Dispersion of a buoyant plume in a turbulent pressure-driven channel flow

被引:6
|
作者
Fabregat, Alexandre [1 ]
Pallares, Jordi [1 ]
Cuesta, Ildefonso [1 ]
Grau, Francesc Xavier [1 ]
机构
[1] Univ Rovira & Virgili, Dept Engn Mecan, Tarragona 43007, Spain
关键词
DNS; Plane channel flow; Turbulent heat transfer; Buoyancy; DIRECT NUMERICAL-SIMULATION; PASSIVE SCALAR DISPERSION; ELEVATED LINE SOURCE; BOUNDARY-LAYER; HOMOGENEOUS TURBULENCE; GRID TURBULENCE; THERMAL DISPERSION; POINT SOURCES; SHEARED FLOW; HEAT-SOURCE;
D O I
10.1016/j.ijheatmasstransfer.2008.10.011
中图分类号
O414.1 [热力学];
学科分类号
摘要
Direct numerical simulations of the turbulent dispersion of a buoyant line of hot fluid released at the inlet of a plane channel flow are reported (Re-tau = 180, Gr = 10(7) and Pr = 0.7). Results of turbulent dispersion of a neutrally buoyant scalar and mixed convection flow are also included. The buoyancy force induces a vertical movement that, although small in mean, exhibits a significant fluctuation in the vertical velocity component and deflects the plume with the consequent loss of symmetry found in the neutrally buoyant results. The modification of the budgets for the time averaged momentum and heat transport equations reflects the rearranging of the different contributions induced by the buoyancy force. (C) 2008 Elsevier Ltd. All rights reserved.
引用
收藏
页码:1827 / 1842
页数:16
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