摘要
建立了适用于黄河中游龙潼河段的一维悬移质泥沙数学模型。利用十年实测水沙资料进行了验证计算,结果表明,实测冲淤量与计算值基本相符。本模型可用于预测不同减水减沙情况下的泥沙冲淤调整过程。
A one-dimensional mathematical model for scour and deposit of suspended load in the middle reach between Longrnen and Tongguan of the Yellow River is established. The model is calibrated by using the 10-year field data in this reach, and it is found that the calculated results agree basically with the field data. Thus, the model can be used to predict the sediment scouring and depositing processes under conditions with decreased quantities of water and sediment.
出处
《西安理工大学学报》
CAS
1996年第3期251-256,共6页
Journal of Xi'an University of Technology
基金
"八五"国家重点科技攻关项目
关键词
悬移质
泥沙
数学模型
冲刷
淤积
黄河
suspended load sediment mathematical model scour deposit