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Physical Modeling of Propagation Features of the 1998 Floods in theJingjiang Reach of the Yangtze River

机译:长江江江江江江洪水繁殖特征的物理建模

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Physical modeling of the propagation features of the 1998 floods in the Jingjiang Reach of the Yangtze River has been conducted under the topographical condition of Oct. 2002 and without consideration of the operation of the Three Gorges Project. The experimental results show that, comparing with the prototype floods in 1998 , the experimental flood peak stages are generally higher with the largest rise being 0.98 m. It takes 21 hr for the flood peak to transport from Zhicheng to Jianli with an average speed of 3. 2 m/s. Under the studied experimental conditions , the flood protection situation of the reach is still severe, especially that of the Lower Jingjiang Reach. The floods at the main stations along the reach exceed the warning stage of the dike for quite long period. The flood peak stages at Shashi, Shishou, Jianli and Lianhuatang exceed the design stage of the dike by 1.20 m, 1. 25 m, 1. 73 m and 1. 68 m, respectively.
机译:1998年10月的荆江涌入1998年洪水的繁殖特征的物理建模,在2002年10月的地形条件下进行了地形条件,不考虑三峡工程的运作。实验结果表明,与1998年的原型洪水相比,实验洪水峰阶段通常较高,最大升高为0.98米。洪水峰预付21小时,从志成到济莲运输,平均速度为3.2米/秒。在研究的实验条件下,泄洪局势仍然是严重的,尤其是荆江下游的恐惧。沿着达到的主要站的洪水超过了很长一段时间的堤防的警告阶段。 Shashi,Shishou,Jianli和Lianuatang的洪水峰阶段超过了堤防的设计阶段1.20米,1.25米,1.73米和1. 68米。

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