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The effects of plasma turbulence are extremely important; for example, turbulent diffusion and transport represent a fundamental limitation on the ability to confine energy within plasma.
This spurious high turbulent intensity in turn causes (i) a high turbulent viscosity to be applied, wrongly stabilizing the jet, and (ii) increased turbulent diffusion of heat, causing too deep and diffuse a stratification to be predicted.
Possible reasons for this are different turbulence modelling approaches with different terms for the turbulent diffusion and rapid pressure strain terms.
Turbulent diffusion, a third-order parameter, was also mentioned in several turbulence researches (da Silva et al. 2014; Elder 1959; Jones and Whitelaw 1982; McComb 1990; Reeks 2014; Taylor 1954).
The design used minimizes particle interference and turbulent diffusion.
There, we are assuming that there is no molecular diffusion and turbulent diffusion of pollutants.
In marine ecosystems, turbulent diffusion can also cause the movement of plankton.
The important mechanism transporting substances in the surface layer of the atmosphere is turbulent diffusion.
The key process considered herein is momentum transfer to the particles with emphasis on turbulent diffusion.
The intensity of turbulent transport is characterized by the turbulent diffusion coefficient.
Results highlight the importance of including turbulent diffusion in the network solution.
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