An investigation into the long-term binding and uptake of PFOS, PFOA and PFHxS in soil - plant systems.

J Hazard Mater

School of Agriculture, Food and Wine, Faculty of Sciences, The University of Adelaide, PMB 1 Waite Campus, Glen Osmond, South Australia, Australia.

Published: February 2021

AI Article Synopsis

  • The study examined the effects of aging and plant bioaccumulation of three perfluoroalkyl acids (PFAS): PFOS, PFOA, and PFHxS in 20 different soils over six months.
  • Sorption coefficients for these chemicals showed some increase over time, but plant concentrations did not significantly differ between aged and fresh treatments.
  • The modeling of sorption and bioaccumulation factors was linked to various soil properties, indicating that aging effects in the soils were minimal during the study period.

Article Abstract

This study investigated the potential aging and plant bioaccumulation of three perfluoroalkyl acids (PFAAs), perfluorosulphonic acid (PFOS), perfluorooctanoic acid (PFOA) and perfluorohexanesulphonic acid (PFHxS) in 20 soils over a six-month period. Sorption coefficients (Log K) ranged from 0.13-1.28 for PFHxS, 0.17-1.06 for PFOA and 0.98-2.03 for PFOS, respectively, and bioaccumulation factors (Log BAFs) ranged from 0.29-1.24, 0.22-1.46 and 0.05-0.65 for PFHxS, PFOA and PFOS, respectively. Over the six-month period, K values significantly increased for PFHxS and PFOA but the magnitude of the increase was very small and did not translate into differences in plant PFAA-concentrations between aged and freshly spiked treatments. The K and BAF values were modelled by multiple linear regression (MLR) to soil physico-chemical properties and by partial least squares regression to soil spectra acquired by mid-infrared spectroscopy (DRIFT-PLSR). Modelling of each PFAA was influenced by different soil properties, including organic carbon, pH, CEC, exchangeable cations (Ca, Mg, Na and K) and oxalate extractable Al. BAF values were not strongly correlated to any soil property but were inversely correlated to K values. Our results indicate that limited aging occurred in these soils over the six-month period.

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Source
http://dx.doi.org/10.1016/j.jhazmat.2020.124065DOI Listing

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