scholarly journals Stochastic algorithm for generation of a divergence-free anisotropic homogeneous turbulent velocity fluctuation field

2020 ◽  
pp. 1-17
Author(s):  
Anatoly Vitalievich Alexandrov ◽  
Ludwig Waclawovich Dorodincyn ◽  
Dmitriy Romanovich Kolyukhin
2020 ◽  
pp. 1-18
Author(s):  
Anatoly Vitalievich Alexandrov ◽  
Ludwig Waclawovich Dorodincyn ◽  
Alexey Petrovich Duben ◽  
Dmitriy Romanovich Kolyukhin

Author(s):  
Yuichi Kaiho ◽  
Shumpei Hara ◽  
Takahiro Tsukahara ◽  
Yasuo Kawaguchi

It is known as the Toms effect that the wall friction coefficient is reduced by adding a small amount of polymer or surfactant into a water flow. In the drag-reducing flow, it is expected that a time scale of turbulent velocity fluctuation is changed by relaxation time due to viscoelasticity. In the present study, experimental analysis of the turbulent velocity fluctuation was performed with temporal characteristics in surfactant solution flow. The velocity fluctuations were measured by using a two-component laser Doppler velocimeter system on turbulent channel flow. And then, we performed statistical operation on those data and examined the time scale. From spectra analysis, it was found that very low frequency velocity fluctuations existed near the wall region in the surfactant solution flow. It was also revealed that the strong anisotropy occurred not only with the intensity but also with frequency distribution in turbulent velocity fluctuations. Moreover, the turbulence contributes nothing to the Reynolds shear stress and behaves as a wave motion. It was concluded that the turbulent eddies and viscoelasticity were two factors contributing to turbulent generation in the viscoelastic turbulent flow, with each factor having its own time scale.


1999 ◽  
Vol 55 (3) ◽  
pp. 143-148
Author(s):  
Kiyomi Sugai ◽  
Kouichi Sano ◽  
Mutsuo Kobayashi ◽  
Koji Matsubara ◽  
Tsuyoshi Takano ◽  
...  

2002 ◽  
Vol 9 (1) ◽  
pp. 11-23 ◽  
Author(s):  
D. M. Summers

Abstract. An impulse-based model is developed to represent a coupling between turbulent flow in the atmosphere and turbulent flow in the ocean. In particular, it is argued that the atmosphere flowing horizontally over the ocean surface generates a velocity fluctuation field in the latter's near-surface flow. The mechanism for this can be understood kinematically in terms of an exchange of tangentially-oriented fluid impulse at the air-sea interface. We represent this exchange numerically through the creation of Lagrangian elements of impulse density. An indication of the efficacy of such a model would lie in its ability to predict the observed fractal dimension of lateral trajectories of submerged floats set adrift in the ocean. To this end, we examine the geometry of lateral tracer-paths determined from the present model.


Sign in / Sign up

Export Citation Format

Share Document