添加电子受体刺激油砂端坑湖厌氧甲烷化

Hanna Davidson, Peter Dunfield
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Methane is probably not the limiting factor for AOM in BML- instead, the electron acceptors used in the absence of oxygen are scarce. If microbiological methane removal were to increase after supplementing electron acceptors such as nitrate, sulfate, or iron, then this could be applied to the reclamation of artificial end pit lake systems. Our research aims to illustrate if AOM are present in BML, and if we can stimulate their metabolism via electron acceptor amendment. We performed amplicon and metagenomic sequencing across 5 sediment cores from BML. These cores penetrate over two meters below the water-sediment interface, up to 14 meters below the water’s surface. We designed anaerobic, 13 C-isotope-spiked incubations for this sediment to track if any CH 4 to CO 2 conversion was underway. By tagging methane molecules with 13 C, we are able to follow the biogeochemical transformations and demonstrate if any 13 CH 4 is converted to 13 CO 2 , which would indicate methanotrophic activity. Additionally, microbes who take up 13 C produce heavier DNA, possibly allowing us to identify the DNA of the players at work. Additionally, Illumina sequencing was done on all incubations to compare how electron acceptor addition prompted community shifts. In the incubation experiments, 13 CO 2 is being produced in several core samples incubated without O 2 . This finding indicates that methanotrophs are, in some capacity, active in anoxic conditions. When comparing different amendments of electron acceptors, there did appear to be a significant amount (p = 0.027) of 13 CO 2 produced in the sulfate-added 13 CH 4 treatment (Fig. 1). Other amendments had encouraging results, but were not statistically significant. 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引用次数: 0

