The role of estuarine convergence on the salinity distribution and the estuary response to short river discharge pulses

IF 2.6 3区 地球科学 Q1 MARINE & FRESHWATER BIOLOGY Estuarine Coastal and Shelf Science Pub Date : 2024-07-27 DOI:10.1016/j.ecss.2024.108893
Guillermo Martín-Llanes, Alejandro López-Ruiz
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Abstract

Estuarine behaviour is primarily controlled by the interaction of river discharge and tidal mixing. Transient increases in river discharge, which occur naturally during the wet season or can be managed in regulated basins, alter estuarine dynamics and reduce salt intrusion. Two characteristic times have been identified in the response to these river pulses: the adjustment time (the time required to adapt to the peak discharge) and the recovery time (the time required to return to steady state conditions). Previous work has analysed the effect of peak discharge and pulse duration in the adjustment process, focusing on long discharges (i.e. longer than the intrinsic estuarine timescale) and straight channels. This paper presents an idealised 3-dimensional model (Delft3D) to assess the effect of estuarine convergence on the response to short river pulses in tide dominated, well-mixed estuaries. The similarity between the tidal period, the estuarine timescale and the duration of the pulse led to the introduction of the time between tidal and river conditions as an additional parameter in the analysis. The results show that salt intrusion in convergent estuaries have a lower sensitivity to variations in river discharge compared to the behaviour of prismatic estuaries. Conversely, the influence of convergence on changes in salt intrusion due to the increased river discharge gains relevance in convergent estuaries. Seaward transport of salt is significantly enhanced by freshwater releases that occur between early and mid ebb, especially during spring tides. Increasing convergence reduces the asymmetry of the estuarine response, shortens the recovery time, and shifts the onset of maximum salt displacement and the minimum adjustment time. The results are particularly relevant for water management and salt intrusion control in regulated basins with limited resources, as the volume of fresh water used to reduce salt intrusion can be optimised considering the timing of the pulse release, which depends on the tidal conditions at the estuary.

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河口辐合对盐度分布的作用以及河口对短时间河流排放脉冲的反应
河口行为主要受河流排水量和潮汐混合作用的控制。河流排放量的瞬时增加会在雨季自然出现,也可在有管制的流域中加以管理,从而改变河口的动态,减少盐分入侵。对这些河流脉冲的反应有两个特征时间:调整时间(适应峰值排水量所需的时间)和恢复时间(恢复到稳定状态所需的时间)。以前的工作分析了调整过程中峰值排水量和脉冲持续时间的影响,重点是长排水量(即长于河口固有时间尺度)和直河道。本文提出了一个理想化的三维模型(Delft3D),以评估在潮汐主导、混合良好的河口,河口辐合对短河流脉冲响应的影响。由于潮汐周期、河口时间尺度和脉冲持续时间之间的相似性,在分析中引入了潮汐和河流条件之间的时间作为附加参数。结果表明,与棱柱型河口的行为相比,会聚型河口的盐入侵对河流排水量变化的敏感性较低。相反,在会聚型河口,由于河流排放量增加,会聚对盐分入侵变化的影响变得更加重要。在早潮和中潮之间,尤其是在春潮期间,淡水的释放会显著增强盐分的向海输送。会聚程度的增加降低了河口反应的不对称性,缩短了恢复时间,并改变了最大盐分迁移的开始时间和最小调整时间。这些结果对于资源有限的调节型流域的水资源管理和盐入侵控制尤为重要,因为考虑到脉冲释放的时间取决于河口的潮汐条件,可以优化用于减少盐入侵的淡水量。
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来源期刊
CiteScore
5.60
自引率
7.10%
发文量
374
审稿时长
9 months
期刊介绍: Estuarine, Coastal and Shelf Science is an international multidisciplinary journal devoted to the analysis of saline water phenomena ranging from the outer edge of the continental shelf to the upper limits of the tidal zone. The journal provides a unique forum, unifying the multidisciplinary approaches to the study of the oceanography of estuaries, coastal zones, and continental shelf seas. It features original research papers, review papers and short communications treating such disciplines as zoology, botany, geology, sedimentology, physical oceanography.
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