窟野河“19580710”洪水特性分析  

Analysis on the No.19580710 Flood of the Kuyehe River

作　　者：马文进[1] 苏念良[1] 王世忠[1] 陈国华[1] 张文彦[1] 

机构地区：[1]黄委中游水文水资源局,山西晋中030600

出　　处：《水资源与水工程学报》2008年第6期125-128,共4页Journal of Water Resources and Water Engineering

摘　　要：窟野河"19580710"洪水是一场十分罕见的高含沙洪水,对其特性进行分析目的是加深对高含沙洪水的认识,对高含沙洪水测报等具有参考、借鉴作用。应用水文学基本原理对这次洪水进行了深入分析,其突出特点是含沙量大、水面比降变化反常、洪水演进速度缓慢、发生了高含沙洪水特有的"浆河"现象。The No. 19580710 flood of the Kuyehe River was a flood with rarely high sediment load. The aims of analysis on its characteristics was to enhance the relevant knowledge which had the reference function for flood measurement and prediction, using the basic hydrological principles, this flood was deeply analyzed. It＇s characteristics was high sediment load, abnormal surface slop change, slow pace of flood routing, and the specific phenomena of ＂Standing River＂ in the sediment-hyperconcentration flow.

关 键 词：“19580710”洪水 洪水演进 水面比降 浆河 窟野河 

分 类 号：TV122[水利工程—水文学及水资源]