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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Detalles Bibliográficos
Autores principales: Dzaugis, Mary E., Spivack, Arthur J., Dunlea, Ann G., Murray, Richard W., D’Hondt, Steven
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Frontiers Media S.A. 2016
Materias:
Microbiology
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4740390/
https://www.ncbi.nlm.nih.gov/pubmed/26870029
http://dx.doi.org/10.3389/fmicb.2016.00076

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4740390/
https://www.ncbi.nlm.nih.gov/pubmed/26870029
http://dx.doi.org/10.3389/fmicb.2016.00076

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