Self-similar turbulence evolution and the dissipation rate transport equation
Self-similar turbulence evolution and the dissipation rate transport equation
复制标题
自相似湍流演化与耗散率输运方程
DOI:
10.1063/1.2046707
复制
发表时间:
2005
影响因子:
4.6
通讯作者:
T. Clark
中科院分区:
文献类型:
--
作者:
R. Rubinstein;T. Clark
The dissipation rate transport equation is analyzed in the setting of time-dependent isotropic turbulence driven by a statistically unsteady force. In the limit of slow spectral variation, the balance between vortex stretching and enstrophy destruction postulated by Tennekes and Lumley [A First Course in Turbulence (MIT Press, Cambridge, MA, 1972)] is verified and spectral closure is used to identify the O(Re0) difference between them; however, no definite formulation of an ϵ-equation results. The ϵ equation is usually calibrated to predict self-similar unit flows such as decaying turbulence and homogeneous shear flow. The limitations of this approach are shown by constructing classes of self-similar states of forced isotropic turbulence. Any choice of constants in the ϵ equation yields a model that is consistent with some self-similar states, but not with all possible states: two-equation models of the standard form select a class of admissible self-similar states and rule out the others.