MISC

2005年1月

Occurrence and production of chloramines in the chlorination of creatinine in aqueous solution

WATER RESEARCH
  • M Tachikawa
  • ,
  • T Aburada
  • ,
  • M Tezuka
  • ,
  • R Sawamura

39
2-3
開始ページ
371
終了ページ
379
記述言語
英語
掲載種別
DOI
10.1016/j.watres.2004.09.029
出版者・発行元
PERGAMON-ELSEVIER SCIENCE LTD

Occurrence and production of stable chloramines in the chlorination of creatinine, a constituent of perspiration and urine, in aqueous media were studied. Creatinine (5 x 10(-5) M) was treated with free chlorine in aqueous solutions at molar ratios of 0.5-8 (chlorine/creatinine) at pH 7.0 at room temperature for several days. At lower ratios of chlorine, two stable N-chlorocreatinine derivatives, which were determined as dichloramine fractions by the DPD method, were isolated by HPLC and identified by EI-MS and H-1-NMR. One was 2-chloroamino-1-methylimidazolin-4-one (creatinine chloramine) and the other was 2-chloroamino-5-hydroxy-1-methylimidazolin-4-one (hydroxycreatinine chloramine). In addition, the formation of methylamine was identified by GC-MS analyses of its imine derivative formed with pentafluorobenzaldehyde. Methylamine forms stable chloramines, which might be determined as mono- and/or di-chloramine fractions together with free chlorine by the DPD method in the reaction mixtures at higher molar ratios of chlorine. In practice, small amounts of methylamine (ca. 19 mug/L) were detected in water samples collected from several swimming pools. Hence, methylamine may be an origin of elusive organic chloramine formed in the chlorination of swimming pools. A probable mechanism of the occurrence and processing of chlorination products of creatinine is suggested. (C) 2004 Elsevier Ltd. All rights reserved.

リンク情報
DOI
https://doi.org/10.1016/j.watres.2004.09.029
Web of Science
https://gateway.webofknowledge.com/gateway/Gateway.cgi?GWVersion=2&SrcAuth=JSTA_CEL&SrcApp=J_Gate_JST&DestLinkType=FullRecord&KeyUT=WOS:000226727600011&DestApp=WOS_CPL
ID情報
  • DOI : 10.1016/j.watres.2004.09.029
  • ISSN : 0043-1354
  • Web of Science ID : WOS:000226727600011

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