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A numerical study on the evolution and structure of a stress-driven free-surface turbulent shear flow

机译:应力驱动的自由表面湍流剪切流的演化与结构的数值研究

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Turbulent shear flow beneath a flat free surface driven by a surface stress is simulated IF numerically to gain a better understanding of the hydrodynamic processes governing the scalar transfer across the air-water interface. The simulation is posed to mimic the subsequent development of a wind-driven shear layer as in a previous experiment except that the initiation of the surface waves is inhibited, thus focusing on the boundary effect of the stress-imposed surface on the underlying turbulent flow and vice versa. Despite the idealizations inherent in conducting the simulation, the computed flow exhibits the major surface features, qualitatively similar to those that appear in the laboratory and field experiments. Two distinct surface signatures, namely elongated high-speed streaks and localized low-speed spots, are observed in the simulated flow. Including temperature as a passive tracer and describing an upward heat flux at the surface, we obtain high-speed streaks that are colder and low-speed spots that are warmer than the surrounding regions. The high-speed streaks, arranged with somewhat equal cross-spacing of centimetres scale, are formed by an array of streamwise jets within the viscous sublayer immediately next to the surface. Beneath the streaks, counter-rotating streamwise vortex pairs are observed among other prevailing elongated vortices. However, they are significantly shorter in length and more irregular than their corresponding high-speed streaks at the surface. Accompanying the more organized high-speed streaks, localized regions of low streamwise velocity emerge randomly on the surface. These low-speed spots are attributed to strong upwelling flows which disrupt the viscous sublayer and also bring up the submerged fluids of low streamwise velocity. The occasional interruptions of the streamwise high-speed Jets by the upwelling flows account for bifurcation or dislocation of the surface streaks. Statistics of the turbulence are presented and their implications for the formation of the flow structures are discussed.
机译:IF数值模拟了由表面应力驱动的平坦自由表面下的湍流剪切流,以更好地理解控制跨空气-水界面的标量传递的流体动力学过程。如先前的实验一样,该模拟被模拟为模仿了风驱动剪切层的后续发展,只是抑制了表面波的产生,因此着重研究了应力施加表面对底层湍流和流动的边界作用。反之亦然。尽管进行模拟具有固有的理想化,但计算的流量仍具有主要的表面特征,在质量上与实验室和现场实验中出现的特征相似。在模拟流中观察到两个不同的表面特征,即细长的高速条纹和局部的低速斑点。包括温度作为被动示踪剂并描述了表面上的向上热通量,我们获得了比周围区域更冷的高速条纹和较温暖的低速点。高速条纹以接近厘米级的横向间距排列,是由紧邻表面的粘性子层内的一系列射流形成的。在条纹下方,在其他主要的细长涡旋中观察到反向旋转的涡流对。但是,它们的长度明显短于表面上的相应高速条纹,并且不规则。伴随更有组织的高速条纹,低水流速度的局部区域随机出现在表面上。这些低速点归因于强烈的上升流,该上升流破坏了粘性子层并且还引起了低流速的淹没流体。上行气流偶尔会中断高速喷气流,这是表面条纹的分叉或错位的原因。介绍了湍流的统计数据,并讨论了其对流动结构形成的影响。

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