Saturation front evolution for liquid infiltration into a gas filled porous medium with counter-current flow

Peter D Hicks, Mark J Cooker, Adrian J Matthews

Research output: Contribution to journalArticle

1 Citation (Scopus)

Abstract

The infiltration of liquid into a gas saturated porous network is investigated. Particular attention is paid to the situation in which a pressure gradient in the porous medium drives a gas flow upwards, while a more dense liquid infiltrates down into the reservoir due to gravity. There are two flows in opposite directions. A model is proposed, based upon a compressible gas phase and an incompressible liquid phase. The volume fluxes in each phase are assumed to be governed by Darcy type flow laws, modified to include the permeability caused by both the solid matrix and the impeding of the gas flow by the liquid phase. Isothermal flows are examined in the absence of phase changes. The proposed model is an extension of the traditional Buckley-Leverett model and is used to consider a variety of flows, including carbon sequestration in a porous medium below the seabed and rainfall infiltration into a lava dome.
Original languageEnglish
Pages (from-to)202-215
Number of pages14
JournalEuropean Journal of Mechanics B, Fluids
Volume43
Early online date27 Sep 2013
DOIs
Publication statusPublished - Jan 2014

Fingerprint

Infiltration
infiltration
Porous Media
Saturation
counters
Liquid
saturation
gas flow
liquid phases
liquids
Gas Flow
gases
isothermal flow
lava
domes
pressure gradients
Dome
Phase Change
permeability
Rainfall

Keywords

  • porous media
  • infiltration
  • counter-current flow
  • compressible gas

Cite this

Saturation front evolution for liquid infiltration into a gas filled porous medium with counter-current flow. / Hicks, Peter D; Cooker, Mark J; Matthews, Adrian J.

In: European Journal of Mechanics B, Fluids, Vol. 43, 01.2014, p. 202-215.

Research output: Contribution to journalArticle

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