Non-equilibrium partitioning tracer transport in porous media: 2-D physical modelling and imaging using a partitioning fluorescent dye
This paper describes an investigation into non-equilibrium partitioning tracer transport and interaction with non-aqueous-phase liquid (NAPL) contaminated water-saturated porous media using a two-dimensional (2-D) physical modelling methodology. A fluorescent partitioning tracer is employed within a...
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Veröffentlicht in: | Water research (Oxford) 2005-12, Vol.39 (20), p.5099-5111 |
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description | This paper describes an investigation into non-equilibrium partitioning tracer transport and interaction with non-aqueous-phase liquid (NAPL) contaminated water-saturated porous media using a two-dimensional (2-D) physical modelling methodology. A fluorescent partitioning tracer is employed within a transparent porous model which when imaged by a CCD digital camera can provide full spatial tracer concentrations and tracer breakthrough curves. Quasi one-dimensional (1-D) benchmarking tests in models packed with various combinations of clean quartz sand and NAPL are described. These modelled residual NAPL saturations,
S
n, of 0–15%. Results demonstrated that the fluorescent partitioning tracer was able to detect and quantify the presence of NAPL at low flow rates. At larger flow rates and/or higher NAPL saturations, the tracer increasingly underpredicted the NAPL volume as expected and this is attributed primarily to non-equilibrium partitioning. Despite little change in permeability, change in NAPL saturations from 4% to 8% resulted in significant NAPL saturation underestimates at the same flow rates implying coalescence of NAPL into wider separated but larger ganglia. A 2-D investigation of an idealised heterogeneous residual NAPL contaminated flow field indicated little permeability change in the NAPL contaminated zone and thus little flow bypassing, leading to reduced underpredictions of NAPL saturations than for equivalent quasi 1-D cases. This was attributed to increased ‘sampling’ of the NAPL by the tracer. The process is clearly visually identifiable from the experimental images. This rapid and relatively inexpensive experimental method is of value in laboratory studies of partitioning tracer behaviour in porous media; in particular, the ability to observe full field concentrations makes it valuable for the study of complex heterogeneous systems. |
doi_str_mv | 10.1016/j.watres.2005.09.044 |
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S
n, of 0–15%. Results demonstrated that the fluorescent partitioning tracer was able to detect and quantify the presence of NAPL at low flow rates. At larger flow rates and/or higher NAPL saturations, the tracer increasingly underpredicted the NAPL volume as expected and this is attributed primarily to non-equilibrium partitioning. Despite little change in permeability, change in NAPL saturations from 4% to 8% resulted in significant NAPL saturation underestimates at the same flow rates implying coalescence of NAPL into wider separated but larger ganglia. A 2-D investigation of an idealised heterogeneous residual NAPL contaminated flow field indicated little permeability change in the NAPL contaminated zone and thus little flow bypassing, leading to reduced underpredictions of NAPL saturations than for equivalent quasi 1-D cases. This was attributed to increased ‘sampling’ of the NAPL by the tracer. The process is clearly visually identifiable from the experimental images. This rapid and relatively inexpensive experimental method is of value in laboratory studies of partitioning tracer behaviour in porous media; in particular, the ability to observe full field concentrations makes it valuable for the study of complex heterogeneous systems.</description><identifier>ISSN: 0043-1354</identifier><identifier>EISSN: 1879-2448</identifier><identifier>DOI: 10.1016/j.watres.2005.09.044</identifier><identifier>PMID: 16298415</identifier><identifier>CODEN: WATRAG</identifier><language>eng</language><publisher>Oxford: Elsevier Ltd</publisher><subject>1-Octanol ; Applied sciences ; Earth sciences ; Earth, ocean, space ; Engineering and environment geology. Geothermics ; Environmental Monitoring - methods ; Exact sciences and technology ; Flow bypass ; Fluorescein ; Fluorescence ; Fluorescent Dyes ; Fluorescent tracer ; Groundwaters ; Image Processing, Computer-Assisted ; Models, Theoretical ; NAPL characterisation ; Natural water pollution ; Non-invasive technique ; Partitioning tracer ; Pollution ; Pollution, environment geology ; Porous media ; Quartz ; Residual saturation ; Ultraviolet Rays ; Water Movements ; Water Pollutants, Chemical ; Water treatment and pollution</subject><ispartof>Water research (Oxford), 2005-12, Vol.39 (20), p.5099-5111</ispartof><rights>2005 Elsevier Ltd</rights><rights>2006 INIST-CNRS</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c421t-8c5ffe3d922a6ef2bc13a45bfea34d4e79d5510381d65f4ecee502f270a45d853</citedby><cites>FETCH-LOGICAL-c421t-8c5ffe3d922a6ef2bc13a45bfea34d4e79d5510381d65f4ecee502f270a45d853</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://www.sciencedirect.com/science/article/pii/S0043135405005567$$EHTML$$P50$$Gelsevier$$H</linktohtml><link.rule.ids>314,776,780,3536,27903,27904,65309</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=17345790$$DView record in Pascal Francis$$Hfree_for_read</backlink><backlink>$$Uhttps://www.ncbi.nlm.nih.gov/pubmed/16298415$$D View this record in MEDLINE/PubMed$$Hfree_for_read</backlink></links><search><creatorcontrib>Jones, Edward H.