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Assessing mechanisms of isotopic fractionation during petroleum hydrocarbon biodegradation - Implications for evaluation of in situ biodegradation.

机译:石油烃生物降解过程中同位素分馏的评估机制-对原位生物降解评估的意义。

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摘要

In this thesis, mechanisms of carbon and hydrogen isotopic fractionation were investigated during biodegradation of petroleum hydrocarbons, benzene and toluene, in order to evaluate the potential to use Compound Specific Isotope Analysis (CSIA) to assess in situ biodegradation under various field conditions. Variation in carbon and hydrogen enrichment factors, determined using a Rayleigh model, was observed for benzene degradation under different terminal electron accepting processes in enrichment cultures derived from three field sites. This variation was controlled by different biodegradation pathways for the nitrate-reducing cultures, and the methanogenic and sulfate-reducing cultures, as determined by a two-element isotopic approach comparing delta 13C and delta2H values between degradation experiments. Significant differences in carbon and hydrogen enrichment factors were also observed in Pseudomonas putida mt-2 cultures grown under low and high iron concentrations during aerobic toluene biodegradation. These differences were related to changes in the rate-limiting steps of the enzyme-controlled reaction whereby a slower enzyme-catalyzed substrate conversion step (k 2) relative to the enzyme-substrate binding step (k-1) was suggested to occur. No significant differences in carbon and hydrogen isotopic fractionation were observed between a methanogenic enrichment culture and cell free extract experiments during toluene degradation. These results indicated that substrate transport across the cell membrane of the microorganisms involved in biodegradation did not influence isotopic fractionation in this culture.;Overall, the results of this thesis demonstrated that resolvable differences in carbon and hydrogen isotopic fractionation were not random but occurred for different microbial communities, biodegradation pathways and growth conditions. Significant 13C and 2H enrichment occurred in all experiments carried out in this thesis, indicating that carbon and hydrogen CSIA has the potential to identify in situ biodegradation of benzene and toluene. In addition, the variability in carbon and hydrogen enrichment factors did not significantly impact the ability to use stable isotope analysis to quantify in situ biodegradation. The measurement of both carbon and hydrogen isotope analysis in laboratory experiments and a field study demonstrated that a two-element isotopic approach is the best approach to differentiate between in situ biodegradation and sources of groundwater contamination, as well as potentially delineate between biodegradation pathways.
机译:本文研究了石油烃,苯和甲苯生物降解过程中碳氢同位素分离的机理,以评估使用化合物特异性同位素分析(CSIA)评估各种田间条件下原位生物降解的潜力。使用瑞利模型确定的碳和氢富集因子的变化,在源自三个场点的富集培养物中,在不同的末端电子接受过程下,苯的降解情况得到了观察。这种变化是由硝酸盐还原培养物,甲烷化和硫酸盐还原培养物的不同生物降解途径控制的,这是通过两元素同位素方法比较降解实验之间的δ13C和delta2H值确定的。在有氧甲苯生物降解过程中,在低铁浓度和高铁浓度下生长的恶臭假单胞菌mt-2培养物中,也发现了碳和氢富集因子的显着差异。这些差异与酶控制反应的限速步骤的改变有关,由此表明相对于酶-底物结合步骤(k-1)发生较慢的酶催化底物转化步骤(k 2)。在甲苯降解过程中,产甲烷富集培养和无细胞提取物实验之间未观察到碳和氢同位素分馏的显着差异。这些结果表明,参与生物降解的微生物在细胞膜上的底物转运不会影响该培养物中的同位素分离。总的来说,本论文的结果表明,碳和氢同位素分离的可分辨差异不是随机的,而是因不同而发生的。微生物群落,生物降解途径和生长条件。在本文进行的所有实验中均发生了13C和2H富集,这表明碳和氢CSIA具有识别苯和甲苯的原位生物降解的潜力。此外,碳和氢富集因子的可变性并未显着影响使用稳定同位素分析定量原位生物降解的能力。在实验室实验和现场研究中对碳和氢同位素分析的测量结果表明,两种元素的同位素方法是区分原位生物降解和地下水污染源以及潜在地描述生物降解途径的最佳方法。

著录项

  • 作者

    Mancini, Silvia Alissa.;

  • 作者单位

    University of Toronto (Canada).;

  • 授予单位 University of Toronto (Canada).;
  • 学科 Petroleum Geology.;Geochemistry.
  • 学位 Ph.D.
  • 年度 2007
  • 页码 191 p.
  • 总页数 191
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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