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黄河府谷吴堡区间泥沙特性初析
引用本文:李学春,高贵成,高国甫,杨峰.黄河府谷吴堡区间泥沙特性初析[J].水资源与水工程学报,2001,12(3):42-44.
作者姓名:李学春  高贵成  高国甫  杨峰
作者单位:黄委会中游水文水资源局,
摘    要:黄河96.8洪水的主要特性是小流量高水位(超过建国以来的最高水位),大漫滩,洪水传播历时长,灾害严重,而形成如此特性的主要原因是泥沙淤积河床抬升,严重萎缩.因此研究和探讨黄河主要产沙区之一府谷吴堡区间的泥沙特性具有其积极的意义.

关 键 词:泥沙特性    侵蚀模数    输沙量    黄河
文章编号:1008-5858(2001)02-0042-03
修稿时间:2001年3月28日

The initial analysis of sediment property in Fugu-Wubao section of Yellow river
LI Xue chun,GAO Gui cheng,GAO Guo fu,YANG Feng.The initial analysis of sediment property in Fugu-Wubao section of Yellow river[J].Journal of water resources and water engineering,2001,12(3):42-44.
Authors:LI Xue chun  GAO Gui cheng  GAO Guo fu  YANG Feng
Abstract:The Yellow River 96.8 flood is mainly charactered with high stage(higher than the highest stage since the PRC's foundation),heavy floodplain,long flood transmission time and severe damage. Such a character is largely due to the elevation and bad shrink of the river bed caused by sedimentation. Therefore,it possesses positive sense to study and discuss the sediment property in Fugu-Wubao section, one of the main sediment-yielding areas in Yellow river.
Keywords:sediment property  erosion modulus  total quantity of transporting sediment  Yellow river  
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