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首页> 外文期刊>Transport in Porous Media >Linear Stability and Convection in a Gravity Modulated Porous Layer Heated from Below: Transition from Synchronous to Subharmonic Solutions
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Linear Stability and Convection in a Gravity Modulated Porous Layer Heated from Below: Transition from Synchronous to Subharmonic Solutions

机译:从下方加热的重力调制多孔层中的线性稳定性和对流:从同步解到次谐波解的过渡

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摘要

The linear stability theory is used to investigate analytically the effects of gravity modulation on convection in a homogenous porous layer heated from below. The linear stability results are presented for both the synchronous and subharmonic solutions and the exact point for the transition from synchronous to subharmonic solutions is computed. It is also demonstrated that increasing the excitation frequency rapidly stabilizes the convection up to the transition point from synchronous to subharmonic convection. Beyond the transition point, the effect of increasing the frequency is to slowly destabilize the convection.
机译:线性稳定性理论用于分析研究重力调制对从下方加热的均匀多孔层中对流的影响。给出了同步和次谐波解决方案的线性稳定性结果,并计算了从同步到次谐波解决方案过渡的精确点。还证明了增加激励频率可以快速稳定对流,直到从同步对流到次谐波对流的过渡点为止。在过渡点之外,增加频率的作用是使对流稳定。

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