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Source: The Open Library
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1Surface tension driven convection experiment (STDCE)
By S. Ostrach
“Surface tension driven convection experiment (STDCE)” Metadata:
- Title: ➤ Surface tension driven convection experiment (STDCE)
- Author: S. Ostrach
- Language: English
- Publisher: ➤ National Aeronautics and Space Administration - National Technical Information Service, distributor
- Publish Date: 1996
- Publish Location: ➤ [Washington, D.C.] - [Springfield, Va
“Surface tension driven convection experiment (STDCE)” Subjects and Themes:
- Subjects: ➤ Microgravity - Temperature distribution - Spaceborne experiments - Surface temperature - Flow distribution - Capillary flow - Flow visualization - Interfacial tension - Surface tension driven convection
Edition Identifiers:
- The Open Library ID: OL15504929M
Access and General Info:
- First Year Published: 1996
- Is Full Text Available: No
- Is The Book Public: No
- Access Status: No_ebook
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Rayleigh–Bénard convection
prisms or spirals. The convective Bénard cells are not unique and will usually appear only in the surface tension driven convection. In general the solutions
STS-50
Crystal Growth Furnace (CGF); Drop Physics Module (DPM); Surface Tension Driven Convection Experiments (STDCE); Zeolite Crystal Growth (ZCG); Protein
Case Western Reserve University
Ostrach and Yasuhiro Kamotani led spacelab projects entitled surface tension driven convection experiment (STDCE) aboard the Space Shuttle STS-50 and the
Navier–Stokes equations
distribution of static pressure to as complicated as multiphase flow driven by surface tension. Generally, application to specific problems begins with some
Convergent boundary
vary depending on crust types. Plate tectonics is driven by convection cells in the mantle. Convection cells are the result of heat generated by the radioactive
Free surface
unless disturbed (except near solids dipping into them, where surface tension distorts the surface in a region called the meniscus). In a free liquid that is
Low-gravity process engineering
formation, and capillary flow dominance. The absence of buoyancy-driven convection alters mixing processes and phase separations, necessitating alternative
Plate tectonics
the large scale convection cells) or secondary. The secondary mechanisms view plate motion driven by friction between the convection currents in the asthenosphere
Boussinesq approximation (buoyancy)
Valentin Boussinesq) is used in the field of buoyancy-driven flow (also known as natural convection). It ignores density differences except where they appear
Gravity wave
frequencies between 3 Hz and .03 Hz). Shorter waves are also affected by surface tension and are called gravity–capillary waves and (if hardly influenced by