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Status of the Korba groundwater resources (Tunisia): observations and three-dimensional modelling of seawater intrusion

机译:Korba地下水资源的状况(突尼斯):海水入侵的观测和三维建模

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摘要

The Korba aquifer is located in the east of the Cape Bon peninsula in Tunisia. A large groundwater depression has been created in the central part of the aquifer since the 1980s, due to intense groundwater pumping for irrigation. The data collected show that the situation continues to deteriorate. Consequently, seawater is continuing to invade a large part of the aquifer. To better understand the situation and try to forecast its evolution, a three-dimensional (3D) transient density-dependent groundwater model has been developed. The model building process was difficult because of data required on groundwater discharge from thousands of unmonitored private wells. To circumvent that difficulty, indirect exhaustive information including remote sensing data and the physical parameters of the aquifer have been used in a multi-linear regression framework. The resulting 3D model shows that the aquifer is over-exploited. It also shows that after 50 years of exploitation, the time needed to turn back to the natural situation would be about 150 years if the authorities would ban all exploitation now. Such an asymmetry in the time scales required to contaminate or remediate an aquifer is an important characteristic of coastal aquifers that must be taken into account in their management.
机译:Korba含水层位于突尼斯Cape Bon半岛的东部。自1980年代以来,由于大力抽水灌溉地下水,在含水层的中部形成了一个大的地下水低压区。收集的数据表明,局势继续恶化。因此,海水继续侵入大部分含水层。为了更好地了解情况并尝试预测其演变,已开发了三维(3D)瞬态密度相关的地下水模型。由于需要成千上万个未经监控的私人井的地下水排放数据,因此模型构建过程非常困难。为了避免这一困难,在多线性回归框架中使用了包括遥感数据和含水层物理参数在内的间接详尽信息。生成的3D模型表明含水层被过度开采。它还表明,经过50年的剥削,如果当局现在禁止一切剥削,恢复自然状态所需的时间将约为150年。污染或补救含水层所需的时间尺度上的这种不对称性是沿海含水层在管理中必须考虑的重要特征。

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