本文介绍在半承压含水层中,依据抽水井中的稳定降深与它的梯度和离抽水井径向距离的对数之比值的比,即 Sm/(δSm/δlog(?)r),确定含水层的导水系数。我们根据这个原理,提出了一种估算含水层参数的新方法,由于这种新方法不包括(适线)过程,从而避免了主观性。我们还将用一个实例来说明这种方法。引言在自然界,完全承压的含水层极少存在,一般情况下,半承压含水层(或漏水 In this paper, we describe the ratio of the ratio of the steady-state depth in a pumping well to the logarithm of its gradient and radial distance from a pumping well, ie Sm / (δSm / δlog (?) R), in a semi-confined aquifer Conductivity of aquifer. Based on this principle, we propose a new method of estimating aquifer parameters that avoids subjectivity as the new method does not include (fit-in) processes. We will also use an example to illustrate this method. Introduction In nature, fully confined aquifers rarely exist. In general, semi-confined aquifers (or leaking water