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Intensively exploited Mediterranean aquifers : resilience to seawater intrusion and proximity to critical thresholds

机译:密集开发的地中海含水层:对海水入侵的抵御能力和接近临界含水层的能力

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摘要

We investigate seawater intrusion in three prominent Mediterranean aquifers that are subject to intensive exploitation and modified hydrologic regimes by human activities: the Nile Delta, Israel Coastal and Cyprus Akrotiri aquifers. Using a generalized analytical sharp interface model, we review the salinization history and current status of these aquifers, and quantify their resilience/vulnerability to current and future seawater intrusion forcings. We identify two different critical limits of seawater intrusion under groundwater exploitation and/or climatic stress: a limit of well intrusion, at which intruded seawater reaches key locations of groundwater pumping, and a tipping point of complete seawater intrusion upto the prevailing groundwater divide of a coastal aquifer. Either limit can be reached, and ultimately crossed, under intensive aquifer exploitation and/or climate-driven change. We show that seawater intrusion vulnerability for different aquifer cases can be directly compared in terms of normalized intrusion performance curves. The site-specific assessments show that: a) the intruding seawater currently seriously threatens the Nile Delta Aquifer, b) in the Israel Coastal Aquifer the sharp interface toe approaches the well location and c) the Cyprus Akrotiri Aquifer is currently somewhat less threatened by increased seawater intrusion.
机译:我们调查了人类活动对三大著名地中海含水层的海水入侵情况,这些含水层受到人类的密集开发和改良的水文制度的影响:尼罗河三角洲,以色列沿海和塞浦路斯阿克罗蒂里含水层。使用广义分析尖锐界面模型,我们回顾了这些含水层的盐化历史和现状,并量化了它们对当前和未来海水入侵强迫的适应力/脆弱性。我们确定了在地下水开采和/或气候应力作用下海水入侵的两个不同的临界极限:井的入侵极限,即入侵的海水到达地下水抽水的关键位置时的极限;以及完全的海水入侵的临界点,直至一个主要的地下水分界点。沿海含水层。在密集的含水层开发和/或气候驱动的变化下,可以达到任何一个极限,甚至最终超过极限。我们表明,可以根据归一化的入侵性能曲线直接比较不同含水层情况下的海水入侵脆弱性。特定地点的评估显示:a)入侵海水目前严重威胁尼罗河三角洲含水层,b)以色列沿海含水层中的锋利界面脚趾接近井位,c)塞浦路斯Akrotiri含水层目前受到的威胁有所减轻海水入侵。

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