PubMed · 6126697
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P C Elwood. 1982-10-09. Mis-lead by the E.E.C.. https://doi.org/10.1016/s0140-6736(82)92717-9
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Chloroform (CHCl3) is a short-lived ozone-depleting substance not currently regulated under the Montreal Protocol. Due to the unique meteorological conditions in East Asia, CHCl3 emitted in this region has a greater potential to reach the stratosphere and contribute to ozone depletion. As an essential component of national CHCl3 emissions, southeastern China has attracted increasing attention. However, long-term observational data in this region remain relatively scarce, with no updates since 2020. In this study, we continuously measured atmospheric CHCl3 concentrations at a remote monitoring station in southeastern China from 1 June 2023 to 31 May 2025. Frequent concentration enhancements were observed during the monitoring period, with mixing ratios ranging from 9.3 to 134.1 ppt and an average value of 36.8 ± 19.7 ppt. Back-trajectory analysis indicated that air masses associated with elevated CHCl3 levels primarily originated from coastal industrial provinces in eastern China. Using the Potential Source Contribution Function and Concentration Weighted Trajectory methods, we identified the Yangtze River Delta (Jiangsu, Anhui, and Zhejiang Provinces) and Jiangxi Province as dominant source regions. Emissions of CHCl3 in southeastern China were estimated using the Tracer Ratio Method to be approximately 30.1 ± 5.3 Gg/yr from 2023-06-01 to 2025-05-31, indicating overall stability relative to earlier estimates and no apparent upward trend. These findings provide updated insights into the current status of CHCl3 emissions in southeastern China and highlight the need for continued monitoring and emission assessment of CHCl3 in East Asia, given its unregulated status and implications for ozone layer recovery.
Metabolism of 2-nitrofluoranthene (2-NFA), one of the most abundant and genotoxic environmental pollutants in air, and of a mixture of 2-nitrofluoranthene and 3-nitrofluoranthene (3-NFA) was studied using (1) the fungus Cunninghamella elegans ATCC 36112 and (2) rat liver microsomes. The fungal metabolites were separated by reversed-phase high-performance liquid chromatography (HPLC) and identified by 1H nuclear magnetic resonance (NMR) spectrometry, ultraviolet (UV)-visible spectroscopy, and online atmospheric-pressure chemical ionization/mass spectrometry (APCI/MS). The fungus metabolized 82% of 2-nitro-[3H]-fluoranthene to 2-nitrofluoranthene 8-sulfate and 2-nitrofluoranthene 9-sulfate. Metabolism of a mixture of 2- and 3-nitrofluoranthene by C. elegans similarly produced 2-nitrofluoranthene 8- and 9-sulfate and 3-nitrofluoranthene 8- and 9-sulfate as major metabolites. In addition, a glucoside conjugate of 3-hydroxy-2-nitrofluoranthene was tentatively identified by APCI/MS analysis. When rat liver microsomes were incubated with a mixture of 2- and 3-nitrofluoranthene for 1 h, in addition to the trans-7,8- and 9,10-dihydrodiols reported previously for 2-nitrofluoranthene, several novel metabolites were produced including 2-nitrofluoranthene trans-4,5-dihydrodiol and 2-nitrofluoranthene trans-8,9-dihydrodiol, the trans-4,5-dihydrodiol of 3-nitrofluoranthene, and phenolic products of both 2- and 3-nitrofluoranthene. The fungal metabolism of the 2- and 3-nitrofluoranthene mixture was similar to the metabolism of individual nitrofluoranthenes; however, the mammalian metabolism of the nitrofluoranthene mixture showed differences in regioselectivity at positions C4, C5, C8, and C9.
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