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首页> 外文期刊>Environmental Science & Technology >Carbon Isotopic Fractionation during Anaerobic Biotransformation of Methyl tert-Butyl Ether and tert-Amyl Methyl Ether
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Carbon Isotopic Fractionation during Anaerobic Biotransformation of Methyl tert-Butyl Ether and tert-Amyl Methyl Ether

机译:甲基叔丁基醚和叔戊基甲基醚厌氧生物转化过程中的碳同位素分馏

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The fuel oxygenate methyl tert-butyl ether (MTBE) has been frequently detected in groundwater and surface water. Since contaminated sites are often subsurface, anaerobic degradation of MTBE will likely be significant for remediation. As traditional approaches to evaluate biodegradation generally involve laboratory microcosm studies, which require time and resources, innovative approaches are needed to demonstrate active in situ biodegradation of MTBE. This study was conducted to gather information at the laboratory level to evaluate the potential of applying carbon isotope fractionation as an indicator for in situ biodegradation of the fuel oxygenates MTBE and ferf-amyl methyl ether (TAME). In this study, MTBE utilization was observed in a methanogenic sediment microcosm after a lengthy lag period of about 400 days. MTBE utilization was sustained upon refeeding and subculturing. tert-Butyl alcohol (TBA) was found to accumulate after propagation of cultures. The MTBE-grown cultures also utilized TAME and produced ferf-amyl alcohol (TAA). The detection of TBA and TAA indicated that ether bond cleavage was the initial step in degradation for both compounds. Carbon isotope fractionation during anaerobic MTBE and TAME degradation was studied, and isotopic enrichmentfactors (ε) with 95% confidence intervals of -15.6 ± 4.1‰ and -13.7 ± 4.5% were estimated for anaerobic MTBE and TAME degradation, respectively. Addition of 2-bromoethanesulfonic acid, an inhibitor of methanogenesis, substantially prolonged the lag period before transformation, but did not influence carbon isotope fractionation. Our experiment provided strong evidence of significant carbon isotope fractionation during anaerobic MTBE and TAME degradation, demonstrating that this technique can be used as an indicator for in situ MTBE and TAME degradation.
机译:经常在地下水和地表水中检测到燃料含氧化合物甲基叔丁基醚(MTBE)。由于受污染的地点通常位于地下,因此MTBE的厌氧降解可能对修复至关重要。由于评估生物降解的传统方法通常涉及实验室缩影研究,这需要时间和资源,因此需要创新的方法来证明MTBE的主动原位生物降解。进行这项研究是为了在实验室水平上收集信息,以评估应用碳同位素分馏作为燃料含氧化合物MTBE和戊戊基甲基醚(TAME)原位生物降解的指标的潜力。在这项研究中,经过约400天的长时间滞后后,在产甲烷沉积物微观世界中观察到了MTBE的利用。重新喂养和继代培养后,MTBE的利用率得以维持。发现在培养物繁殖后会积累叔丁醇(TBA)。 MTBE生长的培养物也利用TAME产生了戊戊醇(TAA)。对TBA和TAA的检测表明,醚键的裂解是两种化合物降解的第一步。研究了厌氧MTBE和TAME降解过程中的碳同位素分馏,估计厌氧MTBE和TAME降解的同位素富集因子(ε)分别为-15.6±4.1‰和-13.7±4.5%的95%置信区间。甲烷生成抑制剂2-溴乙烷磺酸的加入大大延长了转化前的滞后时间,但不影响碳同位素分馏。我们的实验提供了厌氧MTBE和TAME降解过程中碳同位素分馏的显着证据,表明该技术可以用作原位MTBE和TAME降解的指标。

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