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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 fordispersion of pollutants along unsteady groundwater flow in a longitudinal directionthrough semi-infinite aquifers the permeability of which is either uniform or varies withposition. Sources of pollution are both a concentrated point input at the origin and aspatially distributed background source. One expression chosen to represent the seasonalpattern of the time dependent velocity is sinusoidal behaviour over a year. The solutionsobtained predict the time and distance from the location at which an input concentrationis introduced at which the pollution concentration becomes harmless. Also, the time periodfor rehabilitating a polluted aquifer for human use can also be assessed.
机译:通过渗透率均匀或随位置变化的半无限含水层,获得了沿非恒定地下水在纵向上沿不稳定水流扩散的解析和数值解。污染源既是原点的集中输入,又是无源分布的背景源。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。所获得的解决方案预测了从污染浓度变得无害的输入浓度引入位置开始的时间和距离。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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