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页岩气采出水中持久性产硫化物细菌的鉴定

Identification of Persistent Sulfidogenic Bacteria in Shale Gas Produced Waters.

作者信息

Cliffe Lisa, Nixon Sophie L, Daly Rebecca A, Eden Bob, Taylor Kevin G, Boothman Christopher, Wilkins Michael J, Wrighton Kelly C, Lloyd Jonathan R

机构信息

Department of Earth and Environmental Sciences, The University of Manchester, Manchester, United Kingdom.

Department of Soil and Crop Sciences, College of Agricultural Sciences, Colorado State University, Fort Collins, CO, United States.

出版信息

Front Microbiol. 2020 Feb 21;11:286. doi: 10.3389/fmicb.2020.00286. eCollection 2020.

DOI:10.3389/fmicb.2020.00286
PMID:32153553
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC7046593/
Abstract

Produced waters from hydraulically fractured shale formations give insight into the microbial ecology and biogeochemical conditions down-well. This study explores the potential for sulfide production by persistent microorganisms recovered from produced water samples collected from the Marcellus shale formation. Hydrogen sulfide is highly toxic and corrosive, and can lead to the formation of "sour gas" which is costly to refine. Furthermore, microbial colonization of hydraulically fractured shale could result in formation plugging and a reduction in well productivity. It is vital to assess the potential for sulfide production in persistent microbial taxa, especially when considering the trend of reusing produced waters as input fluids, potentially enriching for problematic microorganisms. Using most probable number (MPN) counts and 16S rRNA gene sequencing, multiple viable strains of bacteria were identified from stored produced waters, mostly belonging to the Genus , that were capable of growth via fermentation, and produced sulfide when supplied with thiosulfate. No sulfate-reducing bacteria (SRB) were detected through culturing, despite the detection of relatively low numbers of sulfate-reducing lineages by high-throughput 16S rRNA gene sequencing. These results demonstrate that sulfidogenic produced water populations remain viable for years post production and, if left unchecked, have the potential to lead to natural gas souring during shale gas extraction.

摘要

水力压裂页岩地层产出的水有助于深入了解井下的微生物生态和生物地球化学条件。本研究探讨了从马塞勒斯页岩地层采集的产出水样品中分离出的持久性微生物产生硫化物的可能性。硫化氢具有剧毒和腐蚀性,会导致形成“酸性气体”,精炼成本高昂。此外,水力压裂页岩中的微生物定殖可能导致地层堵塞并降低油井产能。评估持久性微生物类群中产生硫化物的可能性至关重要,特别是考虑到将产出水作为注入液回用的趋势,这可能会富集有问题的微生物。通过最大可能数(MPN)计数和16S rRNA基因测序,从储存的产出水中鉴定出多种存活的细菌菌株,它们大多属于 属,能够通过发酵生长,并在提供硫代硫酸盐时产生硫化物。尽管通过高通量16S rRNA基因测序检测到数量相对较少的硫酸盐还原菌谱系,但通过培养未检测到硫酸盐还原菌(SRB)。这些结果表明,产硫化物的产出水菌群在生产后数年仍保持存活,如果不加以控制,有可能在页岩气开采过程中导致天然气酸化。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c277/7046593/11f5eb76c9a9/fmicb-11-00286-g004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c277/7046593/9c484bcef336/fmicb-11-00286-g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c277/7046593/8cfe2cf2fa83/fmicb-11-00286-g002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c277/7046593/de86a01c13cf/fmicb-11-00286-g003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c277/7046593/11f5eb76c9a9/fmicb-11-00286-g004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c277/7046593/9c484bcef336/fmicb-11-00286-g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c277/7046593/8cfe2cf2fa83/fmicb-11-00286-g002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c277/7046593/de86a01c13cf/fmicb-11-00286-g003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c277/7046593/11f5eb76c9a9/fmicb-11-00286-g004.jpg

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