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首页> 外文期刊>Journal of Fluid Mechanics >Vanishing enstrophy dissipation in two-dimensional Navier-Stokes turbulence in the inviscid limit
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Vanishing enstrophy dissipation in two-dimensional Navier-Stokes turbulence in the inviscid limit

机译:在无粘性极限内二维Navier-Stokes湍流中消失的涡旋消散

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摘要

Batchelor (Phys. Fluids, vol. 12, 1969, p. 233) developed a theory of two-dimensional turbulence based on the assumption that the dissipation of enstrophy (mean-square vorticity) tends to a finite non-zero constant in the limit of infinite Reynolds number Re. Here, by assuming power-law spectra, including the one predicted by Batchelor's theory, we prove that the maximum dissipation of enstrophy is in fact zero in this limit. Specifically, as Re -> infinity, the dissipation approaches zero no slower than (ln Re)(-1/2). The physical reason behind this result is that the decrease of viscosity enhances the production of both palinstrophy (mean-square vorticity gradients) and its dissipation - but in such a way that the net growth of palinstrophy is less rapid than the decrease of viscosity, resulting in vanishing enstrophy dissipation. This result generalizes to a rich class of quasi-geostrophic models as well as to the case of a passive tracer in layerwise-two-dimensional turbulent flows having bounded enstrophy.
机译:Batchelor(Phys.Fluids,vol.12,1969,p.233)建立了二维湍流理论,其假设是涡旋的耗散(均方涡度)趋于在极限内为有限的非零常数雷诺数Re的无穷大。在这里,通过假设幂律谱(包括Batchelor理论预测的谱),我们证明了在此极限内,最大涡旋消散实际上为零。具体来说,当Re→无限时,耗散接近于零,且不慢于(ln Re)(-1/2)。该结果背后的物理原因是,粘度的降低会增强回旋质素的产生(均方涡度梯度)及其消散-但以回旋质素的净增长速度不如回旋而降低。在消失的回旋消散中。该结果推广到一类丰富的准地转模型,并且推广到被动二维示踪剂在层状二维湍流中具有有限回旋的情况。

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