分流河道淤积与洞庭湖萎缩对长江洪灾的影响

INFLUENCES OF THE SHRINK OF DIVIDING CHANNELS AND THE DONGTING LAKE ON THE FLOOD IN THE YANGZTE RIVER

  • 摘要: 1998年长江流域的特大洪水灾害表明,目前长江流域防洪体系在面临特大洪水时仍然显得比较脆弱. 以长江中下游荆江洞庭湖地区为背景,运用有限体积计算方法建立了一维河道和二维湖泊交错的复杂水系洪水演进数值模型,细致分析了由于分流河道淤积以及洞庭湖萎缩对长江洪灾的影响. 得出长江分流河道和洞庭湖由于泥沙淤积产生的萎缩将造成长江干流河道洪水期间水位抬升,从而加重长江的洪水灾害. 其结论可为长江中下游地区的洪水治理提出建设性意见.

     

    Abstract: The flood disaster along the Yangzte river in 1998 which broughtabout enormous economic losses to Chinese people shows that the floodcontrol system of the Yangzte River is still very weak despite ofenhanced capabilities of flood prevention in these years. Focusing onthe Jingjiang River and Dongting Lake area, a numerical FVMmodel is established to study flood routing in this complicated water systemconsisting of one-dimensional rivers and two-dimensional lakes. By applyingthis model, the simulation of flood motion in the river network owing to geographical environment factors are analyzed in detail.Two important factors that may cause high stages in the Jingjiang Riverduring the 1998 Yangzte River flood period have been identified. They are,the blockage of the dividing rivers and shrink of the Dongting Lake.According to this research, a number of measures can be adopted to mitigate theflood disaster in the Yangtze River valley.

     

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