On the nonlinear dynamics of a saline boundary layer formed by throughflow near the surface of a porous medium

DOI10.1016/J.PHYSD.2008.06.004zbMath1407.76153OpenAlexW1963948123MaRDI QIDQ1000690

G. J. M. Pieters, Henk M. Schuttelaars

Publication date: 10 February 2009

Published in: Physica D (Search for Journal in Brave)

Full work available at URL: https://doi.org/10.1016/j.physd.2008.06.004

zbMATH Keywords

flow in porous mediamodel reductionGalerkin projectionnumerical bifurcation analysisnon-self-adjointness

Mathematics Subject Classification ID

Hydrology, hydrography, oceanography (86A05) Diffusion (76R50) Absolute and convective instability and stability in hydrodynamic stability (76E15) Flows in porous media; filtration; seepage (76S05) Stability and instability of geophysical and astrophysical flows (76E20)

Related Items (4)

Coincidence between linear and global nonlinear stability of non-constant throughflows via the Rionero ``auxiliary system method ⋮ On the stability-instability of vertical throughflows in double diffusive mixtures saturating rotating porous layers with large pores ⋮ Transient growth in linearly stable gravity-driven flow in porous media ⋮ Tracking pattern evolution through extended center manifold reduction and singular perturbations

Cites Work

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• Transient growth in linearly stable gravity-driven flow in porous media
• Centre manifold reduction and the Stuart‐Landau equation for fluid motions
• Instability of time-dependent wind-driven ocean gyres
• Oscillatory convection in a porous medium heated from below
• Convection in Porous Media
• Finite bandwidth, finite amplitude convection
• Elements of applied bifurcation theory
• Handbook of stochastic methods for physics, chemistry and natural sciences.

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