Does submarine groundwater discharge contribute to summer hypoxia in the Changjiang (Yangtze) River Estuary?

The Changjiang (Yangtze) River Estuary (CJE) is one of the largest and most intense seasonal hypoxic zones in the world. Here we examine the possibility that submarine groundwater discharge (SGD) may contribute to the summer hypoxia. Spatial distributions of bottom water 222Rn suggest a hotspot disc...

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Published inThe Science of the total environment Vol. 719; p. 137450
Main Authors Guo, Xiaoyi, Xu, Bochao, Burnett, William C., Wei, Qinsheng, Nan, Haiming, Zhao, Shibin, Charette, Matthew A., Lian, Ergang, Chen, Guangquan, Yu, Zhigang
Format Journal Article
LanguageEnglish
Published Netherlands Elsevier B.V 01.06.2020
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Summary:The Changjiang (Yangtze) River Estuary (CJE) is one of the largest and most intense seasonal hypoxic zones in the world. Here we examine the possibility that submarine groundwater discharge (SGD) may contribute to the summer hypoxia. Spatial distributions of bottom water 222Rn suggest a hotspot discharge area in the northern section of the CJE. SGD fluxes were estimated based on a 222Rn mass balance model and were found to range from 0.002 ± 0.004 to 0.022 ± 0.011 m3/m2/day. Higher SGD fluxes were observed during summer hypoxia period. The well-developed overlap of the distribution patterns for SGD flux and dissolved oxygen (DO) implies that SGD could be an important contributor to summer hypoxia in the region off the CJE. We suggest that SGD contributes to the seasonal hypoxia either: (1) directly via discharge of anoxic groundwaters together with reducing substances; and/or (2) indirectly by delivering excess nutrients that stimulate primary productivity with consequent consumption of DO during organic matter decomposition. [Display omitted] •222Rn activities are negatively correlated with bottom water dissolved oxygen within the Changjiang (Yangtze) River Estuary.•The distribution patterns of SGD flux and dissolved oxygen in summer were overlapped.•Submarine groundwater discharge is an important contributor to summer hypoxia in the Changjiang River Estuary.
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ISSN:0048-9697
1879-1026
1879-1026
DOI:10.1016/j.scitotenv.2020.137450