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Monitoring and simulation of salinity changes in response to tide and storm surges in a sandy coastal aquifer system

机译:监测和模拟沙质沿海含水层系统中响应潮汐和风暴潮的盐度变化

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Tidal dynamics and especially storm surges can have an extensive impact on coastal fresh groundwater resources. Combined with the prospect of sea-level rise and the reliance of many people on these resources, this demonstrates the need to assess the vulnerability of coastal areas to these threats. In this study, we investigated the impact of tides and storm surges on coastal groundwater at a pilot location on the Dutch coast (viz., the Sand Engine). To monitor changes in groundwater salinity under a variety of conditions, we performed automated measurements with electrical resistivity tomography for a period of 2 months between November 2014 and January 2015. The obtained resistivity images were converted to salinity images, and these images served effectively as observations of the impact of tidal fluctuations, saltwater overwash during storm surges, and the recovery of the freshwater lens after land-surface inundations. Most of the observed changes in groundwater head and salinity could be reproduced with a two-dimensional variable-density groundwater flow and salt transport model. This shows that groundwater models can be used to make accurate predictions of the impact of tides and storm surges on fresh groundwater resources, given a thorough understanding of the (local) system. Comparisons of measurements and model simulations also showed that morphological changes and wave run-up can have a strong impact on the extent of land-surface inundations in (low-elevation) dynamic coastal environments, and can therefore substantially affect coastal fresh groundwater resources.
机译:潮汐动力,尤其是风暴潮可能对沿海淡水资源产生广泛影响。结合海平面上升的前景以及许多人对这些资源的依赖,这表明需要评估沿海地区对这些威胁的脆弱性。在这项研究中,我们调查了潮汐和风暴潮对荷兰沿岸试点(即,Sand Engine)沿海地下水的影响。为了监控各种条件下的地下水盐度变化,我们在2014年11月至2015年1月的2个月内使用电阻率层析成像进行了自动测量。将获得的电阻率图像转换为盐度图像,这些图像可有效地用作观察结果潮汐波动的影响,风暴潮期间盐水的过度冲洗以及地表淹没后淡水镜的恢复。观察到的大多数地下水位和盐度变化可以用二维可变密度地下水流和盐分运移模型重现。这表明,在充分了解(本地)系统的前提下,可以使用地下水模型来准确预测潮汐和风暴潮对新鲜地下水资源的影响。测量结果和模型模拟的比较还表明,形态变化和波浪上升对(低海拔)动态沿海环境中的地表淹没程度有很大的影响,因此可以极大地影响沿海淡水资源。

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