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在两种不同油砂尾矿中,产甲烷条件下复杂石脑油烃的顺序生物降解。

Sequential biodegradation of complex naphtha hydrocarbons under methanogenic conditions in two different oil sands tailings.

机构信息

Department of Renewable Resources, University of Alberta, Edmonton, AB, Canada.

出版信息

Environ Pollut. 2017 Feb;221:398-406. doi: 10.1016/j.envpol.2016.12.002. Epub 2016 Dec 7.

Abstract

Methane emissions in oil sands tailings ponds are sustained by anaerobic biodegradation of unrecovered hydrocarbons. Naphtha (primarily C-C; n- iso- and cycloalkanes) is commonly used as a solvent during bitumen extraction process and its residue escapes to tailings ponds during tailings deposition. To investigate biodegradability of hydrocarbons in naphtha, mature fine tailings (MFT) collected from Albian and CNRL tailings ponds were amended with CNRL naphtha at ∼0.2 wt% (∼2000 mg L) and incubated under methanogenic conditions for ∼1600 d. Microbial communities in both MFTs started metabolizing naphtha after a lag phase of ∼100 d. Complete biodegradation/biotransformation of all n-alkanes (except partial biodegradation of n-octane in CNRL MFT) followed by major iso-alkanes (2-methylpentane, 3-methylhexane, 2- and 4-methylheptane, iso-nonanes and 2-methylnonane) and a few cycloalkanes (derivatives of cyclopentane and cyclohexane) was observed during the incubation. 16S rRNA gene pyrosequencing showed dominance of Peptococcaceae and Anaerolineaceae in Albian MFT and Anaerolineaceae and Syntrophaceae in CNRL MFT bacterial communities with co-domination of Methanosaetaceae and "Candidatus Methanoregula" in archaeal populations during active biodegradation of hydrocarbons. The findings extend the known range of hydrocarbons susceptible to methanogenic biodegradation in petroleum-impacted anaerobic environments and help refine existing kinetic model to predict greenhouse gas emissions from tailings ponds.

摘要

油砂尾矿池中的甲烷排放是由未回收烃类的厌氧生物降解维持的。石脑油(主要为 C-C;正构和环烷烃)在沥青提取过程中通常用作溶剂,其残留物在尾矿沉积过程中会逸入尾矿池。为了研究石脑油中烃类的生物降解性,从阿尔伯因和 CNRL 尾矿池中采集成熟细尾矿(MFT),并用 CNRL 石脑油在约 0.2 wt%(约 2000 mg/L)进行修正,并在产甲烷条件下孵育约 1600 天。在大约 100 天的滞后期后,两种 MFT 中的微生物群落开始代谢石脑油。在孵育过程中,所有正构烷烃(除了 CNRL MFT 中部分正辛烷的生物降解)完全生物降解/生物转化,随后主要异构烷烃(2-戊烷、3-己烷、2-和 4-庚烷、异壬烷和 2-壬烷)和一些环烷烃(环戊烷和环己烷的衍生物)被大量消耗。16S rRNA 基因焦磷酸测序显示,在阿尔伯因 MFT 中,Peptococcaceae 和 Anaerolineaceae 占优势,而在 CNRL MFT 中,Anaerolineaceae 和 Syntrophaceae 占优势,在烃类生物降解过程中,产甲烷菌科和“Candidatus Methanoregula”在古菌群体中共同占主导地位。这些发现扩展了已知的在受石油影响的厌氧环境中易受产甲烷生物降解影响的烃类范围,并有助于完善现有的动力学模型,以预测尾矿池的温室气体排放。

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