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Resistant sorption of in situ chlorobenzenes and a polychlorinated biphenyl in river Rhine suspended matter
Authors:ten Hulscher Th E M  Vrind B A  van Noort P C M  Govers H A J
Affiliation:

a Institute for Inland Water Management and Waste Water Treatment (RIZA), P.O. Box 17, 8200 AA, Lelystad, The Netherlands

b Department of Environmental and Toxicological Chemistry, Institute for Biodiversity and Ecosystem Dynamics, Nieuwe Achtergracht 166, 1018 WV, Amsterdam, The Netherlands

Abstract:
The desorption kinetics of in situ chlorobenzenes (dichlorobenzenes, pentachlorobenzene and hexachlorobenzene) and 2,4,4-trichlorobiphenyl (PCB-28) were measured with a gas-purge technique for river Rhine suspended matter sampled in Lobith, The Netherlands. This suspended matter is the main source of sediment accumulation in lake Ketelmeer. In lake Ketelmeer sediment earlier observations showed that slow and very slow fractions dominate the desorption profile.

For the river Rhine suspended matter, only for PCB-28 a fast desorbing fraction of around 1.6% could be detected. The observed rate constants were on the average 0.2 h−1 for fast desorption, 0.004 h−1 for slow desorption, and 0.00022 h−1 for very slow desorption. These values are in agreement with previous findings for the sediment from lake Ketelmeer and with available literature data on fast, slow, and very slow desorption kinetics.

The results from this study show the similarity of desorption profiles between river Rhine suspended matter, and the top layer sediment from lake Ketelmeer. This indicates that slow and very slow fractions are already present in material forming the top layer of lake Ketelmeer, and were not formed after deposition of this material in the lake. The absence of detectable fast fractions for most compounds could be caused by the absence of recent pollution of the suspended matter. But, the observations may also be explained by a rapid disappearance of compounds from the fast fraction due to a combination of a high affinity of very slow sites for these compounds, and their relatively high volatility.

Keywords:Desorption kinetics   Field contaminated sediments   Lobith   Slow desorption
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