Helmholtz Zentrum München-German Research Center for Environmental Health, Institute of Ecological Chemistry, Ingolstädter Landstr. 1, 85764, Neuherberg, Germany.
Environ Sci Pollut Res Int. 2011 May;18(4):547-55. doi: 10.1007/s11356-010-0393-0. Epub 2010 Oct 4.
BACKGROUND, AIM, AND SCOPE: 3-Chlorocarbazole and 3,6-dichlorocarbazole were isolated from Bavarian soils. The stereospecific formation of the isomers of these chlorinated carbazols can be explained by quantum mechanical calculations using the DFT method. It was shown that chlorination of carbazole and 3-chlorocarbazole respectively is preferred via the sigma-complexes 3-chlorocarbazole and 3,6-dichlorocarbazole as the most stable products. The dioxin-like toxicological potential of 3,6-dichlorocarbazole, determined by the Micro-EROD Test, is in the range of some picogram TCDD equivalents per milligram carbazole. The degradative fate of 3-chlorocarbazole and 3,6-dichlorocarbazole was analysed within a long-term study (57 days) in soil.
The soil was extracted by ASE (accelerated solvent extraction) and a further clean-up procedure with column chromatography and chromatography with C18-SPE stationary phases. Quantification of 3-chlorocarbazole and 3,6-dichlorocarbazole was performed employing the isotope-dilution method. The samples were measured with high-resolution GC/MS.
The degradation (ln(c/c(0)) vs. time with best-fit line) showed in almost every storage condition a very small degradation (slopes (h(-1)) in -10(-4) range). However, the decay for the controls were two to three times (-28°C) and six times (with sodium azide) higher, than the decrease of 3-chlorocarbazole and 3,6-dichlorocarbazole in the samples of environmental conditions.
Especially because of the toxicological potential of 3-chlorocarbazole and 3,6-dichlorocarbazole the proven degradative fate is of large interest. The results show that the analysed carbazoles are not readily degradable in this time period.
The expected results of exponential decay behaviour could not be proven.
Longer-lasting studies are expected to reveal more accurate half-lives, although it has been shown here, that the compounds are not readily degradable in their native soil environment.
背景、目的和范围:3-氯咔唑和 3,6-二氯咔唑从巴伐利亚土壤中分离出来。使用密度泛函理论 (DFT) 方法进行量子力学计算,可以解释这些氯化咔唑异构体的立体特异性形成。结果表明,咔唑和 3-氯咔唑的氯化分别通过最稳定的产物 3-氯咔唑和 3,6-二氯咔唑的 σ-配合物优先进行。3,6-二氯咔唑的类二恶英毒性潜力通过 Micro-EROD 测试确定,每毫克咔唑的 TCDD 当量为几个皮克。在一项长期研究(57 天)中分析了 3-氯咔唑和 3,6-二氯咔唑在土壤中的降解命运。
通过 ASE(加速溶剂提取)和柱色谱和 C18-SPE 固定相的色谱进一步提取土壤。使用同位素稀释法对 3-氯咔唑和 3,6-二氯咔唑进行定量。使用高分辨率 GC/MS 测量样品。
在几乎所有储存条件下,降解(ln(c/c(0)) 与时间的最佳拟合线)都显示出非常小的降解(斜率(h(-1)) 在-10(-4) 范围内)。然而,与环境条件下样品中 3-氯咔唑和 3,6-二氯咔唑的减少相比,对照物的衰减(-28°C)高两倍到三倍,与带有叠氮化钠的对照物的衰减高六倍。
特别是由于 3-氯咔唑和 3,6-二氯咔唑的毒理学潜力,已证明的降解命运具有重要意义。结果表明,在所分析的咔唑在这段时间内不易降解。
未证明预期的指数衰减行为的结果。
预计更长时间的研究将揭示更准确的半衰期,尽管这里已经表明,这些化合物在其天然土壤环境中不易降解。