微生物による環境負荷の少ないCO₂回収技術(Microbes may hold the key to greener, cheaper carbon capture)

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2025-06-26 コンコルディア大学

コンコルディア大学の研究チームは、微生物を活用してCO₂を安定な鉱物(炭酸塩)に変換・固定する「ミネラル炭素固定」技術を開発した。微生物が自然に炭酸塩化を促進する受動的手法と、酵素活性で能動的にCO₂を鉱物化する方法の2つを検証。鉱山跡地や土壌、セメント、湿地などでの応用が期待され、低コストかつ環境負荷の少ない炭素除去手段となる。水質浄化や土壌改善などの副次効果も見込まれる。

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炭素隔離のための鉱物炭酸化: MCPとMICPのケース Mineral Carbonation for Carbon Sequestration: A Case for MCP and MICP

Samantha M. Wilcox,Catherine N. Mulligan and Carmen Mihaela Neculita
International Journal of Molecular Sciences  Published: 1 March 2025
DOI:https://doi.org/10.3390/ijms26052230

微生物による環境負荷の少ないCO₂回収技術(Microbes may hold the key to greener, cheaper carbon capture)

Abstract

Mineral carbonation is a prominent method for carbon sequestration. Atmospheric carbon dioxide (CO2) is trapped as mineral carbonate precipitates, which are geochemically, geologically, and thermodynamically stable. Carbonate rocks can originate from biogenic or abiogenic origin, whereby the former refers to the breakdown of biofragments and the latter precipitation out of water. Carbonates can also be formed through biologically controlled mechanisms (BCMs), biologically mediated mechanisms (BMMs), and biologically induced mechanisms (BIMs). Microbial carbonate precipitation (MCP) is a BMM occurring through the interaction of organics (extracellular polymeric substances (EPS), cell wall, etc.) and soluble cations facilitating indirect precipitation of carbonate minerals. Microbially induced carbonate precipitation (MICP) is a BIM occurring via different metabolic pathways. Enzyme-driven pathways (carbonic anhydrase (CA) and/or urease), specifically, are promising for the high conversion to calcium carbonate (CaCO3) precipitation, trapping large quantities of gaseous CO2. These carbonate precipitates can trap CO2 via mineral trapping, solubility trapping, and formation trapping and aid in CO2 leakage reduction in geologic carbon sequestration. Additional experimental research is required to assess the feasibility of MICP for carbon sequestration at large scale for long-term stability of precipitates. Laboratory-scale evaluation can provide preliminary data on preferable metabolic pathways for different materials and their capacity for carbonate precipitation via atmospheric CO2 versus injected CO2.

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