Drivers of variability in disinfection by-product formation potential in a chain of thermally stratified drinking water reservoirs. Issue 5 (5th April 2022)

• Record Type: Journal Article
• Authors: Munthali, Elias; Marcé, Rafael; Farré, Maria José
• Is Part Of: Environmental science. Volume 8:Issue 5(2022)
• Page Start: 968
• Page End: 980
• Publication Date: 2022-04-05
• Subjects: Water-supply -- Periodicals; Water security -- Periodicals; Water resources development -- Periodicals; Water chemistry -- Periodicals; 553.705
• DOI: 10.1039/d1ew00788b
• Languages: English
• ISSNs: 2053-1400

Abstract

Abstract : Increasing hydraulic residence time (HRT) along a chain of interconnected reservoirs enhances the formation potential of carbonaceous disinfection by-products (DBPs) and reduces the formation potential of nitrogenous DBPs, particularly N -nitrosodimethylamine (NDMA). Abstract : Eutrophication, run-off and wastewater inputs to lakes have been identified as significant sources of disinfection by-product (DBPs) precursors, which are suspected carcinogens, in chlor(am)inated water. However, studies addressing the impacts of reservoirs and thermal stratification on DBP precursors are scarce. We conducted a seasonal study along a river–reservoir interconnected system, to investigate the effects of hydraulic residence time (HRT), thermal stratification, and seasonality on the levels and speciation of carbonaceous and nitrogenous DBP formation potential (FP) in source waters. Formation of 4 trihalomethanes (THMs), 4 haloacetonitriles (HANs), 2 haloketones and N -nitrosodimethylamine (NDMA) was measured on filtered lake water. Total THMs (TTHMs) FP was below 93 μg L −1, of which 59–87% of it was trichloromethane (TCM). Formation of dichloroacetonitrile (DCAN), 1, 1, 1-trichloropropanone (TCP), and NDMA was under 12 μg L −1, 13 μg L −1 and 73 ng L −1, respectively. The FP of the remaining DBPs was under 2 μg L −1 . While the effect of depth on DBP FP was insignificant, inter-system and seasonal effects were conspicuous. The most significant variable affecting DBP formation was season, where carbonaceous DBP FP was higher in autumn and summer than in winter. TTHM FP ranged from a 160% median increase in the river upstream of the reservoirs, to a 31% median increase in the last reservoir of the system, from winter to summer. On the contrary, NDMA FP ranged from a 145% median decrease in the river upstream of the reservoirs to an 11% median decrease in the middle reservoir, from winter to summer. TTHMs FP increased from the river upstream of the reservoirs to the last reservoir of the system (40.6% median increase), whereas the opposite trend was also observed for NDMA FP (63% median decrease).