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首页> 外文期刊>Acta Geophysica >One-dimensional Uniform and Time Varying Solute Dispersion along Transient Groundwater Flow in a Semi-Infinite Aquifer
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One-dimensional Uniform and Time Varying Solute Dispersion along Transient Groundwater Flow in a Semi-Infinite Aquifer

机译:半无限含水层中沿地下水瞬态流动的一维均匀时变溶质弥散

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An analytical solution for the space-time variation of contaminant concentration in one-dimensional transient groundwater flow in a homogenous semi-infinite aquifer, subjected to time-dependent source contamination, is derived. The uniform and time varying dispersion along transient groundwater flow is investigated under two conditions. First, the flow velocity distribution in the aquifer is considered as a sinusoidally varying function, and second, the flow velocity distribution is treated as an exponentially increasing function of time. It is assumed that initially the aquifer is not solute free, so the initial background concentration is considered as an exponentially decreasing function of the space variable which is tending to zero at infinity. It is assumed that dispersion is directly proportional to the square of the velocity, noting that experimental observations indicate that dispersion is directly proportional to the velocity with a power ranging from 1 to 2. The analytical solution is illustrated using an example and may help benchmark numerical codes and solutions.
机译:推导了均质半无限含水层中一维瞬态地下水流中污染物浓度随时间变化的源污染随时间变化的解析解。在两个条件下研究了沿瞬态地下水流动的均匀和时变分布。首先,将含水层中的流速分布视为正弦变化函数,其次,将流速分布视为时间的指数增长函数。假定初始含水层不是无溶质的,因此初始背景浓度被视为空间变量的指数递减函数,该变量在无穷大处趋于零。假设色散与速度的平方成正比,请注意实验观察表明,色散与速度成正比,幂范围为1到2。代码和解决方案。

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