论文部分内容阅读
我们先后对十几个工程的单孔稀释法进行了试验研究,目前状况下该法求取含水层水文地质参数已卓有成效。但在实际应用中尚存在a系数值的选择问题,本文详细介绍了a系数的数学推导并探讨了其物理意义。
We have carried out experimental research on the single-well dilution method for more than a dozen projects. Under current conditions, this method has been effective in obtaining hydrogeological parameters of aquifers. However, there are still problems in the selection of a coefficient value in practical applications. This paper introduces the mathematical derivation of a coefficient and discusses its physical significance.