Speciation and transformation pathways of chlorophenols formed from chlorination of phenol at trace level concentration.

Trace organic precursors remaining in water after primary treatment can originate a variety of toxic disinfection by-products during chlorination. Therefore, knowledge of conditions leading to their persistence or transformation in chlorinated media is crucial for human health protection. Using phenol as model compound at trace level (50 ppb), the short term formation and degradation of chlorophenols (CPs) in plain water and buffered water (pH 4.8, 7 and 9) treated with typical chlorine doses (1-5 ppm) was investigated. Total phenol consumption and quantitative degradation of formed CPs occurred in < or =5h with 5 ppm chlorine in plain water and alkaline buffer, and with 1 ppm chlorine in phosphate buffer of pH 7. The enhanced reactivity in this buffer was attributed to high ionic strength (0.18 M). On the contrary, phenol was only slowly transformed to monochlorophenols (MCPs) in acidic media. Analysis of phenol and CPs concentration profiles indicated the coexistence of two competing reaction pathways in neutral and alkaline conditions: 1) successive ortho-para chlorination of aromatic ring up to 2,4,6-trichlorophenol followed by ring cleavage, 2) direct oxidation of MCPs to rapidly degradable oxygenated aromatics (dihydroxybenzenes, benzoquinones). Ionic strength and pH had some influence on preferred pathway but chlorine dose was determinant.