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{{AFC submission|t||ts=20150225183353|u=Faportela|ns=118}} <!--- Important, do not remove this line before article has been created. --->
{{AFC submission|t||ts=20150225183353|u=Faportela|ns=118}} <!--- Important, do not remove this line before article has been created. --->


'''Multiscale turbulence''' is a class of [[Turbulence | turbulent]] flows in which the chaotic motion of the [[Fluid|fluid]] is forced at different length and/or time scales<ref>{{cite journal|last1=Laizet|first1=S.|last2=Vassilicos|first2=J. C.|title=Multiscale Generation of Turbulence|journal=Journal of Multiscale Modelling|date=January 2009|volume=01|issue=01|pages=177–196|doi=10.1142/S1756973709000098}}</ref>. This is usually achieved by immersing in a moving fluid a body with a multiscale, often [[Fractal|fractal]]-like, arrangement of length scales. This arrangement of scales can be either passive<ref>{{cite journal|last1=Hurst|first1=D.|last2=Vassilicos|first2=J. C.|title=Scalings and decay of fractal-generated turbulence|journal=Physics of Fluids|date=2007|volume=19|issue=3|pages=035103|doi=10.1063/1.2676448}}</ref> or [[Automatic control|active]]<ref>{{cite journal|last1=Thormann|first1=A.|last2=Meneveau|first2=C.|title=Decay of homogeneous, nearly isotropic turbulence behind active fractal grids|journal=Physics of Fluids|date=February 2014|volume=26|issue=2|pages=025112|doi=10.1063/1.4865232}}</ref>.
'''Multiscale turbulence''' is a class of [[Turbulence | turbulent]] flows in which the chaotic motion of the [[Fluid|fluid]] is forced at different length and/or time scales<ref>{{cite journal|last1=Laizet|first1=S.|last2=Vassilicos|first2=J. C.|title=Multiscale Generation of Turbulence|journal=Journal of Multiscale Modelling|date=January 2009|volume=01|issue=01|pages=177–196|doi=10.1142/S1756973709000098}}</ref>. This is usually achieved by immersing in a moving fluid a body with a multiscale, often [[Fractal|fractal]]-like, arrangement of length scales. This arrangement of scales can be either passive<ref>{{cite journal|last1=Hurst|first1=D.|last2=Vassilicos|first2=J. C.|title=Scalings and decay of fractal-generated turbulence|journal=Physics of Fluids|date=2007|volume=19|issue=3|pages=035103|doi=10.1063/1.2676448}}</ref><ref>{{cite journal|last1=Nagata|first1=K.|last2=Sakai|first2=Y.|last3=Inaba|first3=T.|last4=Suzuki|first4=H.|last5=Terashima|first5=O.|last6=Suzuki|first6=H.|title=Turbulence structure and turbulence kinetic energy transport in multiscale/fractal-generated turbulence|journal=Physics of Fluids|date=2013|volume=25|issue=6|pages=065102|doi=10.1063/1.4811402}}</ref> or [[Automatic control|active]]<ref>{{cite journal|last1=Thormann|first1=A.|last2=Meneveau|first2=C.|title=Decay of homogeneous, nearly isotropic turbulence behind active fractal grids|journal=Physics of Fluids|date=February 2014|volume=26|issue=2|pages=025112|doi=10.1063/1.4865232}}</ref>.


<!---the obstacle may have a specific arrangement of length scales<ref>Queiros-Conde, D., and J. C. Vassilicos. "Turbulent wakes of 3D fractal grids." Intermittency in turbulent flows (2001): 136-167.</ref> or have it's geometry actively changed<ref>{{cite journal|last1=Hideharu|first1=M.|title=Realization of a large-scale turbulence field in a small wind tunnel|journal=Fluid Dynamics Research|date=October 1991|volume=8|issue=1-4|pages=53–64|doi=10.1016/0169-5983(91)90030-M}}</ref> by some [[Control system | control system]] ({{YouTube| id= CU8qg9Jo8o4 | title= as illustrated }}).--->
<!---the obstacle may have a specific arrangement of length scales<ref>Queiros-Conde, D., and J. C. Vassilicos. "Turbulent wakes of 3D fractal grids." Intermittency in turbulent flows (2001): 136-167.</ref> or have it's geometry actively changed<ref>{{cite journal|last1=Hideharu|first1=M.|title=Realization of a large-scale turbulence field in a small wind tunnel|journal=Fluid Dynamics Research|date=October 1991|volume=8|issue=1-4|pages=53–64|doi=10.1016/0169-5983(91)90030-M}}</ref> by some [[Control system | control system]] ({{YouTube| id= CU8qg9Jo8o4 | title= as illustrated }}).--->
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<math>\epsilon = C_\epsilon \frac{\mathcal{U}^3}{\mathcal{L}}</math>
<math>\epsilon = C_\epsilon \frac{\mathcal{U}^3}{\mathcal{L}}</math>


