Abstract

Two piezoelectric series bimorph sensors were embedded below the skin of a NACA 0012 symmetrical airfoil to detect the local state of the boundary layer during wind tunnel testing. Small vanes piercing the airfoil skin were glued onto the bimorphs providing a mechanical coupling to the local mechanical force fluctuations imparted by the local unsteady boundary layer flow. The state of the boundary layer at the sensor sites was varied by changing the angle of attack. The objective of this work was to establish the ability of this sensor concept to accurately distinguish among typical boundary layer states such as attached laminar flow, turbulent flow and separated flow. The output of the sensor was compared to concurrent time-resolved particle image velocimetry measurements, which served as a validation technique. Using the developed sensor response envelope, a single data point time series of the piezo electrical signal was proven to be sufficient to accurately detect the boundary layer state on classical airfoils in the low Reynolds number regime. In projected future applications, single or arrays of bimorph sensors can be used to map the boundary layer of more complex or morphing shape airfoils. The fast response of the sensor can in principle be utilised in closed-loop flow control systems, aimed at drag reduction or lift enhancement.

Highlights

  • The boundary layer plays an important role in the lift-to-drag ratio of airfoils, through the coupling of viscous and inviscid mechanisms

  • The state of the boundary layer can be extracted from the statistical particle image velocimetry (PIV) measurements in various ways

  • We consider the values of the standard deviation, σ, occurring in the flow

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Summary

Introduction

The boundary layer plays an important role in the lift-to-drag ratio of airfoils, through the coupling of viscous and inviscid mechanisms. Boundary layers can be classified as either laminar, which can be described as organised flow containing non-intersecting smoothly developing and predictable paths, or turbulent, which can be described as an almost random chaotic flow. The so-called laminar-to-turbulent transition process, typically (but not exclusively) governed by the emergence and growth of shear layer instabilities. Boundary layers can experience so-called detachment or separation. They are unable to follow the shape of the aerodynamic surface, creating large recirculating areas

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