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Solute dispersion along unsteady groundwater flow in a semi-infinite aquifer

机译:半无限含水层中沿不稳定地下水流的溶质弥散

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Analytical and numerical solutions are obtained for dispersion of pollutants along unsteady groundwater flow in a longitudinal direction through semi-infinite aquifers the permeability of which is either uniform or varies with position. Sources of pollution are both a concentrated point input at the origin and a spatially distributed background source. One expression chosen to represent the seasonal pattern of the time dependent velocity is sinusoidal behaviour over a year. The solutions obtained predict the time and distance from the location at which an input concentration is introduced at which the pollution concentration becomes harmless. Also, the time period for rehabilitating a polluted aquifer for human use can also be assessed.
机译:通过沿渗透率是均匀的或随位置变化的半无限含水层,沿着非恒定地下水在纵向上沿非恒定地下水流扩散而获得了解析和数值解。污染源既是原点的集中输入,又是空间分布的背景源。选择用来表示随时间变化的速度的季节性模式的一个表达式是一年中的正弦行为。所获得的解决方案可预测距污染浓度变得无害的引入输入浓度的位置的时间和距离。此外,还可以评估修复污染的含水层供人类使用的时间。

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