Due to the complexities of the interactions
between ammonia, chlor(am)ine,
and intermediate species such as ONOOH, the radical formation in breakpoint
chlorination and the consequential removal of micropollutants remain
largely unexplored. In this study, the dominant generation pathway
of HO•, as a primary radical in breakpoint chlorination,
was examined, and the generations of HO•, reactive
chlorine species (RCS), and reactive nitrogen species (RNS) were quantitatively
evaluated. A dissolved oxygen (DO)-independent pathway was verified
by 18O labeling and contributed over 90% to HO• generation. The commonly believed pathway, the decomposition of
ONOOH involving DO, contributed only 7% to HO• formation
in breakpoint chlorination. The chlorine to nitrogen (Cl/N) ratio
and pH greatly affected the generations and speciations of the reactive
species. An optimum Cl/N mass ratio for HO•, Cl2
•–, and RNS generations occurred
at the breakpoint (i.e., Cl/N mass ratio = 9), whereas excessive free
chlorine shifted the radical speciation toward ClO• at Cl/N mass ratios above the breakpoint. Basic conditions inhibited
the generations of HO• and RNS but significantly
promoted that of ClO•. These findings improved the
fundamental understanding of the radical chemistry of breakpoint chlorination,
which can be extended to estimate the degradations of micropollutants
of known rate constants toward the reactive species with influences
from the Cl/N ratio and pH in real-world applications.