Vapor-phase diffusion of benzene in soil

The volatilization of benzene (C6H6), a component of volatile emissions from landfills receiving certain industrial wastes, was characterized in the laboratory using a simulated landfill apparatus. The steady‐state vapor diffusion of C6H6 in soil under isothermal conditions and negligible water flow...

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Bibliographic Details
Published inJournal of environmental quality Vol. 16; no. 1; pp. 38 - 43
Main Authors Karimi, A.A, Farmer, W.J, Cliath, M.M
Format Journal Article
LanguageEnglish
Published Madison, WI American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America 01.01.1987
Crop Science Society of America
American Society of Agronomy
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Summary:The volatilization of benzene (C6H6), a component of volatile emissions from landfills receiving certain industrial wastes, was characterized in the laboratory using a simulated landfill apparatus. The steady‐state vapor diffusion of C6H6 in soil under isothermal conditions and negligible water flow was directly related to soil air‐filled porosity. The volatilization flux of C6H6 through a soil cover was greatly reduced by increased soil bulk density and increased soil‐water content. The actual flux through the soil cover could be predicted from the soil porosity term, P10/3a P−2T, where Pa is the soil air‐filled porosity and PT is the total porosity. The diffusion coefficient in air for C6H6 calculated from the experimental results was 8.91 × 10−6 m2 s−1, at 20 °C, which agrees with other reported data.
Bibliography:T01
P33
8730039
Contribution from the Environmental Engineering Program, Univ. of Southern California, Los Angeles, CA 90089, the Dep. of Soil and Environmental Sciences, Univ. of California, Riverside, CA 92521, and USDA‐ARS, Riverside, CA 92521.
ObjectType-Article-2
SourceType-Scholarly Journals-1
ObjectType-Feature-1
content type line 23
ISSN:0047-2425
1537-2537
DOI:10.2134/jeq1987.00472425001600010008x