摘要
金堤河流域是黄淮海平原综合治理的重点地区之一,流域的中下游为黄河北金堤滞洪区,其滞洪影响面积约占全流域面积的57.8％。由于年降水量的时、空分布不均,造成该流域春旱、夏涝和秋旱交替出现。作者在综合分析流域的水文特性及设计洪涝水的基础上,提出了合理的设计洪水数据。同时,根据实测资料分析得出结论:金堤河大洪水不会与黄河下游大洪水遭遇。
Jindi River basin is one of the key areas for comprehensive harnes sing of the Huang-Huai-Hai plain and Beijindi Flood Detention Basin of the Yellow River is located on the middle and lower reaches of the basin, 57.8％ of the total area being affected by detainning flood. The drought in spring, flooding in summer or drought in autumn occurs frequently in the basin because the non-uniform distri bution of rainfall in time and space. Based on synthetic analysis on cha racteristics of hydrogy and design flood, the author puts forward a set of new indexes for flood design, and believes that a large flood in Jindi River should not meet with that in the lower Yellow River
出处
《人民黄河》
CAS
北大核心
1990年第2期11-15,共5页
Yellow River
