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Initial dilution of a vertical round non-buoyant jet in wavy cross-flow environment

机译:波浪状横流环境中垂直圆形非浮力射流的初始稀释

摘要

The phenomenon of wastewater discharged into coastal waters can be simplified as a turbulent jet under the effect of waves and currents. Previous studies have been carried out to investigate the jet behaviors under the current only or the wave only environment. To obtain better understanding of the jet behaviors in a realistic situation, a series of physical experiments on the initial dilution of a vertical round jet in the wavy cross-flow environment are conducted. The diluted processes of the jet are recorded by a high-resolution camcorder and the concentration fields of the jet are measured with a peristaltic suction pumping system. When the jet is discharged into the wavy cross-flow environment, a distinctive phenomenon, namely “effluent clouds”, is observed. According to the quantitative measurements, the jet width in the wavy cross-flow environment increases more significantly than that does in the cross-flow only environment, indicating that the waves impose a positive effect on the enhancement of jet initial dilution. In order to generalize the experimental findings, a comprehensive velocity scale ua and a characteristic length scale l are introduced. Through dimensional analysis, it is found that the dimensionless centerline concentration trajectories yc/l is in proportion to 1/3 power of the dimensionless downstream distance x/l, and the dimensionless centerline dilution ScQ/(ual2) is proportional to the square of the dimensionless centerline trajectory yc/l. Several empirical equations are then derived by using the Froude number of cross-flow Frc as a reference coefficient. This paper provides a better understanding and new estimations of the jet initial dilution under the combined effect of waves and cross-flow current.
机译:在波浪和水流的作用下,排放到沿海水域的废水现象可以简化为湍流射流。已经进行了先前的研究以调查仅在当前或仅在波浪环境下的射流行为。为了更好地了解现实情况下的射流行为,对垂直横射流在波浪错流环境中的初始稀释进行了一系列物理实验。用高分辨率便携式摄录机记录喷射流的稀释过程,并用蠕动抽吸泵系统测量喷射流的浓度场。当喷射流排放到波浪状的横流环境中时,会观察到一种独特的现象,即“流出的云”。根据定量测量结果,波浪状横流环境中的射流宽度比仅横流环境中的射流宽度增加更大,这表明波浪对增强射流初始稀释度有积极作用。为了概括实验结果,引入了综合速度标度ua和特征长度标度l。通过尺寸分析,发现无量纲中心线浓度轨迹yc / l与无量纲下游距离x / l的1/3幂成正比,无量纲中心线稀释度ScQ /(ual2)与无量纲中心线稀释度ScQ /(ual2)成正比。无量纲中心线轨迹yc / l。然后,通过使用错流Frc的弗劳德数作为参考系数来导出几个经验方程。本文提供了对波浪和错流电流共同作用下射流初始稀释度的更好理解和新估计。

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