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Hydrological dynamics of water sources in a Mediterranean lagoon

机译:地中海泻湖中水源的水文动力学

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Lagoons are important ecosystems occupying large coastal areas worldwide. Lagoons contain various mixtures of marine and freshwater sources which are highly dynamic in time. However, it often remains a challenge to identify and quantify dynamic changes of water sources, particularly in heterogeneous lagoon systems like the K?ycegiz–Dalyan lagoon (KDL), which is located at the south-west of Turkey on the Mediterranean Sea coast. The objective of this study was to quantify different contributions of potential water sources i.e. surface water, groundwater and seawater in the lagoon and how these water sources changed over time and space. In the wet- and dry-season stable isotopes of water, chloride concentration (Clsup-/sup) and salinity were measured in two depths in the lagoon and surrounding water bodies (sea, lake, groundwater). Different components of water sources were quantified with a three component endmember mixing analysis. Differences in Clsup-/sup and stable isotopes over time indicated the dynamic behaviour of the system. Generally, none of the groundwater samples was impacted by water of the Mediterranean Sea. During the wet season, most of the lagoon water ( 95%) was influenced by freshwater and vertically well mixed. During the dry season, high Clsup-/sup in the deeper sampling locations indicated a high contribution of marine water throughout the entire lagoon system due to saltwater intrusion. However, a distinct layering in the lagoon was obvious from low Clsup-/sup and depleted isotope contents close to the surface supporting freshwater inflow into the system even during the dry season. Besides temporal dynamics also spatial heterogeneities were identified. Changes in water sources were most evident in the main lagoon channel compared to more isolate lagoon lakes, which were influenced by marine water even in the wet season, and compared to side branches indicating slower turnover times. We found that environmental tracers helped to quantify highly dynamic and heterogeneous contributions of different water sources in the K?ycegiz–Dalyan lagoon.
机译:泻湖是重要的生态系统,遍布世界各地的沿海地区。泻湖包含海洋和淡水源的各种混合物,它们在时间上是高度动态的。但是,识别和量化水资源的动态变化通常仍然是一个挑战,特别是在异质泻湖系统中,例如位于土耳其西南部地中海沿岸的Kyygegiz-Dalyan泻湖(KDL)。这项研究的目的是量化潜在水源(即泻湖中的地表水,地下水和海水)的不同贡献,以及这些水如何随时间和空间变化。在湿季和干季的稳定同位素水中,分别在泻湖和周围水体(海洋,湖泊,地下水)的两个深度处测量了氯化物浓度(Cl -)和盐度。用三组分末端成员混合分析对水的不同组分进行定量。 Cl -和稳定同位素随时间的差异表明了系统的动态行为。通常,没有任何地下水样品受到地中海水的影响。在雨季,大多数泻湖水(> 95%)受到淡水的影响,并垂直混合均匀。在干旱季节,较深采样点的高Cl -表示由于盐水的入侵,整个泻湖系统中海水的贡献很大。然而,由于低Cl -和靠近地表的耗尽的同位素含量,即使在干旱季节,泻湖中仍存在明显的分层,从而支持淡水流入系统。除了时间动态,还发现了空间异质性。与更多的孤立泻湖湖泊相比,在主要的泻湖河道中水源的变化最为明显,后者甚至在雨季也受到海水的影响,而与侧枝相比则表明周转时间较慢。我们发现,环境示踪剂有助于量化Kyycegiz-Dalyan泻湖中不同水源的高度动态和非均质的贡献。

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