Diffusion of Particles in Fully-Developed Turbulence
Open Access
- 1 August 1982
- journal article
- Published by Oxford University Press (OUP) in Progress of Theoretical Physics
- Vol. 68 (2) , 439-447
- https://doi.org/10.1143/PTP.68.439
Abstract
The relative diffusion of a pair of dye particles in homogeneous steady turbulence is studied from the viewpoint that the turbulent transport is due to the vortex stretching of eddies in the inertial range. Thus, with the aid of Mori's (1980) formula for the vortex stretching, it is shown that the eddy diffusion rate is given by dL*2/ dt=AL*(4+2 µ)/ 3 with A=\hatAε1/ 3L-2 µ/ 3, where L*2(t) is the mean square of the relative distance of the pair at time t, ε the mean rate of the energy transfer from large eddies to small eddies, L the length scale of the production range and µ the intermittency exponent. It turns out that \hatA \fallingdotseq1.39 for µ=0 and 1.22 for µ=1/ 3, where Kolmogorov's constant is taken to be 1.5. This diffusion law is valid for L>L*(t) ≫ld, where ld is the length scale of the dissipation range. Hence it turns out that Richardson's (1926) empirical 4/ 3 law holds if µ is very small. If L*(t) ≫L*(0), then L*2(t) ∼t3/ (1-µ). Therefore, if 0.25 ≲µ≲0.5 as experiments indicate, then the intermittency correction leads to an appreciable deviation from the t3 law. The condition L*(t)≪L is written as t≪tL, where L*(tL)=L and the upper limit of tL is given by \hattL ≡tL/ (L2/ ε)1/ 3 \fallingdotseq2.16 for µ=0 and 3.68 for µ=1/ 3 in the limit L*(0)/ L →0.Keywords
This publication has 1 reference indexed in Scilit:
- Atmospheric diffusion shown on a distance-neighbour graphProceedings of the Royal Society of London. Series A, Containing Papers of a Mathematical and Physical Character, 1926