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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 en: | Front Microbiol |
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| Main Authors: | , , , , |
| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado: |
Frontiers Media S.A.
2016
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| Assuntos: | |
| Acceso en liña: | 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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