Combining hydrological investigations and radium isotopes to understand the environmental effect of groundwater discharge to a typical urbanized estuary in China

被引:17
|
作者
Xiao, Kai [1 ]
Li, Gang [2 ,3 ]
Li, Hailong [1 ]
Zhang, Yan [4 ]
Wang, Xuejing [1 ]
Hu, Wenli [1 ]
Zhang, Chengcheng [5 ]
机构
[1] Southern Univ Sci & Technol, State Environm Protect Key Lab Integrated Surface, Sch Environm Sci & Engn, Shenzhen 518055, Peoples R China
[2] China Inst Geoenvironm Monitoring, Beijing 100081, Peoples R China
[3] Hebei Key Lab Geol Resources & Environm Monitorin, Shijiazhuang 050021, Hebei, Peoples R China
[4] China Univ Geosci, Sch Water Resources & Environm Sci, Beijing 100083, Peoples R China
[5] Northwest Inst Nucl Technol, Xian 710024, Shaanxi, Peoples R China
基金
中国国家自然科学基金; 中国博士后科学基金;
关键词
Radium isotopes; Water pollution; Water residence time; Estuary; Eutrophication; SUBTROPICAL MANGROVE SWAMP; JIULONG RIVER ESTUARY; DAYA BAY; POREWATER EXCHANGE; NUTRIENT FLUXES; WATER EXCHANGE; COASTAL WATER; TOLO HARBOR; SUBMARINE; TRANSPORT;
D O I
10.1016/j.scitotenv.2019.133872
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Pollution of urbanized rivers with excess nutrients due to groundwater discharge is an increasing environmental concern worldwide. Dan'ao river, a typical urbanized river in the Guangdong-Hong Kong-Macao Greater Bay Area, is experiencing heavy water pollution. However, the groundwater-derived nutrient loads had not yet been thoroughly quantified. In order to quantify the contribution of groundwater-derived nutrient inputs, we combined the methods of hydrological investigations and radium isotopes. Groundwater and river water samples were collected from the river upstream to the estuary for the analyses of radium quartets and nutrients including DIN, DIP and DSi. The results showed that the radium activities in both surface water and groundwater decreased from the estuary to the upstream. The groundwater discharge rate was estimated by the radium mass balance model using short-lived radium isotopes (Ra-223 and Ra-224). The estimated groundwater discharge rate ranged from 1.99 x 10(5) to 6.67 x 10(5) m(3) d(-1), comparable to the upstream river discharge rate of 4.23 x 10(5) m(3) d(-1). The groundwater-derived nutrient fluxes were 165.66-554.98 mmol m(-2) d(-1) for DIN, 2.47-8.26 mmol m(-2) d(-1) for DIP and 63.73-213.49 mmol m(-2) d(-1) for DSi, respectively. They contributed 19% similar to 44% DIN, 16%similar to 39% DIP, and 31%similar to 60% DSi of all the nutrient inputs into the Dan'ao River, respectively. In addition, the nutrient inputs by groundwater discharge has an average DIN:DIP ratio of as high as 190, which is able to potentially affect the riverine and marine nutrient structures. These findings may provide useful information for designing control strategies for reducing massive nutrient inputs to Dan'ao River in the future. (c) 2019 Elsevier B.V. All rights reserved.
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页数:15
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