Lennart  Löfdahl

Prof. Dr. Lennart Löfdahl

Department of Mechanics and Maritime Sciences, Chalmers University of Technology, 41296 Gothenburg, Sweden

Research Focus & Metrics

Academic Career Length

45Years (1982-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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1 December 2000 in Journal of Fluid Mechanics
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WGWilliam K. George
William K. George
HAHans Abrahamsson
Hans Abrahamsson
JEJan Eriksson
Jan Eriksson
RKRolf I. Karlsson
Rolf I. Karlsson
LLLennart Löfdahl
Lennart Löfdahl
MWMartin Wosnik
Martin Wosnik
A new theory for the turbulent plane wall jet without external stream is proposed based on a similarity analysis of the governing equations. The asymptotic invariance principle (AIP) is used to require that properly scaled profiles reduce to similarity solutions of the inner and outer equations separately in the limit of infinite Reynolds number. Application to the inner equations shows that the appropriate velocity scale is the friction velocity, u∗, and the length scale is v/u∗. For finite Reynolds numbers, the profiles retain a dependence on the length-scale ratio, y+1/2 = u∗y1/2/v, where y1/2 is the distance from the wall at which the mean velocity has dropped to 1/2 its maximum value. In the limit as y+1/2 → ∞, the familiar law of the wall is obtained. Application of the AIP to the outer equations shows the appropriate velocity scale to be Um, the velocity maximum, and the length scale y1/2; but again the profiles retain a dependence on y+1/2 for finite values of it. The Reynolds shear stress in the outer layer scales with u2*, while the normal stresses scale with U2m. Also Um ∼ yn1/2 where n < −1/2 and must be determined from the data. The theory cannot rule out the possibility that the outer flow may retain a dependence on the source conditions, even asymptotically.The fact that both these profiles describe the entire wall jet for finite values of y+1/2, but reduce to inner and outer profiles in the limit, is used to determine their functional forms in the ‘overlap’ region which both retain. The result from near asymptotics is that the velocity profiles in the overlap region must be power laws, but with parameters which depend on Reynolds number y+1/2 and are only asymptotically constant. The theoretical friction law is also a power law depending on the velocity parameters. As a consequence, the asymptotic plane wall jet cannot grow linearly, although the difference from linear growth is small.It is hypothesized that the inner part of the wall jet and the inner part of the zero-pressure-gradient boundary layer are the same. It follows immediately that all of the wall jet and boundary layer parameters should be the same, except for two in the outer flow which can differ only by a constant scale factor. The theory is shown to be in excellent agreement with the experimental data which show that source conditions may determine uniquely the asymptotic state achieved. Surprisingly, only a single parameter, B1 = (Umv/Mo)/ (y+1/2Mo/v2)n = constant where n ≈ −0.528, appears to be required to determine the entire flow for a given source.

23 July 1999 in Measurement Science and Technology
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LLLennart Löfdahl
Lennart Löfdahl
MGMohamed Gad-El-Hak
Mohamed Gad-El-Hak

1 February 1999 in Progress in Aerospace Sciences
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Journal Article
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LLLennart Löfdahl
Lennart Löfdahl
MGMohamed Gad-El-Hak
Mohamed Gad-El-Hak

1 March 1996 in Sensors and Actuators A: Physical
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EKEdvard Kälvesten
Edvard Kälvesten
CVChristian Vieider
Christian Vieider
LLLennart Löfdahl
Lennart Löfdahl
GSGöran Stemme
Göran Stemme

1 March 1992 in Experiments in Fluids
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LLLennart Löfdahl
Lennart Löfdahl
GSG. Stemme
G. Stemme
BJB. Johansson
B. Johansson

1 June 1993 in Physics of Fluids A: Fluid Dynamics
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Journal Article
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DAD. Aronson
D. Aronson
LLLennart Löfdahl
Lennart Löfdahl
Hot wire measurements in the far field region of the plane wake of a cylinder have been carried out. The data obtained indicated that transverse distributions of mean‐velocity and Reynolds stresses were self‐preserving for a downstream distance greater than 400 momentum thicknesses. Dissipation rate and triple velocity correlations were measured at a downstream position of 880 momentum thicknesses, these measured profiles were compared with the profiles obtained from closure models for the Reynolds stress equations. It was found that the dissipation rate anisotropy could essentially be accounted for by the employed model, larger deviations were observed between the measured and modeled profiles for the triple velocity correlations.