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首页> 外文期刊>Journal of Fluid Mechanics >Direct numerical simulations of instability and boundary layer turbulence under a solitary wave
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Direct numerical simulations of instability and boundary layer turbulence under a solitary wave

机译:孤波作用下不稳定性和边界层湍流的直接数值模拟

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A significant amount of research effort has been made to understand the boundary layer instability and the generation and evolution of turbulence subject to periodic/oscillatory flows. However, little is known about bottom boundary layers driven by highly transient and intermittent free-stream flow forcing, such as solitary wave motion. To better understand the nature of the instability mechanisms and turbulent flow characteristics subject to solitary wave motion, a large number of direct numerical simulations are conducted. Different amplitudes of random initial fluctuating velocity field are imposed. Two different instability mechanisms are observed within the range of Reynolds number studied. The first is a short-lived, nonlinear, longwave instability which is observed during the acceleration phase, and the second is a broadband instability that occurs during the deceleration phase. Transition from a laminar to turbulent state is observed to follow two different breakdown pathways: the first follows the sequence of K-type secondary instability of a near-wall boundary layer at comparatively lower Reynolds number and the second one follows a breakdown path similar to that of free shear layers. Overall characteristics of the flow are categorized into four regimes as: (i) laminar; (ii) disturbed laminar; (iii) transitional; and (iv) turbulent. Our categorization into four regimes is consistent with earlier works. However, this study is able to provide more specific definitions through the instability characteristics and the turbulence breakdown process.
机译:为了理解边界层的不稳定性以及受周期性/振荡流影响的湍流的产生和演化,已经进行了大量研究工作。但是,对于由高瞬变和间歇性自由流强迫(例如孤立波运动)驱动的底部边界层知之甚少。为了更好地理解不稳定性机制的性质和受孤立波运动影响的湍流特性,进行了大量直接数值模拟。施加不同幅度的随机初始波动速度场。在研究的雷诺数范围内观察到两种不同的不稳定机制。第一个是在加速阶段观察到的短暂的非线性长波不稳定性,第二个是在减速阶段发生的宽带不稳定。观察到从层流状态到湍流状态的转变遵循两种不同的破坏途径:第一种遵循在相对较低的雷诺数下的近壁边界层的K型二次失稳的序列,第二种遵循与类似的破坏途径。自由剪切层。流动的总体特征可分为以下四种情况:(i)层流; (ii)层流不畅; (iii)过渡性的; (iv)湍流。我们将其分类为四个制度与早期的工作是一致的。但是,这项研究能够通过不稳定性特征和湍流破坏过程提供更具体的定义。

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