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Instability of parallel buoyant flow in a vertical porous layer with an internal heat source

机译:具有内部热源的垂直多孔层中平行浮力流动的不稳定性

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摘要

Buoyant flow in a vertical porous layer whose open boundaries are kept at uniform and different temperatures is analysed. The presence of a uniform volumetric heat source alters the conduction profile of the temperature field for the stationary parallel flow. It is shown that this stationary flow becomes unstable when either the temperature difference between the boundaries or the intensity of the volumetric heat source are sufficiently large. The linear instability is investigated through a study of normal mode disturbances. The stability eigenvalue problem is solved numerically by employing the shooting method. The neutral stability curves are obtained and the critical parameters at onset of instability are determined.
机译:垂直多孔层中的浮力流动,其开放边界保持均匀并且温度不同。均匀体积热源的存在改变了固定平行流的温度场的传导曲线。可以看出,当边界之间的温度差或体积热源的强度足够大时,该固定流变得不稳定。通过研究正常模式干扰来研究线性不稳定性。稳定性特征值问题可以通过射击法来解决。获得了中性稳定性曲线,并确定了不稳定开始时的关键参数。

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