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首页> 外文期刊>Journal of Hydrology >Wave overwash impact on small islands: Generalised observations of freshwater lens response and recovery for multiple hydrogeological settings
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Wave overwash impact on small islands: Generalised observations of freshwater lens response and recovery for multiple hydrogeological settings

机译:波浪过冲对小岛的影响:多种水文地质环境中淡水晶状体响应和恢复的一般观测

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摘要

Wave overwash events have the potential to result in severe consequences to the freshwater resources of small islands as a result of salt contamination of the aquifer. Due to the significant impact of overwash, it is important to characterise the susceptibility of small islands to these events. This study uses numerical modelling to evaluate the freshwater lens response and recovery to overwash events for various island hydrogeological settings (island types) observed worldwide. Models were developed for an example of each island type using a fully coupled surface-subsurface, density-dependent flow and solute transport modelling code. A theoretical overwash event was simulated, and the response and recovery of the freshwater lens were observed for 20 years. The freshwater lens response (degree of aquifer contamination) was largely determined by the vadose zone thickness. Lens recovery ranged from 1 to 19 years for the different island types, and was strongly affected by recharge rate. However, the recovery of potable water in the lens (and restoration of a water supply) was dominantly influenced by geological heterogeneities. The model results demonstrate the cumulative impact of the different factors affecting the freshwater lens response and recovery to the overwash event for each island type, and provide a generalised assessment of island susceptibility to overwash on a global scale, despite limited data availability for many small islands. (C) 2015 Elsevier B.V. All rights reserved.
机译:浪潮冲刷事件可能会由于含水层的盐分污染而对小岛的淡水资源造成严重后果。由于过度冲洗的重大影响,重要的是表征小岛对这些事件的敏感性。这项研究使用数值模型来评估全球观察到的各种岛屿水文地质环境(岛屿类型)的淡水晶状体响应和过冲事件的恢复。使用完全耦合的表面-地下,依赖于密度的流动和溶质迁移建模代码,为每种岛类型的示例开发了模型。模拟了理论上的冲洗事件,并观察了淡水晶状体的响应和恢复长达20年。淡水晶状体的响应(含水层污染的程度)在很大程度上取决于渗流带的厚度。不同岛屿类型的镜头恢复时间为1到19年,并且受充电率的强烈影响。但是,晶状体中饮用水的恢复(以及供水的恢复)主要受地质异质性影响。模型结果表明,影响每种类型岛屿的淡水晶状体响应和对过度冲洗事件的恢复的不同因素的累积影响,尽管许多小岛屿的数据可用性有限,但仍可在全球范围内对岛屿过度冲洗的敏感性进行一般性评估。 。 (C)2015 Elsevier B.V.保留所有权利。

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