摘要
针对黄河水少沙多、水沙不均衡的现状,首次将河道时段来沙总量和时段平均流量的比值L作为判别河道冲淤的中间量,对兰州至巴彦高勒河段冲淤情况进行了研究,结果表明:①L小于0.5时河道处于冲刷状态;②L介于0.5~2.5时,河道基本上处于冲淤平衡状态;③L大于2.5时河道处于淤积状态,明显具有来沙多、淤得多的特点。
The paper studies the scour and fill of Lanzhou-Bayangaole section by firstly using the proportionality L of the total volume of coming sediment of channel time interval and mean discharge of time interval as intermediate volume for discriminating the scour and fill of channel in the light of the present status of uneven runoff and sediment of the Yellow River. The outcomes show the following characteristics: a) when L<0.5,the channel is in the state of scour;b) when L between 0.5~2.5,the channel is basically in equilibrium and;c) when L>2.5,the channel is in the state of fill,obviously possessing the characteristic of more coming sediment and more deposition.
出处
《人民黄河》
CAS
北大核心
2008年第6期25-25,28,共2页
Yellow River
关键词
来沙总量
平均流量
冲淤指标
兰州至巴彦高勒河段
黄河
total volume of coming sediment
mean discharge
scour and fill index
Lanzhou-Bayangaole section
the Yellow River