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Double-diffusive convection caused by coupled molecular diffusion

Published online by Cambridge University Press:  20 April 2006

Trevor J. Mcdougall
Trevor J. Mcdougall
Affiliation:
Research School of Earth Sciences, Australian National University, P.O. Box 4, Canberra, A.C.T. 2600
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Abstract

Double-diffusive convection is studied for the case where a large coupled diffusion (or cross-diffusion) effect is present. The Soret effect is a familiar example of this cross-diffusion where the flux of the solute depends not only on its own spatial gradient but also on the in situ temperature gradient. The linear stability analysis of double-diffusive convection has been extended to include the two cross-diffusion flux terms and it has been shown that, with a sufficiently large coupled diffusion effect, fingers can form even when the concentrations of both components make the fluid's density gradient statically stable. The conditions under which the diffusive instability can occur are compared with those for the formation of fingers and it is shown that these two types of double-diffusive convection cannot occur together in any particular set of linear property gradients. We then consider finite-amplitude, steady, infinitely long fingers and show that a sufficiently large cross-diffusion effect can again allow fingers to exist when the concentrations of both solutes increase with depth. It is also shown that the diffusion of properties from an initially sharp interface may set up vertical gradients that are favourable for the formation of fingers.

Information

Type
Research Article
Information
Journal of Fluid Mechanics , Volume 126 , January 1983, pp. 379 - 397
Copyright
© 1983 Cambridge University Press

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