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Surface-Tension Driven ConvectionThe present experiments are directed to examine surface-tension gradients. The surface-tension induced convection under reduced gravity it's comparison with normal gravity convection with all other identical conditions are studied. The intensities of such flows and their penetration depth below the free surface are also determined. In this way, the dominant role of a free surface in a reduced-gravity environment is indicated. The interface between two fluid phases can influence the motion of fluids when either the interface has finite curvature or when the interfacial tension varies from point to point. In both cases, forces appear in the interfacial region that can affect or generate fluid motions.
Document ID
19860000657
Acquisition Source
Legacy CDMS
Document Type
Other
Authors
Ostrach, S.
(Case Western Reserve Univ. Cleveland, OH, United States)
Kamotani, Y.
(Case Western Reserve Univ. Cleveland, OH, United States)
Date Acquired
August 12, 2013
Publication Date
May 1, 1985
Publication Information
Publication: NASA, Washington Microgravity Sci. and Appl. Program Tasks
Subject Category
Astronautics (General)
Accession Number
86N10124
Funding Number(s)
CONTRACT_GRANT: NAG3-570
Distribution Limits
Public
Copyright
Work of the US Gov. Public Use Permitted.
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