摘要

阿尔伯塔油砂开采行业面临的一个主要问题是,如何在尾矿池的使用寿命结束时使其恢复到原来的生态系统功能。这个问题是石油行业最紧迫的问题之一,虽然许多潜在的解决方案正在试验中,但没有一个是没有问题的。一种解决方案是建立尾坑湖(epl),通过在矿坑或尾矿库中填充流动尾矿,并在其上覆盖淡水盖来形成。随着时间的推移,尾矿沉降到湖底并被隔离。截至2018年,有23个计划在阿尔伯塔省油砂开采作业(COSIA 2021)中实施epl,因此通过epl进行油砂回收研究至关重要。阿尔伯塔省只有一个使用尾矿形成的全尺寸EPL,即基矿湖(BML)。自2011年以来一直在进行填海工程。尽管随着时间的推移,BML的水质正在逐渐改善,但一个长期存在的问题是,根深蒂固的碳氢化合物会产生甲烷气泡。这些气泡的沸腾将污染物带入水柱。因此,通过刺激氧化甲烷菌的代谢来限制甲烷产量的潜力引起了人们的兴趣。氧化甲烷菌是一种消耗甲烷的微生物。这些甲烷氧化菌可以是好氧的,在水柱中,或者在沉积物界面下的厌氧,在那里氧气被耗尽。甲烷的厌氧氧化剂,或AOM,是特别感兴趣的,因为甲烷只在厌氧条件下产生。然而,对AOM的研究并不充分,我们对它的认识还存在许多空白。Base Mine Lake提供了一个重要的机会来记录AOM在油砂生态系统中的存在,并确定AOM是否可以在甲烷进入水柱之前去除甲烷。甲烷可能不是BML中AOM的限制因素——相反,在没有氧气的情况下使用的电子受体很少。如果在补充硝酸盐、硫酸盐或铁等电子受体后微生物甲烷去除率增加,那么这可以应用于人工端坑湖系统的复垦。我们的研究目的是阐明AOM是否存在于BML中,以及我们是否可以通过电子受体修饰来刺激它们的代谢。我们对BML的5个沉积物岩心进行了扩增子和宏基因组测序。这些岩心在水-沉积物界面下超过两米深,达到水面以下14米。我们为这种沉积物设计了厌氧、13个碳同位素增加的培养箱,以跟踪是否有任何甲烷到二氧化碳的转化正在进行。通过用13c标记甲烷分子,我们能够跟踪生物地球化学转化,并证明是否有13ch 4转化为13co 2,这将表明甲烷营养活动。此外,吸收13c的微生物会产生更重的DNA,这可能使我们能够识别工作中的玩家的DNA。此外,Illumina测序在所有孵育中进行,以比较电子受体添加如何促进群落转移。在孵育实验中,在没有o2孵育的几个岩心样品中产生了13co2。这一发现表明,在缺氧条件下,甲烷氧化菌在一定程度上是活跃的。当比较不同的电子受体修正时,在添加硫酸盐的13ch4处理中确实产生了大量的13co 2 (p = 0.027)(图1)。其他修正的结果令人鼓舞,但没有统计学意义。正在进行的试验将通过更大的样本量提供更有启发性的结果,这将在夏末完成。接下来,我们将利用扩增子测序和DNA稳定同位素探测来表征孵育后沉积物中的群落。这将不仅表明生物体的身份,而且还将阐明哪些电子受体对哪些群体最有利。这种分析是复杂的,正在进行中。总体而言,高排放人工生态系统的甲烷化研究是一个非常有趣的领域,因为利用甲烷化菌修复和改善生态系统具有很大的潜力,以及人工生态系统中AOM的不断发现。油砂底坑湖泊作为一个文化和政治重点问题引起了人们的兴趣。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Electron Acceptor Addition to Stimulate Anaerobic Methanotrophy in Oil Sands End Pit Lakes
A major question for the Alberta oilsands extraction industry is how to return tailings ponds to their original ecosystem functions at the end of their lifespan. This question is one of the most pressing in the oil industry, and while many potential solutions are being trialed, none are without issue. One solution is the creation of end pit lakes (EPLs), formed by filling a mine pit or tailings pond with fluid tailings and covering this with a freshwater cap. Over time, tailings settle to the bottom of the lake and become sequestered. As of 2018, there were 23 plans to pursue EPLs in Albertan oilsands mining operations (COSIA 2021), so research in oilsands reclamation via EPLs is essential. Alberta has only one full-scale EPL formed using tailings, Base Mine Lake (BML). It has been under reclamation since 2011. Although BML water quality is gradually improving over time, one persistent problem is the production of methane bubbles from the entrenched hydrocarbons. Ebullition of these bubbles carries contaminants into the water column. The potential to limit methane production biologically by stimulating methanotroph metabolism, is therefore of interest. Methanotrophs are microbes that consume methane. These methanotrophs can be aerobic, in the water column, or anaerobic below the sediment interface, where oxygen is depleted. Anaerobic oxidizers of methane, or AOM, are of particular interest due to methane only being produced in anaerobic conditions. However, AOM are not well-studied and there are many gaps in our knowledge about them. Base Mine Lake presents an important opportunity to document the presence of AOM in oilsands ecosystems, and identify if AOM can remove methane before it enters the water column. Methane is probably not the limiting factor for AOM in BML- instead, the electron acceptors used in the absence of oxygen are scarce. If microbiological methane removal were to increase after supplementing electron acceptors such as nitrate, sulfate, or iron, then this could be applied to the reclamation of artificial end pit lake systems. Our research aims to illustrate if AOM are present in BML, and if we can stimulate their metabolism via electron acceptor amendment. We performed amplicon and metagenomic sequencing across 5 sediment cores from BML. These cores penetrate over two meters below the water-sediment interface, up to 14 meters below the water’s surface. We designed anaerobic, 13 C-isotope-spiked incubations for this sediment to track if any CH 4 to CO 2 conversion was underway. By tagging methane molecules with 13 C, we are able to follow the biogeochemical transformations and demonstrate if any 13 CH 4 is converted to 13 CO 2 , which would indicate methanotrophic activity. Additionally, microbes who take up 13 C produce heavier DNA, possibly allowing us to identify the DNA of the players at work. Additionally, Illumina sequencing was done on all incubations to compare how electron acceptor addition prompted community shifts. In the incubation experiments, 13 CO 2 is being produced in several core samples incubated without O 2 . This finding indicates that methanotrophs are, in some capacity, active in anoxic conditions. When comparing different amendments of electron acceptors, there did appear to be a significant amount (p = 0.027) of 13 CO 2 produced in the sulfate-added 13 CH 4 treatment (Fig. 1). Other amendments had encouraging results, but were not statistically significant. Ongoing trials will provide more illuminating results via larger sample sizes, which will be completed by the end of the summer. Next we will characterize communities in the post-incubation sediment, using both amplicon sequencing and DNA stable isotope probing. This will suggest not only the identity of the organisms at play, but will also illuminate which electron acceptors were most beneficial to which groups. This analysis is complex and underway. Overall, the study of methanotrophy in artificial ecosystems with high emissions is an area of great interest, due to the high potential for amendment and improvement of the ecosystems using methanotrophs, as well as the ongoing discovery on AOM in artificial ecosystems. Oilsands end pit lakes are of interest, as an issue of cultural and political emphasis.
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