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    山丘区典型流域产流模型研究

    Study on the runoff generation model of a typical watershed in a hilly area

    • 摘要: 产流模型研究对暴雨洪水演进模型的构建及区域生态经济协调发展具有深远意义。以山东济宁市典型山丘区——泗河流域书院站控制区域为研究对象,选取46场典型暴雨洪水过程,分析流域水文特征参数,通过绘制降水径流关系中心线和外包线构建流域产流模型。研究表明:①书院站流域最大蓄水容量lm=120.0 mm;②通过绘制流域双累积曲线可以看出书院站流域1971—2023年产流规律未发生明显变化;③根据构建的流域产流模型,在相同影响雨量条件下,书院站流域产流量外包线查线值较中心线查线值的相对差值为9.1%~40.0%;④地表径流洪峰与浅层地下径流洪峰具有高度线性相关性,相关系数达到0.908 1。

       

      Abstract: The study of runoff generation model has far-reaching significance for the construction of rainstorm flood routing model and the coordinated development of regional ecological economy. Taking the control area of Shuyuan Station in Sihe River Basin, a typical hilly area in Jining City, Shandong Province, as the research object, 46 typical rainstorm flood processes were selected to analyze the hydrological characteristic parameters of the basin, and the runoff generation model of the basin was constructed by drawing the center line and outer line of precipitation runoff relationship. Research shows that: ①The maximum water storage capacity of the Shuyuan Station Watershed lm is 120.0 mm; ② By drawing the dual accumulation curve of the watershed, it can be seen that there has been no significant change in the annual flow pattern of the Shuyuan Station Watershed from 1971 to 2023; ③ According to the constructed watershed runoff generation model, under the same influencing rainfall conditions, the relative difference between the outer line value and the center line value of the watershed runoff at Shuyuan Station is 9.1% to 40.0%; ④ The peak of surface runoff has a highly linear correlation with the peak of shallow groundwater runoff, with a correlation coefficient of 0.908 1.

       

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