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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DOI: https://doi.org/10.1007/BF00272425