Dielectric barrier discharge coupled with Fe2+, Mn2+ and Cu2+ scrubbing for toluene removal

By-product ozone emission is one of the challenges for applying dielectric barrier discharge (DBD) technology for volatile organic compounds (VOCs) removal. In this study, a DBD reactor followed by a wet scrubber (WS) containing a solution of metal ions (Fe2+/Mn2+/Cu2+) was used to reuse ozone for f...

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Veröffentlicht in:Chemosphere (Oxford) 2022-03, Vol.290, p.133306-133306, Article 133306
Hauptverfasser: Qin, Caihong, Jiang, Chaochao, Guo, Mengke, Liu, Rongrong, Yu, Rui, Huang, Jiayu, Yan, Dongjie, Li, Shijie, Dang, Xiaoqing
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Sprache:eng
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Zusammenfassung:By-product ozone emission is one of the challenges for applying dielectric barrier discharge (DBD) technology for volatile organic compounds (VOCs) removal. In this study, a DBD reactor followed by a wet scrubber (WS) containing a solution of metal ions (Fe2+/Mn2+/Cu2+) was used to reuse ozone for further oxidation of typical VOC toluene. Compared with the degradation effect of the DBD reactor alone, DBD coupled WS/iron system not only improved the toluene removal efficiency but also significantly reduced the ozone emission. The ozone removal efficiency reached as high as 98% in the DBD coupled WS/Fe2+ system. Electron paramagnetic resonance (EPR) tests showed that ozone was converted into radicals such as hydroxyl radicals in Fe2+ and Cu2+ solution, which further oxidized toluene in WS/iron. Quenching experiments showed that the contribution for toluene degradation by radicals was up to 75% and 62% in Fe2+ and Mn2+ reactor, respectively. This study demonstrates that the DBD coupled WS system has the potential to be an environmentally friendly technology for gaseous VOCs removal. [Display omitted] •DBD coupled with WS was effective in ozone reducing and toluene removal.•The O3 removal efficiency of DBD coupled Fe2+ system was as high as 98%.•O3 was converted in to radicals (·OH) in WS.•The contribution of radicals for toluene degradation in WS/Fe2+ were ∼75%.
ISSN:0045-6535
1879-1298
DOI:10.1016/j.chemosphere.2021.133306