Nitrate contamination of groundwater in the Lower Volta River Basin of Ghana: Sources and related human health risks.

Autor: Egbi CD; Regional Water and Environmental Sanitation Center, Dept of Civil Engineering, Kwame Nkrumah University of Science and Technology, Private Mail Bag, University Post Office, Kumasi, Ghana; National Isotope Hydrology Lab, National Nuclear Research Institute, Ghana Atomic Energy Commission, P. O. Box LG 80, Legon-Accra, Ghana., Anornu GK; Regional Water and Environmental Sanitation Center, Dept of Civil Engineering, Kwame Nkrumah University of Science and Technology, Private Mail Bag, University Post Office, Kumasi, Ghana., Ganyaglo SY; National Isotope Hydrology Lab, National Nuclear Research Institute, Ghana Atomic Energy Commission, P. O. Box LG 80, Legon-Accra, Ghana; Graduate School of Nuclear and Allied Sciences, University of Ghana, P. O. Box LG 80, Legon-Accra, Ghana. Electronic address: sganyaglo@yahoo.co.uk., Appiah-Adjei EK; Regional Water and Environmental Sanitation Center, Dept of Civil Engineering, Kwame Nkrumah University of Science and Technology, Private Mail Bag, University Post Office, Kumasi, Ghana; Geological Engineering Department, Kwame Nkrumah University of Science and Technology, Private Mail Bag, University Post Office, Kumasi, Ghana., Li SL; The State Key Laboratory of Environmental Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences Guiyang, 550002, China; Institute of Surface-Earth System Science, Tianjin University, China., Dampare SB; Graduate School of Nuclear and Allied Sciences, University of Ghana, P. O. Box LG 80, Legon-Accra, Ghana.
Jazyk: angličtina
Zdroj: Ecotoxicology and environmental safety [Ecotoxicol Environ Saf] 2020 Mar 15; Vol. 191, pp. 110227. Date of Electronic Publication: 2020 Jan 22.
DOI: 10.1016/j.ecoenv.2020.110227
Abstrakt: A significant population within the Lower Volta River Basin of Ghana relies solely on untreated groundwater (GW) and surface water (SW) for various purposes. However, negative practices associated with increasing human activities pose threats to particularly GW quality in the basin. Using NO 3 - as a proxy, this study mainly focused on the status of GW contamination, origins of NO 3 - and potential human health risks through integrated hydrochemistry, correlation analysis, isotopes ( 15 N, δ 18 O), Bayesian and USEPA human health risk models. Slightly acidic to alkaline GW and SW environments were observed. Electrical conductivity (EC) values above 1000 μS/cm were recorded in 45% of the GW with a maximum of 19370 μS/cm. NO 3 - in GW ranged from 0.12 to 733 mg/L with average 59.6 mg/L and positively correlated with K + , Ca 2+ , Mg 2+, Cl - , Na + and EC. In SW, a maximum of 5.3 mg/L of NO 3 - was observed. Largely, 75% of the GW exceeded local background NO 3 - value of 2.1 mg/L, while 35% were above the WHO recommended value of 50 mg/L. Bivariate and correlation relationships elucidated human contributions to sources of NO 3 - , Cl - , SO 4 2- and K + to GW in the basin. From NO 3 - /Cl - ratio, 43% of the GW and 21% of SW were affected by effluents and agrochemicals. Values for δ 15 N-NO 3 - and δ 18 O-NO 3 - ranged from +4.2‰ to +27.5‰ and +4.5‰ to +19.9‰ for GW, and from +3.8‰ to +14.0‰ and +10.7‰ to +25.2‰ for SW. Manure, septic effluents and mineralized fertilizers are sources of NO 3 - contamination of water in the basin. The Bayesian model apportioned 80% of GW NO 3 - contamination to sewage/manure. Hazard index indicated 70%, 50% and 48% medium to high-risk levels for infants, children and adults respectively, with 79% high-risk of SW NO 2 - contamination to infants. Immediate measures for GW and SW quality protection are recommended.
Competing Interests: Declaration of competing interests There is no conflict of interest issue regarding the publication of this manuscript.
(Copyright © 2020 Elsevier Inc. All rights reserved.)
Databáze: MEDLINE
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