Enriched iron(III)-reducing bacterial communities are shaped by carbon substrate and iron oxide mineralogy
Iron (Fe) oxides exist in a spectrum of structures in the environment, with ferrihydrite widely considered the most bioavailable phase. Yet, ferrihydrite is unstable and rapidly transforms to more crystalline Fe(III) oxides (e.g., goethite, hematite), which are poorly reduced by model dissimilatory...
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| Hlavní autoři: | , , |
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| Médium: | Artigo |
| Jazyk: | Inglês |
| Vydáno: |
Frontiers Media S.A.
2012-12-01
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| Edice: | Frontiers in Microbiology |
| Témata: | |
| On-line přístup: | http://journal.frontiersin.org/Journal/10.3389/fmicb.2012.00404/full |
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