【摘 要】
：
在分析河道断面状况和水流传播变化情况的基础上,论述了花园口站“05.7”洪水沿程增大的现象,并通过“92·8”、“04·8”等洪峰增值洪水过程的对比,指出花园口站“05·7”洪
【机 构】
：
黄河水利委员会水文局,黄河水利委员会水文局,黄河水利委员会水文局 河南郑州450004,河南郑州450004,河南郑州450004
论文部分内容阅读
在分析河道断面状况和水流传播变化情况的基础上,论述了花园口站“05.7”洪水沿程增大的现象,并通过“92·8”、“04·8”等洪峰增值洪水过程的对比,指出花园口站“05·7”洪水发生洪水增值现象是刚刚结束的调水调沙使河道普遍刷深、河床形态变优造成的。
Based on the analysis of the river channel profile and the variation of water flow, the phenomenon of “05.7” flooding along Huayuankou Station is discussed, and the comparisons of peak flood processes such as “92 · 8” and “04 · 8” , Pointed out that the phenomenon of flood value added in Huayuankou Station during the flood of “05 · 7” is caused by the just-concluded water diversion and sediment control that made the riverway generally deep and deep, and the shape of riverbed became better.
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