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Interaction of external and double-diffusive convection in linearly salt-stratified systems

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Abstract

A series of experiments has been performed for a linearly salt-stratified system heated from below. The experiments were intended to investigate the relative influence of external and double-diffusive convection on (i) entrainment of salt-stratified fluid into adjacent layers of convecting fluid, and (ii) formation of multiple mixed layers within stable, salt-stratified fluid layers. External convection effects were altered by placing a horizontal grid in the convecting fluid layer. An assortment of flow visualization techniques revealed that external convection can strongly influence entrainment of salt-stratified fluid and multiple mixed layer formation. However, the techniques could not resolve the possible significance of the double-diffusive entrainment mechanism.

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Abbreviations

g :

gravitational acceleration

H :

mixed layer height

H m :

grid height

k :

thermal conductivity

m s :

salt mass fraction

q b :

bottom heat flux

Ra Emphasis>/* T :

modified thermal Rayleigh number, g β T q b H 4/κ α ν

Ra s :

solutal Rayleigh number, g β s (∂m s/∂ z ) i H 4/α ν

Ri :

Richardson number

T :

temperature

X :

stability parameter, Ra *T /Ra s

z:

vertical coordinate

α:

thermal diffusivity

βs :

saline expansion coefficient

β T :

thermal expansion coefficient

δ:

interface height in two layer system

ν:

kinematic viscosity

i :

initial

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Bergman, T.L., Incropera, F.P. & Viskanta, R. Interaction of external and double-diffusive convection in linearly salt-stratified systems. Experiments in Fluids 5, 49–58 (1986). https://doi.org/10.1007/BF00272425

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