The thermal decomposition of PFOA was studied in an α-alumina reactor between 400 and 1000 °C under two separate conditions: 1) in a bath gas of air and water vapor (H2O(g)) and 2) in a bath gas of helium, nitrous oxide (N2O) and H2O(g). PFOA decomposition studies undertaken under these conditions, both experimental and modeling analysis, provided insightful information on the conditions leading to the formation of products of incomplete destruction (PIDs).The combination of O2 from air or O from N2O decomposition, combined with H2O(g), resulted in complete mineralization of PFOA at temperatures above 950 °C into HF and CO2. An elementary mass balance of F and C atoms concluded that, at 1000 °C, 105 ± 10 % of F atoms present in PFOA are converted into HF, while 100 ± 5 % of C atoms into CO2. Both H2O(g) and oxygen together are necessary for complete mineralization.
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