Stability of three-dimensional columnar convection in a porous medium

被引:11
|
作者
Hewitt, Duncan R. [1 ]
Lister, John R. [1 ]
机构
[1] Univ Cambridge, Dept Appl Math & Theoret Phys, Wilberforce Rd, Cambridge CB3 0WA, England
关键词
convection in porous media; instability; porous media; RAYLEIGH-NUMBER CONVECTION;
D O I
10.1017/jfm.2017.561
中图分类号
O3 [力学];
学科分类号
08 ; 0801 ;
摘要
The stability of steady convective exchange flow with a rectangular planform in an unbounded three-dimensional porous medium is explored. The base flow comprises a balance between vertical advection with amplitude in interleaving rectangular columns with aspect ratio and xi <= 1 horizontal diffusion between the columns. Columnar flow with a square planform ((xi) = 1) is found to be weakly unstable to a large-scale perturbation of the background temperature gradient, irrespective of , but to have no stronger instability on the scale of the columns. This result provides a stark contrast to two-dimensional columnar flow (Hewitt et al., J. Fluid Mech., vol. 737, 2013, pp. 205231), which, as is increased, is increasingly unstable to a perturbation on the scale of the columnar wavelength. For rectangular planforms xi <= 1 with , a critical aspect ratio is identified, below which a perturbation on the scale of the columns is the fastest growing mode, as in two dimensions. Scalings for the growth rate and the structure of this mode are identified, and are explained by means of an asymptotic expansion in the limit xi -> 1. The difference between the stabilities of two-dimensional and three-dimensional exchange flow provides a potential explanation for the apparent difference in dominant horizontal scale observed in direct numerical simulations of two-dimensional and three-dimensional statistically steady RayleighDarcy convection at high Rayleigh numbers.
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页码:89 / 111
页数:23
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