h i g h l i g h t s• The DBPFP of source waters did not correlate with the DOC value.• SUVA didn't represent the potential to form DBP in low-aromatic waters.• The Hi fraction played an important role in DBPFP for waters.• Phenolic hydroxyl group tended to form TCM and TCAA during chlorination.• Carboxyl and alcoholic hydroxyl groups tended to form DCAA and Br-DBP.
g r a p h i c a l a b s t r a c tThe characterization of DBP precursors from three source waters in China revealed that the DBPFP did not correlate with the DOC value. The Ho fraction mainly contained phenolic hydroxyl and conjugated double bonds which were reactive with chlorine to produce DBP, especially TCM and TCAA. The Hi fraction may contain more amino, carboxyl and alcoholic hydroxyl groups, which had the great potential to form DCAA and Br-DBP during chlorination.
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a b s t r a c tIn this study, the disinfection byproduct formation potential (DBPFP) of three surface waters with the dissolved organic carbon (DOC) content of 2.5, 5.2, and 7.9 mg/L was investigated. The formation and distribution of trihalomethanes and haloacetic acids were evaluated. Samples collected from three surface waters in China were fractionated based on molecular weight and hydrophobicity. The raw water containing more hydrophobic (Ho) fraction exhibited higher formation potentials of haloacetic acid and trihalomethane. The DBPFP of the surface waters did not correlate with the DOC value. The values of DBPFP per DOC were correlated with the specific ultraviolet absorbance (SUVA) for Ho and Hi fractions. The obtained results suggested that SUVA cannot reveal the ability of reactive sites to form disinfection byproducts for waters with few aromatic structures. Combined with the analysis of FTIR and nuclear magnetic resonance spectra of the raw waters and the corresponding fractions, it was concluded that the Ho fraction with phenolic hydroxyl and conjugated double bonds was responsible for the production of trichloromethanes and trichloroacetic acids. The Hi fraction with amino and carboxyl groups had the potential to form dichloroacetic acids and chlorinated trihalomethanes.