Directional effect of a magnetic field on oscillatory low-Prandtl-number convection

被引:11
|
作者
Henry, D. [1 ]
Juel, A. [2 ,3 ]
Ben Hadid, H. [1 ]
Kaddeche, S. [4 ]
机构
[1] Univ Lyon 1, INSA Lyon, ECL, Univ Lyon,Lab Mecan Fluides & Acoust,CNRS, F-69134 Ecully, France
[2] Univ Manchester, Manchester Ctr Nonlinear Dynam, Manchester M13 9PL, Lancs, England
[3] Univ Manchester, Sch Math, Manchester M13 9PL, Lancs, England
[4] INSAT, Unite Rec Mat Mesures & Applicat, Tunis 1080, Tunisia
基金
英国工程与自然科学研究理事会;
关键词
D O I
10.1063/1.2856125
中图分类号
O3 [力学];
学科分类号
08 ; 0801 ;
摘要
The directional effect of a magnetic field on the onset of oscillatory convection is studied numerically in a confined three-dimensional cavity of relative dimensions 4: 2: 1 (length: width: height ) filled with mercury and subject to a horizontal temperature gradient. The magnetic field suppresses the oscillations most effectively when it is applied in the vertical direction, and is the least efficient when applied in the longitudinal direction (parallel to the temperature gradient). In all cases, however, exponential growths of the critical Grashof number, Gr(c) (Gr, ratio of buoyancy to viscous dissipation forces) with the Hartmann number (Ha, ratio of magnetic to viscous dissipation forces) are obtained. Insight into the damping mechanism is gained from the fluctuating kinetic energy budget associated with the time-periodic disturbances at threshold. The kinetic energy produced by the vertical shear of the longitudinal basic flow dominates the oscillatory transition, and when a magnetic field is applied, it increases in order to balance the stabilizing magnetic energy. Moreover, subtle changes in the spatial distribution of this shear energy are at the origin of the exponential growth of Gr(c). The destabilizing effect of the velocity fluctuations strongly decreases when Ha is increased (due to the decay of the velocity fluctuations in the bulk accompanied by the appearance of steep gradients localized in the Hartmann layers), so that an increase of the shear of the basic flow at Gr(c) is required in order to sustain the instability. This yields an increase in Gr(c), which is reinforced by the fact that the shear of the basic flow naturally decreases at constant Gr with the increase of Ha, particularly when the magnetic field is applied in the vertical direction. For transverse and longitudinal fields, the decay of the velocity fluctuations is combined with an increase of the shear energy term due to a sustained growth in stabilizing magnetic energy with Ha. (C) 2008 American Institute of Physics.
引用
收藏
页数:12
相关论文
共 50 条