摘要
本文就线性非齐次地下水系统提出了响应矩阵的直接解法——剩余降深方法,并且给出了较严格的理论证明。它把响应矩阵的求解分为三个步骤:一求附加降深场,二求综合降深场,再求剩余降深场,即得到响应矩阵。该方法不仅为以往的间接解法找到了一种对比解法,而且有可能据此向非线性系统拓展。颇具理论和实际意义。
In this paper a direct method, namely Remanent Drawdown Method, is suggested for solving the response matrix in linear non-homogeneous ground water system, and a strict theoretical proof for it is given. The essence of the new method is to divide the solving process into three steps. The additional drawdown is calculated, first 'the synthetical drawdown, secondly, and the remanent drawdown, thirdly. This remanent drawdown is just the response matrix to he expected. By using the method, is not only possible to compare the results with those by the indirect method, but also to develop management mehtods in the field of non-linear system. The new method may have active meanings both theor eticatly and practically.
出处
《水文地质工程地质》
CAS
CSCD
北大核心
1991年第1期28-30,共3页
Hydrogeology & Engineering Geology
