Numerical Simulation of Convection Depth in Shear Cell Under Microgravity

Details Numerical Simulation of Convection Depth in Shear Cell Under Microgravity Numerical Simulation of Convection Depth in Shear Cell Under Microgravity

Jan 1999

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1999adspr..24.1321z&link_type=abstract

Advances in Space Research, Volume 24, Issue 10, p. 1321-1324.

Physics

1

Scientific paper

By applying the idea of an isotope trace experiment, the concept of isotope trace in hydrodynamics simulation is proposed. The isotope concentration is conceived as a numerical marker to trace the convection and estimate numerically the convection depth due to shearing in shear cell under microgravity. Two different shearing rates, 2mm/s and 20mm/s, are investigated, and results demonstrate that the isotope depths are same for both cases at the termination of shearing, but the effect of residual flow field after shearing is different

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