Abstract

Sediment efflux rates of six polynuclear aromatic hydrocarbons (PAHs) were determined employing a novel boundary-layer flux chamber which concentrates trace organics using solid phase extraction techniques. Sediment cores were collected from the Elizabeth River, Virginia and were monitored over a 48 h period for PAH fluxes into uncontaminated seawater. The observed flux rates were related to solubility and octanol-water partition coefficients (KOW) of the PAHs. Flux rates for the six PAHs varied from 0.028 to 0.646 μg/L/d on a concentration basis and 43.0 to 1,000 μg/m2/d on an areal basis. The resulting flux rate coefficients (k2) were determined to be well correlated to solubility (R2=0.82) and inversely related to KOW (R2=0.75). The empirically determined sediment flux dynamics fit well with theoretical relationships that have been previously established for bioconcentration kinetics and octanol/water partitioning systems. Thus, it appears possible to predict flux rates of other hydrophobic organic chemicals from ambient sediment and water concentrations, KOW information, and the proposed empirical models.

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