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Biological CO2 conversion to acetate in subsurface coal-sand formation using a high-pressure reactor system

机译:使用高压反应器系统将二氧化碳从地下煤砂地层中生物转化为乙酸盐

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摘要

Geological CO2 sequestration in unmineable subsurface oil/gas fields and coal formations has been proposed as a means of reducing anthropogenic greenhouse gasses in the atmosphere. However, the feasibility of injecting CO2 into subsurface depends upon a variety of geological and economic conditions, and the ecological consequences are largely unpredictable. In this study, we developed a new flow-through-type reactor system to examine potential geophysical, geochemical and microbiological impacts associated with CO2 injection by simulating in-situ pressure (0–100 MPa) and temperature (0–70°C) conditions. Using the reactor system, anaerobic artificial fluid and CO2 (flow rate: 0.002 and 0.00001 ml/min, respectively) were continuously supplemented into a column comprised of bituminous coal and sand under a pore pressure of 40 MPa (confined pressure: 41 MPa) at 40°C for 56 days. 16S rRNA gene analysis of the bacterial components showed distinct spatial separation of the predominant taxa in the coal and sand over the course of the experiment. Cultivation experiments using sub-sampled fluids revealed that some microbes survived, or were metabolically active, under CO2-rich conditions. However, no methanogens were activated during the experiment, even though hydrogenotrophic and methylotrophic methanogens were obtained from conventional batch-type cultivation at 20°C. During the reactor experiment, the acetate and methanol concentration in the fluids increased while the δ13Cacetate, H2 and CO2 concentrations decreased, indicating the occurrence of homo-acetogenesis. 16S rRNA genes of homo-acetogenic spore-forming bacteria related to the genus Sporomusa were consistently detected from the sandstone after the reactor experiment. Our results suggest that the injection of CO2 into a natural coal-sand formation preferentially stimulates homo-acetogenesis rather than methanogenesis, and that this process is accompanied by biogenic CO2 conversion to acetate.
机译:有人提出在不可开采的地下油气田和煤层中进行地质二氧化碳封存,作为减少大气中人为温室气体的一种手段。但是,将二氧化碳注入地下的可行性取决于各种地质和经济条件,其生态后果在很大程度上是不可预测的。在这项研究中,我们开发了一种新的流通式反应器系统,通过模拟现场压力(0–100 MPa)和温度(0–70°C)条件来检查与二氧化碳注入相关的潜在地球物理,地球化学和微生物影响。使用反应器系统,在40 MPa(封闭压力:41 MPa)的孔隙压力下,将厌氧人工流体和CO2(流速分别为0.002和0.00001 ml / min)连续补充到由烟煤和沙子组成的塔中。 40°C持续56天。在整个实验过程中,细菌成分的16S rRNA基因分析表明,煤和沙中主要类群的空间分布明显不同。使用次采样液进行的培养实验表明,某些微生物在富含CO2的条件下可以存活或具有代谢活性。但是,即使在20°C的常规分批培养中获得了氢营养型和甲基营养型产甲烷菌,实验期间也没有激活产甲烷菌。在反应器实验过程中,流体中的乙酸和甲醇浓度增加,而δ 13 乙酸盐,H2和CO2浓度降低,表明发生了均相产乙酸。在反应堆实验后,从砂岩中一致地检测到与孢子菌属有关的同产乙酸的产芽孢细菌的16S rRNA基因。我们的结果表明,向天然煤砂地层中注入CO2优先刺激均相产乙酸而不是甲烷生成,并且该过程伴随有生物成因的CO2转化为乙酸盐。

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