Secondary flows of viscoelastic fluids in serpentine microchannels

TL;DR

This study experimentally visualizes and characterizes steady secondary flows of viscoelastic fluids in serpentine microchannels, confirming numerical predictions and advancing understanding of flow instabilities in complex microfluidic geometries.

Contribution

First experimental evidence and detailed characterization of steady secondary flows in serpentine microchannels with viscoelastic fluids, validating numerical models.

Findings

Secondary flows form two counter-rotating vortices.

Experimental results qualitatively agree with numerical predictions.

Insights into flow stability and onset of instabilities in microchannels.

Abstract

Secondary flows are ubiquitous in channel flows, where small velocity components perpendicular to the main velocity appear due to the complexity of the channel geometry and/or that of the flow itself such as from inertial or non-Newtonian effects, etc. We investigate here the inertialess secondary flow of viscoelastic fluids in curved microchannels of rectangular cross-section and constant but alternating curvature: the so-called "serpentine channel" geometry. Numerical calculations (Poole et al, 2013) have shown that in this geometry, in the absence of elastic instabilities, a steady secondary flow develops that takes the shape of two counter-rotating vortices in the plane of the channel cross-section. We present the first experimental visualization evidence and characterization of these steady secondary flows, using a complementarity of microPIV in the plane of the channel, and confocal visualisation of dye-stream transport in the cross-sectional plane. We show that the measured streamlines and the relative velocity magnitude of the secondary flows are in qualitative agreement with the numerical results. In addition to our techniques being broadly applicable to the characterisation of three-dimensional flow structures in microchannels, our results are important for understanding the onset of instability in serpentine viscoelastic flows.