Concentrations of polycyclic aromatic hydrocarbons (PAHs) in groundwater at a coal tar site were elevated by factors ranging from 3 (pyrene) to 50 (indeno1,2,3-cd-pyrene) over purely dissolved concentrations. Air-groundwater surface tension measurements (70.6 ± 3 dyn/cm) were not sufficiently different from air-pure water measures (72.2 ± 0.1 dyn/cm) to ascribe the observed enrichments to either cosolvents or surfactants in the groundwater. Excess pyrene was associated with colloids that passed an ultrafilter at ambient pH but became ultrafilterable when the groundwater pH was lowered to 1. This suggested pyrene association with humic acids. Given the decrease in groundwater total organic carbon (TOC) of 4 mgc/L upon acidification and ultrafiltration, a partition coefficient of 10{sup}5 L/kgc was estimated for this pyrene association. Use of the results for pyrene and scaling for the differences in PAH hydrophobicities enabled good predictions of the observed enrichments of less water-soluble PAHs in the groundwater. This is strong field evidence indicating colloid-facilitated transport of HOCs in groundwater. Assuming that humic-bound PAHs were as mobile as the dissolved PAHs, the fluxes of individual PAHs (e.g., benzoapyrene) from the tar source were as much as 20 times greater than estimates based solely on tar-water partitioning predictions.
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