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• W2110872437 endingPage "595" @default.
• W2110872437 startingPage "587" @default.
• W2110872437 abstract "The chemical composition of lake water and inflowing river water was investigated in Nam Co (lake), Tibetan Plateau, in September 2005. Lake water samples (n = 76) were collected at different depths along a south–north transect of the eastern part of the lake while water samples were collected from 69 rivers flowing into the lake; a sediment core was collected at 64 m midway along the water survey transect to investigate salt precipitation. Na+ and Ca2+ were the dominant cations, accounting for 76.2% and 60.6% of the lake and river water cations, respectively while HCO3− was the dominant anion accounting for 70.8% and 93.4% of lake and river anions, respectively. CaCO3 precipitation from the water column decreased Ca2+ in the lake water, with the relative proportion of other ions increasing significantly. Evaporation–crystallization processes largely control Nam Co lake-water chemistry, while rock weathering is the dominant processes influencing the chemistry of river water; carbonate and silicate weathering are the major sources of ions in these rivers." @default.
• W2110872437 created "2016-06-24" @default.
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• W2110872437 date "2010-12-01" @default.
• W2110872437 modified "2023-10-02" @default.
• W2110872437 title "Comparisons between the chemical compositions of lake water, inflowing river water, and lake sediment in Nam Co, central Tibetan Plateau, China and their controlling mechanisms" @default.
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• W2110872437 doi "https://doi.org/10.1016/j.jglr.2010.06.013" @default.
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