Strongly coupled interaction between a ridge of fluid and an inviscid airflow

Tools

Paterson, C. and Wilson, S. K. and Duffy, B. R. (2015) Strongly coupled interaction between a ridge of fluid and an inviscid airflow. Physics of Fluids, 27 (7). 072104. ISSN 1070-6631 (https://doi.org/10.1063/1.4926623)

[thumbnail of Paterson-etal-POF-2015-Strongly-coupled-interaction-between-a-ridge-of-fluid]
Preview
 Text. Filename: Paterson_etal_POF_2015_Strongly_coupled_interaction_between_a_ridge_of_fluid.pdf
Final Published Version
Download (1MB)| Preview

Abstract

The behaviour of a steady thin sessile or pendent ridge of fluid on an inclined planar substrate which is strongly coupled to the external pressure gradient a rising from an inviscid airflow parallel to the substrate far from the ridge is described. When the substrate is nearly horizontal a very wide ridge can be supported against gravity by capillary and/or external pressure forces; otherwise only a narrower (but still wide) ridge can be supported. Classical thin-aerofoil theory is adapted to obtain the governing singular integro-differential equation for the profile of the ridge in each case. Attention is focused mainly on the case of a very wide sessile ridge. The effect of strengthening the airflow is to push a pinned ridge down near to its edges but to pull it up near to its middle. At a critical airflow strength the upslope contact angle reaches the receding contact angle at which the upslope contact line de-pins, and continuing to increase the airflow strength beyond this critical value results in the de-pinned ridge becoming narrower, thicker and closer to being symmetric in the limit of a strong airflow. The effect of tilting the substrate is to skew a pinned ridge in the downslope direction. Depending on the values of the advancing and receding contact angles, the ridge may first de-pin at either the upslope or the downslope contact line but, in general, eventually both contact lines de-pin. The special cases in which only one of the contact lines de-pins are also considered. It is also shown that the behaviour of a very wide pendent ridge is qualitatively similar to that of a very wide sessile ridge, while the important qualitative difference between the behaviour of a very wide ridge and a narrower ridge is that, in general, for the latter one or both of the contact lines may never de-pin.

ORCID iDs

Paterson, C., Wilson, S. K. ORCID logoORCID: https://orcid.org/0000-0001-7841-9643 and Duffy, B. R. ORCID logoORCID: https://orcid.org/0000-0003-2687-7938;
CORE (COnnecting REpositories)