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Double-Diffusive Convection

Geophysical & Astrophysical Fluid Dynamics, 2015
Double-diffusive convection is the accurate but perhaps awkward name given to convective motions that occur in a fluid when the background density gradient is stably stratified.
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Double-Diffusive Convection

1992
In this chapter we turn our attention to processes of combined (simultaneous) heat and mass transfer that are driven by buoyancy. The density gradients that provide the driving buoyancy force are induced by the combined effects of temperature and species concentration nonuniformities present in the fluid saturated medium.
Donald A. Nield, Adrian Bejan
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Double-Diffusive Experiments

1996
Within a statically stable fluid stratified by gradients of two or more properties with different molecular diffusivities (i.e. heat-salt, salt-sugar, etc.) turbulence and convective transports may take place without energy supply from the outside. In such a system a number of surprising phenomena may be observed depending on the relative gradients of ...
Arne Foldvik, Bert Rudels
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Double Diffusion in Oceanography

Annual Review of Fluid Mechanics, 1994
The modern study of double-diffusive convection began with Melvin Stern's article on "The Salt Fountain and Thermohaline Convection" in 1960. In that paper, he showed how opposing stratifications of two component species could drive convection if their diffusivities differed.
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Double-Diffusive Convection

2018
Josef Tanny, A. B. Tsinober
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