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Simulation of artificial flood releases from Skuifraam Dam to limit its impact on the Berg River morphology

机译:Skuifraam大坝人工洪水释放的仿真限制其对Berg河流形态的影响

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The proposed Skuifraam Dam, South Africa, will be the first major dam on the Berg River and it could have a major impact on the river morphology. The upper reach of the river where the dam is to be constructed is a steep boulder bed river, while 30 km downstream it becomes a sand-bedded stream. A hydrodynamic-morphological study has been carried out to simulate the long-term pre-dam current conditions, the post-dam morphology without any artificial flood releases and the post-dam morphology with artificial flood releases. A one-dimensional model was used with unsteady flow and coupled sediment transport to simulate a representative 10 year period. The hydrodynamic model was calibrated on flow records at two flow gauging stations on the river. The narrowing of the river due to the construction of the dam was taken into account by using an empirical relationship. Analysis indicated that the large boulders would only be transported during major floods and sediment transport simulation therefore focused on graded sand fractions. The effect of the dam was studied by evaluating the simulated total sediment transport balance of the river and by plotting the discharge-sediment load relationship at different locations along the river, for the pre- and post-dam conditions. The simulations considered one annual flood release from the dam during winter in July or August when the reservoir inflow exceeds 50 m~3/s. The artificial flood degrades the upper reach immediately downstream of the dam, but further downstream the sediment transport balance is improved. The simulations carried out in the 73 km river downstream of the dam indicated that artificial floods are required for river maintenance, but that the originally proposed annual flood of 160 m~3/s would be too regular and not effective to limit aggradation of the lower reaches of the river. Alternating artificial floods of 160 m~3/s and 2401 m~3/s have therefore been proposed for river maintenance, which should be released from the dam with freshets and low flow environmental flow requirements. It is proposed that the methodology followed in this investigation is used at any proposed new and existing dams to evaluate the impact of a dam on the downstream river morphology and to design artificial flood releases.
机译:南非建议的斯科瑞拉姆大坝将成为伯格河上的第一个主要大坝,它可能对河流形态产生重大影响。河流的上部到达大坝被建造的是一个陡峭的巨石床河,而下游30公里变成了砂床。已经进行了流体动力学研究,以模拟长期预滤场当前条件,没有任何人工洪水释放的后坝体形态和与人工洪水释放的后坝后形态。一维模型与非定常流量和耦合的沉积物运输一起使用,以模拟代表10年期间。流体动力学模型在河流上的两个流量测量站的流量记录上校准。通过使用实证关系考虑由于大坝的建造而导致的河流缩小。分析表明,大型巨石只会在主要洪水和沉积物运输模拟中运输,因此聚焦在分级砂馏分上。通过评估河流的模拟总泥沙运输平衡,并通过绘制沿河的不同地点的排出沉积物载荷关系来研究大坝的效果。仿真在冬季或八月期间,当水库流入超过50米〜3 /秒时,冬季洪水释放了一个年度洪水。人工洪水降解了大坝下游的上游,但进一步下游沉积物运输平衡得到改善。在大坝下游73公里河流中进行的模拟表明,河流维护需要人工洪水,但最初提出的160米〜3 / s的年度洪水将过于常规,而不有效地限制较低的汇编到达河边。因此,已提出160 m〜3 / s和2401 m〜3 / s的交替的人工洪水用于河流维护,应从水坝释放出新鲜和低流量环境流量要求。建议在该调查中遵循的方法在任何提议的新的和现有的水坝中使用,以评估大坝对下游河流形态的影响和设计人工洪水释放。

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