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Existence of a steady-statewater evaporation front in a horizontally extended low-permeability region

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Abstract

Flow with a phase transition interface in a horizontally extended porous medium is considered when a heavier phase (water) is located above a lighter phase (air-steam mixture). It is shown that if there exists a steady-state flow with a plane phase interface and this flow is stable with respect to infinitely small harmonic surface perturbations then only a local finite perturbation of the upper or lower boundary of the low-conductivity layer directed upward can lead to disappearance of the steady-state solution. This flow restructuring is possible only in the case of immiscible porous medium. Using a numerical experiment, it is shown that there exists a threshold value of the absolute value of the amplitude above which the steady-state flow ceases to exist. This threshold value decreases with increase in the “effective” width of the localized perturbation and tends asymptotically to a value corresponding to infinitely large effective width of the localized perturbation. An analytic expression for this quantity is found.

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Correspondence to A. V. Shargatov.

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Original Russian Text © S.A. Gubin, V.A. Krivosheev, A.V. Shargatov, 2015, published in Izvestiya Rossiiskoi Akademii Nauk, Mekhanika Zhidkosti i Gaza, 2015, Vol. 50, No. 2, pp. 70–80.

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Gubin, S.A., Krivosheev, V.A. & Shargatov, A.V. Existence of a steady-statewater evaporation front in a horizontally extended low-permeability region. Fluid Dyn 50, 240–249 (2015). https://doi.org/10.1134/S0015462815020088

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  • DOI: https://doi.org/10.1134/S0015462815020088

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