Abstract
An analysis is made for the forced convection thermal and solute concentration Marangoni boundary layers (thin dissipative layers) that can be formed along the surface, which separates two immiscible fluids in surface driven flows when the appropriately defined Reynolds number is large enough. Similarity equations for the case in which an external pressure gradient is imposed are derived. These equations are then solved numerically for some values of the involved parameters using very efficient numerical schemes known as Keller-box and superposition methods and the features of the flow and transport characteristics are analysed and discussed.
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