Acid mine drainage and smelter-derived sources affecting water geochemistry in the upper Nakdong River, South Korea

Both the smelter and acid mine drainage (AMD) in uppermost streams impact water geochemistry and deteriorate water quality. Efficient water quality management requires identifying the contribution of each source to stream water geochemistry. In this study, we aimed to determine the natural and anthr...

Ausführliche Beschreibung

Gespeichert in:
Bibliographische Detailangaben
Veröffentlicht in:The Science of the total environment 2023-07, Vol.880, p.163353-163353, Article 163353
Hauptverfasser: Jung, Youn-Young, Choi, Seung-Hyun, Choi, Moojin, Bong, Yeon-Sik, Park, Min-Yeong, Lee, Kwang-Sik, Shin, Woo-Jin
Format: Artikel
Sprache:eng
Schlagworte:
Online-Zugang:Volltext
Tags: Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
Beschreibung
Zusammenfassung:Both the smelter and acid mine drainage (AMD) in uppermost streams impact water geochemistry and deteriorate water quality. Efficient water quality management requires identifying the contribution of each source to stream water geochemistry. In this study, we aimed to determine the natural and anthropogenic sources (AMD and smelting) affecting water geochemistry by considering seasonality. Water samples were collected, from May 2020 to April 2021, in a main channel (Nakdong River) and tributaries in a small watershed including mines and smelters. The watershed is characterized by a carbonate-rich area in the upper-middle reaches and silicate-rich area in the middle-lower reaches. On the plots of Ca/Na vs. Mg/Na and 2(Ca + Mg) vs. HCO3 + 2SO4, the water geochemistry was predominantly explained by the carbonate and silicate weathering associated with sulfuric and carbonic acids. According to typical δ15N values for sources, nitrate contribution from soil-N mainly impacted water geochemistry, regardless of seasonality; the contribution from agricultural activity and sewage was negligible. Water geochemistry in the main channel samples was discriminated before and after passing through the smelter. The effects of the smelter were evident in elevated SO4, Zn, and Tl concentrations and in δ66Zn values; this was further supported by the relationships between Cl/HCO3 and SO4/HCO3 and between δ66Zn and Zn. These results were pronounced during winter, when the flush-out effect was absent. Our results suggest that multi-isotopes and chemical composition analyses can trace multiple sources influencing the water geochemistry in watersheds containing AMD and smelters. [Display omitted] •AMD, sulfide mineral oxidation, and soil SO4 contribute to water geochemistry.•Sulfate sources for most samples are explained by a mix of the three components.•Water geochemistry changed before and after the river passed a Zn-smelter.•Pollutant contribution showed seasonal variation due to the flush-out effect.•Tl and Zn concentration and δ66Zn reflected the smelter's effect on water geochemistry.
ISSN:0048-9697
1879-1026
DOI:10.1016/j.scitotenv.2023.163353