1978
DOI: 10.2514/3.7547
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Transition to turbulence in two-dimensional wakes

Abstract: A new technique is advanced for predicting the location of the laminar turbiiient transition zone in twodimensional wake flows. The technique is based on postulating a minimum turbulence Reynolds number required for sustaining the turbulence once it occurs. Using existing wake turbulence data and compressible laminar wake theory, the turbulence Reynolds number is then algebraically expressed in terms of freestream or wake edge conditions and integral properties. An example is calculated using laminar wake simi… Show more

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Cited by 4 publications
(6 citation statements)
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“…The theoretical approach to predicting transition in the FSL is the same as utilized earlier by this author [1,4], for deriving analogous equations for the wake and boundary layer. The central statement of this method is that the turbulence Reynolds number Thus, according to the above, the present task consists of computing the turbulence Reynolds number, given by Equation (1), along the FSL.…”
Section: Methodsmentioning
confidence: 99%
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“…The theoretical approach to predicting transition in the FSL is the same as utilized earlier by this author [1,4], for deriving analogous equations for the wake and boundary layer. The central statement of this method is that the turbulence Reynolds number Thus, according to the above, the present task consists of computing the turbulence Reynolds number, given by Equation (1), along the FSL.…”
Section: Methodsmentioning
confidence: 99%
“…On the other hand, in applying the theory to wakes, [1], successful predictions were made using the ReA magnitude in the center of the flow. Therefore, despite the misgivings of the preceding paragraph, we will here take the following position: if a turbulent FSL has a maximum Re A equal to or larger than the threshold ReAo, then that flow is permitted to be locally turbulent.…”
Section: -mentioning
confidence: 99%
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“…However there have not been many experiments on the stability of a wake at supersonic flow speeds carried out so far (similar studies in a boundary layer are more numerous -see, for example, Lysenko 1993;Lysenko & Maslov 1984; and many others), though such works as Behrens (1968), Behrens & Ko (1971), Behrens, Lewis & Webb (1971), Demetriades (1964Demetriades ( , 1978Demetriades ( , 1990, McLaughlin (1971), McLaughlin et al (1971) have become classical. In them the development of the natural disturbances is studied.…”
Section: Introductionmentioning
confidence: 99%