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Integrated water quality monitoring and modeling in the Three Gorges Reservoir, China

机译:三峡水库综合水质监测与建模

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Increasing eutrophication and algal bloom events in the Yangtze River Three Gorges Reservoir are widely discussed in relation to hydrodynamics and nutrient transport and distribution processes. Insights into water exchange and interaction dynamics between water masses related to large scale water level fluctuations in the reservoir are crucial to understand water quality and eutrophication dynamics. Therefore, confluence zones of tributaries with the Yangtze River main stream are dedicated key interfaces. In this study, water quality data recorded in-situ and on-line with the MINIBAT towed underwater multi-sensor system is integrated with data obtained from simulations done with TELEMAC hydrodynamic 2D numerical modeling. Key scenario for the current study was a discharge peak and corresponding rising water level in the Yangtze River at its confluence zone with the Daning River following a heavy precipitation event in August 2011. Water quality data obtained from MINIBAT measurements during this specific period suggest that Yangtze River main stream water flowed upstream into the Daning River. Hydrodynamic 2D numerical modeling supports that hypothesis and enables to specify water and substance origins. Observed algal blooming can only be partly explained by the 2D modeling approach. 3D effects like the stabilization of thermal stratification at the water surface forming good conditions for algal blooming cannot be simulated but were measured with the MINIBAT. However, input of higher nutrient loads from Yangtze River water and from waste water discharges into the Wushan Lake are supported by the model and the field measurements and may have played a key role for the observed algal bloom formation.
机译:增加长江三峡库区中的富营养化和藻类盛开事件得到了与流体动力学和营养运输和分配过程的广泛讨论。与储层中大规模水位波动相关的水群之间的水资源交换和相互作用动态的见解对于了解水质和富营养化动态至关重要。因此,与长江主流的支流的汇合区是专用的关键接口。在本研究中,与MINIBAT牵引水下多传感器系统出于原位和在线的水质数据与通过通过Telemac流体动力学2D数值模拟完成的模拟中获得的数据集成。目前研究的关键情景是在2011年8月的大量降水事件之后,在其汇率区的汇流区中的汇率区的排放峰值和相应的水平。在此具体期间从Minibat测量中获得的水质数据表明长江河主流水流在上游进入丹宁河。流体动力学2D数值建模支持该假设和能够指定水和物质起源。观察到的藻类盛开只能通过2D建模方法部分解释。类似于在水面稳定的效果,形成藻类盛开的良好条件的水面,但是用小巴巴测量。然而,通过模型和现场测量,支持从长江水和废水排放到武术湖中的较高营养负荷的输入,并且可能为观察到的藻类盛开形成发挥了关键作用。

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