小江开州港区挖入式港池泥沙模型试验研究*
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国家自然科学基金面上项目(52479058); 中央级公益性科研院所基本科研业务费项目(CKSF20241011/HL,CKSF2024988/HL)


Experimental study on sediment model of excavated basin in Xiaojiang Kaizhou port area
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    摘要:

    针对挖入式港池普遍存在的淤积问题,开展泥沙模型试验,研究不同水沙条件下挖入式港池泥沙淤积规律。结果表明,大水丰沙年的1963年型港池淤积7.42万m3,平均淤积厚度为0.4~0.5 m,泥沙主要淤积在港池口门附近及原主河道内,局部可达1.3 m,港池内部淤积厚度仅为0.1~0.2 m;中水中沙年的1967年型与1963年型淤积规律基本一致,而淤积强度明显减弱。港池运行13 a末,港区河段全断面均产生淤积,平均淤积厚度约为1 m,局部可达2 m,泥沙主要淤积部位保持不变,港池口门约60 m范围淤后高程较高,小流量低水位时可能产生碍航。港池内95%时间水深达3.45 m,随着运行年限的增加,港池内泥沙呈累积性淤积,港池水深逐渐减小。在山区河道,利用回水沱建设挖入式港池工程是可行的,泥沙淤积可控。

    Abstract:

    Aiming at the problem of sedimentation in excavated basin,sediment model tests are conducted to investigate the siltation patterns of excavated basins under different water and sediment conditions.The results indicate that in the year of heavy water and sand,such as 1963,the sedimentation in the harbor basin reached 74,200 m3,with the average silting thickness was about 0.4-0.5 m.Sediment mainly accumulated near the entrance of the harbor basin and within the original main river channel,reaching up to 1.3 m in the local area.However,the sedimentation thickness within the harbor basin was only 0.1-0.2 m.After 13 years of operation,sedimentation occurred in the whole section of the river,with the average silting thickness was about 1.0 m and up to 2.0 m in some areas.The main areas of sediment accumulation remained unchanged.Specifically,an area of approximately 60 m at the entrance of the harbor basin experienced significant elevation after sedimentation,potentially causing navigation obstacles during periods of low water levels and small flow rates.As the years of operation increases,the sediment in the harbor basin accumulates cumulatively and depth of the harbor basin is gradually decreasing.In the mountainous river,it is feasible to construct excavated basins utilizing backwater eddies,and sediment accumulation can be controlled.

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吴华莉.小江开州港区挖入式港池泥沙模型试验研究*[J].水运工程,2025(12):17-26.

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  • 在线发布日期: 2025-12-19
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