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Vortex pattern and wave motion produced by a bottom blunt body moving at a critical speed

机译:底部钝体以临界速度运动产生的涡旋图和波动

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摘要

An underwater object moving at a near-critical speed in a shallow-water domain had been observed to generate a sequence of upstream propagating solitary waves with an elongated depression of water surface and a train of dispersive waves followed in the downstream. This study presents the development of a two-dimensional stream function-vorticity based viscous fluid model with satisfied nonlinear free-surface conditions to study the generation of solitary waves and the induced vortex motion under the forcing of a moving object. A combined finite analytic and finite difference method is adopted to solve the flow field equations and free-surface boundary conditions in a transient curvilinear coordinate system. The model is shown to produce free-surface elevations in fairly good agreements with published results for a test case of a moving smooth bump. Other tests for the generation of recirculation zone behind a body of square shape in a confined fluid domain are also conducted to further verify the model performance. The results showing the generation of upstream advancing solitary waves and downstream vortex pattern by a blunt rectangular body moving at a critical speed along the bottom in a domain with free surface are presented. Comparisons of results from potential flow and viscous flow conditions are made to demonstrate the importance of viscosity to the wave generation. Different from the relatively regular vortex pattern occurred under the case of Re = 3500, the transition of the vortex motion for a larger Reynolds number (e.g. Re = 35,000) evolves without a regular pattern throughout the generation process of the advancing solitons. The effects of the size and bluntness of a moving object on the generated flow field and free-surface elevations are also analyzed and discussed.
机译:已经观察到在浅水域中以近临界速度运动的水下物体会产生一系列上游传播的孤波,水面拉长,并且在下游跟随一列色散波。这项研究提出了一种基于二维流函数-涡度的粘性流体模型,该模型具有令人满意的非线性自由表面条件,以研究孤立波的产生和在运动物体的强迫下引起的涡旋运动。采用有限解析与有限差分相结合的方法求解瞬态曲线坐标系中的流场方程和自由面边界条件。对于移动平滑凹凸的测试案例,该模型显示出与发布的结果相当吻合的自由表面高程。还进行了其他测试,以在密闭流体域中生成方形体后方的回流区,以进一步验证模型的性能。结果表明,由钝的矩形体以临界速度沿具有自由表面的区域中的底部移动,产生了上游行进的孤波和下游涡流模式。比较了潜在流动条件和粘性流动条件的结果,以证明粘度对波浪产生的重要性。与在Re = 3500的情况下发生的相对规则的涡旋模式不同,更大的雷诺数(例如Re = 35,000)的涡旋运动过渡在前进的孤子的整个生成过程中都没有规则的模式。还分析和讨论了移动物体的大小和钝度对所产生的流场和自由表面标高的影响。

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