Selection criteria for oxidation method in total organic carbon measurement
During the measurement of total organic carbon (TOC), dissolved organic carbon is converted into CO2 by using high temperature combustion (HTC) or wet chemical oxidation (WCO). However, the criteria for selecting the oxidation methods are not clear. In this study, the chemical structures of organic...
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Veröffentlicht in: | Chemosphere (Oxford) 2018-05, Vol.199, p.453-458 |
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Zusammenfassung: | During the measurement of total organic carbon (TOC), dissolved organic carbon is converted into CO2 by using high temperature combustion (HTC) or wet chemical oxidation (WCO). However, the criteria for selecting the oxidation methods are not clear. In this study, the chemical structures of organic material were considered as a key factor to select the oxidation method used. Most non-degradable organic compounds showed a similar oxidation efficiency in both methods, including natural organic compounds, dyes, and pharmaceuticals, and thus both methods are appropriate to measure TOC in waters containing these compounds. However, only a fraction of the carbon in the halogenated compounds (perfluorooctanoic acid and trifluoroacetic acid) were oxidized using WCO, resulting in measured TOC values that are considerably lower than those determined by HTC. This result is likely due to the electronegativity of halogen elements which inhibits the approach of electron-rich sulfate radicals in the WCO, and the higher bond strength of carbon-halogen pairs as compared to carbon-hydrogen bonds, which results in a lower degree of oxidation of the compounds. Our results indicate that WCO could be used to oxidize most organic compounds, but may not be appropriate to quantify TOC in organic carbon pools that contain certain halogenated compounds.
•Concentration of organic matter is not suitable to determine oxidation method.•Chemical structure is a key factor determining oxidation of organic matter.•Wet chemical oxidation oxidized partially halogenated compounds. |
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ISSN: | 0045-6535 1879-1298 |
DOI: | 10.1016/j.chemosphere.2018.02.074 |