摘要
探讨了地下水向承压水完整井的稳定运动,比较了在Darcy流和非Darcy流情况下井周围水位降深的计算方法。运用Darcy定律、Forchheimer公式及指数型公式对井周围的水头分布进行求解,并对结果进行了比较,得到不能单纯用线性渗流规律代替非线性渗流规律的结论,及非线性渗流不同公式之间的区别与联系。
The authors discussed the steady movement from ground water to fully penetrating well in a confined aquifer, and compared the calculation method of drawdown around fully penetrating well in the conditions of Darcy flow and non-Darcy flow. Using Darcy's law, Forchheimer equation and the exponential formula of wells to solve the distribution around the head, and compared with the results. It was proved that the linear seepage regularity could not be simply replaced by the non-linear seepage regularity, and the difference and connection between different non-linear flow equations.
出处
《地质学刊》
CAS
2010年第4期397-399,共3页
Journal of Geology
关键词
承压水完整井
Darcy流
非Darcy流
水头分布
Fully penetrating well in a confined aquifer
Darcy flow
Non-Darcy flow
Head distribution