Fluorinated Precursor Compounds in Sediments as a Source of Perfluorinated Alkyl Acids (PFAA) to Biota

Abstract

The environmental behavior of perfluorinated alkyl acids (PFAA) and their precursors was investigated in lake Tyrifjorden, downstream a factory producing paper products coated with per- and polyfluorinated alkyl substances (PFAS). Low water concentrations (max 0.18 ng L^-1 linear perfluorooctanesulfonic acid, L-PFOS) compared to biota (mean 149 μg kg^-1 L-PFOS in perch livers) resulted in high bioaccumulation factors (L-PFOS BAF_{Perch liver}: 8.05 × 10⁵-5.14 × 10⁶). Sediment concentrations were high, particularly for the PFOS precursor SAmPAP diester (max 1 872 μg kg^-1). Biota-sediment accumulation factors (L-PFOS BSAF_{Perch liver}: 22-559) were comparable to elsewhere, and concentrations of PFAA precursors and long chained PFAA in biota were positively correlated to the ratio of carbon isotopes (¹³C/¹²C), indicating positive correlations to dietary intake of benthic organisms. The sum fluorine from targeted analyses accounted for 54% of the extractable organic fluorine in sediment, and 9-108% in biota. This, and high trophic magnification factors (TMF, 3.7-9.3 for L-PFOS), suggests that hydrophobic precursors in sediments undergo transformation and are a main source of PFAA accumulation in top predator fish. Due to the combination of water exchange and dilution, transformation of larger hydrophobic precursors in sediments can be a source to PFAA, some of which are normally associated with uptake from water.

Keywords: PFAS; PFOS; SAmPAP diester; bioaccumulation factors (BAF); extractable organic fluorine (EOF); sediment−pore water partitioning coefficients (KD); trophic magnification.