NASA NTRS ยท 19780064807
Convection due to surface-tension gradients
Abstract
The use of dimensionless parameters to study fluid motions that could occur in a reduced-gravity environment is discussed. The significance of the Marangoni instability is considered, and the use of dimensionless parameters to investigate problems such as thermo and diffusocapillary flows is described. Characteristics of fluid flow in space are described, and the relation and interaction of motions due to capillarity and buoyancy is examined.
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Ostrach, S.. 1978-05-01. Convection due to surface-tension gradients. https://ntrs.nasa.gov/citations/19780064807
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