Surface entrainment of air by high veloc
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E. Van de Sande; John M. Smith
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Article
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1973
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Elsevier Science
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English
⚖ 559 KB
theory is given of the aeration produced by the impact of a high speed water jet on a water surface. Experimental verification agrees more than satisfactorily with the developed theory over a wide range. The boundary conditions for the theory have a physical meaning. The jet must be submitted to air