Submarine groundwater discharge as an important nutrient source influencing nutrient structure in coastal water of Daya Bay, China

摘要

As an important nutrient source for coastal waters, submarine groundwater discharge (SGD) has long been largely ignored in Daya Bay, China. In this study, we estimate the fluxes of SGD and associated nutrients into this region using a 224 Ra mass balance model and assess the contribution/importance of nutrients by SGD, benthic sediments, local rivers, and atmospheric deposition. The results of 224 Ra mass balance show that the estimated SGD ranges from (2.76 +/- 1.43) x 10(6) m(3)/d to (1.03 +/- 0.53) x 10(7) m(3)/d with an average of (6.32 +/- 2.42) x 10(6) m(3) /d, about 16 times the total discharge rate of local rivers. The nutrient loading from SGD is estimated to be (1.05-1.99) x 10(5) mol/d for NO3-N, (4.04-12.16) x 10(3) mol/d for DIP, and (3.54-11.35) x 10(5) mol/d for Si. Among these considered nutrient sources, we find that SGD is the primary source for Si and NO3-N, contributing 68% and 42% of all considered sources, respectively. The atmospheric NO3-N flux is comparable to that from SGD. The local rivers are the most important source for DIP, contributing 75% of all considered sources. SGD with high N:P ratio (NO3-N/DIP) of 37.0 delivers not only a large quantity of nutrients, but also changes nutrient structure in coastal water. Based on a DIP budget, primary productivity is evaluated to be 54-73 mg C/m(2) d, in which SGD accounts for approximately 30% of total production. This study indicates that SGD is a key source of nutrients to coastal waters and may cause an obvious change of primary production and nutrient structure in Daya Bay. (C) 2018 Elsevier Ltd. All rights reserved.