Mixed-mode instability of a miscible interface due to coupling between Rayleigh-Taylor and double-diffusive convective modes

被引:46
作者
Carballido-Landeira, J. [1 ,2 ]
Trevelyan, P. M. J. [1 ,3 ]
Almarcha, C. [1 ,4 ]
De Wit, A. [1 ]
机构
[1] Univ Libre Bruxelles, Nonlinear Phys Chem Unit, Serv Chim Phys & Biol Theor, Fac Sci, B-1050 Brussels, Belgium
[2] Univ Santiago de Compostela, Grp Nonlinear Phys, E-15782 Santiago De Compostela, Spain
[3] Univ Glamorgan, Div Math & Stat, Pontypridd CF37 1DL, M Glam, Wales
[4] IRPHE, UMR 7342, F-13013 Marseille, France
关键词
BUOYANCY-DRIVEN INSTABILITIES; FINGER CONVECTION; POROUS-MEDIA; DISPLACEMENTS; COEFFICIENTS; SIMULATION; STABILITY;
D O I
10.1063/1.4790192
中图分类号
O3 [力学];
学科分类号
08 ; 0801 ;
摘要
In a gravitational field, a horizontal interface between two miscible fluids can be buoyantly unstable because of double diffusive effects or because of a Rayleigh-Taylor instability arising when a denser fluid lies on top of a less dense one. We show here both experimentally and theoretically that, besides such classical buoyancy-driven instabilities, a new mixed mode dynamics exists when these two instabilities act cooperatively. This is the case when the upper denser solution contains a solute A, which diffuses sufficiently faster than a solute B initially in the lower layer to yield non-monotonic density profiles after contact of the two solutions. We derive analytically the conditions for existence of this mixed mode in the (R, delta) parameter plane, where R is the buoyancy ratio between the two solutions and delta is the ratio of diffusion coefficient of the solutes. We find an excellent agreement of these theoretical predictions with experiments performed in Hele-Shawcells and with numerical simulations. (C) 2013 American Institute of Physics. [http://dx.doi.org/10.1063/1.4790192]
引用
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页数:10
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