Three-phase flow analysis of dense nonaqueous phase liquid infiltration in horizontally layered porous media

We considered dense nonaqueous phase liquid (DNAPL) infiltration into a water-unsaturated porous medium that consists of two horizontal layers, of which the top layer has a lower intrinsic permeability than the bottom layer. DNAPL is the intermediate-wetting fluid with respect to the wetting water and the nonwetting air. The layer interface forms a barrier to DNAPL flow, which causes the DNAPL to spread out horizontally just above the interface. An analytical approximation has been developed to estimate the DNAPL pressure and saturation and the horizontal extension of the DNAPL above the layer interface at steady state for low water saturations. The analytical approximation shows that the DNAPL infiltration is determined by five dimensionless numbers: the heterogeneity factor ¿, the capillary pressure parameter ¿, the gravity number N g , the ratio of the capillary and gravity numbers N c /N g , and the critical DNAPL pressure P o c . Its predictions were compared with the results of a numerical three-phase flow simulator for a number of parameter combinations. For most of these combinations the analytical approximation predicts the DNAPL pressure and saturation profiles at the interface adequately. Using the analytical approximation, we carried out a sensitivity study with respect to the maximum horizontal extension of the plume. The extension of the plumes appears to be highly sensitive to variation of the dimensionless numbers P o c , ¿ and ¿

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Main Authors: Wipfler, E.L., van Dijke, M.I.J., van der Zee, S.E.A.T.M.
Format: Article/Letter to editor biblioteca
Language:English
Subjects:capillary forces, groundwater, groundwater flow, hydrology, infiltration, porous media, redistribution, soil water movement, water quality, bodemwaterbeweging, grondwater, grondwaterstroming, hydrologie, infiltratie, poreus medium, waterkwaliteit,
Online Access:https://research.wur.nl/en/publications/three-phase-flow-analysis-of-dense-nonaqueous-phase-liquid-infilt
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spelling dig-wur-nl-wurpubs-3521552024-12-04 Wipfler, E.L. van Dijke, M.I.J. van der Zee, S.E.A.T.M. Article/Letter to editor Water Resources Research 40 (2004) ISSN: 0043-1397 Three-phase flow analysis of dense nonaqueous phase liquid infiltration in horizontally layered porous media 2004 We considered dense nonaqueous phase liquid (DNAPL) infiltration into a water-unsaturated porous medium that consists of two horizontal layers, of which the top layer has a lower intrinsic permeability than the bottom layer. DNAPL is the intermediate-wetting fluid with respect to the wetting water and the nonwetting air. The layer interface forms a barrier to DNAPL flow, which causes the DNAPL to spread out horizontally just above the interface. An analytical approximation has been developed to estimate the DNAPL pressure and saturation and the horizontal extension of the DNAPL above the layer interface at steady state for low water saturations. The analytical approximation shows that the DNAPL infiltration is determined by five dimensionless numbers: the heterogeneity factor ¿, the capillary pressure parameter ¿, the gravity number N g , the ratio of the capillary and gravity numbers N c /N g , and the critical DNAPL pressure P o c . Its predictions were compared with the results of a numerical three-phase flow simulator for a number of parameter combinations. For most of these combinations the analytical approximation predicts the DNAPL pressure and saturation profiles at the interface adequately. Using the analytical approximation, we carried out a sensitivity study with respect to the maximum horizontal extension of the plume. The extension of the plumes appears to be highly sensitive to variation of the dimensionless numbers P o c , ¿ and ¿ en application/pdf https://research.wur.nl/en/publications/three-phase-flow-analysis-of-dense-nonaqueous-phase-liquid-infilt 10.1029/2003WR002948 https://edepot.wur.nl/10262 capillary forces groundwater groundwater flow hydrology infiltration porous media redistribution soil water movement water quality bodemwaterbeweging grondwater grondwaterstroming hydrologie infiltratie poreus medium waterkwaliteit Wageningen University & Research
institution WUR NL
collection DSpace
country Países bajos
countrycode NL
component Bibliográfico
access En linea
databasecode dig-wur-nl
tag biblioteca
region Europa del Oeste
libraryname WUR Library Netherlands
language English
topic capillary forces
groundwater
groundwater flow
hydrology
infiltration
porous media
redistribution
soil water movement
water quality
bodemwaterbeweging
grondwater
grondwaterstroming
hydrologie
infiltratie
poreus medium
waterkwaliteit
capillary forces
groundwater
groundwater flow
hydrology
infiltration
porous media
redistribution
soil water movement
water quality
bodemwaterbeweging
grondwater
grondwaterstroming
hydrologie
infiltratie
poreus medium
waterkwaliteit
spellingShingle capillary forces
groundwater
groundwater flow
hydrology
infiltration
porous media
redistribution
soil water movement
water quality
bodemwaterbeweging
grondwater
grondwaterstroming
hydrologie
infiltratie
poreus medium
waterkwaliteit
capillary forces
groundwater
groundwater flow
hydrology
infiltration
porous media
redistribution
soil water movement
water quality
bodemwaterbeweging
grondwater
grondwaterstroming
hydrologie
infiltratie
poreus medium
waterkwaliteit
Wipfler, E.L.
