首页> 外文期刊>Journal of Hydrology >Insights into saline intrusion and freshwater resources in coastal karstic aquifers using a lumped Rainfall-Discharge-Salinity model (the Port-Miou brackish spring, SE France)
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Insights into saline intrusion and freshwater resources in coastal karstic aquifers using a lumped Rainfall-Discharge-Salinity model (the Port-Miou brackish spring, SE France)

机译:使用集总的降雨-排放-盐度模型(法国东南部米奥港咸淡水)对沿海岩溶含水层中的盐分入侵和淡水资源进行洞察

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The aim of this study was to develop a conceptual model of saline intrusion within coastal karst aquifers by analyzing Rainfall-Discharge-Salinity data and to assess freshwater resources using a lumped modeling approach. In a first step, we analyzed 4 years of data (rainfall, discharge and salinity times series) of the Port-Miou brackish submarine spring in South France (400 km(2)). A conceptual model of the aquifer was then designed to differentiate a deep brackish reservoir and a shallower fresh one. Salinity variations at the spring are assumed to be controlled mainly by dilution originating from the fresh water in the shallower reservoir. In a second step, a lumped modeling approach was developed based on the conceptual model to simulate discharge as well as salinity over time. We proposed a reservoir-model to take into account slow and fast components in the shallower part of the aquifer and a saline intrusion in the deeper one. This Rainfall-Discharge-Salinity model was calibrated and validated for two periods of 1.5 years at a daily time step and was also tested to reproduce a multi-annual evolution of the available discharge and salinity time series. Good simulation results were obtained to reproduce water and mass budgets as well as discharge and salinity dynamics during several hydrological cycles. The simultaneous modeling of hydrodynamics and quality data showed the robustness of the model in addition to its easy implementation. Our results led us to propose a new type of seawater mixing mechanism for brackish springs: the dilution type, in addition to the well-known Ventury suction and Head balance types. The application of the lumped model on the Port-Miou brackish spring validated the hydrogeological processes deduced from experimental data, given an initial quantification of the freshwater resources available in such complex brackish karstic aquifers. (C) 2016 Elsevier B.V. All rights reserved.
机译:这项研究的目的是通过分析降雨-流量-盐度数据,并使用集总建模方法评估淡水资源来建立沿海喀斯特含水层中盐分入侵的概念模型。第一步,我们分析了法国南部(400 km(2))的Miou港微咸海底弹簧的4年数据(降雨,流量和盐度时间序列)。然后设计了含水层的概念模型,以区分深咸水库和浅淡淡水库。假定春季的盐度变化主要是由较浅水库中淡水引起的稀释来控制的。第二步,基于概念模型开发了集总建模方法,以模拟随时间变化的排放量和盐度。我们提出了一种储层模型,要考虑到含水层较浅部分的慢速和快速成分,以及较深部分的盐水侵入。该降雨-排放-盐度模型在每天的时间步长上经过了两次校准和验证,为期1.5年,并且还进行了测试,以再现可用排放量和盐度时间序列的多年演变。在几个水文循环中,获得了良好的模拟结果,可以再现水和物质预算以及流量和盐度动态。流体动力学和质量数据的同步建模除了易于实现之外,还显示了该模型的鲁棒性。我们的结果使我们提出了一种用于咸淡水弹簧的新型海水混合机制:稀释方式,以及著名的Ventury吸力式和Head平衡式。集总模型在Port-Miou咸淡水上的应用验证了从实验数据推导出的水文地质过程,并给出了对这种复杂咸淡的岩溶含水层中可用的淡水资源的初步量化。 (C)2016 Elsevier B.V.保留所有权利。

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