Growth of Iron(III)-Reducing Bacteria on Clay Minerals as the Sole Electron Acceptor and Comparison of Growth Yields on a Variety of Oxidized Iron Forms
Smectite clay minerals are abundant in soils and sediments worldwide and are typically rich in Fe. While recent investigations have shown that the structural Fe(III) bound in clay minerals is reduced by microorganisms, previous studies have not tested growth with clay minerals as the sole electron a...
محفوظ في:
| الحاوية / القاعدة: | Appl Environ Microbiol |
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| المؤلفون الرئيسيون: | , , , , |
| التنسيق: | Artigo |
| اللغة: | Inglês |
| منشور في: |
American Society for Microbiology (ASM)
2002
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| الموضوعات: | |
| الوصول للمادة أونلاين: | https://ncbi.nlm.nih.govhttps://pmc.ncbi.nlm.nih.gov/articles/PMC134413/ https://ncbi.nlm.nih.govhttps://pubmed.ncbi.nlm.nih.gov/12450850/ https://ncbi.nlm.nih.govhttps://doi.org/10.1128/AEM.68.12.6256-6262.2002 |
| الوسوم: |
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