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- W4224854593 abstract "Riverine lithium (Li) isotopes have been considered as a robust tracer for silicate weathering, but processes controlling riverine δ 7 Li ratios remain controversial. To address the impacts of weathering and hydrology on riverine δ 7 Li, the seasonal variation of water chemistry in the Min Jiang at the eastern Tibetan Plateau was investigated over December of 2009 to the end of 2010. The results showed distinct seasonal variations in ionic chemistry and δ 7 Li. Increased river discharge in the monsoon season diluted dissolved ions, and monsoonal hydrological changes caused frequent δ 7 Li fluctuations. High discharge caused by monsoonal rainfall reduced Li isotope fractionation by shortened rock–fluid interaction time, resulting in lower δ 7 Li, whereas the input of high δ 7 Li groundwater and landslide seepage elevated riverine δ 7 Li, together with lengthened rock–fluid interaction time in less rain intervals. Based on the high-resolution sampling strategy and dataset over one hydrological year, this study highlights that changes of hydrological conditions can have a significant impact on weathering processes and water sources, and therefore on riverine δ 7 Li variation." @default.
- W4224854593 created "2022-04-27" @default.
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- W4224854593 date "2022-04-25" @default.
- W4224854593 modified "2023-10-05" @default.
- W4224854593 title "Seasonal River Chemistry and Lithium Isotopes in the Min Jiang at Eastern Tibetan Plateau: Roles of Silicate Weathering and Hydrology" @default.
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- W4224854593 doi "https://doi.org/10.3389/feart.2022.838867" @default.
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