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地下水中甲烷氧化与甲基营养菌种群动态。

Methane oxidation and methylotroph population dynamics in groundwater mesocosms.

机构信息

Department of Geoscience, University of Calgary, Calgary, Alberta, Canada.

Shell International Exploration and Production Inc, Westhollow Technology Center, Houston, TX, USA.

出版信息

Environ Microbiol. 2020 Apr;22(4):1222-1237. doi: 10.1111/1462-2920.14929. Epub 2020 Feb 7.

Abstract

Extraction of natural gas from unconventional hydrocarbon reservoirs by hydraulic fracturing raises concerns about methane migration into groundwater. Microbial methane oxidation can be a significant methane sink. Here, we inoculated replicated, sand-packed, continuous mesocosms with groundwater from a field methane release experiment. The mesocosms experienced thirty-five weeks of dynamic methane, oxygen and nitrate concentrations. We determined concentrations and stable isotope signatures of methane, carbon dioxide and nitrate and monitored microbial community composition of suspended and attached biomass. Methane oxidation was strictly dependent on oxygen availability and led to enrichment of C in residual methane. Nitrate did not enhance methane oxidation under oxygen limitation. Methylotrophs persisted for weeks in the absence of methane, making them a powerful marker for active as well as past methane leaks. Thirty-nine distinct populations of methylotrophic bacteria were observed. Methylotrophs mainly occurred attached to sediment particles. Abundances of methanotrophs and other methylotrophs were roughly similar across all samples, pointing at transfer of metabolites from the former to the latter. Two populations of Gracilibacteria (Candidate Phyla Radiation) displayed successive blooms, potentially triggered by a period of methane famine. This study will guide interpretation of future field studies and provides increased understanding of methylotroph ecophysiology.

摘要

水力压裂法从非常规碳氢化合物储层中提取天然气引起了人们对甲烷迁移到地下水中的担忧。微生物甲烷氧化可以成为一个重要的甲烷汇。在这里,我们用来自现场甲烷释放实验的地下水接种了复制的、沙填充的、连续的中观模型。中观模型经历了 35 周的动态甲烷、氧气和硝酸盐浓度。我们测定了甲烷、二氧化碳和硝酸盐的浓度和稳定同位素特征,并监测了悬浮和附着生物量的微生物群落组成。甲烷氧化严格依赖于氧气的可用性,并导致残留甲烷中 C 的富集。在氧气限制下,硝酸盐并没有增强甲烷氧化。在没有甲烷的情况下,甲基营养菌可以存活数周,这使它们成为活跃的和过去的甲烷泄漏的有力标志物。观察到 39 种不同的甲基营养细菌种群。甲基营养菌主要附着在沉积物颗粒上。在所有样品中,甲烷营养菌和其他甲基营养菌的丰度大致相似,表明代谢物从前一种转移到后一种。两个 Gracilibacteria 种群(候选门辐射)相继出现,可能是由一段甲烷匮乏期引发的。本研究将指导未来现场研究的解释,并提高对甲基营养菌生理生态学的理解。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/cb5f/7187433/5f4c00dff0e2/EMI-22-1222-g001.jpg

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