Institute of Mineralogy and Geochemistry, Karlsruhe Institute of Technology , Karlsruhe 76131, Germany.
Environ Sci Technol. 2014 Jul 15;48(14):7798-806. doi: 10.1021/es501132k. Epub 2014 Jul 2.
The impoundment of the Three Gorges Reservoir (TGR) on the Yangtze River in China burdened its tributary backwaters with severe environmental problems.1 Confluence zones of reservoir tributaries with the Yangtze River main channel are main drivers of pollutant dynamics in the TGR2 and are thus keys to develop mitigation measures. Here, we show a novel experimental approach of spatiotemporal water quality analysis to trace water mass movements and identify pollutant transport pathways in reservoir water bodies. Our results show the movements of density currents in a major tributary backwater of the TGR. A huge interflow density current from the Yangtze River main channel transported its heavy metal carriage to the upstream reaches of the tributary backwater. Water from the upstream backwater moved counterwise and carried less but pollutant-enriched suspended sediments. This scenario illustrates the importance of confluence zone hydrodynamics for fates and pathways of pollutants through the widely unknown hydrodynamics of new reservoirs.
三峡水库(TGR)的蓄水给长江支流带来了严重的环境问题。1 水库支流与长江干流的汇流区是 TGR 污染物动态的主要驱动因素,因此是制定缓解措施的关键。在这里,我们展示了一种新的时空水质分析实验方法,以追踪水体运动并识别水库水体中的污染物输运途径。我们的结果显示了 TGR 一条主要支流回水区域内密度流的运动。一股来自长江干流的巨大底流将其重金属携带物输送到支流回水的上游。来自上游回水的水体则反向流动,携带的悬浮泥沙较少,但污染物含量较高。这种情况说明了汇流区水动力对于通过广泛未知的新水库水动力的污染物命运和途径的重要性。