A very interesting sequence of events begins to develop when Re reaches 40, the point at which the wake behind the cylinder becomes unstable. Experiments show that for Re ∼ 10
2 the wake develops a slow oscillation in which the velocity is periodic in time and downstream distance, with the amplitude of the oscillation increasing downstream. The oscillating
wake rolls up into two staggered rows of vortices with opposite sense of rotation (
Figure 10.19). von Karman investigated the phenomenon as a problem of superposition of irrotational vortices; he concluded that a non-staggered row of vortices is unstable, and a staggered row is stable only if the ratio of lateral distance between the vortices to their longitudinal distance is 0.28. Because of the similarity of the wake with footprints on a street, the staggered row of vortices behind a blunt body is called a
von Karman vortex street. The vortices move downstream at a speed smaller than
U∞. This means that the vortex pattern slowly follows the cylinder if it is pulled through a stationary fluid.
In the range 40 < Re < 80, the vortex street does not interact with the pair of attached vortices. As Re increases above 80, the vortex street forms closer to the cylinder, and the attached eddies (whose downstream length has now grown to be about twice the diameter of the cylinder) themselves begin to oscillate. Finally the attached eddies periodically break off alternately from the two sides of the cylinder. While an eddy on one side is shed, that on the other side forms, resulting in an unsteady flow near the cylinder. As vortices of opposite circulations are shed off alternately from the two sides, the circulation around the cylinder changes sign, resulting in an oscillating lift or lateral force perpendicular to the upstream flow direction. If the frequency of vortex shedding is close to the natural frequency of some structural mode of vibration of the cylinder and its supports, then an appreciable lateral vibration may be observed. Engineered structures such as suspension bridges, oil drilling platforms, and even automobile components are designed to prevent coherent shedding of vortices from cylindrical structures. This is done by including spiral blades protruding out of the cylinder's surface, which break up the spanwise coherence of vortex shedding, forcing the vortices to detach at different times along the length of these structures (
Figure 10.20).
The passage of regular vortices causes velocity measurements in the cylinder's wake to have a dominant periodicity, and this frequency Ω is commonly expressed as a
Strouhal number (4.102),
St = Ω
d/
U∞. Experiments show that for a circular cylinder the value of
St remains close to 0.2 for a large range of Reynolds numbers. For small values of cylinder diameter and moderate values of
U∞, the resulting frequencies of the vortex shedding and oscillating lift lie in the acoustic range. For example, at
U∞ = 10m/s and a wire diameter of 2
mm, the frequency corresponding to a Strouhal number of 0.2 is 1000 cycles per second. The
singing of telephone and electrical transmission lines and automobile radio antennae have been attributed to this phenomenon. The value of
St given here is that observed in
three-dimensional flows with nominally two-dimensional boundary conditions. Moving soap-film experiments and calculations suggest a somewhat higher value of
St = 0.24 in perfectly two-dimensional flow (see
Wen & Lin, 2001).
Below Re = 200, the vortices in the wake are laminar and continue to be so for very large distances downstream. Above 200, the vortex street becomes unstable and irregular, and the flow within the vortices themselves becomes chaotic. However, the flow in the wake continues to have a strong frequency component corresponding to a Strouhal number of St = 0.2. However, above a Reynolds number of several thousand, periodicity in the wake is only perceptible near the cylinder, and the wake may be described as fully turbulent beyond several cylinder diameters downstream.
Striking examples of vortex streets have also been observed in stratified atmospheric flows.
Figure 10.21 shows a satellite photograph of the wake behind several isolated mountain peaks when the wind is blowing toward the lower right of picture. The mountains pierce through the cloud level, and the flow pattern becomes visible in the cloud pattern. The wakes behind at least two mountain peaks display the characteristics of a von Karman vortex street. The strong density stratification in this flow has prevented vertical motions, giving the flow the two-dimensional character necessary for the formation of vortex streets.