HEAL DSpace

A 2-D pore-network model of the drying of single-component liquids in porous media

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dc.contributor.author Yiotis, AG en
dc.contributor.author Stubos, AK en
dc.contributor.author Boudouvis, AG en
dc.contributor.author Yortsos, YC en
dc.date.accessioned 2014-03-01T01:15:58Z
dc.date.available 2014-03-01T01:15:58Z
dc.date.issued 2001 en
dc.identifier.issn 0309-1708 en
dc.identifier.uri https://dspace.lib.ntua.gr/xmlui/handle/123456789/13860
dc.subject drying en
dc.subject porous media en
dc.subject pore network en
dc.subject capillary pressure en
dc.subject invasion percolation en
dc.subject.classification Water Resources en
dc.subject.other IMMISCIBLE DISPLACEMENT en
dc.subject.other INVASION PERCOLATION en
dc.subject.other VISUALIZATION en
dc.subject.other EVAPORATION en
dc.subject.other SIMULATION en
dc.subject.other TRANSPORT en
dc.subject.other MIXTURE en
dc.title A 2-D pore-network model of the drying of single-component liquids in porous media en
heal.type journalArticle en
heal.identifier.primary 10.1016/S0309-1708(00)00066-X en
heal.identifier.secondary http://dx.doi.org/10.1016/S0309-1708(00)00066-X en
heal.language English en
heal.publicationDate 2001 en
heal.abstract The drying of liquid-saturated porous media is typically approached using macroscopic continuum models involving phenomenological coefficients. Insight on these coefficients can be obtained by a more fundamental study at the pore- and pore-network levels. In this paper, we present a model based on a pore-network representation of porous media that accounts for various processes at the pore-scale. These include mass transfer by advection and diffusion in the gas phase, viscous flow in liquid and gas phases and capillary effects at the gas-liquid menisci in the pore throats. We consider isothermal drying in a rectilinear horizontal geometry, with no-how conditions in all but one boundary, at which a purge gas is injected at a constant rate. The problem is mainly characterized by two dimensionless parameters, a diffusion-based capillary number, Ca, and a Peclet number, Pe, in addition to the various geometrical parameters of the pore network. Results on the evolution of the liquid saturation, the trapped liquid islands and the drying rate are obtained as a function of time and the dimensionless parameters. The importance of trapped liquid islands on screening mass transfer to the continuous liquid cluster is emphasized. For fixed parameter values, the drying front does not in general obey invasion percolation rules. However, as drying progresses, and depending on the relative magnitude of the capillary and Peclet numbers, a transition to a percolation-controlled problem occurs. Effects of capillarity and mass transfer on Saturation profiles and drying rates are discussed. The results are then used to discuss upscaling to continuum models. (C) 2001 Elsevier Science Ltd. All rights reserved. en
heal.publisher ELSEVIER SCI LTD en
heal.journalName ADVANCES IN WATER RESOURCES en
dc.identifier.doi 10.1016/S0309-1708(00)00066-X en
dc.identifier.isi ISI:000166845100013 en
dc.identifier.volume 24 en
dc.identifier.issue 3-4 en
dc.identifier.spage 439 en
dc.identifier.epage 460 en


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