</creatorcontrib><creatorcontrib>Smith, Colin C.</creatorcontrib><title>Non-equilibrium partitioning tracer transport in porous media: 2-D physical modelling and imaging using a partitioning fluorescent dye</title><title>Water research (Oxford)</title><addtitle>Water Res</addtitle><description>This paper describes an investigation into non-equilibrium partitioning tracer transport and interaction with non-aqueous-phase liquid (NAPL) contaminated water-saturated porous media using a two-dimensional (2-D) physical modelling methodology. A fluorescent partitioning tracer is employed within a transparent porous model which when imaged by a CCD digital camera can provide full spatial tracer concentrations and tracer breakthrough curves. Quasi one-dimensional (1-D) benchmarking tests in models packed with various combinations of clean quartz sand and NAPL are described. These modelled residual NAPL saturations,
S
n, of 0–15%. Results demonstrated that the fluorescent partitioning tracer was able to detect and quantify the presence of NAPL at low flow rates. At larger flow rates and/or higher NAPL saturations, the tracer increasingly underpredicted the NAPL volume as expected and this is attributed primarily to non-equilibrium partitioning. Despite little change in permeability, change in NAPL saturations from 4% to 8% resulted in significant NAPL saturation underestimates at the same flow rates implying coalescence of NAPL into wider separated but larger ganglia. A 2-D investigation of an idealised heterogeneous residual NAPL contaminated flow field indicated little permeability change in the NAPL contaminated zone and thus little flow bypassing, leading to reduced underpredictions of NAPL saturations than for equivalent quasi 1-D cases. This was attributed to increased ‘sampling’ of the NAPL by the tracer. The process is clearly visually identifiable from the experimental images. This rapid and relatively inexpensive experimental method is of value in laboratory studies of partitioning tracer behaviour in porous media; in particular, the ability to observe full field concentrations makes it valuable for the study of complex heterogeneous systems.</description><subject>1-Octanol</subject><subject>Applied sciences</subject><subject>Earth sciences</subject><subject>Earth, ocean, space</subject><subject>Engineering and environment geology. Geothermics</subject><subject>Environmental Monitoring - methods</subject><subject>Exact sciences and technology</subject><subject>Flow bypass</subject><subject>Fluorescein</subject><subject>Fluorescence</subject><subject>Fluorescent Dyes</subject><subject>Fluorescent tracer</subject><subject>Groundwaters</subject><subject>Image Processing, Computer-Assisted</subject><subject>Models, Theoretical</subject><subject>NAPL characterisation</subject><subject>Natural water pollution</subject><subject>Non-invasive technique</subject><subject>Partitioning tracer</subject><subject>Pollution</subject><subject>Pollution, environment geology</subject><subject>Porous media</subject><subject>Quartz</subject><subject>Residual saturation</subject><subject>Ultraviolet Rays</subject><subject>Water Movements</subject><subject>Water Pollutants, Chemical</subject><subject>Water treatment and pollution</subject><issn>0043-1354</issn><issn>1879-2448</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2005</creationdate><recordtype>article</recordtype><sourceid>EIF</sourceid><recordid>eNp9kE1v1DAQhi0EokvhHyDkC9yS-nOTcECqyqdU0Us5W157XLxK7NR2QPsH-rtx2JUqLpxmZD0zfudB6DUlLSV0e7Fvf-uSILeMENmSoSVCPEEb2ndDw4Ton6INIYI3lEtxhl7kvCeEMMaH5-iMbtnQCyo36OF7DA3cL370u-SXCc86FV98DD7c4ZK0gbSWkOeYCvYB1xqXjCewXr_HrPmI55-H7I0e8RQtjOM6qIPFftJ3a7_kvy__bnbjEmt4A6Fge4CX6JnTY4ZXp3qOfnz-dHv1tbm--fLt6vK6MYLR0vRGOgfcDozpLTi2M5RrIXcONBdWQDdYKSnhPbVb6QQYAEmYYx2plO0lP0fvjnvnFO8XyEVNvoYYRx2gXqVoxyijhFRQHEGTYs4JnJpTPSgdFCVq9a_26uhfrf4VGVT1X8fenPYvu2rocegkvAJvT4DOVZmrZo3Pj1zHheyG9f8PRw6qjV8eksrGQzDVegJTlI3-_0n-AK1mqR0</recordid><startdate>20051201</startdate><enddate>20051201</enddate><creator>Jones, Edward H.</creator><creator>Smith, Colin C.</creator><general>Elsevier Ltd</general><general>Elsevier Science</general><scope>IQODW</scope><scope>CGR</scope><scope>CUY</scope><scope>CVF</scope><scope>ECM</scope><scope>EIF</scope><scope>NPM</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7QH</scope><scope>7TV</scope><scope>7UA</scope><scope>C1K</scope><scope>F1W</scope><scope>H96</scope><scope>L.G</scope></search><sort><creationdate>20051201</creationdate><title>Non-equilibrium partitioning tracer transport in porous media: 2-D physical modelling and imaging using a partitioning fluorescent dye</title><author>Jones, Edward H. ; Smith, Colin C.