Search NASAโŒ• Search

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.

Keep this discovery

Explore connections, maps & timelines

BibTeXRIS

Ostrach, S.. 1978-05-01. Convection due to surface-tension gradients. https://ntrs.nasa.gov/citations/19780064807

Cite the original work for its findings. Save a collection to share your selection of sources.