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Estimating the thickness of unconsolidated coastal aquifers along the global coastline

机译:估算全球海岸线上未合并的沿海含水层的厚度

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Knowledge of aquifer thickness is crucial for setting up numerical groundwater flow models to support groundwater resource management and control. Fresh groundwater reserves in coastal aquifers are particularly under threat of salinization and depletion as a result of climate change, sea-level rise, and excessive groundwater withdrawal under urbanization. To correctly assess the possible impacts of these pressures we need better information about subsurface conditions in coastal zones. Here, we propose a method that combines available global datasets to estimate, along the global coastline, the aquifer thickness in areas formed by unconsolidated sediments. To validate our final estimation results, we collected both borehole and literature data. Additionally, we performed a numerical modelling study to evaluate the effects of varying aquifer thickness and geological complexity on simulated saltwater intrusion. The results show that our aquifer thickness estimates can indeed be used for regional-scale groundwater flow modelling but that for local assessments additional geological information should be included.
机译:含水层厚度的知识对于建立数值地下水流模型以支持地下水资源管理和控制至关重要。气候变化,海平面上升以及城市化过程中过多的地下水抽取导致沿海含水层中的新鲜地下水储量特别受到盐碱化和枯竭的威胁。为了正确评估这些压力的可能影响,我们需要有关沿海地区地下条件的更好信息。在这里,我们提出了一种方法,该方法结合了可用的全球数据集,以沿着全球海岸线估算由未固结沉积物形成的区域中的含水层厚度。为了验证我们的最终估算结果,我们收集了钻孔和文献数据。此外,我们进行了数值模拟研究,以评估不同含水层厚度和地质复杂性对模拟盐水入侵的影响。结果表明,我们的含水层厚度估计的确可以用于区域规模的地下水流模拟,但是对于局部评估,应该包括其他地质信息。

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