Abstract
In this work we study the fingering double diffusive convection, namely, the buoyancy-driven convection flow within a fluid layer experiencing an unstable salinity gradient and a stable thermal gradient. In particular, we investigate the influences from a background shear with uniform strength. Linear stability analysis indicates that the unstable modes shift from a circular shape to a sheetlike shape as the shear becomes stronger. Three-dimensional direct numerical simulations are conducted for five groups of cases, each of which has the same combination of thermal and salinity gradients (measured by corresponding Rayleigh numbers) and gradually increasing shear strength. The same properties of seawater are used for all simulations, i.e., the Prandtl number (the ratio of kinematic viscosity to thermal diffusivity) and the Schmidt number (the ratio of kinematic viscosity to salinity diffusivity). Numerical results reveal that a very weak shear organizes the salt fingers into a very regular pattern, which enhances the salinity flux. This enhancement effect, however, reduces as the Rayleigh number increases. For stronger shear the dominant structures shift from salt fingers to salt sheets, and the coherence length scale increases in the streamwise direction. Meanwhile, salinity and heat fluxes decrease. These findings suggest that even a weak shear can notably alter the morphology and transport properties of fingering double diffusive convection.
7 More- Received 20 December 2021
- Accepted 19 April 2022
DOI:https://doi.org/10.1103/PhysRevFluids.7.053501
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