Institute of Oceanology, Polish Academy of Sciences, ul. Powstancow Warszawy 55, 81712 Sopot, Poland.
Sci Total Environ. 2012 Nov 1;438:86-93. doi: 10.1016/j.scitotenv.2012.08.058. Epub 2012 Sep 11.
Submarine groundwater discharge (SGD) has been recognized as an important exchange pathway between hydrologic reservoirs due to its impact on biogeochemical cycles of the coastal ocean. This study reports nutrient concentrations and loads delivered by SGD into the Bay of Puck, the southern Baltic Sea. Measurements were carried out between September, 2009 and October, 2010 at groundwater seepage sites identified by low salinity of pore water. Groundwater fluxes, measured using seepage meters, ranged from 3 to 22 L m(-2)day(-1). Average concentrations of nutrients in groundwater samples collected were as follows: 0.4 μmol L(-1) nitrate (NO(3)), 0.8 μmol L(-1) nitrite (NO(2)), 18.2 μmol L(-1) ammonium (NH(4)) and 60.6 μmol L(-1) orthophosphate (PO(4)). Levels of NH(4) and PO(4) were significantly higher in samples from SGD sites than in seawater. Seawater and SGD samples showed similar NO(2) concentrations but SGD samples exhibited lower NO(3) levels than those observed in seawater samples. Measured seepage water fluxes and nutrient concentrations were used to calculate nutrient loads discharged into the study area while the literature groundwater flux and the measured nutrient concentrations were used to estimate nutrient loads discharged into the Bay of Puck. The estimates suggest that SGD delivers a dissolved inorganic nitrogen (DIN) load of 49.9 ± 18.0 t yr(-1) and a PO(4)(-) load of 56.3 ± 5.5tyr(-1) into the Bay of Puck. The projected estimates are significant in comparison with loads delivered to the bay from other, well-recognized sources (705 ty r(-1) and 105 ty r(-1) respectively for DIN and PO(4)). Nutrient discharge input loads were projected to the entire Baltic Sea The extrapolated values indicate SGD contributes a significant proportion of phosphate load but only an insignificant proportion of DIN load. Further studies are necessary to better understand SGD contributions to the nutrient budget in the Baltic Sea.
海底地下水排泄(SGD)已被认为是水文储层之间重要的交换途径,因为它对沿海水体的生物地球化学循环有影响。本研究报告了通过 SGD 输送到波罗的海南部的 Puck 湾的营养物浓度和负荷。测量工作于 2009 年 9 月至 2010 年 10 月期间在通过孔隙水低盐度识别的地下水渗出点进行。使用渗漏计测量的地下水通量范围为 3 至 22 L m(-2)day(-1)。从采集的地下水样本中测得的营养物平均浓度如下:硝酸盐(NO(3))为 0.4 μmol L(-1)、亚硝酸盐(NO(2))为 0.8 μmol L(-1)、铵(NH(4))为 18.2 μmol L(-1)和正磷酸盐(PO(4))为 60.6 μmol L(-1)。与海水相比,来自 SGD 点的 NH(4)和 PO(4)样本的浓度明显更高。海水和 SGD 样本的 NO(2)浓度相似,但 SGD 样本的 NO(3)水平低于海水样本。测量的渗漏水通量和营养物浓度用于计算排入研究区的营养物负荷,而文献中的地下水通量和测量的营养物浓度则用于估算排入 Puck 湾的营养物负荷。估计表明,SGD 向 Puck 湾输送的溶解无机氮(DIN)负荷为 49.9 ± 18.0 t yr(-1)和正磷酸盐(PO(4))负荷为 56.3 ± 5.5tyr(-1)。与从其他公认来源输送到海湾的负荷(DIN 分别为 705 ty r(-1)和 PO(4)分别为 105 ty r(-1))相比,这些预测估计是显著的。将营养物排放输入负荷预测到整个波罗的海。推断值表明,SGD 贡献了相当大比例的磷酸盐负荷,但仅贡献了微不足道的 DIN 负荷。需要进一步的研究来更好地了解 SGD 对波罗的海营养物预算的贡献。