We have located links that may give you full text access.
Microbially Induced Formation of Fe Carbonates by Metal-Reducing Bacteria Enriched from a CO₂ Repository Candidate Site.
Journal of Nanoscience and Nanotechnology 2018 Februrary 2
The objectives of this research were to study the microbial diversity of metal-reducing bacteria enriched from sedimentary rock collected from a CO2 repository candidate site and to examine the effect that the bicarbonate concentration had on the iron reduction and biomineralization by the cultures. The enriched metal-reducing bacteria (i.e., JG-3) consisted mostly of Exiguobacterium sp. and Shewanella sp., and the microbial reduction of akaganeite (β-FeOOH), an Fe(III) oxyhydroxide, was examined over 7 days of bacterial cultivation at 30 °C under different concentrations of bicarbonate (0~210 mM). The akaganeite (β-FeOOH) transformed into goethite (α-FeOOH) and magnetite (Fe3O4) in low HCO-3 buffered medium (<70 mM) and was transformed to magnetite and siderite (FeCO3) in high HCO-3 buffered medium (>140 mM). These results indicate that metal- reducing bacteria from a deep subsurface environment reduce and transform an iron oxyhydroxide to siderite (FeCO3) in HCO-3 buffered medium and that microbial iron reduction may accelerate the mineral trapping of CO2 for deep geologic sequestration.
Full text links
Related Resources
Get seemless 1-tap access through your institution/university
For the best experience, use the Read mobile app
All material on this website is protected by copyright, Copyright © 1994-2024 by WebMD LLC.
This website also contains material copyrighted by 3rd parties.
By using this service, you agree to our terms of use and privacy policy.
Your Privacy Choices
You can now claim free CME credits for this literature searchClaim now
Get seemless 1-tap access through your institution/university
For the best experience, use the Read mobile app