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Investigation of transient freshwater storage in island aquifers

机译:岛屿含水层中暂态淡水存储的调查

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Fresh groundwater in an island aquifer is an extremely important resource that is highly vulnerable to variations in natural weather cycles and climate change effects. On small islands, precipitation creates subsurface freshwater lenses that float on top of coalesced saltwater that has intruded from the surrounding seawater. The volume and shape of these highly vulnerable freshwater lenses depend on the size and shape of the island, underlying geology, and the rate and duration of groundwater recharge. This study focuses on the transient changes in freshwater storage volume within these lenses. We completed a sand tank experiment to visualize an evolving freshwater lens that undergoes a dry- and -wet recharge cycle resulting in forming a shrinking and an expanding lens. The physical experiments provided a dataset to develop a robust numerical model that can rigorously simulate different types of evolving transient freshwater lenses. Our laboratory data along with past literature information have indicated that the shrinking of a freshwater lens occurred at a slower rate relative to an expanding freshwater lens. This aspect of a rather rapid freshwater volume recovery was investigated further using the numerical model by imposing cyclic recharge patterns to study the impacts of shortened recharge periods on freshwater storage in island aquifers. The results show that a sustainable dynamic equilibrium condition can be achieved within a few cycles of periodic recharge. Unsustainable conditions were only encountered at extremely short recharge periods. The model was then extended to simulate a freshwater lens in Dauphin Island, Alabama, to assess changes in freshwater storage under realistic wet and dry recharge cycles. The experimental data together with the modeling results presented in this study provide a better understanding of transient changes in freshwater storage patterns in small islands.
机译:岛屿含水层中的淡水是极为重要的资源,极易受到自然天气周期变化和气候变化影响的影响。在小岛上,降水会产生地下淡水晶状体,这些晶状体漂浮在从周围海水侵入的聚结咸水上方。这些高度脆弱的淡水晶状体的体积和形状取决于岛屿的大小和形状,基础地质状况以及地下水补给的速率和持续时间。这项研究的重点是这些镜片中淡水存储量的瞬时变化。我们完成了一个沙缸实验,以可视化不断演变的淡水晶状体,该晶状体经历了干湿循环,从而形成了收缩和膨胀的晶状体。物理实验提供了一个数据集,用于开发一个鲁棒的数值模型,该模型可以严格模拟不同类型的瞬态淡水透镜的演变。我们的实验室数据以及过去的文献信息表明,相对于膨胀的淡水晶状体,淡水晶状体的收缩发生的速度较慢。通过使用数值补给模式,通过施加循环补给模式以研究补给时间缩短对岛屿含水层中淡水存储的影响,进一步研究了相当快速的淡水量恢复方面。结果表明,可持续的动态平衡条件可以在几个周期的循环充电中实现。仅在极短的充电时间遇到不可持续的条件。然后将模型扩展为模拟阿拉巴马州多芬岛的淡水透镜,以评估在现实的干湿补给循环下淡水存储量的变化。本研究中提供的实验数据以及建模结果可以更好地理解小岛淡水存储模式的瞬态变化。

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