Abstract
Flow of a fluid through a porous medium is considered with allowance for heat conduction. Both fronts at which the liquid is transformed into steam or a liquid-steam mixture and fronts with inverse transformations are studied. The evolutionarity conditions of these fronts are considered and a model of their structure is proposed.
This is a preview of subscription content, log in via an institution to check access.
Similar content being viewed by others
REFERENCES
G. G. Tsypkin, “Occurrence of two moving phase transition boundaries in the recovery of steam from a watersaturated hydrothermal reservoir,” Dokl. Ros. Akad. Nauk, 337, 748 (1994).
A.A. Barmin and G.G. Tsypkin, “Mathematical model of water injection into a steam-saturated geothermal reservoir,” Izv. Ros. Akad. Nauk, Mekh. Zhidk. Gaza, No. 6, 92 (1996).
A.V. Kondrashov and G.G. Tsypkin, “Regimes of water injection into a steam-saturated geothermal reservoir,” Izv. Ros. Akad. Nauk, Mekh. Zhidk. Gaza, No. 2, 86 (1999).
A. A. Barmin and A.V. Kondrashov, “Two-front mathematical model of water injection into a steam-saturated geothermal reservoir,” Izv. Ros. Akad. Nauk, Mekh. Zhidk. Gaza, No. 3, 105 (2000).
R. J. Briggs, Electron Stream Interaction with Plasma, MIT Press, Cambridge (1964).
A.G. Kulikovskii and E. I. Sveshnikova, Nonlinear Waves in Elastic Media, CRS Press, Boca Raton, etc. (1995).
Rights and permissions
About this article
Cite this article
Kulikovskii, A.G. Evaporation and Condensation Fronts in Porous Media. Fluid Dynamics 37, 740–746 (2002). https://doi.org/10.1023/A:1021372403318
Issue Date:
DOI: https://doi.org/10.1023/A:1021372403318