Department of Earth and Space Sciences, West Chester University of Pennsylvania, West Chester, PA, USA.
Department of Ocean Environmental Sciences, Chungnam National University, Daejeon, Republic of Korea.
Chemosphere. 2017 Aug;181:390-399. doi: 10.1016/j.chemosphere.2017.04.085. Epub 2017 Apr 22.
In order to evaluate water quality and biological productivity, observation data sets were collected and analyzed in Yeongsan River Estuary, Korea. We also set up a numerical model to resolve hydrodynamics and fate of water quality variables in the system. Results show that most of nutrients loading are trapped in the lake and higher concentrations of nutrients and organic matters (OM) are present only inside of the artificial sea dike. There exist episodial discharges at the dam, which coincide mostly with rainfall events during summer monsoon periods. During this discharge event, lower salinity and higher suspended solids, nutrients, and OM are observed in surface layer of the estuarine section. Hydrodynamic model results show that circulation in the estuarine section is governed by freshwater discharge from the lake, resulting in an enhanced two-layer estuarine circulation being dominated, during and after the freshwater is discharged. Such two-layer estuarine circulation combined with higher concentration of nutrients in the surface layer results in that outfluxes of nutrients in the surface layer dominate over the influxes in the bottom layer during summer high precipitation periods. Meanwhile, numerical dye experiment results show that the discharged water with elevated nutrients levels have a short residence time (∼5-10 days) in the estuarine section. Due to this fast flushing rate, excessive nutrient loadings are not used to produce biological matters in the estuarine section. This limited biological productivity, characterized by seaward side of the artificial sea dike, makes Yeongsan estuarine system excluded from acting as an active carbon sink.
为了评估水质和生物生产力,我们在韩国的延山河口收集和分析了观测数据集,并建立了一个数值模型来解决该系统中水力学和水质变量的命运。结果表明,大部分养分负荷都被困在湖中,只有在人工海堤内部才能检测到更高浓度的养分和有机物(OM)。大坝存在间歇性排放,主要与夏季季风期间的降雨事件同时发生。在这种排放事件中,在河口部分的表层观察到较低的盐度和较高的悬浮物、养分和 OM。水动力模型结果表明,河口部分的循环受湖水排放的影响,导致在淡水排放期间和之后,增强的两层河口循环占主导地位。这种两层河口循环加上表层较高的养分浓度,导致在夏季高降水期,表层的养分流出量超过底层的流入量。同时,数值示踪剂实验结果表明,含有高浓度养分的排放水在河口段的停留时间较短(约 5-10 天)。由于这种快速冲洗率,河口段没有利用过量的养分负荷来产生生物物质。这种有限的生物生产力,以人工海堤的向海一侧为特征,使得延山河口系统无法充当活跃的碳汇。