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Abstract
The nature of the hydrodynamic flow of water down an inclined plane in the presence of static gas is discussed. The effects of liquid flow rates and angles of inclination of the plane on the film thickness and ripple inception are recorded. The ripples differ in number and character from those usually associated with liquid flow on a vertical wall
Mass transfer of carbon dioxide into a water film on an inclined plane is determined more accurately than hitherto by introduction of modifications to the apparatus and the use of novel methods for determining end-effects. This makes possible more meaningful comparisions between experimental results and model theory. Penetration concentration profiles in the falling liquid film are presented