Physicochemical factors controlling the retention and transport of perfluorooctanoic acid (PFOA) in saturated sand and limestone porous media.

Comprehensively understanding the fate and transport of perfluorooctanoic acid (PFOA) in subsurface environment is crucial to assess its environmental impacts. In this work, column experiments were conducted to investigate the effects of physicochemical factors on the retention and transport of 14C-labeled PFOA in saturated sand and limestone porous media. The retention of PFOA in limestone columns was higher than that in sand columns under the same solution chemistry conditions. This can be attributed to that the limestone had less negative zeta-potential and larger specific surface area than the sand. Changes in ionic strength (low to high) and cation type (Na+ to Ca2+) had little influences on the mobility of PFOA in sand porous media, but significantly enhanced the retention of PFOA in limestone porous media. Nearly no PFOA was retained in the sand columns, but relatively high levels of PFOA retention (28.7-48.4%) were achieved in the limestone columns. Higher input concentration resulted in lower PFOA retention in limestone porous media, reflecting the blocking effect of the sorption sites. The blocking effect was insignificant in sand porous media, probably because the experimental conditions were unfavorable for PFOA sorption on sand media. A two-site kinetic retention model effectively simulated both the breakthrough and retention behaviors of the PFOA in the sand and limestone porous media.