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Impacts of NO 2 Impurities on the Indigenous Microbial Community Structure and Diversity in CO 2 -Saline-Sandstone Interaction System

Author

Listed:
  • Chenyang Li

    (Key Laboratory of Groundwater Resources and Environment, Ministry of Education, Jilin University, Changchun 130021, China
    Key Laboratory of Songliao Aquatic Environment, Ministry of Education, Jilin Jianzhu University, Changchun 130118, China
    Jilin Provincial Key Laboratory of Water Resources and Environment, Jilin University, Changchun 130026, China)

  • Yunpeng Song

    (Key Laboratory of Groundwater Resources and Environment, Ministry of Education, Jilin University, Changchun 130021, China
    Tianjin Municipal Engineering Design & Research Institute, Tianjin 300392, China)

  • Yongjuan Zhu

    (School of Chemistry and Materials Engineering, Huizhou University, Huizhou 516007, China)

  • Qingwei Meng

    (Changchun Monitoring Station of National Urban Water Supply Quality Monitoring Network, Changchun 130000, China)

  • Ying Lyu

    (Key Laboratory of Groundwater Resources and Environment, Ministry of Education, Jilin University, Changchun 130021, China
    Jilin Provincial Key Laboratory of Water Resources and Environment, Jilin University, Changchun 130026, China)

Abstract

Laboratory experiments (150 days) were performed to analyze the influence of NO 2 impurities on indigenous microbial communities and diversity with 16S rRNA sequence at real GCS site (Geological CO 2 Sequestration, ordos, China) conditions (pressure: 15 MPa, temperature: 55 °C). The possible impact of metabolic activity on the GCS process was investigated through the BLASTn search. Compared with the pure CO 2 , results demonstrate that the biomass and biodiversity were lower, due to the lower pH, within 60 days after the co-injection of 0.1% NO 2 . Subsequently, the pH was quickly buffered through the corrosion of feldspar and clay, and the impact of NO 2 had almost no obvious effect on the microbial structure except the abundance of phylum and genus after 90 days. In addition, acid-producing bacteria appeared after 60 days, such as Bacillus , Acinetobacter, and Lactococcus , etc., lower the pH in the solution and accelerate the dissolution of minerals. The Fe (III)-reducing microbes Citrobacter freundii reduce the Fe (III) released from minerals to Fe (II) and induce siderite (FeCO 3 ) biomineralization through biogeochemical processes. Therefore, the co-injection of trace NO 2 will not significantly affect the growth of microorganisms on long timescale.

Suggested Citation

  • Chenyang Li & Yunpeng Song & Yongjuan Zhu & Qingwei Meng & Ying Lyu, 2021. "Impacts of NO 2 Impurities on the Indigenous Microbial Community Structure and Diversity in CO 2 -Saline-Sandstone Interaction System," Sustainability, MDPI, vol. 13(11), pages 1-16, May.
  • Handle: RePEc:gam:jsusta:v:13:y:2021:i:11:p:5916-:d:561283
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