Effect of water content on transient nonequilibrium NAPL–gas mass transfer during soil vapor extraction

The effect of water content on the volatilization of nonaqueous phase liquid (NAPL) in unsaturated soils was characterized by one-dimensional venting experiments conducted to evaluate the lumped mass transfer coefficient. An empirical correlation based upon the modified Sherwood number, Peclet numbe...

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Veröffentlicht in:Journal of contaminant hydrology 2002, Vol.54 (1), p.1-18
Hauptverfasser: Yoon, Hongkyu, Kim, Joong Hoon, Liljestrand, Howard M, Khim, Jeehyeong
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container_issue 1
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container_title Journal of contaminant hydrology
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creator Yoon, Hongkyu
Kim, Joong Hoon
Liljestrand, Howard M
Khim, Jeehyeong
description The effect of water content on the volatilization of nonaqueous phase liquid (NAPL) in unsaturated soils was characterized by one-dimensional venting experiments conducted to evaluate the lumped mass transfer coefficient. An empirical correlation based upon the modified Sherwood number, Peclet number, and normalized mean grain size was used to estimate initial lumped mass transfer coefficients over a range of water content. The effects of water content on the soil vapor extraction SVE process have been investigated through experimentation and mathematical modeling. The experimental results indicated that a rate-limited NAPL–gas mass transfer occurred in water-wet soils. A severe mass transfer limitation was observed at 61.0% water saturation where the normalized effluent gas concentrations fell below 1.0 almost immediately, declined exponentially from the initiation of venting, and showed long tailing. This result was attributed to the reduction of interfacial area between the NAPL and mobile gas phases due to the increased water content. A transient mathematical model describing the change of the lumped mass transfer coefficient was used. Simulations showed that the nonequilibrium mass transfer process could be characterized by the exponent β, a parameter which described the reduction of the specific area available for NAPL volatilization. The nonequilibrium mass transfer limitations were controlled by the soil mean grain size and pore gas velocity, were well described by β values below 1.0 at low water saturation, and were well predicted with β values greater than 1.0 at high water saturation.
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Simulations showed that the nonequilibrium mass transfer process could be characterized by the exponent β, a parameter which described the reduction of the specific area available for NAPL volatilization. The nonequilibrium mass transfer limitations were controlled by the soil mean grain size and pore gas velocity, were well described by β values below 1.0 at low water saturation, and were well predicted with β values greater than 1.0 at high water saturation.</description><subject>Computer simulation</subject><subject>Contaminants</subject><subject>Earth sciences</subject><subject>Earth, ocean, space</subject><subject>Effluents</subject><subject>Empirical analysis</subject><subject>Engineering and environment geology. Geothermics</subject><subject>Exact sciences and technology</subject><subject>Gas phases</subject><subject>Gases</subject><subject>Hydrogeology</subject><subject>Hydrology</subject><subject>Hydrology. 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Simulations showed that the nonequilibrium mass transfer process could be characterized by the exponent β, a parameter which described the reduction of the specific area available for NAPL volatilization. The nonequilibrium mass transfer limitations were controlled by the soil mean grain size and pore gas velocity, were well described by β values below 1.0 at low water saturation, and were well predicted with β values greater than 1.0 at high water saturation.</abstract><cop>Amsterdam</cop><pub>Elsevier B.V</pub><pmid>11848263</pmid><doi>10.1016/S0169-7722(01)00164-4</doi><tpages>18</tpages></addata></record>
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subjects Computer simulation
Contaminants
Earth sciences
Earth, ocean, space
Effluents
Empirical analysis
Engineering and environment geology. Geothermics
Exact sciences and technology
Gas phases
Gases
Hydrogeology
Hydrology
Hydrology. Hydrogeology
Mass transfer
Mathematical models
Models, Theoretical
Moisture content
Nonaqueous phase liquid (NAPL)
Pollution, environment geology
Porosity
Soil (material)
Soil Pollutants - analysis
Soil vapor extraction
Soils
Surficial geology
Vapors
Velocity
Venting
Volatilization
Water
Water saturation
title Effect of water content on transient nonequilibrium NAPL–gas mass transfer during soil vapor extraction
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