4.6 Article

Phosphorus release flux and mechanism at the sediment-water interface of the Three Gorges Reservoir in the Yangtze River basin, China

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JOURNAL OF SOILS AND SEDIMENTS
卷 -, 期 -, 页码 -

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SPRINGER HEIDELBERG
DOI: 10.1007/s11368-023-03591-y

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Phosphorus; Sediment-water interface; Chemical sequential extraction; Diffusive gradients in thin films (DGT); Three Gorges Reservoir

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This study evaluated the contribution of sediment internal phosphorus (P) and revealed the mechanisms controlling sediment P release in the Three Gorges Reservoir (TGR). The results indicated that sediment P release may trigger harmful algal blooms in the overlying water. These findings provide important scientific and technical support for mitigating internal P pollution in large deep-water reservoirs.
PurposeThe Three Gorges Reservoir (TGR) is the largest water conservation project in the world but suffers from harmful algal blooms (HABs) currently. A large amount of phosphorus (P) has accumulated in the sediment due to the construction of the Three Gorges Dam. Phosphorus release from sediment may provide an important P source for overlying water that further triggers HABs. This study aimed to evaluate the contribution of sediment internal P and reveal the mechanisms controlling sediment P release.Material and methodsChemical sequential extraction approach and diffusive gradients in thin films (DGT) techniques were employed to determine the P fractions in sediments and the vertical distribution of P, iron (Fe), and sulfur (S) at the sediment-water interface (SWI).Results and discussionResults indicated that the total P content in the sediments of the TGR is high, with a mean content of 1368 mg kg(-1). The P concentration of different fractions in sediments followed the order HCl-P > NaOH-P > BD-P. The averaged P release flux at the SWI was estimated at 0.42 mg m(-2) day(-1), suggesting that sediment P release is a potential P source for the overlying water. Significant positive relationships between DGT-P and DGT-Fe concentrations from sampling sites Wushan County (WS), Zigui County (ZG), and Xiangxi River (XX) were observed with correlation coefficients (R-2) of 0.91, 0.39, and 0.29, respectively. Furthermore, DGT-P and DGT-S concentrations were also significantly positively correlated at the sampling sites WS, ZG, and XX, with R-2 of 0.71, 0.87, and 0.50, respectively.ConclusionThe internal P load is severe in the TGR. The reductive dissolution of Fe-P is likely one of the main mechanisms causing P release in the sediments. Furthermore, sulfate reduction associated coprecipitation with Fe promotes the release of Fe-P. These results provide important scientific and technical support for the mitigation of internal P pollution in large deep-water reservoirs.

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