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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

Carbon isotopic fractionation during anaerobic biotransformation of methyl tert-butyl ether and tert-amyl methyl ether.

作者信息

Somsamak Piyapawn, Richnow Hans H, Häggblom Max M

机构信息

Department of Biochemistry and Microbiology and Biotechnology, Center for Agriculture and the Environment, Rutgers, The State University of New Jersey, New Brunswick, New Jersey 08901, USA.

出版信息

Environ Sci Technol. 2005 Jan 1;39(1):103-9. doi: 10.1021/es049368c.

Abstract

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 tert-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 tert-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 enrichment factors (epsilon) 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.

摘要

燃料含氧化合物甲基叔丁基醚(MTBE)经常在地下水和地表水中被检测到。由于受污染场地通常在地下,MTBE的厌氧降解对于修复可能具有重要意义。由于评估生物降解的传统方法通常涉及实验室微观研究,需要耗费时间和资源,因此需要创新方法来证明MTBE在原位的生物降解活性。本研究旨在在实验室层面收集信息,以评估应用碳同位素分馏作为燃料含氧化合物MTBE和叔戊基甲基醚(TAME)原位生物降解指标的潜力。在本研究中,经过约400天的漫长滞后期后,在产甲烷沉积物微观模型中观察到了MTBE的利用情况。重新投喂和传代培养后,MTBE的利用得以持续。培养物繁殖后发现叔丁醇(TBA)积累。以MTBE培养的培养物也利用TAME并产生叔戊醇(TAA)。TBA和TAA的检测表明,醚键断裂是这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)及其95%置信区间分别为-15.6±4.1%和-13.7±4.5%。添加产甲烷抑制剂2-溴乙烷磺酸可显著延长转化前的滞后期,但不影响碳同位素分馏。我们的实验提供了有力证据,证明厌氧MTBE和TAME降解过程中存在显著的碳同位素分馏,表明该技术可作为MTBE和TAME原位降解的指标。

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