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首页> 外文期刊>Environmental Modelling & Software >Modelling the effects of reservoir construction on tidal hydrodynamics and suspended sediment distribution in Danshuei River estuary
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Modelling the effects of reservoir construction on tidal hydrodynamics and suspended sediment distribution in Danshuei River estuary

机译:模拟淡水河口水库建设对潮汐水动力和悬浮泥沙分布的影响

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摘要

A vertical (laterally integrated) two-dimensional numerical model was implemented to study the hydrodynamics, saltwater intrusion, and suspended sediment in the Danshuei River—Tahan Stream due to the Shihmen Reservoir construction in the upriver reaches. The construction of the reservoir and water diversion in the upper reaches of the river system significantly reduces the freshwater inflow and drastically changes the river bathymetry. The model was calibrated and verified with the available hydrographic data measured in 1977, 1978, and 1999 as well as measured salinity and suspended sediment concentration in 1999. The overall performance of the model is in reasonable agreement with the field data. The validated model was then used to investigate the change in hydrodynamics, saltwater intrusion, suspended sediment distribution, and flushing time as a result of reservoir construction in upper river of Tahan Stream. The model simulations indicate that more tidal energy propagates into the estuarine system after reservoir construction because of the substantial increase in river cross-sections. The limits of saltwater intrusion after reservoir construction extended farther inland 2—3 km than those after reservoir construction. The modelling results also reveal that the suspended sediment concentration before reservoir construction was higher than that after reservoir construction along the river mouth to Kuan-Du due to the significant bathymetric change after the reservoir construction. The calculated estuary flushing time was strongly dependent on river flow and reduced 2.3—25 h under different river discharges after reservoir construction due to the change in river bathymetry.
机译:为了研究上游上游的石门水库的建设,淡水河-大汉溪水流动力学,咸水入侵和悬浮沉积物被采用了一个垂直(横向整合)的二维数值模型。河流系统上游的水库建设和引水大大减少了淡水的流入,并大大改变了河流的水深。该模型已通过1977年,1978年和1999年测得的可用水文数据以及1999年测得的盐度和悬浮泥沙浓度进行了校准和验证。该模型的总体性能与现场数据基本吻合。然后,使用经过验证的模型来研究由于塔汉溪上游河流水库建设而引起的水动力变化,盐水入侵,悬浮泥沙分布和冲洗时间的变化。模型模拟表明,由于河道断面的大量增加,更多的潮汐能在水库建设后传播到河口系统。水库建设后的盐水入侵范围比水库建设后的范围内陆延伸了2-3公里。模拟结果还表明,由于水库建设后的水深变化较大,沿河口至关都的水库建设前的悬浮泥沙浓度高于水库建设后的沙尘浓度。计算得出的河口冲刷时间主要取决于河流流量,并且由于水深的变化,在水库建设后不同河流流量下河口冲刷时间减少了2.3-25小时。

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