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      瓯江引水工程对感潮河段河床冲淤影响研究

      Influence study of Oujiang Water Diversion Project on riverbed scour and deposition in tidal reach

      • 摘要: 瓯江引水工程取水口位于瓯江感潮河段上,受潮流影响大,水势复杂,取水口局部和工程河段在工程作用下的冲淤情况不明。利用历史断面数据对瓯江感潮河段冲淤趋势进行分析,并使用二维水流泥沙模型对瓯江引水工程建设后的取水口局部和工程河段冲淤情况进行模拟。研究结果表明:工程建成后,受工程引水影响,工程前沿局部区域存在一定程度冲刷,最大冲刷深度约2 m; 工程混凝土挡墙上下游侧存在一定程度的淤积,其中,取水口下游侧淤积范围、淤积幅度均较上游侧偏大,最大淤积幅度约2.5 m。工程运行后,取水口头部所在的凸岸滩坡可能进一步淤积,需加强监测,必要时采取清淤措施加以维护。

         

        Abstract: The water intake of Oujiang River Diversion Project is located in the tidal reach of Oujiang River, which is significantly influenced by tidal currents and features complex flow conditions.The local scour and deposition patterns around the intake and within the project reach under engineering conditions remain unclear.Based on historical cross-sectional data, this study analyzed the erosion-deposition trends in the tidal reach of Oujiang River.A two-dimensional flow sediment model was employed to simulate the scour and deposition near the intake and along the project reach after the construction of the diversion project.The results indicated that after project completion, localized scour occurred in the frontal area of the intake due to the diversion effect, with a maximum scour depth of approximately 2 m.Meanwhile, deposition was observed both upstream and downstream of the concrete retaining wall of the project.The deposition extent and magnitude downstream of the intake were greater than those upstream, with a maximum deposition thickness of about 2.5 m.After the project operation, the convex bank slope where the intake head is located may experience further deposition.Enhanced monitoring is therefore recommended, and dredging measures should be implemented when necessary to maintain the project′s functionality.

         

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