scholarly journals Data-driven CFD modeling of turbulent flows through complex structures

2016 ◽  
Vol 62 ◽  
pp. 138-149 ◽  
Author(s):  
Jian-Xun Wang ◽  
Heng Xiao
2020 ◽  
Vol 129 ◽  
pp. 103286
Author(s):  
Zhong Yi Wan ◽  
Petr Karnakov ◽  
Petros Koumoutsakos ◽  
Themistoklis P. Sapsis

Author(s):  
Ricardo Vinuesa ◽  
Oriol Lehmkuhl ◽  
Adrian Lozano-Duran ◽  
Jean Rabault

In this review we summarize existing trends of flow control used to improve the aerodynamic efficiency of wings. We first discuss active methods to control turbulence, starting with flat-plate geometries and building towards the more complicated flow around wings. Then, we discuss active approaches to control separation, a crucial aspect towards achieving high aerodynamic efficiency. Furthermore, we highlight methods relying on turbulence simulation, and discuss various levels of modelling. Finally, we thoroughly revise data-driven methods, their application to flow control, and focus on deep reinforcement learning (DRL). We conclude that this methodology has the potential to discover novel control strategies in complex turbulent flows of aerodynamic relevance.


2016 ◽  
Vol 4 (2) ◽  
pp. 391-405 ◽  
Author(s):  
Jon D. Pelletier ◽  
Jason P. Field

Abstract. The fully rough form of the law of the wall is commonly used to quantify velocity profiles and associated bed shear stresses in fluvial, aeolian, and coastal environments. A key parameter in this law is the roughness length, z0. Here we propose a predictive formula for z0 that uses the amplitude and slope of each wavelength of microtopography within a discrete-Fourier-transform-based approach. Computational fluid dynamics (CFD) modeling is used to quantify the effective z0 value of sinusoidal microtopography as a function of the amplitude and slope. The effective z0 value of landscapes with multi-scale roughness is then given by the sum of contributions from each Fourier mode of the microtopography. Predictions of the equation are tested against z0 values measured in  ∼ 105 wind-velocity profiles from southwestern US playa surfaces. Our equation is capable of predicting z0 values to 50 % accuracy, on average, across a 4 order of magnitude range. We also use our results to provide an alternative formula that, while somewhat less accurate than the one obtained from a full multi-scale analysis, has an advantage of being simpler and easier to apply.


2021 ◽  
Vol 11 (1) ◽  
Author(s):  
Omstavan Samant ◽  
Jaya Kumar Alageshan ◽  
Sarveshwar Sharma ◽  
Animesh Kuley

AbstractInertial particles advected by a background flow can show complex structures. We consider inertial particles in a 2D Taylor–Green (TG) flow and characterize particle dynamics as a function of the particle’s Stokes number using dynamic mode decomposition (DMD) method from particle image velocimetry (PIV) like-data. We observe the formation of caustic structures and analyze them using DMD to (a) determine the Stokes number of the particles, and (b) estimate the particle Stokes number composition. Our analysis in this idealized flow will provide useful insight to analyze inertial particles in more complex or turbulent flows. We propose that the DMD technique can be used to perform similar analysis on an experimental system.


2020 ◽  
Vol 416 ◽  
pp. 109513 ◽  
Author(s):  
Saddam Hijazi ◽  
Giovanni Stabile ◽  
Andrea Mola ◽  
Gianluigi Rozza

Kerntechnik ◽  
2013 ◽  
Vol 78 (1) ◽  
pp. 68-71
Author(s):  
C. Lifante ◽  
B. Krull ◽  
T. Frank ◽  
R. Franz ◽  
U. Hampel

2015 ◽  
Vol 3 (4) ◽  
pp. 1107-1142
Author(s):  
J. D. Pelletier ◽  
J. P. Field

Abstract. The fully rough form of the law of the wall is commonly used to quantify velocity profiles and associated bed shear stresses in fluvial, aeolian, and coastal environments. A key parameter in this law is the roughness length, z0. Here we propose a predictive formula for z0 that uses the amplitude and slope of each wavelength of microtopography within a discrete-Fourier-transform-based approach. Computational fluid dynamics (CFD) modeling is used to quantify the effective z0 value of sinusoidal microtopography as a function of the amplitude and slope. The effective z0 value of landscapes with multi-scale roughness is then given by the sum of contributions from each Fourier mode of the microtopography. Predictions of the equation are tested against z0 values measured in ~105 wind velocity profiles from southwestern US playa surfaces. Our equation is capable of predicting z0 values to 50 % accuracy, on average, across a four order-of-magnitude range.


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