Control of halophenol formation in seawater during chlorination using pre-ozonation treatment

The reverse osmosis process is widely used for seawater desalination, whereas the pre-chlorination step for controlling membrane biofouling results in undesirable disinfection by-products, such as halophenols (HPs) which are not yet regulated but of increasing concerns. The formation and speciation...

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Veröffentlicht in:Environmental science and pollution research international 2018-10, Vol.25 (28), p.28050-28060
Hauptverfasser: Ding, Ning, Sun, Yingxue, Ye, Tao, Yang, Zhe, Qi, Fei
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Sun, Yingxue
Ye, Tao
Yang, Zhe
Qi, Fei
description The reverse osmosis process is widely used for seawater desalination, whereas the pre-chlorination step for controlling membrane biofouling results in undesirable disinfection by-products, such as halophenols (HPs) which are not yet regulated but of increasing concerns. The formation and speciation of HPs during chlorination of three filtered seawater samples (SA, SB, and SC) with various phenol concentrations (0.25, 0.5, 1.0 mg/L) were evaluated. 4-Bromophenol (4-BrP), 2,4,6-trichlorophenol (2,4,6-TClP), 2,4-dibromophenol (2,4-DBrP), and 2,4,6-tribromophenol (2,4,6-TBrP) were identified during chlorination, with 2,4,6-TBrP as the predominant HP. Ozone as a common oxidant in water and wastewater treatment was subsequently applied to assess its effect in dissolved organic matter (DOM) and its ability of reducing HP precursors in the seawater samples. An initial ozone dose of 5 mg O 3 /L was capable of reducing dissolved organic carbon (DOC) in SA, and UV absorbance at 254 nm (UV 254 ) in SB, whereas it induced an elevation of UV 254 in SC. When ozone dose increased to 10 mg O 3 /L, the DOC and UV 254 levels in all seawater samples were reduced. Ozone was more powerful on degrading DOM with molecular weight (MW) of near 1000 Da than those with MW of 20–100 Da, both of which composed the majority of DOM in the seawater samples. As determined by excitation emission matrix fluorescence spectroscopy, the most ozone-susceptible fraction of DOM was soluble microbial by-product-like substances, while the least was tryptophan-like aromatic proteins. Despite that the initial ozone of 5 mg O 3 /L was less effective in DOM degradation than the higher dose, it successfully degraded HP precursors. By pre-ozonation at 5 mg O 3 /L, no chlorophenol was detected during chlorination, and the mean reductions of the three bromophnols formed were above 92% in all seawater samples, with the reduction of 2,4,6-TBrP being the highest of 99.7, 99.6, and 99.1% in SA, SB, and SC, respectively.
doi_str_mv 10.1007/s11356-018-2828-y
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The formation and speciation of HPs during chlorination of three filtered seawater samples (SA, SB, and SC) with various phenol concentrations (0.25, 0.5, 1.0 mg/L) were evaluated. 4-Bromophenol (4-BrP), 2,4,6-trichlorophenol (2,4,6-TClP), 2,4-dibromophenol (2,4-DBrP), and 2,4,6-tribromophenol (2,4,6-TBrP) were identified during chlorination, with 2,4,6-TBrP as the predominant HP. Ozone as a common oxidant in water and wastewater treatment was subsequently applied to assess its effect in dissolved organic matter (DOM) and its ability of reducing HP precursors in the seawater samples. An initial ozone dose of 5 mg O 3 /L was capable of reducing dissolved organic carbon (DOC) in SA, and UV absorbance at 254 nm (UV 254 ) in SB, whereas it induced an elevation of UV 254 in SC. When ozone dose increased to 10 mg O 3 /L, the DOC and UV 254 levels in all seawater samples were reduced. 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The formation and speciation of HPs during chlorination of three filtered seawater samples (SA, SB, and SC) with various phenol concentrations (0.25, 0.5, 1.0 mg/L) were evaluated. 