前言自从地下水非稳定运动理论问世以来,传统的求解地下水运动的有关水文地质参数以及研究地下水运动规律的解析法对一些水文地质条件复杂的地区往往是无能为力的。因为无论是饱水带还是饱气带,其地下水运动的基本方程式大都是非线性的,且参数之间彼此又有复杂的函数关系。所以具体应用 Introduction Since the advent of groundwater non-steady motion theory, the traditional analytical methods for solving hydrogeological parameters of groundwater movement and studying groundwater movement laws are often powerless for some areas with complex hydrogeological conditions. Because the basic equations of groundwater movement are mostly non-linear, regardless of whether they are saturated or saturated, and the parameters have complex functional relationships with each other. So the specific application