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Radiolytic Hydrogen Production in the Subseafloor Basaltic Aquifer
Hydrogen (H(2)) is produced in geological settings by dissociation of water due to radiation from radioactive decay of naturally occurring uranium ((238)U, (235)U), thorium ((232)Th) and potassium ((40)K). To quantify the potential significance of radiolytic H(2) as an electron donor for microbes wi...
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| Publicado no: | Front Microbiol |
|---|---|
| Main Authors: | , , , , |
| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
Frontiers Media S.A.
2016
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| Assuntos: | |
| Acesso em linha: | https://ncbi.nlm.nih.gov/pmc/articles/PMC4740390/ https://ncbi.nlm.nih.gov/pubmed/26870029 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.3389/fmicb.2016.00076 |
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