Laminar and axisymmetric vertical jets in a stably stratified environment
Laminar and axisymmetric vertical jets in a stably stratified environment
复制标题
稳定分层环境中的层流和轴对称垂直射流
DOI:
10.1016/0017-9310(71)90027-5
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发表时间:
1971
影响因子:
5.2
通讯作者:
B. Gebhart
中科院分区:
文献类型:
--
作者:
A. Tenner;B. Gebhart
Experiments have shown that an axisymmetric, laminar, buoyant jet in a stably stratified environment induces the flow of a toroidal cell around itself. The inner portion of the cell is driven upward by the viscous shearing of the jet, and the outer portion descends due to a negative buoyancy force. Under certain limiting conditions, this cell draws along a thin layer of the lower density jet and surrounds itself with it in the form of a shroud. The shroud flows in a direction opposite to the jet, and its density is similar to that of the jet. Conditions favorable to shroud production require that the environment be stably stratified and that the molecular diffusivities of the fluids involved be extremely small. Turbulent jets are not expected to produce an appreciable shroud.