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添加营养物质或微生物联合体刺激非生产性煤甲烷生成。

Stimulation of methane generation from nonproductive coal by addition of nutrients or a microbial consortium.

机构信息

U.S. Geological Survey, MS430, 12201 Sunrise Valley Drive, Reston, VA 20192, USA.

出版信息

Appl Environ Microbiol. 2010 Nov;76(21):7013-22. doi: 10.1128/AEM.00728-10. Epub 2010 Sep 3.

Abstract

Biogenic formation of methane from coal is of great interest as an underexploited source of clean energy. The goal of some coal bed producers is to extend coal bed methane productivity and to utilize hydrocarbon wastes such as coal slurry to generate new methane. However, the process and factors controlling the process, and thus ways to stimulate it, are poorly understood. Subbituminous coal from a nonproductive well in south Texas was stimulated to produce methane in microcosms when the native population was supplemented with nutrients (biostimulation) or when nutrients and a consortium of bacteria and methanogens enriched from wetland sediment were added (bioaugmentation). The native population enriched by nutrient addition included Pseudomonas spp., Veillonellaceae, and Methanosarcina barkeri. The bioaugmented microcosm generated methane more rapidly and to a higher concentration than the biostimulated microcosm. Dissolved organics, including long-chain fatty acids, single-ring aromatics, and long-chain alkanes accumulated in the first 39 days of the bioaugmented microcosm and were then degraded, accompanied by generation of methane. The bioaugmented microcosm was dominated by Geobacter sp., and most of the methane generation was associated with growth of Methanosaeta concilii. The ability of the bioaugmentation culture to produce methane from coal intermediates was confirmed in incubations of culture with representative organic compounds. This study indicates that methane production could be stimulated at the nonproductive field site and that low microbial biomass may be limiting in situ methane generation. In addition, the microcosm study suggests that the pathway for generating methane from coal involves complex microbial partnerships.

摘要

从煤中生物成因甲烷的形成作为一种未充分开发的清洁能源来源具有重要意义。一些煤层生产商的目标是延长煤层甲烷的生产力,并利用烃类废物(如煤浆)来产生新的甲烷。然而,控制这一过程的因素和机制,以及刺激这一过程的方法,还了解甚少。当向原生种群中添加营养物质(生物刺激)或添加从湿地沉积物中富集的营养物质和细菌及产甲烷菌共生体(生物增强)时,来自德克萨斯州南部一口非生产性油井的次烟煤在微环境中被刺激产生甲烷。营养物质添加富集的原生种群包括假单胞菌属、韦荣氏球菌科和巴氏甲烷八叠球菌。与生物刺激微环境相比,生物增强微环境产生甲烷的速度更快,浓度更高。在生物增强微环境的前 39 天内,溶解有机物(包括长链脂肪酸、单环芳烃和长链烷烃)积累,然后被降解,同时产生甲烷。生物增强微环境以地杆菌属为主,大部分甲烷生成与产甲烷菌 Methanosaeta concilii 的生长有关。培养物与代表性有机化合物孵育证实了生物增强培养物从煤中间产物产生甲烷的能力。本研究表明,在非生产性现场可以刺激甲烷的产生,原位甲烷生成可能受到低微生物生物量的限制。此外,微环境研究表明,从煤中生成甲烷的途径涉及复杂的微生物伙伴关系。

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