This study systematically investigates the formation of trichloronitromethane (TCNM) from 2 natural waters, 6 humic substances and 16 phenolic compounds during UV/monochloramine (UV/NHCl) followed by post-chloramination. Using N-NHCl as an isotope tracer, we found that N-TCNM accounted for 70.7-76.5% of total TCNM during UV/NHCl treated 2 natural waters, which was significantly higher than the proportion of N-TCNM in chloramination (NHCl alone). This is a direct evidence that NHCl, rather than the nitrogenous matters in waters, was the predominant nitrogen source of TCNM during UV/NHCl treatment. Phenol derivatives with meta-substituents and with electron-withdrawing groups facilitated the formation of TCNM precursors during UV/NHCl treatment. Significant correlations were found between Hammett constants (σ) of substituents and TCNM formation potentials. The formation mechanisms of TCNM were revealed using resorcinol as a representative phenolic compound. During UV/NHCl treatment, HO, reactive chlorine species and reactive nitrogen species contributed to 28.1%, 29.0% and 19.4% of resorcinol degradation. Five nitro(so)-intermediates were identified as the main TCNM precursors. The formation pathways of TCNM were proposed. Alkaline pH was recommended to reduce the formation of TCNM precursors during UV/NHCl treatment.
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http://dx.doi.org/10.1016/j.jhazmat.2021.126813 | DOI Listing |
Sci Total Environ
April 2024
Water Reclamation (Plants) Department, PUB Singapore, 40 Scotts Road, Environment Building, Singapore 228231, Singapore.
Sequential utilization of ozone (O) and biological activated carbon (BAC) followed by UV/chlor(am)ine advanced oxidation process (AOP) has drawn attention in water reuse. However, the formation of disinfection by-products (DBPs) in this process is less evaluated. This study investigated the DBP formation and the relevant toxicity during the O-BAC-UV/chlor(am)ine treatment of sand-filtered municipal secondary effluent.
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