前言大型岩溶泉水的动态分析对研究岩溶含水层的水动力性质有着重要作用。对于消耗期内流量不断衰减并具多亚动态的泉水流量,目前常采用迭加形式的衰减方程来表征。然而以该方程反演的流量曲线与实际曲线有着明显的差异,其误差值有的可达50％以上(迭加型水位方程亦是),笔者 Preface The dynamic analysis of large karst springs plays an important role in studying the hydrodynamic properties of karst aquifers. At present, the decay equation of superposition form is often used to characterize the flow rate of spring water with decaying flow rate and multi-sub-dynamic during the consumption period. However, the flow curve inversed by this equation has obvious difference from the actual curve, and the error value can reach more than 50% (superposition type water level equation is also)