摘要
根据参证站(所市水文站)资料外推了关门峡水库至电站厂址处的径流资料,分析了水库蓄水前后下游干沟、纸厂河、薛家大槽河口汇入白溪河处的年际径流、年内径流、各典型年典型月径流的变化规律,指出泥沙对下游影响不大,对下游河势河态无明显影响。
According to the data from bench-mark station （Suoshi Hydrologic Station）, we extrapolate the runoff data from Guanmenxia Reservoir to the power station. Characteristics of runoff change before and after the impoundment of the reservoir, including interannual, annual, typical month and typical year, at the estuary of the Gangou, Zhichanghe and Xuejiadachao stream into Baixi River, are analyzed. And then it points out that the sediment has little impact on the downstream and has no obvious effect on downstream river regime and river pattern.
出处
《水电能源科学》
北大核心
2013年第5期24-26,共3页
Water Resources and Power
基金
国家自然科学基金资助项目(40972218)
中国地质大学(武汉)中央高校基本科研业务费专项资金资助项目(G1323521125
G1323521225)
关键词
白溪河
关门峡水库
电站厂址处
径流
泥沙
河势
Baixi River
Guanmenxia reservoir
power station site
runoff
sediment
river regime