is not constant, as required by the [[Lewis Fry Richardson|Richardson]]-[[Andrey Kolmogorov|Kolmogorov]] [[Energy cascade|energy cascade]]. This new [[Scientific law|law]]<ref name="DissipationJCV15"/> can be expressed as <math>C_\epsilon \propto \frac{Re_I^m}{Re_L^n}</math>, with <math>m \approx n</math>, where <math>Re_I</math> and <math>Re_L</math> are respectively [[Reynolds number|Reynolds numbers]] based on initial (such as [[Freestream|free-stream velocity]] and the object's [[Length scale|length scale]]) and local conditions (such as the [[Root mean square|rms]] velocity and integral length scale). This new [[dissipation]] law characterises non-equilibrium turbulence apparently universally in various flows and results from non-equilibrium unsteady [[energy cascade]]. This imbalance implies that new mean flow scalings exist for free shear turbulent flows<ref name="DissipationJCV15"/>.
is not constant, as required by the [[Lewis Fry Richardson|Richardson]]-[[Andrey Kolmogorov|Kolmogorov]] [[Energy cascade|energy cascade]]. This new [[Scientific law|law]]<ref name="DissipationJCV15"/> can be expressed as <math>C_\epsilon \propto \frac{Re_I^m}{Re_L^n}</math>, with <math>m \approx 1 \approx n</math>, where <math>Re_I</math> and <math>Re_L</math> are [[Reynolds number|Reynolds numbers]] based, respectively, on initial/global conditions (such as [[Freestream|free-stream velocity]] and the object's [[Length scale|length scale]]) and local conditions (such as the [[Root mean square|rms]] velocity and integral length scale). This new [[dissipation]] law characterises non-equilibrium turbulence apparently universally in various flows and results from non-equilibrium unsteady [[energy cascade]]. This imbalance implies that new mean flow scalings exist for free shear turbulent flows<ref name="DissipationJCV15"/>.


<!---The region of the flow where this new law holds is termed non-equilibrium [[turbulence]] as it implies an imbalance between the [[Turbulence kinetic energy|energy]] fed down the [[Energy cascade|cascade]] by the large ([[Turbulence kinetic energy|energy]] containing) scales and that which is [[Dissipation |dissipated]] (at the [[Kolmogorov microscales|smallest scales]]).--->
<!---The region of the flow where this new law holds is termed non-equilibrium [[turbulence]] as it implies an imbalance between the [[Turbulence kinetic energy|energy]] fed down the [[Energy cascade|cascade]] by the large ([[Turbulence kinetic energy|energy]] containing) scales and that which is [[Dissipation |dissipated]] (at the [[Kolmogorov microscales|smallest scales]]).--->

Revision as of 17:21, 1 March 2015

Multiscale turbulence is a class of turbulent flows in which the chaotic motion of the fluid is forced at different length and/or time scales[1]. This is usually achieved by immersing in a moving fluid a body with a multiscale, often fractal-like, arrangement of length scales. This arrangement of scales can be either passive[2][3] or active[4].


Three examples of multiscale turbulence generators. From left to right, a fractal cross grid, a fractal square grid and a fractal I grid. See on YouTube the manufacturing of a fractal grid.

As turbulent flows contain eddies with a wide range of scales, exciting the turbulence at particular scales (or range of scales) allows one to fine-tune the properties of that flow. Multiscale turbulent flows have been successfully applied in different fields[5], such as reducing acoustic noise from wings by modifying the geometry of spoilers[6], enhancing heat transfer from impinging jets passing through grids[7], reducing the vortex shedding intensity of flows past normal plates without changing the shedding frequency[8], enhancing mixing by energy-efficient stirring[9], improving flow metering and flow conditioning in pipes[10] and improving combustion[11]. In 2013 the EU awarded a Marie Curie grant of 3.8M Euros for research and training of 13 young scientists and engineers in multiscale turbulence in order to further explore and apply the properties of these flows[12][13].

