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

机译:大量开发的地中海含水层:对海水入侵的抵御能力和接近临界阈值的能力

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摘要

We investigate seawater intrusion in three promi- nent Mediterranean aquifers that are subject to intensive ex-ploitation and modi?ed hydrologic regimes by human ac-tivities: 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 iden-tify 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 lo-cations of groundwater pumping, and a tipping point of com-plete seawater intrusion up to the prevailing groundwater di-vide of a coastal aquifer. Either limit can be reached, and ul-timately crossed, under intensive aquifer exploitation and/or climate-driven change. We show that seawater intrusion vul-nerability for different aquifer cases can be directly com-pared in terms of normalized intrusion performance curves. The site-speci?c assessments show that (a) the intruding sea-water currently seriously threatens the Nile Delta aquifer, (b) in the Israel Coastal aquifer the sharp interface toe ap-proaches 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引起的三大主要地中海含水层的海水入侵,这些含水层受到密集的勘探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的阿克罗蒂里含水层。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/或气候压力下海水入侵的两个不同的临界极限:井的极限,即入侵的海水到达地下水泵送的关键位置的极限;以及完全的海水入侵的临界点到沿海含水层的主要地下水分配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,并最终跨越。我们表明,根据归一化的入侵性能曲线,可以直接比较不同含水层情况下的海水入侵脆弱性。现场评估表明,(a)入侵的海水目前严重威胁着尼罗河三角洲含水层,(b)以色列沿海含水层中尖锐的脚趾靠近井位,以及(c)塞浦路斯Akrotiri目前,含水层受到海水入侵的威胁有所减轻。

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