Distribution of polycyclic aromatic hydrocarbons in soil–water system containing a nonionic surfactant

The effect of a nonionic surfactant, Triton X-100 (TX100), on the distribution of four representative polycyclic aromatic hydrocarbons (PAHs), phenanthrene, fluorene, acenaphthene and naphthalene, in soil–water system was studied on a natural soil. The apparent soil–water distribution coefficient wi...

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Vydáno v:Chemosphere (Oxford) Ročník 60; číslo 9; s. 1237 - 1245
Hlavní autoři: Zhou, Wenjun, Zhu, Lizhong
Médium: Journal Article
Jazyk:angličtina
Vydáno: Oxford Elsevier Ltd 01.09.2005
Elsevier
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ISSN:0045-6535, 1879-1298
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Shrnutí:The effect of a nonionic surfactant, Triton X-100 (TX100), on the distribution of four representative polycyclic aromatic hydrocarbons (PAHs), phenanthrene, fluorene, acenaphthene and naphthalene, in soil–water system was studied on a natural soil. The apparent soil–water distribution coefficient with surfactant ( K d ∗ ) for these compounds increased when TX100 equilibrium concentration from zero to around the critical micelle concentration (CMC), followed by a decrease in K d ∗ at TX100 equilibrium concentration greater than CMC. This is a direct result of surfactant sorption onto soil followed by PAHs partitioning to the sorbed surfactant. The values of carbon-normalized solute distribution coefficient ( K ss) with the sorbed TX100 are greater than the corresponding partition coefficients with soil organic matter ( K oc), which indicates the soil-sorbed nonionic surfactant is more effective per unit mass as a partitioning medium than the native soil organic matter for PAHs. When K d ∗ = K d the corresponding initial concentration of surfactant was defined as critical washing concentration (CWC). Depending on the surfactant initial concentration below or above the CWC, the addition of nonionic surfactant can enhance the retardation of soil for PAHs or promote the removal of PAHs from soil, respectively. The values of K d ∗ and CWC can be predicted by a model, which correlates them with the compounds’ octanol–water partition coefficients ( K ow), soil property and the amount of soil-sorbed surfactant.
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ISSN:0045-6535
1879-1298
DOI:10.1016/j.chemosphere.2005.02.058