Direct numerical simulation of the fully developed turbulent free convection flow in an asymmetrically heated vertical channel

被引:2
|
作者
Pallares, Jordi [1 ]
Fabregat, Alexandre [1 ]
Lei, Chengwang [2 ]
机构
[1] Univ Rovira & Virgili, Dept Engn Mecan, Ave Paisos Catalans 16, Tarragona 43007, Spain
[2] Univ Sydney, Ctr Wind Waves & Water, Sch Civil Engn, Sydney, NSW 2006, Australia
基金
澳大利亚研究理事会;
关键词
Turbulent flow; Natural convection; Vertical channel; Asymmetrical heating; Direct numerical simulation; LAMINAR FREE-CONVECTION; NATURAL-CONVECTION; SOLAR CHIMNEY; WALL; PLATES; INFINITE;
D O I
10.1016/j.ijthermalsci.2023.108352
中图分类号
O414.1 [热力学];
学科分类号
摘要
We report direct numerical simulations of the fully developed turbulent natural convection flow of a Boussinesq fluid (Pr = 0.71) in a vertical channel. One wall is heated with a constant heat flux and the other is assumed to be perfectly insulated. Simulations were performed at three different Rayleigh numbers (Ra = 5 x 10(5), 10(6) and 5 x 10(6)). Predictions of the time averaged velocities, temperatures and intensities of the fluctuations agree with experiments reported in the literature. Under the fully developed flow conditions considered in this study the shear stress is greater on thermally active wall than that on the adiabatic wall, but the turbulent intensities and the turbulent shear stress are greater near the insulated wall. Conversely, the intensities of the temperature fluctuations and turbulent heat fluxes are higher near the thermally active wall than those near the adiabatic wall. Contrary to the vertical channel with constant but different wall temperatures, where buoyancy and tur-bulent shear dominate the generation of turbulent kinetic energy, in the asymmetrically heated channel the turbulent shear stress is the principal mechanism of turbulent kinetic energy production as in a forced convection channel flow.
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页数:9
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