Heat and mass transfer by convection in multicomponent Navier-Stokes mixtures: absence of subcritical instabilities and global nonlinear stability via the Auxiliary System Method (Q484644)

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scientific article; zbMATH DE number 6384250
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Heat and mass transfer by convection in multicomponent Navier-Stokes mixtures: absence of subcritical instabilities and global nonlinear stability via the Auxiliary System Method
scientific article; zbMATH DE number 6384250

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    Heat and mass transfer by convection in multicomponent Navier-Stokes mixtures: absence of subcritical instabilities and global nonlinear stability via the Auxiliary System Method (English)
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    7 January 2015
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    The author has investigated the problem of mass had heat transfer by convection in horizontal layers filled by Navier-Stokes fluid mixtures with arbitrary number of different chemicals (salts) dissolved in. This problem is investigated in the general case of Navier-Stokes multicomponent fluid mixture heated from below and salted, partly from below and partly from above by \(S_{1}\), \(S_{2}\), \(\ldots\), \(S_{m}\) salts. It is shown that: \(1^{\circ}\) for each Fourier component of the perturbations to the thermal conduction solution there exists an own nonlinear system of equations as auxiliary system; \(2^{\circ}\) subcritical instabilities do not exist and the global nonlinear asymptotic \(L^{2}\)-stability is guaranteed by the condition of linear stability; \(3^{\circ}\) by the Routh-Hurwitz conditions applied to the spectral equation governing the eigenvalues of the linear associated problem rigorous stability conditions are obtained for any number of salts; \(4^{\circ}\) the Auxiliary System Method introduced by the author in [Phys. Fluids 24, No. 10, Paper No. 104101, 17 p. (2012; Zbl 1315.76018)] for the Darcy-Boussinesq fluid mixtures is extended for the Navier-Stokes fluid mixtures; \(5^{\circ}\) the looking hidden symmetries and skew symmetries allows to guarantee the global nonlinear stability by an obtained simple algebraic condition in a closed form.
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    convection
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    global stability
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    auxiliary system method
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