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通过对娘子关泉域桃河岩溶渗漏段上下断面14次洪峰过程测流结果分析,建立了河流来水量与渗漏量间的非线性方程,对河流来水量大小、水量在时间上的动态分布特征和计算过程中所采用的时间尺度对河流渗漏量的影响进行了讨论。
Based on the analysis of 14 times of peak flow in the upper and lower sections of karst seepage section in Niangziguan spring basin, a nonlinear equation between river water inflow and seepage was established. The dynamic characteristics of water quantity and water flow in time The distribution characteristics and the time scale used in the calculation process are discussed.