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首页> 外文期刊>Environmental fluid mechanics >The flow of high-Reynolds axisymmetric gravity currents of a stratified fluid into a stratified ambient: Shallow-water and box model solutions
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The flow of high-Reynolds axisymmetric gravity currents of a stratified fluid into a stratified ambient: Shallow-water and box model solutions

机译:分层流体的高雷诺轴对称重力流向分层环境的流动:浅水和箱模型解决方案

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We consider the axisymmetric flow (in a full cylinder or a wedge) of high-Reynolds-number Boussinesq gravity currents and intrusions systems in which both the ambient and the propagating "current" are linearly stratified. The main focus is on a current of fixed volume released from a cylinder lock; the height ratio of the fluids H, and the stratification parameter of the ambient S, are quite general. We develop a one-layer shallow-water model. The internal stratification enters as a new dimensionless parameter, σ ∈ [0, 1]. In general, the time-dependent motion is obtained by standard finite-difference solutions; a self-similar analytical solution exists for S = 0. We show that, in general, the speed of propagation decreases when the internal stratification becomes more pronounced (σ increases). We also developed a box-model approximation, and show that the resulting radius of propagation is in good agreement with the more rigorous shallow-water prediction.
机译:我们考虑了高雷诺数Boussinesq重力流和侵入系统的轴对称流动(在整个圆柱体或楔形中),其中环境和传播的“电流”都线性地分层。主要关注的是从锁芯释放的固定电流。流体H的高度比和环境S的分层参数相当笼统。我们开发了一层浅水模型。内部分层作为新的无量纲参数σ∈[0,1]输入。通常,与时间有关的运动是通过标准的有限差分解获得的。对于S = 0,存在一个自相似的解析解。我们证明,通常,当内部分层变得更加明显(σ增大)时,传播速度降低。我们还开发了一种箱形模型近似方法,并证明了由此产生的传播半径与更严格的浅水预测非常吻合。

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