Mn (442.0–5100.0, 107.0–3930.0), respectively. In the rocks, Cu, Ni, Pb, Co, Cr, V, and Zn, concentrations (ppm) were below detection limit (BDL)-0.05, BDL-38.00; 6.23–12.00, BDL-20.00; 3.78–6.23, BDL-5.00; BDL-0.20, BDL-4.00; 5.00–9.00, BDL-66.00; 15.99–32.00, BDL-130.00; and 18.00–26.00, BDL-48.00, respectively, with Cu, Pb, Zn, Cd, and Mn of elevated concentrations in sediments compared with that of the rocks, being indication of additional anthropogenic sourcing. Calculated contamination indices revealed contamination for sediment from the urban areas compared to those from the sub-urban. High percentage of Pb (2.94–81.92%), Cu (31.69–45.95%), Zn (49.2–65.5%), Cd (31.69–45.95%), and Mn (12.13–37.50%) are hosted by the bio-available phases (carbonate, organic, and sulfide). The geochemical distribution of metals in the sediments of the Osun and Erinle rivers is governed by both geogenic (Ni-Cr-Co-V) and anthropogenic (Pb-Cd-Zn) activities. Elevated concentration and occurrences of the selected metals in the bio-available phases pose potential health risk to people in the urban area.

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Correspondence to A. S. Olatunji.

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Okunola, O.W., Olatunji, A.S. Geochemical assessment and speciation of metals in sediments of Osun and Erinle Rivers, Southwestern Nigeria. Arab J Geosci 10, 366 (2017). https://doi.org/10.1007/s12517-017-3110-1

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  • DOI: https://doi.org/10.1007/s12517-017-3110-1

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