基于混蓄电站运行的水源区水库水温结构模拟预测研究

Simulation and prediction of reservoir water temperature structure in a water source area under hybrid pumped-storage operation

  • 摘要: 混合式抽水蓄能电站(混蓄电站)作为清洁能源对实现我国“双碳”战略目标具有重要意义,然其日周期抽水-发电往复循环运行模式会扰动水体原有生态平衡,尤其饮用水水源保护区等水环境敏感区域的水温影响需准确评估。本文选取钱塘江上游某混蓄电站为研究对象,基于CE-QUAL-W2构建立面二维水温数值模型,模拟典型枯水年库区水温演变过程,预测该电站运行期上下库区水温分层结构特征,并量化评估混蓄电站运行对库区水温结构的扰动影响。研究结果表明:该混蓄电站上游水库垂向水温高温期呈“混合-温跃-滞温-温跃-滞温”五层结构,低温期呈“混合-温跃-滞温”三层结构;下游水库分层特征较弱,无明显表温层和滞温层。与现状常规电站运行相比,混蓄电站运行后库区水温结构整体保持稳定,局部略有变化,上游水库高温期抽蓄口附近温跃层发生轻微波动,下游水库低温期坝前水温略升高约0.5 ℃。本文研究结果可为饮用水水源区水库生态友好调度方案制定及环境影响评价提供科学依据。

     

    Abstract: Hybrid pumped-storage power stations, as clean energy facilities, are of great significance for achieving China’s “Dual Carbon” strategic goals. However, their daily pumping-generation cycles may disturb the existing aquatic ecological balance. In particular, water temperature impacts in environmentally sensitive water areas such as drinking water source protection zones require accurate assessment. Taking a hybrid pumped-storage power station in the upper reaches of the Qiantang River as a case study, this study constructs a vertical two-dimensional numerical water temperature model using CE-QUAL-W2 to simulate reservoir water temperature evolution in a typical dry year, predict the thermal stratification characteristics of the upper and lower reservoirs during operation, and quantitatively evaluate the effects of hybrid pumped-storage operation on reservoir water temperature structure. The hybrid pumped-storage project is located on a tributary of the upper reaches of the Qiantang River. Three hydraulic and hydropower projects, namely the upper reservoir, the lower reservoir and a water diversion project, have been built sequentially from upstream to downstream, alongside a hybrid pumped-storage power station currently under construction. Full-year daily meteorological and hydrological time series of a typical dry year (1985) in the watershed are adopted in this study, which are compiled from measured meteorological and hydrological data. Meteorological variables include air temperature, solar radiation, cloud cover, dew point temperature, wind speed, etc. The dew point temperature is calculated from local air temperature and relative humidity. Hydrological data consist of daily inflow discharge and water temperature, outflow discharge, and hourly pumping and generation flows of the hybrid pumped-storage station. The simulated outflow discharge and water temperature processes of the upper reservoir are used as the inflow boundary series for the lower reservoir. Combined with the hydrological characteristics of the watershed, May, August and December are selected as representative months for wet, normal and dry seasons, corresponding to the warming period, high-temperature period and cooling period, respectively. The contour plots of reservoir-wide water temperature distribution and monthly vertical water temperature profiles at typical cross-sections are adopted to analyze the thermal stratification characteristics of the upper and lower reservoirs after the operation of the hybrid pumped-storage station and assess its impacts on the baseline water temperature structure of the water source area. The results show that the operation of the hybrid pumped-storage station does not alter the fundamental thermal stratification pattern of the reservoirs. As a deep and large reservoir, the upper reservoir presents a five-layer vertical water temperature structure of “mixed layer–thermocline–hypolimnion–thermocline–hypolimnion” in high-temperature seasons and a three-layer structure of “mixed layer–thermocline–hypolimnion” in low-temperature seasons. Owing to its small storage capacity and shallow water depth, the lower reservoir exhibits weak thermal stratification with no distinct epilimnion and hypolimnion and small vertical temperature differences. The station operation induces slight local disturbances to the reservoir thermal structure. The upper pumping-generation intake is located near the upper layer of the reservoir; its pumping and generation processes impose limited disturbance on the thermocline around the intake during high-temperature seasons, accompanied by a slight increase in thermocline thickness. For the shallow lower reservoir, warmer inflow water in winter after station operation raises the vertical water temperature in front of the dam by approximately 0.5 ℃. After commissioning, the monthly trends of outflow water temperature from both reservoirs remain generally consistent with the baseline condition. The outflow water temperature rises slightly from June to December, with an overall temperature difference not exceeding 0.7 ℃. In general, the hybrid pumped-storage operation exerts minor impacts on the existing thermal stratification of the water source reservoirs. The studied river reach lies within the core zone of a national wetland park, which has high standards for biodiversity conservation and occupies an important ecological position. It is recommended that in situ water temperature monitoring be strengthened in the early operation stage of the power station, and real-time assessment of ecological effects induced by water temperature variations be carried out to support the optimization of eco-friendly reservoir operation and adaptive management schemes for the water source area.

     

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