We use the lubrication approximation to analyze three closely related problems involving a thin rivulet or ridge (i.e., a two-dimensional droplet) of fluid subject to a prescribed uniform transverse shear stress at its free surface due to an external airflow, namely a rivulet draining under gravity down a vertical substrate, a rivulet driven by a longitudinal shear stress at its free surface, and a ridge on a horizontal substrate, and find qualitatively similar behaviour for all three problems. We show that, in agreement with previous numerical studies, the free surface profile of an equilibrium rivulet/ridge with pinned contact lines is skewed as the shear stress is increased from zero, and that there is a maximum value of the shear stress beyond which no solution with prescribed semi-width is possible. In practice, one or both of the contact lines will de-pin before this maximum value of the shear stress is reached, and so we consider situations in which the rivulet/ridge de-pins at one or both contact lines. In the case of de-pinning only at the advancing contact line, the rivulet/ridge is flattened and widened as the shear stress is increased from its critical value, and there is a second maximum value of the shear stress beyond which no solution with a prescribed advancing contact angle is possible. In contrast, in the case of de-pinning only at the receding contact line, the rivulet/ridge is thickened and narrowed as the shear stress is increased from its critical value, and there is a solution with a prescribed receding contact angle for all values of the shear stress. In general, in the case of de-pinning at both contact lines there is a critical “yield” value of the shear stress beyond which no equilibrium solution is possible and the rivulet/ridge will evolve unsteadily. In the Appendix, we show that an equilibrium rivulet/ridge with prescribed flux/area is quasi-statically stable to two-dimensional perturbations.
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August 2012
Research Article|
August 24 2012
A thin rivulet or ridge subject to a uniform transverse shear stress at its free surface due to an external airflow
J. M. Sullivan;
J. M. Sullivan
Department of Mathematics and Statistics,
University of Strathclyde
, 26 Richmond Street, Glasgow G1 1XH, United Kingdom
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C. Paterson;
C. Paterson
Department of Mathematics and Statistics,
University of Strathclyde
, 26 Richmond Street, Glasgow G1 1XH, United Kingdom
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S. K. Wilson;
S. K. Wilson
a)
Department of Mathematics and Statistics,
University of Strathclyde
, 26 Richmond Street, Glasgow G1 1XH, United Kingdom
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B. R. Duffy
B. R. Duffy
Department of Mathematics and Statistics,
University of Strathclyde
, 26 Richmond Street, Glasgow G1 1XH, United Kingdom
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a)
Author to whom correspondence should be addressed. Electronic mail: [email protected]. Telephone: + 44 (0) 141 548 3820. Fax: + 44 (0) 141 548 3345. Presently also a Visiting Fellow in the Oxford Centre for Collaborative Applied Mathematics (OCCAM), University of Oxford, Mathematical Institute, 24–29 St. Giles’, Oxford OX1 3LB, United Kingdom.
Physics of Fluids 24, 082109 (2012)
Article history
Received:
February 06 2012
Accepted:
July 05 2012
Citation
J. M. Sullivan, C. Paterson, S. K. Wilson, B. R. Duffy; A thin rivulet or ridge subject to a uniform transverse shear stress at its free surface due to an external airflow. Physics of Fluids 1 August 2012; 24 (8): 082109. https://doi.org/10.1063/1.4744980
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