摘要
根据渭河下游平滩流量及来水来沙资料,分析了渭河下游平滩流量和水沙条件的变化情况,建立了平滩流量与河段前期水沙系列之间的定量关系,为研究渭河下游河槽演变提供科学依据。
Based on the data of bank-full discharge and runoff-sediment condition of the downstream of Weihe River, the transformation of bank-full discharge and runoff-sediment condition have been analyzed, and this paper established the quantitative relationship between the bank-full discharge and runoff-sediment condition in prophase. It can be supplied the scientific base for the riverbed evolution in downstream of Weihe River.
出处
《水资源与水工程学报》
2006年第3期79-82,共4页
Journal of Water Resources and Water Engineering
关键词
河道演变
平滩流量
水沙条件
渭河下游
river bed evolution
bank-full discharge
runoff-sediment condition
downstream of Weihe River
