Bounds on dissipation for Navier-Stokes flow with Kolmogorov forcing

被引:25
作者
Childress, S
Kerswell, RR
Gilbert, AD
机构
[1] NYU, Courant Inst Math Sci, New York, NY 10012 USA
[2] Univ Bristol, Dept Math, Bristol BS8 1TW, Avon, England
[3] Univ Exeter, Sch Math Sci, Exeter EX4 4QE, Devon, England
来源
PHYSICA D | 2001年 / 158卷 / 1-4期
关键词
Kolmogorov flow; dissipation; bounds; Navier-Stokes; forcing;
D O I
10.1016/S0167-2789(01)00320-7
中图分类号
O29 [应用数学];
学科分类号
070104 ;
摘要
In this paper, bounds on average viscous dissipation are derived for Kolmogorov flow in a spatially periodic domain with steady and unsteady forcing, at arbitrarily large Grash of number G. For a force of the form F-0 sin mzi or F-0 sin mz cos omega ti, we derive various bounds on the total dissipation in the flow, D-u,, as well as on the dissipation D-m obtained from the x-velocity averaged over the x, y plane (the mean velocity of the flow). We derive upper bounds on D-u and D-v = D-u - D-m, as well as lower bounds on D-m and D-m /D-u, adopting constraints of the kind introduced by Howard and Busse and assuming a steady force. The background flow method introduced by Doering and Constantin is used to obtain an improved lower bound on D-m/D-u of O(G(-1)), and a lower bound on D-u, of O(G(-1/2)) where G := F0L3/nu (2) is the Grashof number. Some of these results are then generalized to time-periodic forcing. Direct numerical simulation of the flow indicates that these bounds leave substantial gaps at large Grashof number G, the calculated D-m (G) and D-u (G) being 0 (G(-1/2)) and O(1), respectively, as G --> infinity. Our theoretical bounds on D-m, D-u are shown to be attained by steady laminar-type flows for neighboring forcing functions, which seems to indicate that these bounds cannot be improved by adding further dynamical constraints. However, our elementary upper bound on D-v can probably be improved by placing more constraints on the flows. These results serve to emphasize the difference between boundary-driven turbulence and body-force driven turbulence where the appropriate dissipation bound is believed saturated at least up to logarithms. (C) 2001 Elsevier Science B.V. All rights reserved.
引用
收藏
页码:105 / 128
页数:24
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