Abstract

Black carbon (BC; soot and charcoal) can be an extremely strong sorbent for organic compounds. In a previous study, sorption of d 10-phenanthrene ( d 10-PHE) to BC in an unmodified contaminated sediment was found to be nine times less than that for BC isolated from this sediment. To find out the mechanism of this sorption attenuation (competition for BC sites between d 10-PHE and native PAHs or blocking of BC sites by natural organic matter), we determined the effect on d 10-PHE-BC sorption isotherms of additions of either PAHs or precipitated humic acid. Addition of humic acid did not significantly decrease BC sorption, whereas PAH additions (equal to the native PAH content in the original sediment) did, by about one order of magnitude. Therefore, competition between d 10-PHE and the native PAHs could explain the whole attenuation of sorption to BC in unmodified sediments.

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