Abstract

The interaction of disturbance modes behind an isolated cylindrical roughness element in a laminar boundary layer is investigated by means of hot-film anemometry and particle image velocimetry in a low-turbulence laminar water channel. Both sinuous and varicose disturbance modes are found in the wake of a roughness with unit aspect ratio (diameter/height $=$ 1). Interestingly, the frequency of the varicose mode synchronizes with the first harmonic of the sinuous mode when the critical Reynolds number from three-dimensional global linear stability theory is exceeded. The coupled motion of sinuous and varicose modes is explained by frequency lock-in. This mechanism is of great importance in many aspects of nature, but has not yet received sufficient attention in the field of boundary-layer theory. A Fourier mode decomposition provides detailed analyses of sinuous and varicose modes. The observation is confirmed by a second experiment with the same aspect ratio at a different position in the laminar boundary layer. When the aspect ratio is increased, the flow is fully governed by the varicose mode. Thus, no frequency lock-in can be observed in this case. The significance of this work is to explain how sinuous and varicose modes can co-exist behind a roughness and to propose a mechanism which is well established in physics but not encountered often in boundary-layer theory.

Highlights

  • Frequency lock-in is the synchronization phenomenon between two or more oscillators

  • Hot-film anemometry and particle image velocimetry have been performed in a laminar water channel to investigate the flow downstream of a cylindrical roughness element in a laminar boundary layer

  • Three different roughness elements are considered with aspect ratios η = 1 and η = 3

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Summary

Introduction

Frequency lock-in is the synchronization phenomenon between two or more oscillators. The first known report of this fundamental concept dates back to the year 1665, when Christiaan Huygens described the synchronous motion of two pendulum clocks mounted on a wooden beam (Huygens 1893). Cherubini et al (2013) discovered large energy gain of varicose perturbations when the boundary layer is perturbed by a three-dimensional roughness hump This result was confirmed for a hemispherical roughness element by Citro et al (2015) and is in agreement with the experimental observation of symmetric hairpin vortices emerging from the recirculation zone of the roughness (Ye, Schrijer & Scarano 2018). The set-up of Bucci et al (2018) and Puckert & Rist (2018a) is reproduced to investigate the nonlinear interaction between sinuous and varicose modes and to suggest synchronization as an important nonlinear mechanism in boundary layers.

Experimental set-up
Literature
Roughness-induced instabilities
Downstream disturbance evolution
Frequency behaviour
Synchronization of sinuous and varicose modes
Findings
Discussion
Conclusions
Full Text
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