SORPTION OF BENZO[A]PYRENE AND PHENANTHRENE ON SUSPENDED HARBOR SEDIMENT AS A FUNCTION OF SUSPENDED SEDIMENT CONCENTRATION AND SALINITY - ALABORATORY STUDY USING THE COSOLVENT PARTITION-COEFFICIENT

Citation
Wjm. Hegeman et al., SORPTION OF BENZO[A]PYRENE AND PHENANTHRENE ON SUSPENDED HARBOR SEDIMENT AS A FUNCTION OF SUSPENDED SEDIMENT CONCENTRATION AND SALINITY - ALABORATORY STUDY USING THE COSOLVENT PARTITION-COEFFICIENT, Environmental science & technology, 29(2), 1995, pp. 363-371
Citations number
39
Categorie Soggetti
Environmental Sciences","Engineering, Environmental
ISSN journal
0013936X
Volume
29
Issue
2
Year of publication
1995
Pages
363 - 371
Database
ISI
SICI code
0013-936X(1995)29:2<363:SOBAPO>2.0.ZU;2-D
Abstract
The sorption of benzo[a]pyrene (BaP) and phenanthrene (PHE) on sedimen t collected in the harbor of Rotterdam was studied in batch experiment s using C-14-labeled compounds. In order to simulate various estuarine conditions, we investigated the effects of various sediment concentra tions and salinities on sorption of these compounds. We determined the apparent partitioning as well as the cosolvent partitioning between t he liquid and solid phases. The apparent partition coefficient (K-p(Ap p)) is influenced by the presence of colloids and dissolved organic ma tter. The influence of these components is minimized by the use of the cosolvent method in which the partition coefficient (K-p) is determi ned by extrapolation of the partition coefficients obtained in a varie ty of solutions with water and methanol. The effect of sediment concen tration on sorption was investigated at five different sediment concen trations ranging from 0.064 to 10.8 g/L. In contrast to K-p, K-p(App) was found to be sensitive to the sediment concentration. Log K-p (wi th K-p in L/kg), determined for different sediment concentrations, wa s 5.2-6.3 for BaP and 2.8-3.6 for PHE, whereas log K-p(App) was 4.1-5. 6 for BaP and 2.9-4.0 for PHE. The salt concentration was varied with dilutions of Milli-Q water and seawater; the salinity ranged from 0 to 35. The influence of salinity on K-p was small; the increase in log K-p from freshwater to seawater is approximately 0.2 for BaP and 0.1 for PHE.