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Research on entrance training and reclamation project of Dongshuigang, Chengmai county, Hainan

机译:海南省澄迈县东水港入学培训与填海工程研究

摘要

According to the measured and statistical data, this paper outlined the natural conditions, the characteristics of hydrodynamic, sediment, geomorphic and geological conditions near the lagoon of Dongshuigang, Chengmai County, Hainan. It also analyzed the formation processes of sand barrier, sand spit, lagoon system and the seabed revolution. The analysis results show that the terrain erosion and disposition at the entrance and near theudsandbank on the east of Dongshuigang is of great changes and the erosion and siltation rate in the lagoon is small. The sand from the river basin and human activities are the main causes for deposition in the lagoon. The tidal current numerical model for partial Chengmai Bay is verified based on the measured data and the project scheme is researchedudwith this model. The research shows that the reclamation project inside the lagoon slightly reduces the tidal prism of lagoon; the flow velocity near the project decreases somewhat after reclamation outside the entrance, entrance expansion and excavation of the waterway. The influences of Scheme I, Scheme II and Scheme III on tidal prism of lagoon are equally small and the reclamation project serves as a sand dike, playing a role in maintaining the stability of the channel at the entrance of Dongshuigang.
机译:根据实测资料,概述了海南省澄迈县东水港泻湖附近的自然条件,水动力特征,沉积物,地貌和地质条件。还分析了阻沙层,吐沙口,泻湖系统和海床公转的形成过程。分析结果表明,东水港东侧和南滩附近的地形侵蚀和分布变化很大,泻湖的侵蚀和淤积率很小。流域的沙子和人类活动是泻湖中沉积的主要原因。根据实测数据验证了澄迈湾部分地区的潮流数值模型,并研究了该方案的方案。研究表明,泻湖内的填海工程使泻湖的潮汐棱柱略有减小。在入口外进行填海,入口扩展和水道开挖后,项目附近的流速有所降低。方案一,方案二,方案三对泻湖潮汐棱镜的影响较小,围垦工程作为挡沙堤,在保持东水港入口处河道稳定方面发挥了作用。

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