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Stability and stationary convection induced by gravity and centrifugal forces in a rotating porous layer distant from the axis of rotation

机译:重力和离心力在远离旋转轴的旋转多孔层中引起的稳定性和固定对流

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摘要

The stability and onset of stationary convection in a rotating fluid saturated porous layer placed at an arbitrary positive distance from the rotation axis and subject to gravity and centrifugal body forces is investigated analytically. The stability of a basic gravity driven convection is analyzed. The marginal stability criterion is established in terms of critical centrifugal Rayleigh numbers and a critical wave number. The results show that apart from providing a non-motionless basic state and dictating the direction of the wave number, the gravity plays a relatively passive role, without affecting the stability results. Furthermore, it is demonstrated that the neutral curves for combined centrifugal and gravity convection in the stationary case are identical to the case when the gravity effects are neglected. The results also provide a simple stability map for a wide range of values of the parameter controlling the offset distance from the axis of rotation.
机译:解析地研究了旋转流体饱和多孔层中固定对流的稳定性和起因,该多孔流体层位于与旋转轴成任意正距离并受到重力和离心力作用下。分析了基本重力驱动对流的稳定性。根据临界离心瑞利数和临界波数建立了边际稳定性判据。结果表明,重力除了提供非静止的基本状态并指示波数的方向外,还起相对被动的作用,而不会影响稳定性结果。此外,证明了在静止情况下用于离心和重力对流组合的中性曲线与忽略重力效应时的情况相同。结果还为控制与旋转轴的偏移距离的参数值的宽范围提供了简单的稳定性图。

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