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INFLUENCE OF WATER CONTROL FACILITIES ON THERMAL STRATIFICATION OF OGOUCHI RESERVOIR FOR 58 YEARS

机译:水控制设施对58年来OGOUCHI水库热分层的影响

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Selective withdrawal (SW) systems regulate the temperature of water released downstream of dam while vertical curtains (VC) prevent phytoplanktons from the shallow upstream reaches to disperse into the main reservoir. These water control facilities can affect the reservoir’s temperature distribution. Through long term analysis of Ogouchi’s temperature data together with numerical simulation, this paper explains the variation in temperature profiles during the three distinct periods in the reservoir’s operation namely, (1) deep penstock withdrawal (DPW), (2) purely SW and (3) combined SW and VC. Schmidt’s Stability Index (SSI) and Thermocline Strength Index (TSI) were computed to define thermal stratification. DPW promotes mixing and makes the reservoir generally warmer while SW creates a strong thermocline (high TSI) and when combined with VC, increases thermal stability (high SSI). Using 3-D hydrodynamic simulation, the conditions were successfully replicated. Results showed that outflow location and facilities largely affect the temperature and velocity profiles and the mixing and transport of river water within the reservoir.
机译:选择性提取(SW)系统调节水坝下游水的温度,而垂直窗帘(VC)防止浅层上游的浮游植物分散到主储存器中。这些水控制设施可能会影响水库的温度分布。通过长期分析OGOUCHI的温度数据与数值模拟,本文解释了水库操作中三个不同时期温度曲线的变化即(1)深管撤退(DPW),(2)纯粹SW和(3 )组合SW和VC。施密特的稳定性指数(SSI)和热控强度指数(TSI)被计算为定义热分层。 DPW促进混合,使储库一般温暖,而SW产生强大的热管(高TSI),并且与VC结合时,增加热稳定性(高SSI)。使用3-D流体动力学模拟,成功复制了条件。结果表明,流出的位置和设施在很大程度上影响了水库内河水的温度和速度谱和混合和运输。

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