Turbulent natural convection in an air-water system with evaporation across the free surface by Julien CARLIER

IMMC

28 February 2024

13:00

Louvain-la-Neuve

Place du Levant 2, Seminar room b.044

In this talk, I will present numerical results for turbulent convection in a pool that contains liquid water in the lower part and air in the upper one. The bottom wall is uniformly heated and natural convection is established in both phases, accompanied by water evaporation across the free surface of the water. First I will briefly describe the governing equations, including the jump relations across the free surface. The descent of the free surface due to evaporation is computed via a newly developed tracking algorithm based on the ghost-fluid method. The efficiency of the proposed algorithm is illustrated via comparisons with analytical solutions and experimental data for various test cases.

Next, I will present results from direct numerical simulations of three different cases, corresponding to different pool heights. In all of them, the natural convection in the water lies in the soft-turbulence regime. Whereas in the gas, it lies in the laminar, transitional and soft-turbulence regimes, respectively. Our analysis focuses on the characteristics of the convective patterns in the two phases and the statistics of the various flow quantities of interest. According to our simulations, the flow in the water is organized in a single-roll large-scale circulation (LSC). In the gas, it is organized in single or dual-roll LSCs, depending on the aspect ratio of the pool. Interestingly, the impingement points of the LSCs of the two phases at the free surface remain very close to one another, which is attributed to the continuity of the shear stresses at the free surface. Further, after the initial transient period, both the free-surface temperature and the evaporative mass flux are stabilized and remain almost constant, but they exhibit small-scale fluctuations in time due to turbulence. Also, the transport of water vapor in air has similar properties as the heat transport, and the ratio between the Sherwood and Nusselt numbers is very close to the Lewis number for air.

 

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