Department of Civil and Environmental Engineering, University of Massachusetts, Amherst, MA 01003, USA.
J Hazard Mater. 2012 Mar 30;209-210:92-8. doi: 10.1016/j.jhazmat.2011.12.067. Epub 2012 Jan 9.
Although 1,2-dibromoethane (EDB) is a common groundwater contaminant, there is the lack of knowledge surrounding EDB biodegradation, especially under aerobic conditions. We have performed an extensive microcosm study to investigate the biodegradation of EDB under simulated in situ and biostimulated conditions. The materials for soil microcosms were collected from an EDB-contaminated aquifer at the Massachusetts Military Reservation in Cape Cod, MA. This EDB plume has persisted for nearly 40 years in both aerobic and anaerobic EDB zones of the aquifer. Microcosms were constructed under environmentally relevant conditions (field EDB and DO concentrations; incubated at 12°C). The results showed that natural attenuation occurred under anaerobic conditions but not under aerobic conditions, explaining why aerobic EDB contamination is so persistent. EDB degradation rates were greater under biostimulated conditions for both the aerobic and anaerobic microcosms. Particularly for aerobic biostimulation, methane-amended microcosms degraded EDB, on average, at a first order rate eight times faster than unamended microcosms. The best performing replicate achieved an EDB degradation rate of 7.0 yr(-1) (half-life (t(1/2))=0.10 yr). Residual methane concentrations and the emergence of methanotrophic bacteria, measured by culture independent bacterial analysis, provided strong indications that EDB degradation in aerobic methane-amended microcosms occurred via cometabolic degradation. These results indicate the potential for enhanced natural attenuation of EDB and that methane could be considered co-substrate for EDB bioremediation for the EDB-contaminated groundwater in aerobic zone.
尽管 1,2-二溴乙烷(EDB)是一种常见的地下水污染物,但人们对其生物降解知之甚少,尤其是在有氧条件下。我们进行了广泛的微宇宙研究,以调查在模拟原位和生物刺激条件下 EDB 的生物降解情况。土壤微宇宙的材料取自马萨诸塞州军事保留地科德角的一个 EDB 污染含水层。这个 EDB 羽流在含水层的有氧和无氧 EDB 区已经持续了近 40 年。微宇宙是在环境相关条件下构建的(现场 EDB 和 DO 浓度;在 12°C 下孵育)。结果表明,在厌氧条件下会发生自然衰减,但在有氧条件下不会,这解释了为什么有氧 EDB 污染如此持久。在有氧和厌氧微宇宙中,生物刺激条件下的 EDB 降解速率都更高。特别是对于有氧生物刺激,添加甲烷的微宇宙中 EDB 的降解速度比未添加甲烷的微宇宙快一级,平均快八倍。表现最好的复制品的 EDB 降解速率达到了 7.0 年(半衰期(t(1/2))=0.10 年)。通过非培养细菌分析测量的残留甲烷浓度和甲烷营养细菌的出现,强烈表明有氧添加甲烷的微宇宙中 EDB 的降解是通过共代谢降解发生的。这些结果表明,EDB 的自然衰减增强的潜力,并且可以考虑甲烷作为有氧区 EDB 污染地下水的 EDB 生物修复的共底物。