三门湾海域悬沙输运特征及其影响机制*
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国家自然科学基金资助项目(41406101)


Characteristics of suspended sediment transport in Sanmen Bay and its influencing mechanism
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    摘要:

    基于2013年洪枯季三门湾海域12个测站潮流和含沙量同步观测资料,运用机制分解法研究三门湾枯季和洪季悬沙输移变化特征,探讨不同水动力因子的贡献率。结果表明:1)无论是洪季还是枯季,三门湾的欧拉余流和斯托克斯余流从小潮至大潮逐渐增大。欧拉余流方向基本向海,斯托克斯余流绝大部分向陆。单宽输水量的大小和方向主要由欧拉余流决定。2)枯季时三门湾海域“平流输沙(T1+T2)”对单宽输沙量绝对值的贡献率最大,其中T1项最大贡献率可达83%;“潮泵输沙项(T3+T4+T5)”的贡献率在湾中区域最大。洪季时,三门湾的平流输沙项的贡献率降低,而潮泵输沙项贡献率增大。3)无论是洪季和枯季时,三门湾泥沙净输运个别站位(SM08和SM11)输沙方向相反,其他站位的规律基本一致。

    Abstract:

    Based on the simultaneous observation data of tidal current and sediment content at 12 stations in the Sanmen Bay during dry and flood seasons in 2013,the mechanism decomposition method was used to analyze the transport mechanism of suspended sediment in the dry and flood seasons,and to explore the contribution rate of different hydrodynamic factors. Results show that:1)Whether it is the flood season or the dry season,the Euler residual current and Stokes residual current increase gradually from neap tide to spring tide. The direction of Euler residual current is seaward,and the direction of Stokes residual current is landward in the study area. The size and direction of the single-width water delivery are mainly determined by the Euler residual current. 2)During the dry season,the advection transport term is the principal constituent of the suspended sediment transport in Sanmen Bay,and the largest contribution rate of T1 is 83% in the study area. The contribution rate of the tidal pumping transport term (T3+T4+T5)is the largest in the middle of the bay. During the flood season,the contribution rate of the advection transport item in Sanmen Bay decreases,while the contribution rate of the tidal pumping transport term increases. 3)Regardless of the flood season and the dry season,the net transport of sediment at individual stations (SM08 and SM11) in Sanmen Bay is in the opposite direction,and the laws of other stations are basically the same.

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吴创收,黄世昌,罗向欣.三门湾海域悬沙输运特征及其影响机制*[J].水运工程,2021(7):7-13.

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  • 在线发布日期: 2021-07-07
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