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The influence of non-equilibrium pressure on rotating flows.

机译:非平衡压力对旋转流的影响。

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摘要

This study was undertaken to investigate the influence of pressure relaxation on steady, incompressible flows with strong streamline curvature. In the early part of this dissertation research, the significance of non-equilibrium pressure forces in controlling the structure of a steady, two dimensional axial vortex was demonstrated. In order to extend the study of pressure relaxation influences on more complex rotating flows, this dissertation has examined other rotating flow features that can be associated with hurricanes, tornadoes and dust devils. To model these flows, modified boundary layer equations were developed for a fluid column rotating near a solid plane including the influence of non-equilibrium pressure forces. The far-field boundary conditions were inferred using the asymptotic behavior of the governing equations, and the boundary conditions for the axial and radial components of velocity were shown to be dependent on the pressure relaxation coefficient, η p, and the characteristic angular velocity of the rotating fluid column, ω. This research has shown for the first time that the inclusion of non-equilibrium pressure results in a free-standing stagnation plane at the top of a funnel shaped rotating fluid column, which is consistent with observational data for hurricanes, tornadoes and dust devils. It has also been shown that in the absence of non-equilibrium pressure, the stagnation plane for rotating flows cannot be observed. The velocity and pressure distributions resulting from incorporating non-equilibrium pressure effects were then compared with available observational data for tornadoes and dust devils. The general profiles of the velocity and pressure distributions were found to be in good agreement with physical measurements, which was not possible without introducing empirical turbulence effects, in the absence of non-equilibrium pressure effects.
机译:进行这项研究以研究压力松弛对具有强流线曲率的稳定不可压缩流的影响。在本文的早期研究中,证明了非平衡压力在控制稳定的二维轴向涡旋结构中的意义。为了扩展对更复杂的旋转流的压力弛豫影响的研究,本文研究了可能与飓风,龙卷风和尘土飞扬有关的其他旋转流特征。为了对这些流动建模,针对在固体平面附近旋转的流体柱(包括非平衡压力的影响)开发了改进的边界层方程。利用控制方程的渐近行为推导了远场边界条件,并且表明了速度的轴向和径向分量的边界条件取决于压力松弛系数ηp和特征速度的角速度。旋转液柱,ω。这项研究首次表明,不平衡压力的引入会在漏斗形旋转流体柱顶部形成一个独立的停滞平面,这与飓风,龙卷风和尘埃的观测数据一致。还已经表明,在没有非平衡压力的情况下,不能观察到旋转流动的停滞平面。然后将由于引入了非平衡压力效应而产生的速度和压力分布与龙卷风和尘土魔鬼的可用观测数据进行了比较。发现速度和压力分布的一般曲线与物理测量值非常吻合,在没有非平衡压力效应的情况下,如果不引入经验湍流效应就不可能实现。

著录项

  • 作者

    Zardadkhan, Irfan Rashid.;

  • 作者单位

    Old Dominion University.;

  • 授予单位 Old Dominion University.;
  • 学科 Engineering Geophysical.;Engineering Mechanical.;Engineering Aerospace.
  • 学位 Ph.D.
  • 年度 2012
  • 页码 92 p.
  • 总页数 92
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 古生物学;
  • 关键词

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