The Hydrochemistry, Ionic Source, and Chemical Weathering of a Tributary in the Three Gorges Reservoir

Riverine dissolved matter reflects geochemical genesis information, which is vital to understand and manage the water environment in a basin. The Ganjing River located in the hinterland of the Three Gorges Reservoir was systematically investigated to analyze the composition and spatial variation of riverine ions, probe the source and influencing factors, and assess the chemical weathering rates and CO2 consumption. The results showed that the total dissolved solid value (473.31 +/- 154.87 mg/L) with the type of HCO3--Ca2+ was higher than that of the global rivers' average. The hydrochemical parameters were relatively stable in the lower reservoir area of the Ganjing River, which was largely influenced by the backwater of Three Gorges Reservoir. The carbonate weathering source contributed 69.63% of TDS (Total dissolved solids), which generally dominated the hydrochemical characteristics. The contribution rates of atmospheric rainfall were relatively low and stable in the basin, with an average of 4.01 +/- 1.28%. The average contribution rate of anthropogenic activities was 12.05% in the basin and even up to 27.80% in the lower reservoir area of the Ganjing River, which illustrated that the impoundment of Three Gorges Reservoir had brought great challenges to the water environment in the reservoir bay. The empirical power functions were tentatively proposed to eliminate the dilution effect caused by runoff discharge on the basis of previous studies. Accordingly, the rock weathering rate was calculated as 23.54 t/km(2) in the Ganjing River Basin, which consumed atmospheric CO2 with a flux of 6.88 x 10(5) mol/y/km(2). These results highlight the geochemical information of tributaries in the hinterland of the Three Gorges Reservoir, have significant implications for understanding the impact of impoundment, and provide data support for the integrated management of water resources in the Ganjing River Basin.

Automated summary

Riverine dissolved matter provides important geochemical information for understanding and managing water environment. The study on the Ganjing River reveals high levels of dissolved solids, mainly due to carbonate weathering. The contribution of atmospheric rainfall is relatively low, while anthropogenic activities, especially in the reservoir area, have a significant impact. The rates of rock weathering and CO2 consumption highlight the challenges of integrated water resource management in reservoir areas.