van Dijke, M.I.J.
van der Zee, S.E.A.T.M.
Three-phase flow analysis of dense nonaqueous phase liquid infiltration in horizontally layered porous media
description We considered dense nonaqueous phase liquid (DNAPL) infiltration into a water-unsaturated porous medium that consists of two horizontal layers, of which the top layer has a lower intrinsic permeability than the bottom layer. DNAPL is the intermediate-wetting fluid with respect to the wetting water and the nonwetting air. The layer interface forms a barrier to DNAPL flow, which causes the DNAPL to spread out horizontally just above the interface. An analytical approximation has been developed to estimate the DNAPL pressure and saturation and the horizontal extension of the DNAPL above the layer interface at steady state for low water saturations. The analytical approximation shows that the DNAPL infiltration is determined by five dimensionless numbers: the heterogeneity factor ¿, the capillary pressure parameter ¿, the gravity number N g , the ratio of the capillary and gravity numbers N c /N g , and the critical DNAPL pressure P o c . Its predictions were compared with the results of a numerical three-phase flow simulator for a number of parameter combinations. For most of these combinations the analytical approximation predicts the DNAPL pressure and saturation profiles at the interface adequately. Using the analytical approximation, we carried out a sensitivity study with respect to the maximum horizontal extension of the plume. The extension of the plumes appears to be highly sensitive to variation of the dimensionless numbers P o c , ¿ and ¿
format Article/Letter to editor
topic_facet capillary forces
groundwater
groundwater flow
hydrology
infiltration
porous media
redistribution
soil water movement
water quality
bodemwaterbeweging
grondwater
grondwaterstroming
hydrologie
infiltratie
poreus medium
waterkwaliteit
author Wipfler, E.L.
van Dijke, M.I.J.
van der Zee, S.E.A.T.M.
author_facet Wipfler, E.L.
van Dijke, M.I.J.
van der Zee, S.E.A.T.M.
author_sort Wipfler, E.L.
title Three-phase flow analysis of dense nonaqueous phase liquid infiltration in horizontally layered porous media
title_short Three-phase flow analysis of dense nonaqueous phase liquid infiltration in horizontally layered porous media
title_full Three-phase flow analysis of dense nonaqueous phase liquid infiltration in horizontally layered porous media
title_fullStr Three-phase flow analysis of dense nonaqueous phase liquid infiltration in horizontally layered porous media
title_full_unstemmed Three-phase flow analysis of dense nonaqueous phase liquid infiltration in horizontally layered porous media
title_sort three-phase flow analysis of dense nonaqueous phase liquid infiltration in horizontally layered porous media
url https://research.wur.nl/en/publications/three-phase-flow-analysis-of-dense-nonaqueous-phase-liquid-infilt
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AT vanderzeeseatm threephaseflowanalysisofdensenonaqueousphaseliquidinfiltrationinhorizontallylayeredporousmedia
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