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首页> 外文期刊>Korean Journal of Fisheries and Aquatic Sciences >Temporal and Spatial Variation of Nutrient Concentrations in Shallow Pore Water in Intertidal Sandflats of Jeju Island
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Temporal and Spatial Variation of Nutrient Concentrations in Shallow Pore Water in Intertidal Sandflats of Jeju Island

机译:济州岛潮间带滩涂浅孔水中营养物浓度的时空变化

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摘要

To examine temporal and spatial variation in salinity and nutrients in the shallow pore water of intertidal sandflats, we measured salinity and nutrient concentrations (dissolved inorganic nitrogen [DIN], phosphorus [DIP], and silicate [DSi]) in porewater of the intertidal zone along the coastline of Jeju Island at two and/or three month intervals from May 2009 to December 2010. Geochemical parameters (grain size, ignition loss [IL], chemical oxygen demand [COD], and acid volatile sulfur [AVS]) in sediment were also investigated. The surface sediments in intertidal sandflats of Jeju Island were mainly composed of sand, slightly gravelly sand and gravelly sand, with a range of mean grain size from 0.5 to 2.5 0. Concentrations of IL and COD in sediment were higher along the eastern coast, as compared to the western coast, due to differences in biogenic sediment composition. Salinity and nutrient concentrations in pore water were markedly different across time and space during rainy seasons, whereasconcentrations were temporally and spatially more stable during dry seasons. These results suggest that salinity and nutrient concentrations in pore water depend on the advective flow of fresh groundwater. We also observed an imbalance of the DIN/DIP ratio in pore water due to the influenee of contaminated sources of DIN. In particular, nutrient concentrations during rainy and dry seasons were characterized by high DIN/DIP ratios (mean-127) and low DIN/DIP ratios (mean-10), respectively, relative to theRedfield ratio (16) in offshore seawater. Such an imbalance of DIN/DIP ratios in pore water can affect the coastal ecosystem and appears to cause outbreaks of benthic seaweed along the coastline of Jeju Island.
机译:为了检查潮间带滩涂浅层盐度中盐分和养分的时空变化,我们测量了潮间带砂层中盐分和养分的浓度(溶解的无机氮[DIN],磷[DIP]和硅酸盐[DSi])于2009年5月至2010年12月,每隔两个月和/或三个月沿着济州岛海岸线航行一次。还进行了调查。济州岛潮间带滩涂的表层沉积物主要由砂,微砾砂和砾砂组成,平均粒径范围为0.5至2.50。东海岸的沉积物中IL和COD的浓度较高,如与西部海岸相比,由于生物沉积物成分的差异。在雨季,孔隙水中的盐分和养分浓度在时间和空间上显着不同,而在旱季,盐分和盐分在时间和空间上更稳定。这些结果表明,孔隙水中的盐度和养分浓度取决于新鲜地下水的对流。我们还观察到由于受到污染的DIN源的影响,孔隙水中的DIN / DIP比不平衡。尤其是雨季和旱季的营养物浓度分别以相对于近海红场比率(16)的高DIN / DIP比(平均值127)和低DIN / DIP比(平均值10)为特征。孔隙水中DIN / DIP比例的这种不平衡会影响沿海生态系统,并可能导致济州岛沿岸的底栖海藻爆发。

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