长江口拦门沙河段航道回淤的波浪动力环境 Ⅱ:洪枯季作用差异*
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上海市自然科学基金(16ZR1415800)


Wave dynamic environment of channel deposition in mouth bars of the Yangtze River estuary Ⅱ:Differences between flood and dry seasons
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    摘要:

    开展了长江口拦门沙河段波浪对河床作用的洪枯季差异及规律研究,结果表明:1)长江口拦门沙河段波能随周期的分布曲线在洪季表现为“窄峰”特征,波能主要集中在4.0~7.0 s,而洪季表现为“宽峰”或“双峰”特征,波能主要集中在4.0~12.0 s;2)与枯季相比,洪季长周期的高能波发生频率及其波能所占年总波能的比例显著提高,其中波能增加数十倍;3)长江口拦门沙区域的波浪按周期可分为3种类型,即低能波、高能波以及过渡波,其中低能波对拦门沙区域的深水河床基本无作用,高能波对拦门沙区域的深水河床作用非常显著,但过渡波对拦门沙区域的深水河床作用不确定,视波向变化而定。

    Abstract:

    This article researches the seasonal differences caused by wave dynamics impacting on the riverbed during the flood and dry seasons in the mouth bars of the Yangtze River estuary.Some perceptions are as follows:1)For the distribution curve of wave energy,during the dry season,wave energy is focused on the range of 4.0~7.0 s,waveform presents a narrow peak,while during the flood season,the energy concentrates in the 4.0~12.0 s,waveform appears broad or double peaks;2)Compared with the dry season,the long period waves occurring in the flood season are more frequent,and the proportion of energy to the overall increases significantly,the quantity reaches dozens of times;3)In the mouth bars,according to different periods,waves can be divided into 3 types,i.e.low-energy wave,high-energy wave and transitional wave.Low-energy waves almost unchange the riverbed in deep water while high-energy waves are completely reverse,but the influence of transitional waves on the mouth bar area is uncertain,and it in determined according to the change of the wave direction.

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刘猛.长江口拦门沙河段航道回淤的波浪动力环境 Ⅱ:洪枯季作用差异*[J].水运工程,2016(6):110-115.

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  • 在线发布日期: 2016-06-16
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