Kolmogorov microscales: Difference between revisions
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In his 1941 theory, [[A. N. Kolmogorov]] introduced the idea that the smallest scales of [[turbulence]] are universal (similar for every [[turbulent flow]]) and that they depend only on <math>\epsilon</math> and <math>\nu</math>. The definitions of the Kolmogorov microscales can be obtained using this idea and [[dimensional analysis]]. Since the dimension of kinematic viscosity is length<sup>2</sup>/time, and the dimension of the [[energy dissipation]] rate per unit mass is length<sup>2</sup>/time<sup>3</sup>, the only combination that has the dimension of time is <math> \tau_\eta=(\nu / \epsilon)^{1/2}</math> which is the Kolmorogov time scale. Similarly, the Kolmogorov length scale is the only combination of <math>\epsilon</math> and <math>\nu</math> that has dimension of length. |
In his 1941 theory, [[A. N. Kolmogorov]] introduced the idea that the smallest scales of [[turbulence]] are universal (similar for every [[turbulent flow]]) and that they depend only on <math>\epsilon</math> and <math>\nu</math>. The definitions of the Kolmogorov microscales can be obtained using this idea and [[dimensional analysis]]. Since the dimension of kinematic viscosity is length<sup>2</sup>/time, and the dimension of the [[energy dissipation]] rate per unit mass is length<sup>2</sup>/time<sup>3</sup>, the only combination that has the dimension of time is <math> \tau_\eta=(\nu / \epsilon)^{1/2}</math> which is the Kolmorogov time scale. Similarly, the Kolmogorov length scale is the only combination of <math>\epsilon</math> and <math>\nu</math> that has dimension of length. |
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The Kolmogorov 1941 theory is a [[mean field theory]] since it assumes that the relevant dynamical parameter is the mean energy dissipation rate. In [[fluid turbulence]], the energy dissipation rate fluctuates in space and time, so it is possible to think of the microscales as quantities that also vary in space and time. However, standard practice is to use mean field values since they represent the typical values of the smallest scales in a given flow. |
The Kolmogorov 1941 theory is a [[mean field theory]] since it assumes that the relevant dynamical parameter is the mean energy dissipation rate. In [[fluid turbulence]], the energy dissipation rate fluctuates in space and time, so it is possible to think of the microscales as quantities that also vary in space and time. However, standard practice is to use the mean field values since they represent the typical values of the smallest scales in a given flow. |
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==See also== |
==See also== |
Revision as of 22:59, 29 December 2010
Kolmogorov microscales are the smallest scales in turbulent flow. They are defined[1] by
Kolmogorov length scale | |
Kolmogorov time scale | |
Kolmogorov velocity scale |
where is the average rate of energy dissipation per unit mass, and is the kinematic viscosity of the fluid.
In his 1941 theory, A. N. Kolmogorov introduced the idea that the smallest scales of turbulence are universal (similar for every turbulent flow) and that they depend only on and . The definitions of the Kolmogorov microscales can be obtained using this idea and dimensional analysis. Since the dimension of kinematic viscosity is length2/time, and the dimension of the energy dissipation rate per unit mass is length2/time3, the only combination that has the dimension of time is which is the Kolmorogov time scale. Similarly, the Kolmogorov length scale is the only combination of and that has dimension of length.
The Kolmogorov 1941 theory is a mean field theory since it assumes that the relevant dynamical parameter is the mean energy dissipation rate. In fluid turbulence, the energy dissipation rate fluctuates in space and time, so it is possible to think of the microscales as quantities that also vary in space and time. However, standard practice is to use the mean field values since they represent the typical values of the smallest scales in a given flow.
See also
References
- ^ Landahl, M.T. & E. Mollo-Christensen. Turbulence and Random Processes in Fluid Mechanics. Cambridge, 2ed, 1992.