Abstract

The phenomenon of liquid entrainment is investigated experimentally and theoretically for the condition of simultaneous discharge from two small orifices located on the side of a high-pressure reservoir containing stratified layers of two immiscible fluids. The measured critical height for air-water layers is found to be a function of the two discharge rates and the vertical distance separating the centrelines of the orifices. An independent theoretical analysis is conducted which gives good agreement with the experimental data.

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