三峡电站日调度驱动的重力波对其支流动力过程造成显著影响,其中的高频水流波动会显著影响支流库湾的物质、能量等垂向扩散和输运过程,进而影响水华暴发等环境问题。基于三峡水库香溪河支流2021年蓄水期末的水动力及水温垂向结构监测数据,分析了三峡电站日调度驱动的支流库湾高频振荡对水温结构的影响。研究发现,三峡出库流量日波动驱动支流水位也呈日波动和高频波动特征,其中水位日波动振幅约0.3~0.5 m,高频水位波幅约0.04 m。库湾底层水温高频波动比中上层更加明显,与香溪河库湾水深从河口向上游逐渐变浅有关系。支流近底水温波动功率谱分析显示,香溪河湍流耗散速率(6.5×10-7 W/kg)明显高出一般水库的近底耗散率,表明水库调度驱动的水体高频波动导致较强的湍流发育和耗散。
Abstract
The gravity wave driven by the daily operation of Three Gorges Reservoir (TGR) has a significant influence on the dynamic process of its tributaries. In particular, the high-frequency water fluctuation remarkably affects the vertical transport or diffusion of materials and energy, and further on the algal blooming process. The influence of high-frequency oscillation in tributary bay driven by TGR’s daily operation on water temperature structure was examined based on the monitoring data of hydrodynamics and vertical structure of water temperature in Xiangxi Bay of TGR at the end of 2021 impoundment period. Results demonstrated that the daily fluctuation of outflow of the TGR also gave rise to daily fluctuation and high frequency fluctuation of the water level of its tributaries. The amplitude of daily fluctuation of water level was about 0.3-0.5 m, and the high frequency fluctuation reached around 0.04 m. The high-frequency fluctuation in the bottom of the bay was more obvious than that in the mid-and-upper layer due to the water depth reduction from the estuary to the upper reaches. Power spectrum analysis of near-bottom water temperature fluctuation in tributaries showed that the turbulent dissipation rate of Xiangxi Bay (6.5×10-7 W/kg) is significantly higher than that of other reservoirs, indicating that the high frequency fluctuation of water driven by reservoir operation leads to strong turbulent development and dissipation.
关键词
流量日调节 /
支流振荡 /
水温波动 /
功率谱分析 /
湍流耗散
Key words
daily discharge regulation /
tributary oscillation /
water temperature fluctuation /
power spectrum analysis /
turbulent dissipation
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参考文献
[1] 刘德富, 杨正健, 纪道斌, 等. 三峡水库支流水华机理及其调控技术研究进展. 水利学报, 2016, 47(3): 443-454.
[2] JANE S F, HANSEN G J A, KRAEMER B M, et al. Widespread Deoxygenation of Temperate Lakes. Nature, 2021, 594: 66-70.
[3] 刘晋高, 徐雅倩, 马 骏, 等. 三峡水库香溪河库湾不同异重流下水温分层模式研究. 长江科学院院报, 2018, 35(4): 37-42.
[4] 章国渊.三峡水库典型支流水华机理研究进展及防控措施浅议. 长江科学院院报, 2012, 29(10): 48-56.
[5] 杨忠勇, 钱门亮, 纪道斌, 等. 香溪河初冬降温过程中垂向混合结构特征分析. 中国环境科学, 2021, 41(6): 2862-2870.
[6] 赵星星, 纪道斌, 龙良红, 等. 汛期水位波动对香溪河库湾热分层特性及水质的影响. 水力发电学报, 2021,40(2):31-41.
[7] 纪道斌, 刘德富, 杨正健, 等. 汛末蓄水期香溪河库湾倒灌异重流现象及其对水华的影响. 水利学报, 2010, 41(6): 691-696,702.
[8] 谢奇珂, 刘昭伟, 陈永灿, 等. 溪洛渡水库水温日变化的测量与分析. 水科学进展, 2018, 29(4): 523-536.
[9] LONG L H, JI D B, YANG Z Y, et al. Tributary Oscillations Generated by Diurnal Discharge Regulation in Three Gorges Reservoir. Environmental Research Letters, 2020, 15(8): 084011.
[10] 徐 慧, 龙良红, 纪道斌, 等. 三峡水库泄水-蓄水过程香溪河库湾水流振荡特性. 水科学进展, 2022, 33(2): 264-273.
[11] 纪道斌, 周哲轩, 杨忠勇, 等. 三峡出库流量日调节模式驱动的重力波问题. 水利学报, 2021, 52(1): 111-119.
[12] YANG Z, ZHU Y, JI D,et al. Discharge and Water Level Fluctuations in Response to Flow Regulation in Impounded Rivers: An Analytical Study. Journal of Hydrology, 2020, 590: 125519.
[13] 纪道斌, 刘德富, 杨正健, 等. 三峡水库香溪河库湾水动力特性分析. 中国科学:物理学 力学 天文学, 2010, 40(1): 101-112.
[14] 杨正健. 分层异重流背景下三峡水库典型支流水华生消机理及其调控.武汉:武汉大学, 2014.
[15] 浦 祥. 长江河口重力环流、潮汐应变、混合与层化.上海:上海交通大学, 2017.
[16] 熊龙兵. 长江河口环流与湍流混合:数学模拟与理论计算.上海:上海交通大学, 2014.
[17] WÜEST A, LORKE A. Small-scale Turbulence and Mixing: Energy Fluxes in Stratified Lakes . Encyclopedia of Inland Waters, 2009, doi: 10.1016/B978-012370626-3.00084-3.
[18] LORKE A, UMLAUF L, MOHRHOLZ V. Stratification and Mixing on Sloping Boundaries. Geophysical Research Letters, 2008, 35(14): L14610.
[19] SUTHERLAND G, REVERDIN G, MARIÉ L, et al. Mixed and Mixing Layer Depths in the Ocean Surface Boundary Layer under Conditions of Diurnal Stratification. Geophysical Research Letters, 2014, 41(23): 8469-8476.
[20] LÓPEZ M, IGLESIAS G, KOBAYASHI N. Long Period Oscillations and Tidal Level in the Port of Ferrol. Applied Ocean Research, 2012, 38: 126-134.
[21] BOCANIOV S A, UMANN C, RINKE K, et al. Internal Waves and Mixing in a Stratified Reservoir: Insights from Three-Dimensional Modeling. Limnologica, 2014, 49: 52-67.
基金
国家自然科学基金项目(52079069,52009066,U2040220);湖北省高校优秀中青年科技创新团队项目(T2021003);长江科学院开放研究基金资助项目(CKWV20221003/KY)