1989
DOI: 10.1016/0169-7722(89)90023-5
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Removing volatile contaminants from the unsaturated zone by inducing advective air-phase transport

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Cited by 145 publications
(45 citation statements)
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“…When soil gas concentration decreases, the local chemical equilibrium is perturbed, causing the transfer of volatile oil from the NAPL phase into the soil gas, where it can be removed. Traditionally, an equilibrium mass transfer approach is used to describe NAPL volatilization where the time needed for oil to transfer from the NAPL to the gas phase at local scale is assumed to be very short compared to bulk gas movement (e.g., Corapcioglu and Baehr 1987;Baehr 1987;Wilson et al 1987;Wilson et al 1988;Baehr et al 1989;Johnson et al 1990). However, an equilibrium mass transfer approach is a maximum rate and can overestimate NAPL volatilization.…”
Section: 1mentioning
confidence: 99%
See 1 more Smart Citation
“…When soil gas concentration decreases, the local chemical equilibrium is perturbed, causing the transfer of volatile oil from the NAPL phase into the soil gas, where it can be removed. Traditionally, an equilibrium mass transfer approach is used to describe NAPL volatilization where the time needed for oil to transfer from the NAPL to the gas phase at local scale is assumed to be very short compared to bulk gas movement (e.g., Corapcioglu and Baehr 1987;Baehr 1987;Wilson et al 1987;Wilson et al 1988;Baehr et al 1989;Johnson et al 1990). However, an equilibrium mass transfer approach is a maximum rate and can overestimate NAPL volatilization.…”
Section: 1mentioning
confidence: 99%
“…Experimental results using natural geological materials often show effluent concentrations below the theoretical maximum based on contaminant partial pressures (Baehr et al 1989;Mackay et al 1990;Rainwater et al, 1989). Gierke et al (1992) used a mathematical model and laboratory column experiments to examine the impacts of mass partitioning and other factors on subsurface movement of organic vapors.…”
Section: 1mentioning
confidence: 99%
“…NAPL saturation used was varied from 13.8% -71% . For each NAPL saturation experiment, pore gas velocity was varied between 0.1-2 cm/sec as pore gas velocity is found to be less than 2cm/sec in a typical SVE system (Baehr et al, 1989). Each experiment with one NAPL saturation and different pore gas velocities were run for 42-62 minutes.…”
Section: 2 Volatilization Experimentsmentioning
confidence: 99%
“…The models range in complexity from those that use steady-state flow fields coupled with analytical solutions (Roy and Griffin 1991;Zaidel and Russo 1993) to others that use steady-state flow fields and numerical transport solutions (Massmann and Farrier 1992;Johnson et al 1990). More complex models consider geologic heterogeneity while still assuming steady-state flow conditions (Baehr et al 1989;Benson et al 1993). …”
Section: Computer Code and Modelsmentioning
confidence: 99%