Rapid microbial methanogenesis during CO2 storage in hydrocarbon reservoirs

Article

关键词: METHANE CLUMPED ISOTOPES;    PANNONIAN BASIN SYSTEM;    CARBON-DIOXIDE;    NOBLE-GAS;    NATURAL-GAS;    STABLE-ISOTOPE;    ANAEROBIC OXIDATION;    PALEOCENE-EOCENE;    DEEP SUBSURFACE;    FORMATION WATER;   

DOI  :  10.1038/s41586-021-04153-3

来源: SCIE

【 摘 要 】

Carbon capture and storage (CCS) is a key technology to mitigate the environmental impact of carbon dioxide (CO2) emissions. An understanding of the potential trapping and storage mechanisms is required to provide confidence in safe and secure CO2 geological sequestration(1,2). Depleted hydrocarbon reservoirs have substantial CO2 storage potential(1,3), and numerous hydrocarbon reservoirs have undergone CO2 injection as a means of enhanced oil recovery (CO2-EOR), providing an opportunity to evaluate the (bio)geochemical behaviour of injected carbon. Here we present noble gas, stable isotope, clumped isotope and gene-sequencing analyses from a CO2-EOR project in the Olla Field (Louisiana, USA). We show that microbial methanogenesis converted as much as 13-19% of the injected CO2 to methane (CH4) and up to an additional 74% of CO2 was dissolved in the groundwater. We calculate an in situ microbial methanogenesis rate from within a natural system of 73-109 millimoles of CH4 per cubic metre (standard temperature and pressure) per year for the Olla Field. Similar geochemical trends in both injected and natural CO2 fields suggest that microbial methanogenesis may be an important subsurface sink of CO2 globally. For CO2 sequestration sites within the environmental window for microbial methanogenesis, conversion to CH4 should be considered in site selection.

【 授权许可】

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