淤泥质海岸环境沙滩存在原因分析——以连云港天然沙滩为例
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Analysis on causes of sandy beach in muddy coastal environment:a case of natural sandy beaches in Lianyungang
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    摘要:

    基于连云港淤泥质海岸存在的4处天然沙滩,对沙滩平面和剖面形态特征、潮流条件、波浪条件以及泥沙运动特征进行详细分析,以研究淤泥质海岸环境存在沙质沙滩的原因。结果表明:天然沙滩均为两端有岬角的内凹弧形地貌形态,主要来浪方向与湾口方向一致,不利于产生显著的沿岸输沙,避免沙滩沙流失;剖面具有明显转折特征,较大的前沿水深有利于减少外海波浪传播过程中的损耗,可以维持较大的滩前波浪动力条件;来浪方向中大浪要达到一定的集中度和频率,H1/10波高大于0.40 m的大浪维持在36.6%以上的沙滩才能具备较好的沙滩滩面特征;波浪是淤泥起动悬扬的主要动力因素,波流挟沙力大于背景含沙量有利于沙滩形成,且挟沙力越大沙滩宽度越大。

    Abstract:

    Based on four natural sandy beaches in Lianyungang muddy coast,this study analyzes the morphological characteristics of beach plane and profile,tidal current conditions,wave conditions and sediment movement characteristics to study the reasons for the existence of sandy beaches in muddy coast environment.The results show that the natural beaches are concave arc-shaped landforms with headlands at both ends,and the main direction of the incoming waves is consistent with the direction of the bay mouth,which is not conducive to significant coastal sediment transport and avoids sediment loss.The natural beach profile has obvious turning characteristics,and the larger front water depth is conducive to reducing loss during the propagation of offshore waves,which can maintain larger wave dynamic conditions in front of the beach.The large waves in the direction of the natural beach should reach a certain concentration and frequency,and the large waves of the beach with H1/10 wave height greater than 0.40 m accounting for more than 36.6% is conducive to better beach surface characteristics.Waves are the main driving force of the mud resuspension.The sand carrying capacity of the tidal current is greater than the background sand concentration,which is conducive to the formation of the beach,and the larger the sand carrying capacity,the wider the beach width.

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张 磊,徐 岢,韩雪健,等.淤泥质海岸环境沙滩存在原因分析——以连云港天然沙滩为例[J].水运工程,2025(7):51-57.

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  • 在线发布日期: 2025-07-15
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