Partitioning characteristics of PAHs between sediment and water in a shallow lake
Author(s) -
Min Qiao,
Shengbiao Huang,
Zijian Wang
Publication year - 2007
Publication title -
journal of soils and sediments
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.885
H-Index - 73
eISSN - 1614-7480
pISSN - 1439-0108
DOI - 10.1065/jss2008.03.279
Subject(s) - environmental chemistry , sediment , environmental science , water column , surface water , bay , aquatic ecosystem , water quality , hydrology (agriculture) , chemistry , environmental engineering , ecology , geology , oceanography , paleontology , geotechnical engineering , biology
Goal, Scope and BackgroundDistribution of hydrophobic organic contaminants in abiotic compartments is essential for describing their transfer and fate in aquatic ecosystems. Taihu Lake is the third largest freshwater lake in China. Water quality of Taihu Lake has deteriorated greatly during the last decades and has threatened the water supply. The aim of the present study was to investigate the partitioning of polycyclic aromatic hydrocarbons (PAHs) among overlying water, suspended particulate matter (SPM), sediments, and pore water in Meiliang Bay, Taihu Lake and to provide useful information for the ecological engineering in this area.Materials and MethodsOverlying water and surface sediment were sampled from six sites in Meiliang Bay, Taihu Lake, China. Within 72 h of sampling, sediments were centrifuged to obtain the pore water. Overlying water samples were filtered to separate dissolved and SPM samples. After extraction, samples were purified following a clean-up procedure. PAH fraction was obtained by elution with a mixture of hexane: DCM (7:3, V/V) and analyzed by GC/MS.ResultsPAHs concentrations in overlying water varied from 37.5 ng/L to 183.5 ng/L. Concentrations of PAHs in pore water were higher than those in overlying water. The total concentrations of 16 priority PAHs in sediments ranged from 2091.8 ng/g-dw to 4094.4 ng/g-dw. PAHs concentrations on SPM were decreased with suspended solid concentrations (SSC). Total PAHs concentrations on SPM varied in the range of 3369.6 ng/g-dw to 7531.1 ng/g-dw. The partition coefficients between sediment and overlying water (log Koc) for PAHs with log Kow<5 were positively correlated with their octanol-water partition coefficients (log Kow) (n=39, r=0.79, p<0.0001). Partition coefficients between sediment and pore water (log Koc′) for all PAHs were also significantly correlated with their log Kow values (n=48, r=0.82, p<0.0001).DiscussionIn general, PAHs derived from combustion sources tend to bind strongly to soot particles in natural sediment. Consequentially, Koc values observed in the natural environment could be orders of magnitude higher than those predicted by linear correlation relationships under laboratory conditions. In the present study, the ratio of log Koc values to log Kow values falls consistently above 1, indicating that the sediment soot carbon in the bay was more attractive for PAHs than n-octanol. The log Koc′ was also higher than that predicted under laboratory conditions, suggesting that the measured pore water PAH concentrations were lower than those predicted. That is to say, not all the sediment PAHs can be available to partition rapidly into sediment pore waters. A variation in soot content is a possible reason. Furthermore, concentrations of PAHs on SPM were higher than those in sediments. The compositions of PAHs on SPM and in sediments were similar, indicating the importance of re-suspension process of sediments in the partitioning process of the shallow lake.ConclusionsThe results indicated the equilibrium partitioning model could be used to predict PAHs distribution in various phases of a shallow lake in the stagnation period, but re-suspension processes should be considered to modify the relationship between log Kocs and log Kows.Recommendations and PerspectivesConcentration, particle size and composition of resuspended particles could affect the relationship between log Kocs and log Kows. Further work should be done under field conditions, especially where a steady thermodynamic equilibrium state could be assumed.
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