朱博渊, 刘凌峰, 李江夏, 程永舟, 胡旭跃. 径流变化下长江口多分汊系统冲淤分布差异及动力机制[J]. 水科学进展, 2023, 34(4): 585-598. DOI: 10.14042/j.cnki.32.1309.2023.04.011
引用本文: 朱博渊, 刘凌峰, 李江夏, 程永舟, 胡旭跃. 径流变化下长江口多分汊系统冲淤分布差异及动力机制[J]. 水科学进展, 2023, 34(4): 585-598. DOI: 10.14042/j.cnki.32.1309.2023.04.011
ZHU Boyuan, LIU Lingfeng, LI Jiangxia, CHENG Yongzhou, HU Xuyue. Erosion-deposition change pattern and hydrodynamic mechanism for the multilevel bifurcating system of Yangtze River Estuary under runoff variation[J]. Advances in Water Science, 2023, 34(4): 585-598. DOI: 10.14042/j.cnki.32.1309.2023.04.011
Citation: ZHU Boyuan, LIU Lingfeng, LI Jiangxia, CHENG Yongzhou, HU Xuyue. Erosion-deposition change pattern and hydrodynamic mechanism for the multilevel bifurcating system of Yangtze River Estuary under runoff variation[J]. Advances in Water Science, 2023, 34(4): 585-598. DOI: 10.14042/j.cnki.32.1309.2023.04.011

径流变化下长江口多分汊系统冲淤分布差异及动力机制

Erosion-deposition change pattern and hydrodynamic mechanism for the multilevel bifurcating system of Yangtze River Estuary under runoff variation

  • 摘要: 为探究水库调平径流过程下长江口多分汊系统冲淤规律, 根据1950—2021年水沙、地形和工程资料, 拟定径流强度指标(Da, 60 000 m3/s以上流量多年平均持续天数)、追踪滞流点位置和按航道疏浚还原北槽冲淤量辨析长江口冲淤分布差异和动力机制。结果表明: Da越大, 越利于北部和南部汊道落潮分流比增大和减小, 促进北部汊道冲刷加剧、淤积减缓和南部汊道淤积加剧、冲刷减缓, 且利于北部和南部汊道淤积重心向下游和上游移动; 冲淤差异受水流惯性和南岸节点挑流驱动, 径流流量变化使得落潮主流北偏或南偏, 形成南北汊道横向和纵向冲淤的联动机制; 随着径流过程持续坦化, 长江口北部汊道整体和上段将维持淤积加剧或冲刷减缓趋势、下段将维持冲刷加剧或淤积减缓趋势, 南部汊道冲淤趋势相反; 北槽滞流点在上下段间迁移的临界径流流量为35 000 m3/s, 未来上段淤积可能增强, 建议适时调整航道维护区段。

     

    Abstract: This paper examines the application of the erosion-deposition law to the multilevel bifurcating system of Yangtze River Estuary under dam-induced runoff flattening.The spatiotemporal pattern of erosion-deposition change and associated hydrodynamic mechanism are identified by analyzing water-sediment, terrain and engineering data from 1950 to 2021 in terms of a runoff intensity index Da (i.e., multiyear average days of runoff discharge ≥60 000 m3/s), tracked positions of stagnation points, and estimates of restored erosion-deposition volume of the north passage according to navigation dredging data.It is found that the ebb partition ratios of the north and south branching channels tend to increase and decrease, respectively, as Da grows; this aggravates erosion and impedes deposition in the north branching channels while facilitating deposition and restraining erosion in the south branching channels.Meanwhile, depo-centers in north and south branching channels move downstream and upstream.The foregoing changes in erosion-deposition are driven by hydrodynamic inertia and the flow-deflecting effect of nodes along the south bank.More specifically, the ebb flow axis swings either northward or southward as the runoff discharge varies, forming a linkage mechanism for the lateral-longitudinal erosion-deposition pattern between the north and south branching channels.As the runoff process becomes continuously flattened owing to upstream dam regulation activities, the north branching channels and their upper sub-reaches are likely to maintain a trend of deposition aggravation and erosion impediment, whereas their lower sub-reaches maintain a trend of erosion aggravation and deposition impediment.Conversely, the south branching channels are likely to witness an opposite trend in erosion-deposition.The critical runoff discharge for migration of the stagnation point between upper and lower sub-reaches in the north passage is 35 000 m3/s.At such a situation, additional deposition is expected to occur in the upper sub-reach, and timely maintenance adjustments would be required along key segments of the navigational channel.

     

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