Dissipation of Energy in Isotropic Turbulence

Author(s):  
V. M. Tikhomirov

The statistical theory of turbulence, initiated by Taylor (1935) and v. Kármán & Howarth (1938), has recently been developed so far that a satisfactory explanation of the spectral distribution of energy among the turbulent eddies can be given. In fact Kolmogoroff (1941 a, b ) and independently Onsager (1945) and v. Weizsaecker (1948) have introduced a similarity hypothesis, which allows a determination of the spectrum for eddies with large Reynolds numbers, and the author (Heisenberg 1948) has extended these calculations to include those frequency components which have small Reynolds numbers. Since the distribution of energy among the largest eddies must be a geometrical and not a statistical problem, one may say that the statistical part of the spectrum is now well understood. Recently Batchelor & Townsend (1947, 1948 a, b ) have studied the decay of turbulent motion caused by a mesh grating in a wind tunnel, and the following discussions will apply the statis­tical theory to this problem. For the calculations the notation of Heisenberg (1948) will be used. If pF(k)dk denotes the energy contained between the wave numbers k and k + dk , the following equation for the dissipation of energy was given (Heisenberg 1948, equation (13)): S k = { μ + pk ∫( F ( k '') / k '' 3 ) dk " } ∫ k 0 2 F ( k ') k ' 2 dk '.


The connexion between the statistical representation of turbulence and dissipation of energy has been discussed in relation to the decay of the isotropic turbulence which is produced in a wind tunnel by means of regular grids. It was shown that a length λ can be defined which may be taken as a measure of the scale of the small eddies which are responsible for dissipation. This λ can be found by measuring the correlation R y between the indications of two hot wire anemometers set at a distance y apart on a line perpendicular to the axis of the tunnel. Then 1/ λ 2 = Lt y→0 1 - R y / y 2 , and the mean rate of dissipation of energy per unit volume is W ¯ = 15 μ u 2 ¯ / λ 2 , (1) where u 2 ¯ is the mean of the square of one component of velocity. When turbulence is generated in a wind stream by a grid of regularly spaced bars it may be expected to possess a definite scale proportional to the linear dimensions of the grid. In any complete statistical description of turbulence this scale must be implicitly or explicitly involved. One way in which the scale can be defined is to measure the distance y apart by which the two hot wires must be separated before the correlation between the indications disappears. Another way is to define the scale as l 2 = ∫ 0 y R y d y . (2)


In my note (Kolmogorov 1941 a ) I defined the notion of local isotropy and introduced the quantities B d d ( r ) = [ u d ( M ′ ) − u d ( M ) ] 2 , ¯ [ u n ( M ′ ) − u n ( M ) ¯ ] 2 , where r denotes the distance between the points M and M' , u d (M) and u d (M') are the velocity components in the direction MM' ¯¯ at the points M and M' , and u n (M) and u n (M') are the velocity components at the points M and M' in some direction, perpendicular to MM' .


1938 ◽  
Vol 34 (4) ◽  
pp. 534-539
Author(s):  
A. E. Green

1. Taylor has shown (1) that two characteristic lengthsλ and λη may be defined for turbulent fluid motion. The length λ, which is connected with the dissipation of energy, is, for isotropic turbulence, given bywhere is the mean rate of dissipation of energy per unit volume and represents the mean square value of any component of velocity. The length λη can be defined in terms of thuswhere For isotropic turbulence Taylor assumed thatwhere B is a constant. Since the turbulence is isotropic,and so, from (1), (2), (3) and (4) we have


AIAA Journal ◽  
1999 ◽  
Vol 37 ◽  
pp. 1420-1425
Author(s):  
Farzad Mashayek
Keyword(s):  

2019 ◽  
Vol 4 (10) ◽  
Author(s):  
Mohamad Ibrahim Cheikh ◽  
James Chen ◽  
Mingjun Wei

2020 ◽  
Vol 5 (2) ◽  
Author(s):  
Richard D. J. G. Ho ◽  
Andres Armua ◽  
Arjun Berera

Sign in / Sign up

Export Citation Format

Share Document