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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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| 出版年: | Front Microbiol |
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| 主要な著者: | , , , , |
| フォーマット: | Artigo |
| 言語: | Inglês |
| 出版事項: |
Frontiers Media S.A.
2016
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| 主題: | |
| オンライン･アクセス: | 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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