汉江下游分水咀滩段通航水流条件及整治效果分析

Analysis of navigational flow conditions and regulation effectiveness in the Fenshuiju shoal section of the Lower Hanjiang River

  • 摘要: 汉江下游分水咀滩段受长江水位顶托与上游径流共同影响,水位变幅显著,水流条件复杂。2022年受长江特枯水情影响,顶托作用锐减时,滩段局部急流、陡比降问题加剧,威胁船舶通航安全。基于平面二维水动力模型,分析天然条件下水流特征与碍航成因,提出针对性航道整治方案并验证其效果,主要结论如下:(1)研究河段受上游径流和下游长江水位顶托共同作用,枯水期顶托作用减弱导致局部比降骤,设计水位条件下局部比降达0.45‰,横向流速达0.8 m/s,形成“跌水卡口”,引发航槽流态紊乱,船舶上行阻力增大、下行舵效降低。2022年长江特枯水位使卡口效应放大,船舶通航条件恶化,罕见枯水碍航态势凸显。(2)随着长江水位抬升或径流量的增大,河段比降呈现先降后升的非线性变化,水位抬升反而削弱了卡口段束窄效应,横向流速降低,通航条件得以改善。(3)研究河段上游为抗冲性强的泥坪段,下游为可动性较高的粉砂段,河床高程骤降达4 m,局部河床坡降显著,河床的异质性加剧了枯水期局部流态的恶化。(4)针对枯水碍航问题,提出航槽疏浚与切除卡口边滩的整治方案,数值模拟表明,工程实施后设计水位下纵向与横向流速最大降幅分别达0.4 m/s和0.6 m/s,航道内水流比降趋于平缓,主流流向与航道夹角显著缩小,有效缓解了弯道段流态紊乱问题。研究表明,针对性整治工程可缓解水位顶托与河床异质性的叠加碍航效应,为类似河段治理提供参考。

     

    Abstract: The Fenshuiju shoal section in the lower reaches of the Hanjiang River is subject to the combined influence of backwater effects from the Yangtze River and upstream runoff, resulting in significant water level fluctuations and complex flow conditions. In 2022, due to an exceptionally low water level in the Yangtze River, the diminished backwater effect exacerbated local rapid flows and steep longitudinal gradients in the shoal area, posing serious threats to navigational safety. Using a two-dimensional hydrodynamic model, this study investigates the natural flow characteristics and navigation obstructions, proposes targeted channel regulation strategies, and evaluates their effectiveness. Key findings are as follows: (1) The study reach is jointly affected by upstream runoff and the backwater effect of the Yangtze River. During low-flow periods, the weakening backwater effect leads to steepened local gradients—up to 0.45‰ under design water level conditions—with transverse velocities reaching 0.8 m/s. This creates a "waterfall choke point," inducing disturbed flow patterns, increased upstream navigation resistance, and reduced downstream rudder effectiveness. In 2022, the extreme low water level of the Yangtze significantly intensified this choke point effect, leading to deteriorated navigational conditions and highlighting the rare low-flow navigation obstruction. (2) As the Yangtze River water level or runoff increases, the longitudinal gradient exhibits a nonlinear response—first decreasing and then increasing. The elevated water level weakens the constriction effect at the choke point, reduces transverse velocity, and thus improves navigational conditions. (3) The upstream reach of the study section consists of erosion-resistant mudbanks, while the downstream segment comprises more mobile silt deposits. A sharp riverbed elevation drop of up to 4 meters contributes to significant local bed gradients. The heterogeneity of the riverbed intensifies flow disturbances during low-flow periods. (4) In response to low-flow navigation constraints, a regulation scheme involving channel dredging and removal of the shoal at the choke point was proposed. Numerical simulations show that, after implementation, the maximum reductions in longitudinal and transverse flow velocities under design water levels reach 0.4 m/s and 0.6 m/s, respectively. The flow gradient within the navigation channel becomes more moderate, and the alignment between the main flow direction and channel axis improves markedly, effectively mitigating disturbed flow conditions in curved segments. This study demonstrates that targeted regulation measures can alleviate the compounded effects of backwater weakening and riverbed heterogeneity on navigation, offering reference solutions for similar river reaches.

     

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