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首页> 外文期刊>農業土木学会論文集 >Analysis of seawater intrusion into a Ryukyu limestone coastal aquifer using an immiscible approach: -- development and conservation of groundwater resources on a small island (I) --
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Analysis of seawater intrusion into a Ryukyu limestone coastal aquifer using an immiscible approach: -- development and conservation of groundwater resources on a small island (I) --

机译:用一种不混溶的方法分析琉球石灰岩沿海含水层中的海水入侵:-在一个小岛上开发和保护地下水资源(I)-

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摘要

In order to study proposals for meeting increasing water demands on a small island where the source of freshwater is coastal groundwater, it is important to be able to analyse the movement of the freshwater-saltwater interface where seawater intrudes into the coastal aquifer. This paper describes a numerical analysis that can reproduce measured freshwater-saltwater interface levels in a Ryukyu limestone coastal aquifer. Numerical analysis of quasi 3D groundwater density flow using the finite difference method can model the movement of the tip of the saltwater intrusion and the distribution of basement rock. This method was adopted for the reverse operation of the permeability coefficient and porosity based on the groundwater level. The numerical solutions show good agreement with the measured values for movement of the freshwater-saltwater interface It is concluded that this is a practical method for analysing the movement of the freshwater-saltwater interface where seawater intrudes into a large coastal aquifer, because the measured value is affected by hydrogeological characteristics.
机译:为了研究在一个淡水来源为沿海地下水的小岛上满足不断增长的用水需求的建议,重要的是能够分析海水侵入沿海含水层的淡水-盐水界面的运动。本文介绍了一种数值分析方法,可以再现琉球石灰石沿海含水层中测得的淡水-盐水界面水平。使用有限差分法对准3D地下水密度流进行数值分析,可以对盐水侵入尖端的运动和基底岩石的分布进行建模。该方法用于基于地下水位的渗透系数和孔隙率的反演。数值解与淡水-盐水界面运动的测量值具有很好的一致性。结论是,这是一种分析海水侵入大型沿海含水层的淡水-盐水界面运动的实用方法,因为测量值受水文地质特征的影响。

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