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Depth-dependent geochemical and microbiological gradients in Fe(III) deposits resulting from coal mine-derived acid mine drainage

We evaluated the depth-dependent geochemistry and microbiology of sediments that have developed via the microbially-mediated oxidation of Fe(II) dissolved in acid mine drainage (AMD), giving rise to a 8–10 cm deep “iron mound” that is composed primarily of Fe(III) (hydr)oxide phases. Chemical analys...

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Hlavní autoři: Brantner, Justin S., Haake, Zachary J., Burwick, John E., Menge, Christopher M., Hotchkiss, Shane T., Senko, John M.
Médium: Artigo
Jazyk:Inglês
Vydáno: Frontiers Media S.A. 2014
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On-line přístup:https://ncbi.nlm.nih.gov/pmc/articles/PMC4030175/
https://ncbi.nlm.nih.gov/pubmed/24860562
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.3389/fmicb.2014.00215
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