Nitrate sources and processes in the surface water of a tropical reservoir by stable isotopes and mixing model.

Autor: Fadhullah W; Environmental Technology Section, School of Industrial Technology, Universiti Sains Malaysia, 11800 USM Penang, Malaysia; Environmental and Occupational Health Program, School of Health Sciences, Health Campus, Universiti Sains Malaysia 16150 USM, Kubang Kerian, Kelantan, Malaysia. Electronic address: widad@usm.my., Yaccob NS; Environmental Technology Section, School of Industrial Technology, Universiti Sains Malaysia, 11800 USM Penang, Malaysia., Syakir MI; Environmental Technology Section, School of Industrial Technology, Universiti Sains Malaysia, 11800 USM Penang, Malaysia; Centre for Global Sustainability Studies (CGSS), Universiti Sains Malaysia, 11800 USM Penang, Malaysia., Muhammad SA; Environmental Technology Section, School of Industrial Technology, Universiti Sains Malaysia, 11800 USM Penang, Malaysia; Analytical Biochemistry Research Centre, Universiti Sains Malaysia, 11800 USM Penang, Malaysia., Yue FJ; State Key Laboratory of Environmental Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550081, China; Institute of Surface-Earth System Science, Tianjin University, Tianjin 300072, China., Li SL; Institute of Surface-Earth System Science, Tianjin University, Tianjin 300072, China.
Jazyk: angličtina
Zdroj: The Science of the total environment [Sci Total Environ] 2020 Jan 15; Vol. 700, pp. 134517. Date of Electronic Publication: 2019 Oct 08.
DOI: 10.1016/j.scitotenv.2019.134517
Abstrakt: Nitrate is one of the primary nutrients associated with sedimentation and fuels eutrophication in reservoir systems. In this study, water samples from Bukit Merah Reservoir (BMR) were analysed using a combination of water chemistry, water stable isotopes (δ 2 H-H 2 O and δ 18 O-H 2 O) and nitrate stable isotopes (δ 15 N-NO 3 - and δ 18 O-NO 3 - ). The objective was to evaluate nitrate sources and processes in BMR, the oldest man-made reservoir in Malaysia. The δ 15 N-NO 3 - values in the river and reservoir water samples were in the range +0.4 to +14.9‰ while the values of δ 18 O-NO 3 - were between -0.01 and +39.4‰, respectively. The dual plots of δ 15 N-NO 3 - and δ 18 O-NO 3 - reflected mixing sources from atmospheric deposition (AD) input, ammonium in fertilizer/rain, soil nitrogen, and manure and sewage (MS) as the sources of nitrate in the surface water of BMR. Nitrate stable isotopes suggested that BMR undergoes processes such as nitrification and mixing. Denitrification and assimilation were not prevalent in the system. The Bayesian mixing model highlighted the dominance of MS sources in the system while AD contributed more proportion in the reservoir during both seasons than in the river. The use of δ 13 C, δ 15 N, and C:N ratios enabled the identification of terrestrial sources of the organic matter in the sediment, enhancing the understanding of sedimentation associated with nutrients previously reported in BMR. Overall, the nitrate sources and processes should be considered in decision-making in the management of the reservoir for irrigation, Arowana fish culture and domestic water supply.
(Copyright © 2019 Elsevier B.V. All rights reserved.)
Databáze: MEDLINE
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