Multiscale turbulence has also played an important role into probing the internal structure of turbulence[14]. This sort of turbulence allowed researchers to unveil a novel dissipation law in which the parameter in

is not constant, as required by the Richardson-Kolmogorov energy cascade. This new law[14] can be expressed as , with , where and are Reynolds numbers based, respectively, on initial/global conditions (such as free-stream velocity and the object's length scale) and local conditions (such as the rms velocity and integral length scale). This new dissipation law characterises non-equilibrium turbulence apparently universally in various flows and results from non-equilibrium unsteady energy cascade. This imbalance implies that new mean flow scalings exist for free shear turbulent flows[14].





References

  1. ^ Laizet, S.; Vassilicos, J. C. (January 2009). "Multiscale Generation of Turbulence". Journal of Multiscale Modelling. 01 (01): 177–196. doi:10.1142/S1756973709000098.
  2. ^ Hurst, D.; Vassilicos, J. C. (2007). "Scalings and decay of fractal-generated turbulence". Physics of Fluids. 19 (3): 035103. doi:10.1063/1.2676448.
  3. ^ Nagata, K.; Sakai, Y.; Inaba, T.; Suzuki, H.; Terashima, O.; Suzuki, H. (2013). "Turbulence structure and turbulence kinetic energy transport in multiscale/fractal-generated turbulence". Physics of Fluids. 25 (6): 065102. doi:10.1063/1.4811402.
  4. ^ Thormann, A.; Meneveau, C. (February 2014). "Decay of homogeneous, nearly isotropic turbulence behind active fractal grids". Physics of Fluids. 26 (2): 025112. doi:10.1063/1.4865232.
  5. ^ Laizet, S.; Sakai, Y.; Vassilicos, J. C. (1 December 2013). "Special issue of selected papers from the second UK–Japan bilateral Workshop and First ERCOFTAC Workshop on Turbulent Flows Generated/Designed in Multiscale/Fractal Ways, London, March 2012". Fluid Dynamics Research. 45 (6): 061001. doi:10.1088/0169-5983/45/6/061001.
  6. ^ Nedić, J., B. Ganapathisubramani, J. C. Vassilicos, J. Boree, L. E. Brizzi, A. Spohn. "Aeroacoustic performance of fractal spoilers". AIAA journal 2012.
  7. ^ Cafiero, G.; Discetti, S.; Astarita, T. (August 2014). "Heat transfer enhancement of impinging jets with fractal-generated turbulence". International Journal of Heat and Mass Transfer. 75: 173–183. doi:10.1016/j.ijheatmasstransfer.2014.03.049.
  8. ^ Nedić, J.; Ganapathisubramani, B.; Vassilicos, J. C. (1 December 2013). "Drag and near wake characteristics of flat plates normal to the flow with fractal edge geometries". Fluid Dynamics Research. 45 (6): 061406. doi:10.1088/0169-5983/45/6/061406.
  9. ^ Laizet, S.; Vassilicos, J. C. (23 December 2014). "Stirring and scalar transfer by grid-generated turbulence in the presence of a mean scalar gradient". Journal of Fluid Mechanics. 764: 52–75. doi:10.1017/jfm.2014.695. {{cite journal}}: no-break space character in |first2= at position 3 (help)
  10. ^ Manshoor, B.; Nicolleau, F. C. G. A.; Beck, S. B. M. (June 2011). "The fractal flow conditioner for orifice plate flow meters". Flow Measurement and Instrumentation. 22 (3): 208–214. doi:10.1016/j.flowmeasinst.2011.02.003.
  11. ^ Goh, K. H. H.; Geipel, P.; Lindstedt, R. P. (September 2014). "Lean premixed opposed jet flames in fractal grid generated multiscale turbulence". Combustion and Flame. 161 (9): 2419–2434. doi:10.1016/j.combustflame.2014.03.010.
  12. ^ "Multisolve". Retrieved 25 February 2015.
  13. ^ "Multisolve Marie Curie grant".
  14. ^ a b c Vassilicos, J. C. (2015). "Dissipation in Turbulent Flows". Annual Review of Fluid Mechanics: 95-114. doi:10.1146/annurev-fluid-010814-014637.
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