Demonstrating a natural origin of chloroform in groundwater using stable carbon isotopes

Daniel Hunkeler, Troels Laier, Florian Breider, Ole Stig Jacobsen

Publikation: Bidrag til tidsskriftArtikelForskningpeer review

41 Citationer (Scopus)

Abstrakt

Chloroform has been for a long time considered only as an anthropogenic contaminant. The presence of chloroform in forest soil and groundwater has been widely demonstrated. The frequent detection of chloroform in groundwater in absence of other contaminants suggests that chloroform is likely produced naturally. Compound-specific isotope analysis of chloroform was performed on soil-gas and groundwater samples to elucidate whether its source is natural or anthropogenic. The δ 13C values of chloroform (-22.8 to -26.2‰) present in soil gas collected in a forested area are within the same range as the soil organic matter (-22.6 to -28.2‰) but are more enriched in 13C compared to industrial chloroform (-43.2 to -63.6‰). The δ 13C values of chloroform at the water table (-22.0‰) corresponded well to the δ 13C of soil gas chloroform, demonstrating that the isotope signature of chloroform is maintained during transport through the unsaturated zone. Generally, the isotope signature of chloroform is conserved also during longer range transport in the aquifer. These δ 13C data support the hypothesis that chloroform is naturally formed in some forest soils. These results may be particularly relevant for authorities' regulation of chloroform which in the case of Denmark was very strict for groundwater (<1 μg/L).

OriginalsprogEngelsk
Sider (fra-til)6096-6101
Antal sider6
TidsskriftEnvironmental Science & Technology
Vol/bind46
Udgave nummer11
DOI
StatusUdgivet - 5 jun. 2012

Programområde

  • Programområde 5: Natur og klima

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