Abstract
The “Water-Sediment Regulation Scheme” (WSRS) is critically important to the hydrologic evaluation of the Yellow River estuary since a huge pulse of water and sediment are delivered into the sea during a short period. We used the natural geochemical tracers radium (223Ra, 224Ra, 226Ra) and radon (222Rn) isotopes as well as other hydrological parameters to investigate the mixing variations and submarine groundwater discharge (SGD) in the Yellow River estuary under the influence of the 2013 WSRS. Dramatically elevated radium and radon isotopic activities were observed during this WSRS compared with activities measured during a non-WSRS period. Radium “water ages” indicated that the offshore transport rate nearly tripled when the river discharge increased from 400 to 3400 m3/s. We calculated the SGD flux in the Yellow River estuary based on a radium mass balance model as well as radium and radon time-series models. The SGD flux was estimated at 0.02~0.20 m/day during a non-WSRS period and 0.67~1.22 m/day during the 2013 WSRS period. The results also indicate that large river discharge tends to lead more intense SGD along the river channel direction with a large amount of fresh SGD.
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Acknowledgments
This study was funded by the National Natural Science Foundation of China (NSFC grant 41206064, 41376085, and 41221004) and the Ministry of Land and Resources of the People’s Republic of China (GZH201200505) and the Fundamental Research Funds for the Central Universities (No. 201262014, 201213030). We would like to thank Liu Jixin, Liu Jun, Liu Sen, and Zhang Tingting for assistance during sample collection. We also acknowledge Professor Wang Houjie and Zhang Longjun for sharing the cruises and Professor William C. Burnett and Willard S. Moore for helpful comments. This is MCTL Contribution No.73.
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Xia, D., Yu, Z., Xu, B. et al. Variations of Hydrodynamics and Submarine Groundwater Discharge in the Yellow River Estuary Under the Influence of the Water-Sediment Regulation Scheme. Estuaries and Coasts 39, 333–343 (2016). https://doi.org/10.1007/s12237-015-9994-7
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DOI: https://doi.org/10.1007/s12237-015-9994-7