Abstract
The N-nitrosodimethylamine (NDMA) formation pathway in chloraminated drinking water remains unresolved. In pH 7-10 waters amended with 10 μM total dimethylamine and 800 μeq Cl(2)·L(-1) dichloramine (NHCl(2)), NDMA, nitrous oxide (N(2)O), dissolved oxygen (DO), NHCl(2), and monochloramine (NH(2)Cl) were kinetically quantified. NHCl(2), N(2)O, and DO profiles indicated that reactive nitrogen species (RNS) formed during NHCl(2) decomposition, including nitroxyl/nitroxyl anion (HNO/NO(-)) and peroxynitrous acid/peroxynitrite anion (ONOOH/ONOO(-)). Experiments with uric acid (a ONOOH/ONOO(-) scavenger) implicated ONOOH/ONOO(-) as a central node for NDMA formation, which were further supported by the concomitant N-nitrodimethylamine formation. A kinetic model accurately simulated NHCl(2), NH(2)Cl, NDMA, and DO concentrations and included (1) the unified model of chloramine chemistry revised with HNO as a direct product of NHCl(2) hydrolysis; (2) HNO/NO(-) then reacting with (i) HNO to form N(2)O, (ii) DO to form ONOOH/ONOO(-), or (iii) NHCl(2) or NH(2)Cl to form nitrogen gas; and (3) NDMA formation via ONOOH/ONOO(-) or their decomposition products reacting with (i) dimethylamine (DMA) and/or (ii) chlorinated unsymmetrical dimethylhydrazine (UDMH-Cl), the product of NHCl(2) and DMA. Overall, updated NHCl(2) decomposition pathways are proposed, yielding (1) RNS via NHCl2 → HNO/NO- → O2ONOOH/ONOO- and (2) NDMA via ONOOH/ONOO- → UDMH - Cl or DMANDMA.