摘要
本文研究了江河水位变化所引起的地下水位上升变化过程,并推导了地下水位上升及渗流量的计算公式。这些公式能够用来计算不同时间、不同位置的地下水位、渗流量及贮水量。研究这些问题,对于水资源规划设计等方面具有实用意义。
In this paper, the rise of groundwater table owing toriver level variation is studied and formulas are derived for calculating the groundwater table and seepage discharge variation with time and place. These problems are very important for the designing and planning of water resources,
