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Effect Of Velocity And Temperature Boundary Conditions On Convective Instability In A Ferrofluid Layer

机译:速度和温度边界条件对铁磁流体层对流不稳定性的影响

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A variety of velocity and temperature boundary conditions on the onset offerroconvection in an initially quiescent ferrofluid layer in the presence of a uniform magnetic field is investigated. The lower boundary of the ferrofluid layer is assumed to be rigid-ferromagnetic, while the upper boundary is considered to be either rigid-ferromagnetic or stress-free. The thermal conditions include a fixed heat flux at the lower boundary and a general convective, radiative exchange at the upper boundary, which encompasses fixed temperature and fixed heat flux as particular cases. The resulting eigenvalue problem is solved using the Galer-kin technique and also by the regular perturbation technique when both boundaries are insulated to temperature perturbations. It is observed that an increase in the magnetic number and the nonlinearity of fluid magnetization as well as a decrease in Biot number are to destabilize the system. Further, the nonlinearity of fluid magnetization is found to have no effect on the onset of ferroconvection in the absence of the Biot number.
机译:研究了在均匀磁场存在下,初始静止的铁磁流体层中,对流对流的各种速度和温度边界条件。假定铁磁流体层的下边界是刚性铁磁的,而认为上边界是刚性铁磁的或无应力的。热条件包括下边界处的固定热通量和上边界处的一般对流,辐射交换,具体情况下包括固定温度和固定热通量。当将两个边界都与温度扰动隔离时,可以使用Galer-kin技术以及常规扰动技术来解决由此产生的特征值问题。可以看到,磁数的增加和流体磁化强度的非线性以及Biot数的减少都会破坏系统的稳定性。此外,发现在没有比奥数的情况下,流体磁化的非线性对铁对流的开始没有影响。

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