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The natural chlorine cycle - Formation of the carcinogenic and greenhouse gas compound chloroform in drinking water reservoirs

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    SYSNO ASEP0461919
    Document TypeJ - Journal Article
    R&D Document TypeJournal Article
    Subsidiary JČlánek ve WOS
    TitleThe natural chlorine cycle - Formation of the carcinogenic and greenhouse gas compound chloroform in drinking water reservoirs
    Author(s) Forczek, Sándor (UEB-Q) RID, ORCID
    Pavlík, Milan (UEB-Q) RID, ORCID
    Holík, Josef (UEB-Q) RID, ORCID
    Rederer, L. (CZ)
    Ferenčík, M. (CZ)
    Source TitleChemosphere. - : Elsevier - ISSN 0045-6535
    Roč. 157, AUG (2016), s. 190-199
    Number of pages10 s.
    Languageeng - English
    CountryGB - United Kingdom
    KeywordsClimate relevant compounds ; Trichloromethane ; Adsorbable organohalogens
    Subject RIVEF - Botanics
    R&D ProjectsGA13-11101S GA ČR - Czech Science Foundation (CSF)
    Institutional supportUEB-Q - RVO:61389030
    UT WOS000378452400024
    AnnotationChlorine cycle in natural ecosystems involves formation of low and high molecular weight organic compounds of living organisms, soil organic matter and atmospherically deposited chloride. Chloroform (CHCl3) and adsorbable organohalogens (AOX) are part of the chlorine cycle. We attempted to characterize the dynamical changes in the levels of total organic carbon (TOC), AOX, chlorine and CHCl3 in a drinking water reservoir and in its tributaries, mainly at its spring, and attempt to relate the presence of AOX and CHCl3 with meteorological, chemical or biological factors.

    Water temperature and pH influence the formation and accumulation of CHCl3 and affect the conditions for biological processes, which are demonstrated by the correlation between CHCl3 and Sigma AOX/Cl- ratio, and also by CHCl3/Sigma AOX, CHCl3/AOX(LMW), CHCl3/Sigma TOC, CHCl3/TOCLMW and CHCl3/Cl- ratios in different microecosystems (e.g. old spruce forest, stagnant acidic water, humid and warm conditions with high biological activity). These processes start with the biotransformation of AOX from TOC, continue via degradation of AOX to smaller molecules and further chlorination, and finish with the formation of small chlorinated molecules, and their subsequent volatilization and mineralization. The determined concentrations of chloroform result from a dynamic equilibrium between its formation and degradation in the water; in the Hamry water reservoir, this results in a total amount of 0.1-0.7 kg chloroform and 5.2-15.4 t chloride. The formation of chloroform is affected by Cl- concentration, by concentrations and ratios of biogenic substrates (TOC and AOX), and by the ratios of the substrates and the product (feedback control by chloroform itself).
    WorkplaceInstitute of Experimental Botany
    ContactDavid Klier,, Tel.: 220 390 469
    Year of Publishing2017
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