4-Bromophenol (4-BrP), 2,4,6-trichlorophenol (2,4,6-TClP), 2,4-dibromophenol (2,4-DBrP), and 2,4,6-tribromophenol (2,4,6-TBrP) were identified during chlorination, with 2,4,6-TBrP as the predominant HP. Ozone as a common oxidant in water and wastewater treatment was subsequently applied to assess its effect in dissolved organic matter (DOM) and its ability of reducing HP precursors in the seawater samples. An initial ozone dose of 5 mg O 3 /L was capable of reducing dissolved organic carbon (DOC) in SA, and UV absorbance at 254 nm (UV 254 ) in SB, whereas it induced an elevation of UV 254 in SC. When ozone dose increased to 10 mg O 3 /L, the DOC and UV 254 levels in all seawater samples were reduced. Ozone was more powerful on degrading DOM with molecular weight (MW) of near 1000 Da than those with MW of 20–100 Da, both of which composed the majority of DOM in the seawater samples. As determined by excitation emission matrix fluorescence spectroscopy, the most ozone-susceptible fraction of DOM was soluble microbial by-product-like substances, while the least was tryptophan-like aromatic proteins. Despite that the initial ozone of 5 mg O 3 /L was less effective in DOM degradation than the higher dose, it successfully degraded HP precursors. 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The formation and speciation of HPs during chlorination of three filtered seawater samples (SA, SB, and SC) with various phenol concentrations (0.25, 0.5, 1.0 mg/L) were evaluated. 4-Bromophenol (4-BrP), 2,4,6-trichlorophenol (2,4,6-TClP), 2,4-dibromophenol (2,4-DBrP), and 2,4,6-tribromophenol (2,4,6-TBrP) were identified during chlorination, with 2,4,6-TBrP as the predominant HP. Ozone as a common oxidant in water and wastewater treatment was subsequently applied to assess its effect in dissolved organic matter (DOM) and its ability of reducing HP precursors in the seawater samples. An initial ozone dose of 5 mg O 3 /L was capable of reducing dissolved organic carbon (DOC) in SA, and UV absorbance at 254 nm (UV 254 ) in SB, whereas it induced an elevation of UV 254 in SC. When ozone dose increased to 10 mg O 3 /L, the DOC and UV 254 levels in all seawater samples were reduced. Ozone was more powerful on degrading DOM with molecular weight (MW) of near 1000 Da than those with MW of 20–100 Da, both of which composed the majority of DOM in the seawater samples. As determined by excitation emission matrix fluorescence spectroscopy, the most ozone-susceptible fraction of DOM was soluble microbial by-product-like substances, while the least was tryptophan-like aromatic proteins. Despite that the initial ozone of 5 mg O 3 /L was less effective in DOM degradation than the higher dose, it successfully degraded HP precursors. By pre-ozonation at 5 mg O 3 /L, no chlorophenol was detected during chlorination, and the mean reductions of the three bromophnols formed were above 92% in all seawater samples, with the reduction of 2,4,6-TBrP being the highest of 99.7, 99.6, and 99.1% in SA, SB, and SC, respectively.</abstract><cop>Berlin/Heidelberg</cop><pub>Springer Berlin Heidelberg</pub><pmid>30066078</pmid><doi>10.1007/s11356-018-2828-y</doi><tpages>11</tpages></addata></record>
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subjects 2,4,6-Trichlorophenol
Aquatic Pollution
Atmospheric Protection/Air Quality Control/Air Pollution
Biofouling
Byproducts
Chemical analysis
Chlorination
Chlorophenol
Degradation
Desalination
Dibromophenol
Disinfection
Dissolved organic carbon
Dissolved organic matter
Earth and Environmental Science
Ecotoxicology
Environment
Environmental Chemistry
Environmental Health
Environmental science
Filtration
Fluorescence
Fluorescence spectroscopy
Halogenation
Microorganisms
Molecular weight
Oxidizing agents
Ozonation
Ozone
Ozone - chemistry
Phenols
Phenols - analysis
Precursors
Proteins
Research Article
Reverse osmosis
Seawater
Seawater - chemistry
Speciation
Tribromophenol
Trichlorophenol
Trichlorophenols
Tryptophan
Waste Water - chemistry
Waste Water Technology
Wastewater treatment
Water analysis
Water Management
Water Pollutants, Chemical - analysis
Water Pollution Control
Water Purification - methods
Weight reduction
title Control of halophenol formation in seawater during chlorination using pre-ozonation treatment
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