Asymmetry and penetration of transitional plane fountains in stratified fluid
Asymmetry and penetration of transitional plane fountains in stratified fluid
复制标题
分层流体中过渡平面喷泉的不对称性和穿透性
DOI:
10.1016/j.ijheatmasstransfer.2015.07.062
复制
发表时间:
2015-11
影响因子:
5.2
通讯作者:
Yinghe He
中科院分区:
文献类型:
--
作者:
Mohammad Ilias Inam;林文贤;S.W. Armfield;Yinghe He
Fountains injected into stratified fluids are widely found in environmental and industrial settings. The onset of asymmetry and entrainment that occurs in transitional fountains is the key to understanding turbulence generation and entrainment mechanisms in fountains. In addition to the Reynolds number (Re) and the Froude number (Fr), the stratification of the ambient fluid, represented by the dimensionless temperature stratification parameter (s), also has a significant effect on the onset of asymmetry, unsteadiness, and entrainment in a fountain, and on the maximum height that the fountain penetrates in the ambient fluid. In this study, a series of three-dimensional direct numerical simulations (DNS) were carried out using ANSYS Fluent for transitional plane fountains in linearly-stratified fluids with Re and s in the ranges of 25⩽ Re⩽ 300 and 0⩽ s⩽ 0.5, all at Fr= 10. The transient behavior of the fountains, in particular the effects of Re and s on the asymmetric transition and the maximum fountain penetration heights, is analysed and quantified using the DNS results. It is found that fountains are generally symmetric in the early developing stage, but become asymmetric and unsteady subsequently. The stratification of the ambient fluid is shown to stabilize the fountain flow and to reduce its asymmetry and unsteadiness. However, the effect of s on the asymmetric behavior of a fountain is found to be weaker than that of Re. Empirical correlations were developed, using the numerical results, to quantify such effects on the time for the asymmetric transition. The effects of Re and s on the initial and time-averaged maximum fountain heights (z m, i and z m, a, respectively), and the time to attain z m, i are also analysed. Quantified correlations are developed using the DNS results, which demonstrate that both z m, i and z m, a increase with Re, but decrease with s, apparently due to the increasing negative buoyancy that the fountain must overcome to penetrate the ambient fluid. The results further show that the effect of s on z m, i and z m, a is much stronger than that of Re.
登录
查看更多内容
DOI:
10.1017/s0022112099006953
发表时间:
2000-01
期刊:
J.Fluid Mech.
影响因子:
--
作者:
Wenxian Lin;S.W.Armfield
通讯作者:
S.W.Armfield
DOI:
10.1016/j.ijheatmasstransfer.2008.02.022
发表时间:
2008-09
影响因子:
5.2
作者:
G. D. McBain;N. Srinarayana;林文贤;S. W. Armfield
通讯作者:
S. W. Armfield
影响因子:
3.7
作者:
O. J. Myrtroeen;G. Hunt
通讯作者:
O. J. Myrtroeen;G. Hunt
影响因子:
2
作者:
W. Lin;S. Armfield
通讯作者:
W. Lin;S. Armfield
DOI:
10.1016/j.ijheatmasstransfer.2008.02.047
发表时间:
2008-10
影响因子:
5.2
作者:
Wenxian Lin;S. Armfield
通讯作者:
Wenxian Lin;S. Armfield