1981
DOI: 10.1016/0043-1354(81)90074-9
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Residual oxidant decay and bromate formation in chlorinated and ozonated sea-water

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Cited by 52 publications
(13 citation statements)
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“…It is known, however, that bromate may enter the aquatic environment as a result of various anthropogenic activities. These activities include the chlorination or ozonation of power plant cooling waters, the disinfection of drinking waters using chlorine, ozone, or perozone, and the use of sodium hypochlorite as an industrial and domestic disinfectant (Burton and Richardson, 1981;Richardson et al, 1981a;Garny, 1994). Given the potential for bromate to enter aquatic ecosystems, a critical review has been undertaken of the available data on the effects of bromate on aquatic organisms.…”
Section: Introductionmentioning
confidence: 99%
“…It is known, however, that bromate may enter the aquatic environment as a result of various anthropogenic activities. These activities include the chlorination or ozonation of power plant cooling waters, the disinfection of drinking waters using chlorine, ozone, or perozone, and the use of sodium hypochlorite as an industrial and domestic disinfectant (Burton and Richardson, 1981;Richardson et al, 1981a;Garny, 1994). Given the potential for bromate to enter aquatic ecosystems, a critical review has been undertaken of the available data on the effects of bromate on aquatic organisms.…”
Section: Introductionmentioning
confidence: 99%
“…Firstly, ozone can act directly as a disinfectant, readily oxidizing microbial pathogens in the systems. Secondly, the reaction of ozone with halides present in seawater, such as the bromide ion, generates more stable residual oxidant by-products, such as bromine and bromate (Crecelius 1979;Richardson, Burton, Helz & Rhoderick 1981;Grguric, Trefry & Kea¡aber 1994;Tango & Gagnon 2003), which can provide longerlasting microbial disinfection. For many seawater systems using ozone disinfection, the residual oxidants will often be the primary mode of disinfection, due to the instability and transience of ozone in seawater (Crecelius 1979).…”
Section: Introductionmentioning
confidence: 99%
“…These reactions are pH-dependent since 'OBr is in equilibrium with hypobromous acid (HOBr) and ozone does not oxidize HOBr to BrO 3 ' in the direct ozone pathway. The formation of BrO 3 " through a radical pathway is influenced by both pH and alkalinity (Richardson et al, 1981;Siddiqui et al, 1995).…”
Section: Introductionmentioning
confidence: 99%