The multiple reactive
oxidants produced during chlorine photolysis
effectively degrade organic contaminants during water treatment, but
their role in disinfection byproduct (DBP) formation is unclear. The
impact of chlorine photolysis on dissolved organic matter (DOM) composition
and DBP formation is investigated using lake water collected after
coagulation, flocculation, and filtration at pH 6.5 and pH 8.5 with
irradiation at three wavelengths (254, 311, and 365 nm). The steady-state
concentrations of hydroxyl radical and chlorine radical decrease by
38–100% in drinking water compared to ultrapure water, which
is primarily attributed to radical scavenging by natural water constituents.
Chlorine photolysis transforms DOM through multiple mechanisms to
produce DOM that is more aliphatic in nature and contains novel high
molecular weight chlorinated DBPs that are detected via high-resolution
mass spectrometry. Quenching experiments demonstrate that reactive
chlorine species are partially responsible for the formation of halogenated
DOM, haloacetic acids, and haloacetonitriles, whereas trihalomethane
formation decreases during chlorine photolysis. Furthermore, DOM transformation
primarily due to direct photolysis alters DOM such that it is more
reactive with chlorine, which also contributes to enhanced formation
of novel DBPs during chlorine photolysis.