Demonstrating a Natural Origin of Chloroform in Groundwater Using Stable Carbon Isotopes

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• 作者：Daniel Hunkeler ; Troels Laier ; Florian Breider ; Ole Stig Jacobsen
• 刊名：Environmental Science & Technology (ES&T)
• 出版年：2012
• 出版时间：June 5, 2012
• 年：2012
• 卷：46
• 期：11
• 页码：6096-6101
• 全文大小：292K
• 年卷期：v.46,no.11(June 5, 2012)
• ISSN：1520-5851

文摘

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 未¹³C values of chloroform (鈭?2.8 to 鈭?6.2鈥? present in soil gas collected in a forested area are within the same range as the soil organic matter (鈭?2.6 to 鈭?8.2鈥? but are more enriched in ¹³C compared to industrial chloroform (鈭?3.2 to 鈭?3.6鈥?. The 未¹³C values of chloroform at the water table (鈭?2.0鈥? corresponded well to the 未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 未¹³C data support the hypothesis that chloroform is naturally formed in some forest soils. These results may be particularly relevant for authorities鈥?regulation of chloroform which in the case of Denmark was very strict for groundwater (<1 渭g/L).