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Optimization and Regulation of Operational Mode in Xiaolangdi Reservoir during Later Sediment Retaining Period

机译:小浪底水库淤积后期作业方式的优化与调度。

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摘要

The designed sediment storage capacity in Xiaolangdi Reservoir is7.5 × 109 m3.The reservoir deposition morphology during the whole sediment retaining period is as follows: in initial sediment retaining period,the deposition morphology is a delta.With the continuous deposition in reservoir,the delta vertex moves gradually downstream to dam.And at last,the deposition morphology will be a cone.After that,deposition sufaace will increase and reach designed elevation.During later sediment retaining period,in the process of water and sediment regulation,in most time the reservoir is in water storage condition.The delta deposition morphology can keep relatively large storage capacity.With the same amount of sediment and water storage,compared with cone deposition morphology,the water lever before dam of delta deposition morphology is obviously lower,the backwater length is obviously shorter.The analysis shows that delta deposition morphology is obviously superior to cone deposition morphology in the aspects of optimizing outlet water and sediment process,effectivly utilizing tributary storage capacity,trapping the coarse sand and discharging the fine sand,maintaining effective storage capacity for a long time and so on.The results of mathematical model and physical model preliminarily show that optimizing operational mode of reservoir can keep delta deposition morphology for a relatively long period,slow reservoir deposition velocity,extend sediment retaining life,and increase the amount of sand into the sea.At the same time,it does not obviously decrease sedimentation reducton effect of downstream Gao-cun reach.
机译:小浪底水库的设计泥沙储量为7.5×109 m3。整个泥沙淤积期的沉积形态为:在初期泥沙淤积时期,沉积形态为三角洲。三角洲的顶点逐渐向下游移动至大坝。最后,沉积形态为圆锥形。此后,沉积表面将增加并达到设计的高度。在沉积物滞留期的后期,在水和泥沙调节的过程中,大部分时间三角洲沉积形态可保持相对较大的储水能力。在沉积物和蓄水量相同的情况下,与锥状沉积形态相比,三角洲沉积形态大坝前的水位明显降低,回水长度明显更短。分析表明,三角洲沉积形态明显优于锥状沉积形态在优化出水和输沙过程方面,有效利用支流蓄水能力,截留粗砂,排出细砂,长期保持有效蓄水能力等。数学模型和物理模型的初步结果表明:优化水库运行模式可以使三角洲沉积形态保持相对较长的时间,降低水库的沉积速度,延长沉积物的保质期,并增加入海的沙量。下游高村到达。

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