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A note on unsteady laminar plumes/jets

机译:关于不稳定层流/喷气的注意事项

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We consider the laminar downstream evolution of a time-varying source of momentum and buoyancy in a boundary-layer formulation. The recent work of Hewitt and Duck (2011) showed that pulsatile laminar jets (in a boundary-layer model) are susceptible to a propagating wave disturbance that grows downstream. However, the work of Marzouk et al. (2003) presented results for a periodic pulsatile laminar (vertical) jet with heat transfer, for which the pulsation decayed downstream. This motivates the present investigation, to examine if the thermal effects included by Marzouk et al. inhibit the growing wave phenomenon that has been found in the momentum driven case. However, in contrast to Marzouk et al., the present results demonstrate that downstream growth still exists in (vertical) laminar boundary layers when buoyancy effects are included. Our results are carefully validated against known similarity solutions in the steady case, and with both a linearised spectral decomposition for the pulsatile case and an asymptotic description of the resulting wave's spatial growth.
机译:我们考虑边界层公式中动量和浮力的时变源的层流下游演化。 Hewitt和Duck(2011)的最新工作表明,脉动层流射流(在边界层模型中)易受下游传播的波扰动的影响。但是,Marzouk等人的工作。 (2003年)提出了具有传热的周期性脉动层流(垂直)射流的结果,其脉动向下游衰减。这激发了当前的研究,以检查Marzouk等人的研究是否包括热效应。抑制在动量驱动的情况下发现的增长波现象。但是,与Marzouk等人相反,目前的结果表明,当包括浮力作用时,下游生长仍然存在于(垂直)层流边界层中。我们的结果在稳定情况下针对已知的相似性解决方案进行了仔细验证,并针对脉动情况进行了线性化频谱分解,并对所得波的空间增长进行了渐近描述。

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