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c421t-8c5ffe3d922a6ef2bc13a45bfea34d4e79d5510381d65f4ecee502f270a45d853</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2005</creationdate><topic>1-Octanol</topic><topic>Applied sciences</topic><topic>Earth sciences</topic><topic>Earth, ocean, space</topic><topic>Engineering and environment geology. Geothermics</topic><topic>Environmental Monitoring - methods</topic><topic>Exact sciences and technology</topic><topic>Flow bypass</topic><topic>Fluorescein</topic><topic>Fluorescence</topic><topic>Fluorescent Dyes</topic><topic>Fluorescent tracer</topic><topic>Groundwaters</topic><topic>Image Processing, Computer-Assisted</topic><topic>Models, Theoretical</topic><topic>NAPL characterisation</topic><topic>Natural water pollution</topic><topic>Non-invasive technique</topic><topic>Partitioning tracer</topic><topic>Pollution</topic><topic>Pollution, environment geology</topic><topic>Porous media</topic><topic>Quartz</topic><topic>Residual saturation</topic><topic>Ultraviolet Rays</topic><topic>Water Movements</topic><topic>Water Pollutants, Chemical</topic><topic>Water treatment and pollution</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Jones, Edward H.</creatorcontrib><creatorcontrib>Smith, Colin C.</creatorcontrib><collection>Pascal-Francis</collection><collection>Medline</collection><collection>MEDLINE</collection><collection>MEDLINE (Ovid)</collection><collection>MEDLINE</collection><collection>MEDLINE</collection><collection>PubMed</collection><collection>CrossRef</collection><collection>Aqualine</collection><collection>Pollution Abstracts</collection><collection>Water Resources Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><jtitle>Water research (Oxford)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Jones, Edward H.</au><au>Smith, Colin C.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Non-equilibrium partitioning tracer transport in porous media: 2-D physical modelling and imaging using a partitioning fluorescent dye</atitle><jtitle>Water research (Oxford)</jtitle><addtitle>Water Res</addtitle><date>2005-12-01</date><risdate>2005</risdate><volume>39</volume><issue>20</issue><spage>5099</spage><epage>5111</epage><pages>5099-5111</pages><issn>0043-1354</issn><eissn>1879-2448</eissn><coden>WATRAG</coden><abstract>This paper describes an investigation into non-equilibrium partitioning tracer transport and interaction with non-aqueous-phase liquid (NAPL) contaminated water-saturated porous media using a two-dimensional (2-D) physical modelling methodology. A fluorescent partitioning tracer is employed within a transparent porous model which when imaged by a CCD digital camera can provide full spatial tracer concentrations and tracer breakthrough curves. Quasi one-dimensional (1-D) benchmarking tests in models packed with various combinations of clean quartz sand and NAPL are described. These modelled residual NAPL saturations,
S
n, of 0–15%. Results demonstrated that the fluorescent partitioning tracer was able to detect and quantify the presence of NAPL at low flow rates. At larger flow rates and/or higher NAPL saturations, the tracer increasingly underpredicted the NAPL volume as expected and this is attributed primarily to non-equilibrium partitioning. Despite little change in permeability, change in NAPL saturations from 4% to 8% resulted in significant NAPL saturation underestimates at the same flow rates implying coalescence of NAPL into wider separated but larger ganglia. A 2-D investigation of an idealised heterogeneous residual NAPL contaminated flow field indicated little permeability change in the NAPL contaminated zone and thus little flow bypassing, leading to reduced underpredictions of NAPL saturations than for equivalent quasi 1-D cases. This was attributed to increased ‘sampling’ of the NAPL by the tracer. The process is clearly visually identifiable from the experimental images. This rapid and relatively inexpensive experimental method is of value in laboratory studies of partitioning tracer behaviour in porous media; in particular, the ability to observe full field concentrations makes it valuable for the study of complex heterogeneous systems.</abstract><cop>Oxford</cop><pub>Elsevier Ltd</pub><pmid>16298415</pmid><doi>10.1016/j.watres.2005.09.044</doi><tpages>13</tpages></addata></record> |
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subjects | 1-Octanol Applied sciences Earth sciences Earth, ocean, space Engineering and environment geology. Geothermics Environmental Monitoring - methods Exact sciences and technology Flow bypass Fluorescein Fluorescence Fluorescent Dyes Fluorescent tracer Groundwaters Image Processing, Computer-Assisted Models, Theoretical NAPL characterisation Natural water pollution Non-invasive technique Partitioning tracer Pollution Pollution, environment geology Porous media Quartz Residual saturation Ultraviolet Rays Water Movements Water Pollutants, Chemical Water treatment and pollution |
title | Non-equilibrium partitioning tracer transport in porous media: 2-D physical modelling and imaging using a partitioning fluorescent dye |
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