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Hydrogen peroxide photoproduction by humic substances and their model compounds |
LI Jian-hua1, ZHANG Ya2, WU Xin-an3, WANG Meng-jie3, SHI Qin-ren3, PENG Jian-biao4, GAO Shi-xiang3 |
1. Jiangsu Key Laboratory of Chemical Pollution Control and Resources Reuse, School of Environmental and Biological Engineering, Nanjing University of Science and Technology, Nanjing 210094, China; 2. Nanjing Institute of Environmental Sciences, Ministry of Ecology and Environmental of the People's Republic of China, Nanjing 210042, China; 3. State Key Laboratory of Pollution Control and Resource Reuse, School of the Environment, Nanjing University, Nanjing 210023, China; 4. School of Environment, Henan Normal University, Key Laboratory for Yellow River and Huai River Water Environmental and Pollution Control, Ministry of Education, Henan Key Laboratory for Environmental Pollution Control, Xinxiang 453007, China |
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Abstract The present study systematically investigated H2O2 generation kinetics and potential mechanism from irradiated humic substances (HS) and their model compounds under simulated sunlight. Our results indicated that all the selected HS with different sources or forms can produce H2O2 under irradiation, and no significant difference was observed between them, with the generation rate ranging from 6.379 to 15.784nmol/(L·min). The H2O2 generation rate from humic acid (HA) was slightly faster than that from fulvic acid (FA). In the case of humus model compounds, 7compounds including veratryl alcohol, p-aminobenzoic acid, 3,5-dihydroxybenzoic acid (DHBA), 2,5-dihydroxy-1,4-benzoquinone, phenol, benzoic acid and aniline could produce detectable H2O2, while other compounds including catechol, resorcinol, hydroquinone, quinone, o-anisidine, p-anisidine, salicylic acid and 2,6-dimethoxy-1,4-benzoquinone can't. Nevertheless, the H2O2 generation rate from the model compounds varies from each other, with one or two orders of magnitude. Among them, 2,5-dihydroxyl-1,4-benquione and DHBA exhibited the highest H2O2 yields, while phenol, benzoic and p-aminobenzoic acid showed a relative low H2O2 generation potential. Based on the generation mechanism of H2O2 from HS, a possible H2O2 formation mechanism from a typical model compound, i.e. DHBA, was proposed. DHBA was believed to excite to a singlet state, after an intramolecular electron transfer process, giving a reducing intermediate. The intermediate could further react with O2 to form O2·- and subsequently generate H2O2.
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Received: 30 June 2020
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