In
this study, we found that thermal decomposition of per- and
polyfluoroalkyl substances (PFAS) in soil was rapid at moderate temperatures
of 400–500 °C, regardless of whether the soil was contaminated
by a single PFAS compound or a PFAS mixture in aqueous film-forming
foams. Substantial degradation (>99%) of PFAS in soil, including
perfluorooctanoic
acid (PFOA), perfluorooctane sulfonate (PFOS), short-chain homologues,
cationic and zwitterionic precursors, and PFOA and PFOS alternatives,
occurred in 30 min at 500 °C in both a sealed reactor in air
and a horizontal reactor under a continuous flow of N2.
The effect of the initial PFAS level in soil (0.001–10 μmol/g)
and soil texture was insignificant, provided a sufficiently high temperature
was applied. Furthermore, this study showed, for the first time, that
kaolinite dramatically decreased the apparent yield of F from PFAS
heated at >300 °C, likely due to the chemisorption of F radicals
on kaolinite. This phenomenon was not observed when kaolinite and
an inorganic fluoride salt (NaF) were thermally treated. Lastly, various
nonpolar thermal degradation products of PFOA and PFOS were reported
for the first time. The profile of fluorinated volatiles, particularly
perfluoroalkenes, was similar between these two chemicals. The results
support a radical-mediated degradation pathway of PFAS.