Aspects of THM formation in drinking-water

T. J. Casey, Kok Hua Chua

Research output: Contribution to journalArticle

19 Citations (Scopus)

Abstract

The formation of trihalomethanes (THMs) in drinking water is the result of reaction between chlorine and organic matter, mainly of natural origin (NOM). This paper presents some of the findings of a laboratory study of THM formation in 12 Irish surface waters that are important water supply sources. At the production plants these waters are treated by conventional chemical coagulation, rapid gravity filtration and chlorination, using aluminium sulphate as primary coagulant. The same processes were applied at laboratory scale. A standard chlorination was used throughout, based on the chlorine dose required to produce a residual free chlorine (RFC) concentration of 0.5 mg/L after a 30-min contact time. It was found that the RFC decay rate could be approximately modelled as a first order reaction using the 2 h RFC concentration to quantify the reaction rate constant. The applied standard chlorination dose, which is that recommended by World Health Organisation (WHO), gave a wide spread of Ct values. The results indicate that a chlorination norm, expressed as RFC at a contact time of 2 h, would provide a more consistent set of Ct values for the waters tested in this study. It was found that the rate of total THM (TTHM) formation could be modelled as a hyperbolic growth function, defined by two parameters, t50 and TTHMmax, where I50 is the reaction time required for the TTHM concentration to reach half TTHMmax, its ultimate value. For the set of waters studied, the t50 values varied in the range 1.06-2.48 h, while the TTHMmax values varied in the range 22-56 μg/L. The THM species formed in the test set of waters included chloroform (CHCl3), bromodichloromethane (CHBrCl2) and dibromochloromethane (CHBr2Cl). Bromoform (CHBr3) was not detected in any of the samples. In the case of the high alkalinity waters of the test set, a downward adjustment of the coagulation pH to the region 5.5-6.5 resulted in lower coagulant and chlorine demands, improved TOC removal and reduced THM formation.

Original languageEnglish
Pages (from-to)31-39
Number of pages9
JournalJournal of Water Supply: Research and Technology - AQUA
Volume46
Issue number1
Publication statusPublished - 01 Feb 1997

Fingerprint

Trihalomethanes
Chlorine
Potable water
Drinking Water
chlorine
drinking water
Chlorination
Halogenation
chlorination
Water
Coagulants
Coagulation
coagulation
water
Water Supply
World Health Organization
Gravitation
Alkalinity
Chloroform
Chlorine compounds

All Science Journal Classification (ASJC) codes

  • Environmental Engineering
  • Water Science and Technology
  • Health, Toxicology and Mutagenesis

Cite this

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title = "Aspects of THM formation in drinking-water",
abstract = "The formation of trihalomethanes (THMs) in drinking water is the result of reaction between chlorine and organic matter, mainly of natural origin (NOM). This paper presents some of the findings of a laboratory study of THM formation in 12 Irish surface waters that are important water supply sources. At the production plants these waters are treated by conventional chemical coagulation, rapid gravity filtration and chlorination, using aluminium sulphate as primary coagulant. The same processes were applied at laboratory scale. A standard chlorination was used throughout, based on the chlorine dose required to produce a residual free chlorine (RFC) concentration of 0.5 mg/L after a 30-min contact time. It was found that the RFC decay rate could be approximately modelled as a first order reaction using the 2 h RFC concentration to quantify the reaction rate constant. The applied standard chlorination dose, which is that recommended by World Health Organisation (WHO), gave a wide spread of Ct values. The results indicate that a chlorination norm, expressed as RFC at a contact time of 2 h, would provide a more consistent set of Ct values for the waters tested in this study. It was found that the rate of total THM (TTHM) formation could be modelled as a hyperbolic growth function, defined by two parameters, t50 and TTHMmax, where I50 is the reaction time required for the TTHM concentration to reach half TTHMmax, its ultimate value. For the set of waters studied, the t50 values varied in the range 1.06-2.48 h, while the TTHMmax values varied in the range 22-56 μg/L. The THM species formed in the test set of waters included chloroform (CHCl3), bromodichloromethane (CHBrCl2) and dibromochloromethane (CHBr2Cl). Bromoform (CHBr3) was not detected in any of the samples. In the case of the high alkalinity waters of the test set, a downward adjustment of the coagulation pH to the region 5.5-6.5 resulted in lower coagulant and chlorine demands, improved TOC removal and reduced THM formation.",
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Aspects of THM formation in drinking-water. / Casey, T. J.; Chua, Kok Hua.

In: Journal of Water Supply: Research and Technology - AQUA, Vol. 46, No. 1, 01.02.1997, p. 31-39.

Research output: Contribution to journalArticle

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AB - The formation of trihalomethanes (THMs) in drinking water is the result of reaction between chlorine and organic matter, mainly of natural origin (NOM). This paper presents some of the findings of a laboratory study of THM formation in 12 Irish surface waters that are important water supply sources. At the production plants these waters are treated by conventional chemical coagulation, rapid gravity filtration and chlorination, using aluminium sulphate as primary coagulant. The same processes were applied at laboratory scale. A standard chlorination was used throughout, based on the chlorine dose required to produce a residual free chlorine (RFC) concentration of 0.5 mg/L after a 30-min contact time. It was found that the RFC decay rate could be approximately modelled as a first order reaction using the 2 h RFC concentration to quantify the reaction rate constant. The applied standard chlorination dose, which is that recommended by World Health Organisation (WHO), gave a wide spread of Ct values. The results indicate that a chlorination norm, expressed as RFC at a contact time of 2 h, would provide a more consistent set of Ct values for the waters tested in this study. It was found that the rate of total THM (TTHM) formation could be modelled as a hyperbolic growth function, defined by two parameters, t50 and TTHMmax, where I50 is the reaction time required for the TTHM concentration to reach half TTHMmax, its ultimate value. For the set of waters studied, the t50 values varied in the range 1.06-2.48 h, while the TTHMmax values varied in the range 22-56 μg/L. The THM species formed in the test set of waters included chloroform (CHCl3), bromodichloromethane (CHBrCl2) and dibromochloromethane (CHBr2Cl). Bromoform (CHBr3) was not detected in any of the samples. In the case of the high alkalinity waters of the test set, a downward adjustment of the coagulation pH to the region 5.5-6.5 resulted in lower coagulant and chlorine demands, improved TOC removal and reduced THM formation.

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