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Simulation to investigate the essential reasons of typhoon induced siltation in Chang iang River Estuary and the impact to water source area

机译:仿真以研究台风诱导沉锡的基本原因湖河河口及水源区的影响

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A well-validated wave model with No. 9912 typhoon is established using Delft-SWAN mode to study the effect of wind wave caused by typhoon on the navigation channel of Changjiang River Estuary. The wave factors including the wave height, wave length, wave period and wave steepness under one typhoon wind scenario - with velocity of 20m/s and direction of NNE35°, obtained from the statistical data, are simulated to show the wave fields under the typhoon wind. The difference between wave orbital velocity near bottom and threshold velocity of the suspended bed sediment in navigation channel and the carrying capacity of suspended sediment in Changjiang River Estuary are calculated to analyze the mechanism of sudden siltation caused by typhoons on the basis of the three basic conditions that of Changjiang River Estuary. The computed results show that in the effort of typhoon, wave height increases sharply and the huge energy induced by broken wave erodes the sediment on the shoals. The sediment carried by wave enters into the navigation channel and causes the sudden siltation in the navigation channel of Changjiang River Estuary.
机译:用9912号台风甲充分验证的波模型建立使用代尔夫特-SWAN模式来研究大江口的导航信道引起的台风波的影响。波因素,包括波高,波长,波周期和下一个台风场景波陡 - 与NNE35的为20m / S和方向°,从统计数据获得的速度,进行了模拟,以显示台风下波场风。近在导航信道悬浮床沉积物的底部和阈值速度波轨道速度和在大江口悬浮沉积物的承载能力之间的差进行计算,分析的三个基本条件的基础上造成的台风突然淤积的机制是长江口。计算结果表明,在台风的努力,浪高急剧增加和破碎波引起的巨大能量削弱的浅滩泥沙。由波携带的沉积物进入导航信道和引起大江口的导航信道突然淤积。

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