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PFAS remediation: Evaluating the infrared spectra of complex gaseous mixtures to determine the efficacy of thermal decomposition of PFAS

Due to their widespread production and known environmental contamination, the need for the detection and remediation of per- and polyfluoroalkyl substances (PFAS) has grown quickly. While destructive thermal treatment of PFAS at low temperatures (e.g., 200–500 °C) is of interest due to lower energy...

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Bibliographic Details
Published in:Chemosphere (Oxford) 2024-08, Vol.362 (C), p.142631, Article 142631
Main Authors: Hughey, Kendall D., Gallagher, Neal B., Zhao, Yuwei, Thakur, Nikita, Bradley, Ashley M., Koster van Groos, Paul G., Johnson, Timothy J.
Format: Article
Language:English
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Summary:Due to their widespread production and known environmental contamination, the need for the detection and remediation of per- and polyfluoroalkyl substances (PFAS) has grown quickly. While destructive thermal treatment of PFAS at low temperatures (e.g., 200–500 °C) is of interest due to lower energy and infrastructure requirements, the range of possible degradation products remains underexplored. To better understand the low temperature decomposition of PFAS species, we have coupled gas-phase infrared spectroscopy with a multivariate curve resolution (MCR) analysis and a database of high-resolution PFAS infrared reference spectra to characterize and quantify a complex mixture resulting from potassium perfluorooctanesulfonate (PFOS–K) decomposition. Beginning at 375 °C, nine prevalent decomposition products (namely smaller perfluorocarbon species) are identified and quantified. [Display omitted] •Low-T thermal decomposition of potassium perfluorooctanesulfonate investigated.•IR spectroscopy and MCR reveal gas-phase decomposition products.•Nine perfluorocarbon species identified as products of PFOS thermal decomposition. SYNOPSIS; We report a method to assess both the efficacy and gas-phase products of low temperature decomposition of PFAS chemicals from water or soil.
ISSN:0045-6535
1879-1298
1879-1298
DOI:10.1016/j.chemosphere.2024.142631