低地河流下游低压水系回水重塑研究

K. Baymanov, R. Baymanov
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摘要

本文介绍了对塔希塔什水电站区内河道改造进行长期实地研究的结果。人们注意到,由于一年中的大部分时间水位低,塔希塔什大坝在所有跨度的闸门都是完全关闭的。近年来,调节盾构坝水位机制的作用几乎丧失,主要渠道末端调节机制被调节。给出了塔希塔什水电站的实际费用、浊度和备用与计算值的比较数据。研究结果表明,坝前水位的急剧波动和渠道的进水导致了盾构坝和渠道的水力和冲积状态的变化。塔希塔什水电站源区河床断面调查分析表明,在运行初期,上游底纹增加,下游底纹减少。在以后的运行年份(1982年之后),其特点是河床流动过程的稳定性,每个特征年份都有自己的水位和消耗机制。值得注意的是,在高水位年份,水的摄入没有困难,主要的困难与洪水通过盾坝有关。近年来,尽管打开了大坝闸门、船闸和取水设施,但上游水位仍迅速上升,这可以解释为流道对盾坝容量的影响。实验证明,在不破坏生长期取水的情况下,可以在取水系数Kv < 0.55不断降低的情况下,对上游进行有效冲刷。实际上,这意味着塔希塔什水电站的冲洗流量不应低于Q≥250 - 300 m3/s。
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A study of the re-shaping of the backwaters of low-pressure hydrosystems in the lower reaches of lowland rivers
The article presents the results of long-term field studies of the re-formation of water courses in the zone of the Takhiatash hydroelectric complex. It was noted that due to low water, for a significant part of the year, the Takhiatash dam worked with fully closed gates in all spans. In these years, the role of regulating the level regime of the shield dam is almost lost, and the end regulators of the main channels are regulated. The data of comparison of actual expenses, turbidity and back-up at the Takhiatash hydroelectric power plant with the calculated ones are presented. It is proved that sharp fluctuations in the water level in front of the dam and water intake into the channels lead to changes in the hydraulic and alluvial regime of the shield dam and channels. As the analysis of the survey of the riverbed cross-sections in the headwaters of the Takhiatash hydroelectric complex showed, in the initial period of operation, the bottom marks in the upper stream are increasing and the bottom marks in the lower stream are decreasing. Further years of operation (after 1982) were characterized by the stability of the flowing riverbed processes, that each characteristic year has its own level and consumption regime. It is noted that in high-water years there were no difficulties with water intakes, and the main difficulties are associated with the passage of flood flows through the shield dam. In recent years, there has been a rapid rise in the water level in the upper reaches, despite all the open dam gates, shipping locks and water intake structures, which are explained by the influence of the drifted streams on the capacity of the shield dam. It is proved that without any damage to the water intake during the growing season, it is possible to effectively flush the upstream with a constant decrease in the water intake coefficient - Kv < 0.55. Practically, this means for the Takhiatash hydroelectric unit that the flushing flow rate should not be lower than Q ≥ 250 – 300 m3/s.
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