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NUMERICAL SIMULATION OF ICE-COVER INFLUENCE ON NEARFIELD MIXING

机译:覆冰对近场混合影响的数值模拟

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This paper presents the results of a numerical-simulation investigation of ice-coverrninfluence on the mixing and transport of a neutrally buoyant contaminant released inrna straight reach of a dune-bed channel. The investigation used a three-dimensionalrncomputational fluid dynamics model, validated against flume data for flow distributionrnin the channel and against a simple analytical solution for mixing in the channel.rnThe model was used to simulate contaminant release near the ice-cover undersidernand near the bed. The results show that, for constant water discharge, coverrnpresence reduces near-field mixing because it redistributes the flow, increases flowrndepth, decreases bulk velocity, reduces maximum level of turbulence, and modifiesrndune geometry. For the ice-covered flow, a contaminant released near the bed orrnnear the cover underside remains closer to those boundaries over a longer distancernthan for openwater flow. The simulation shows that cover presence reduces therndepth-averaged diffusivity to about 45% of the corresponding diffusivity forrnopenwater flow. The distance to attain full mixing across the flow depth increases byrna commensurate amount.
机译:本文介绍了数值模拟研究的结果,该研究涵盖了冰覆盖对沙丘床河道直段释放的中性浮力污染物的混合和运输的影响。该研究使用了三维计算流体动力学模型,该模型针对通道中的流量分布的水槽数据和针对通道中混合的简单分析解决方案进行了验证。该模型用于模拟冰盖下侧和床附近的污染物释放。结果表明,对于恒定的排水量,覆盖层会减少近场混合,因为它会重新分配流量,增加流量深度,降低体积速度,减小最大湍流并修改几何形状。对于被冰覆盖的水流,在离床近的地方或靠近盖底面的地方释放的污染物比开放水流在更长的距离上仍更靠近那些边界。模拟表明,覆盖物的存在将深度平均扩散率降低到相应的非开放水流扩散率的约45%。在整个流动深度上达到完全混合的距离增加了相应的数量。

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