Trace element distribution, sources, toxicity risk characteristics associated with lacustrine groundwater discharge in boreal lakes: Implications for the eco-environmental security in the Yellow River Basin, China

• Trace elements in boreal lake systems in the Yellow River Basin were investigated. • LGD trace element fluxes in lake Ulansuhai were greater than those in lake Daihai. • Natural sources are the main suppliers of trace elements in the two lake basins. • The total toxicity risk level of trace elements in lake Ulansuhai was high. • Results provide new insights for eco-environmental security in Yellow River basin. Although the pollution of trace elements has been extensively studied, there is still a lack of comprehensive understanding regarding accumulation of these elements in lake ecosystems within the Yellow River basin, specifically the effects of lacustrine groundwater discharge (LGD) on trace elements. This study investigated the distribution, sources, and toxicity risks associated with 20 target trace elements (i.e., Li, Sc, Ti, V, Mn, Cr, Co, Ni, Cu, Zn, Rb, Y, Mo, Sb, Ba, W, Tl, Pb, U and Sr) in lake water (LW), groundwater (GW), and river water (RW) influenced by the LGD process in lake Ulansuhai and lake Daihai. The natural source is the primary contributor of trace elements in both LW and GW within the two lake basins, while industrial discharge plays a secondary role. The average LGD fluxes in lake Ulansuhai and Daihai basins were 6.39 × 10 5 m 3 /d and 1.07 × 10 5 m 3 /d, respectively. Additionally, the trace element fluxes from LGD in lake Ulansuhai (mean of 106,659.37 g/d) exceeded those observed in lake Daihai (mean of 3236.57 g/d). The overall toxicity risk was found to be higher in lake Ulansuhai (LW (17.36) > RW (16.81) > GW (12.76)) compared to lake Daihai (GW (10.43) > LW (9.10) > RW (4.63)). As well as the toxicity levels of trace elements in lake Ulansuhai were elevated compared to Daihai, which can be attributed to the influenced of ion compositions and water nutrients. Among them, Ca 2+ , Mg 2+ , and SO 4 2+ were identified as key ions impacting the toxicity of trace elements in lake Ulansuhai. These findings provide crucial insights for targeted monitoring and mitigation of trace element pollution in the Yellow River basin’s lake ecosystems.

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Publication Details

Journal
Ecological Indicators
Published
2024-09-13
DOI
https://doi.org/10.1016/j.ecolind.2024.112600
Citations
6
Primary Topic
Groundwater and Isotope Geochemistry
Type
article
Field-Weighted Citation Impact
2.08

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article

Trace element distribution, sources, toxicity risk characteristics associated with lacustrine groundwater discharge in boreal lakes: Implications for the eco-environmental security in the Yellow River Basin, China

Yuanzhen Zhao, Shaogang Dong, Xiaohui Ren, Ruihong Yu et al.
6 citations
Ecological Indicators
Groundwater and Isotope Geochemistry
2.08
article

Trace element distribution, sources, toxicity risk characteristics associated with lacustrine groundwater discharge in boreal lakes: Implications for the eco-environmental security in the Yellow River Basin, China

Yuanzhen Zhao, Shaogang Dong, Xiaohui Ren, Ruihong Yu, Juliang Wang, Xu Yang, Shen Qu
article en
6 citations

Abstract

• Trace elements in boreal lake systems in the Yellow River Basin were investigated. • LGD trace element fluxes in lake Ulansuhai were greater than those in lake Daihai. • Natural sources are the main suppliers of trace elements in the two lake basins. • The total toxicity risk level of trace elements in lake Ulansuhai was high. • Results provide new insights for eco-environmental security in Yellow River basin. Although the pollution of trace elements has been extensively studied, there is still a lack of comprehensive understanding regarding accumulation of these elements in lake ecosystems within the Yellow River basin, specifically the effects of lacustrine groundwater discharge (LGD) on trace elements. This study investigated the distribution, sources, and toxicity risks associated with 20 target trace elements (i.e., Li, Sc, Ti, V, Mn, Cr, Co, Ni, Cu, Zn, Rb, Y, Mo, Sb, Ba, W, Tl, Pb, U and Sr) in lake water (LW), groundwater (GW), and river water (RW) influenced by the LGD process in lake Ulansuhai and lake Daihai. The natural source is the primary contributor of trace elements in both LW and GW within the two lake basins, while industrial discharge plays a secondary role. The average LGD fluxes in lake Ulansuhai and Daihai basins were 6.39 × 10 5 m 3 /d and 1.07 × 10 5 m 3 /d, respectively. Additionally, the trace element fluxes from LGD in lake Ulansuhai (mean of 106,659.37 g/d) exceeded those observed in lake Daihai (mean of 3236.57 g/d). The overall toxicity risk was found to be higher in lake Ulansuhai (LW (17.36) > RW (16.81) > GW (12.76)) compared to lake Daihai (GW (10.43) > LW (9.10) > RW (4.63)). As well as the toxicity levels of trace elements in lake Ulansuhai were elevated compared to Daihai, which can be attributed to the influenced of ion compositions and water nutrients. Among them, Ca 2+ , Mg 2+ , and SO 4 2+ were identified as key ions impacting the toxicity of trace elements in lake Ulansuhai. These findings provide crucial insights for targeted monitoring and mitigation of trace element pollution in the Yellow River basin’s lake ecosystems.

Ecological IndicatorsVol. 167
Inner Mongolia Agricultural University (CN), Inner Mongolia University (CN)
National Natural Science Foundation of China
Openalex Percentile: Top 14%
Groundwater and Isotope Geochemistry
2.08
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