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Variations of Acidic Compounds in Crude Oil during Simulated Aerobic Biodegradation: Monitored by Semiquantitative Negative-Ion ESI FT-ICR MS

机译:需氧生物降解过程中原油中酸性化合物的变化:通过半定量负离子ESI FT-ICR MS监测

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摘要

Simulations of aerobic biodegradation have been widely employed to investigate the mechanisms of crude oil biodegradation in geological environments. In this study, a simulated biodegradation experiment was performed with crude oil under aerobic conditions, in which n-alkanes were nearly depleted, thus providing an opportunity to study the biodegradation mechanisms of n-alkanes in crude oils. The sequences of biodegraded oils with a slight to moderate degree of biodegradation were characterized by negative-ion electrospray (ESI) Fourier transform ion cyclotron resonance mass spectrometry (FT-ICR MS) and gas chromatography (GC). Semiquantitative results on the molecular compositions of heteroatom classes were obtained by coinjection of internal standards. The biodegradation mechanisms for n-alkanes and n-fatty acids, as well as some other heteroatomic compounds, are discussed, Evidence from FT-ICR MS and GC analyses of biodegraded oils indicates that n-alkanes can be progressively biodegraded to n-fatty acids through beta-oxidation, or to hydroxycarboxylic and dicarboxylic acids though omega-oxidation. The O-3 class species which have a high relative abundance in the carbon number range of C-33-C-38 with a Double Bond Equivalent (DBE) of 1-3 were assigned and speculated to be bacterial metabolites, which could be a conspicuous indicator of bacterial activity. Neutral nitrogen compounds, such as carbazoles, exhibited a very slight decrease in the stage of biodegradation that was investigated.
机译:有氧生物降解的模拟已被广泛用于研究地质环境中原油生物降解的机理。在这项研究中,在好氧条件下对原油进行了模拟生物降解实验,其中正构烷烃几乎被耗尽,从而为研究原油中正构烷烃的生物降解机理提供了机会。通过负离子电喷雾(ESI)傅里叶变换离子回旋共振质谱(FT-ICR MS)和气相色谱(GC)对具有轻度到中度生物降解的生物降解油序列进行了表征。通过内标共注射获得杂原子类分子组成的半定量结果。讨论了正构烷烃和正脂肪酸以及其他一些杂原子化合物的生物降解机理。来自FT-ICR MS和GC分析的生物降解油的证据表明,正构烷烃可以逐步被生物降解为正脂肪酸。通过β-氧化,或通过ω-氧化成羟基羧酸和二羧酸。在C-33-C-38的碳数范围内具有较高相对丰度且双键当量(DBE)为1-3的O-3类物质被指定为细菌代谢产物,可能是细菌代谢产物。细菌活动的明显指标。在研究的生物降解阶段,中性氮化合物(例如咔唑)表现出非常轻微的下降。

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  • 来源
    《Energy & fuels》 |2017年第2期|1126-1135|共10页
  • 作者单位

    Chinese Acad Sci, Guangzhou Inst Geochem, State Key Lab Organ Geochem, 511 Kehua St,Wushan Rd, Guangzhou 510640, Guangdong, Peoples R China|Univers Chinese Acad Sci, Yuquan Rd, Beijing 100049, Peoples R China|Sinopec Petr Explorat & Prod Res Inst, Wuxi Res Inst Petr Geol, Sinopec Key Lab Petr Accumulat Mech, 2060 Lihu Rd, Wuxi 214000, Jiangsu, Peoples R China;

    Chinese Acad Sci, Guangzhou Inst Geochem, State Key Lab Organ Geochem, 511 Kehua St,Wushan Rd, Guangzhou 510640, Guangdong, Peoples R China;

    China Univ Petr, State Key Lab Heavy Oil Proc, Beijing 102249, Peoples R China;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《生物学医学文摘》(MEDLINE);
  • 原文格式 PDF
  • 正文语种 eng
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