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首页> 外文期刊>The Science of the Total Environment >A modeling study of light extinction due to cohesive sediments in a shallow coastal lagoon under well mixed conditions
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A modeling study of light extinction due to cohesive sediments in a shallow coastal lagoon under well mixed conditions

机译:良好混合条件下浅海沿海泻湖中粘性沉积物引起的光消光的模型研究

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Cohesive sediments play an important ecological role in coastal systems, affecting light penetration in the water column and consequently the local biogeochemical processes. The main aim of this work is to study the water-column light extinction coefficient (k) dependence on cohesive sediment dynamics within Ria de Aveiro lagoon under sea level rise and extreme freshwater discharges events. A coupled estuarine hydrodynamic and transport model is explored, following previous modeling frameworks developed for the Ria de Aveiro. Three scenarios were simulated: a reference scenario (SC1), wherein present hydrodynamic, mean sea level and present freshwater discharges were used to simulate present hydrodynamic and cohesive sediments; a scenario considering local projections of sea level rise of 0.42 m (SC2); and a third one corresponding to maximum freshwater inflow for the lagoon's tributaries (SC3). Results show higher concentrations of cohesive sediments near the rivers mouths, gradually decreasing toward the lagoon's inlet. From SC2 scenario was found that the effect of sea level rise in sediment dynamics and in water-column light extinction coefficient is not significant. However, the tidal prism increase in this case induces a dilution of the sediments concentration from fluvial origin and consequently a slightly k decrease. Contrarily, in SC3 scenario, the extreme freshwater inflow enhances the cohesive sediment concentration in the entire lagoon, limiting the light penetration in the water column. In summary, extreme river discharge events have a highest impact on water-column light penetration in Ria the Aveiro than predicted sea level rise. (C) 2019 Elsevier B.V. All rights reserved.
机译:粘性沉积物在沿海系统中起着重要的生态作用,影响光在水柱中的渗透,从而影响局部生物地球化学过程。这项工作的主要目的是研究在海平面上升和极端淡水排放事件下,Ria de Aveiro泻湖内粘性沉积物动力学的水柱光消光系数(k)。遵循先前为Ria de Aveiro开发的建模框架,探索了河口水动力和运输耦合模型。模拟了三种情景:参考情景(SC1),其中使用当前的水动力,平均海平面和当前的淡水排放量来模拟当前的水动力和粘性沉积物;考虑本地预测的0.42 m海平面上升(SC2)的情景;第三个对应于泻湖支流(SC3)的最大淡水流入量。结果表明,河口附近的粘性沉积物浓度较高,向泻湖入口逐渐减少。从SC2情景中发现,海平面上升对沉积物动力学和水柱光消光系数的影响不显着。然而,在这种情况下,潮汐棱镜的增加引起了河流源性沉积物浓度的稀释,因此k值略有减小。相反,在SC3方案中,极端的淡水流入增加了整个泻湖中粘性沉积物的浓度,从而限制了水在水柱中的渗透。总之,极端河流排放事件对阿威罗河Ria的水柱光穿透的影响最大,超过了预期的海平面上升。 (C)2019 Elsevier B.V.保留所有权利。

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