1995
DOI: 10.1021/es00006a016
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Sediment Porewater Partitioning of Polycyclic Aromatic Hydrocarbons in Three Cores from Boston Harbor, Massachusetts

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Cited by 297 publications
(267 citation statements)
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“…The system sediments-mussels show a mean value of BSAF of 0.67. This value is similar to those obtained by Boese et al (20) in identical aquatic ecosystems, where values lower than 4.00 were observed for neutral compounds in water-sediment systems at thermodynamic equilibrium (21,22). Nevertheless, it is important to notice that this thermodynamic equilibrium often is difficult to obtain in natural systems, because individual isomers differ with the duration needed to achieve steady-state concentration in a living organism.…”
Section: Sediments and Musselssupporting
confidence: 90%
“…The system sediments-mussels show a mean value of BSAF of 0.67. This value is similar to those obtained by Boese et al (20) in identical aquatic ecosystems, where values lower than 4.00 were observed for neutral compounds in water-sediment systems at thermodynamic equilibrium (21,22). Nevertheless, it is important to notice that this thermodynamic equilibrium often is difficult to obtain in natural systems, because individual isomers differ with the duration needed to achieve steady-state concentration in a living organism.…”
Section: Sediments and Musselssupporting
confidence: 90%
“…Also, most of logK oc,obs between sediment and PW in the three streams were also higher than the predicted partition coefficients. This could be explained by the strong and nonlinear sorption of PAHs by carbonaceous geosorbents including BC in the sediment (Mcgroddy and Farrington 1995;Bucheli and Gustafsson 2000;Lohmann et al 2005;Cornelissen et al 2005Cornelissen et al , 2006. In addition, the rather slow release of PAHs after an initial rapid release from sediments collected from Yongding New River, South Drainage Canal, and North Drainage Canal PAHs which we reported previously in the desorption experiment (Qi et al 2010b) also proved this strong sorption of PAHs by carbonaceous particles in the sediment.…”
Section: Resultssupporting
confidence: 74%
“…The maximum PAH concentrations in pore water were recorded at about 10 to 25 cm depth that corresponded to the maximum sedimentary PAH concentrations at nearly the same depth (unpublished data). Similar trends were also observed by other investigations (Gao et al 1998;McGroddy and Farrington 1995). The concentrations of total PAHs in pore water were correlated with the DOC contents.…”
Section: Profiles Of Pahs In Pore Watersupporting
confidence: 90%