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Effect of tidal regime on estuarine residence time spatial variation

机译:潮汐制度对河口停留时间空间变化的影响

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The hydrology and the ecology of shallow estuaries are strongly influenced by the freshwater inflow and the adjacent open sea, due to tide and wind generated water exchange, creating salinity gradients, thermal stratification and assuring large transport of silt, organic material and inorganic nutrients into the estuarine waters. Nutrient enrichment is a key-factor for habitat degradation, leading to sensible structural changes in estuarine ecosystems with the consequent occurrence of episodic algal blooms. In the last two decades, the south arm of the Portuguese river Mondego estuary was stressed by an eutrophication process due to massive nutrient loading from urbanised areas and from intensively agricultural land runoff. The aim of this work is to calculate estuarine water residence time values, which are broadly recognised as important descriptors of estuarine circulation patterns and constitute key-parameters to assess estuarine eutrophication vulnerability. In fact, estuaries with nutrients residence time values, shorter than the algal cells doubling time, will inhibit algae blooms occurrence. The increase of estuarine flushing capacity can be seen as a management measure to mitigate or to invert eutrophication processes. In this work, the MONDEST model, a 2-DH water quality model, was developed and applied to calculate water residence time, at different simulated management scenarios. The results shows the effect of simulated tides on the spatial distribution of estuarine residence time values, which are related with the eutrophication gradients, observed in the Mondego estuary south arm during the last decades. This integrated model constitutes a powerful tool to support authorities' decisions concerning the best water management practices and restoration measures for the environmental sustainable management of this complex ecosystem.
机译:浅河口的水文和生态学受到淡水流入和邻近海洋的强烈影响,由于潮汐和风力产生的水交换,创造盐度梯度,热分层,并确保大型淤泥,有机材料和无机营养素的大型运输河口水域。营养丰富是栖息地降解的关键因素,导致雌卤素生态系统的明智结构变化,随着地下的藻类盛开的发生。在过去的二十年中,由于城市化地区的大规模养分负荷以及集中的农业土地径流,葡萄牙河南部的南部蒙富河河口受到富营养化过程的强调。这项工作的目的是计算河口水停留时间值,这些时间值广泛地被认为是河口循环模式的重要描述符,并构成评估河口富营养化脆弱性的关键参数。事实上,患有营养物的河口停留时间值,比藻类细胞倍增时间倍增,将抑制藻类绽放的发生。河口冲洗能力的增加可以被视为减轻或倒置富营养化过程的管理措施。在这项工作中,在不同的模拟管理场景下,开发和应用了Mondest模型,2 DH水质模型,以计算水停留时间。结果表明,模拟潮汐对在过去几十年中Mondego河口南臂中观察到的河口停留时间值的空间分布的效果。这种综合型号构成了支持当局决策的强大工具,了解该复杂生态系统环境可持续管理的最佳水管理实践和恢复措施。

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