Radiolytic hydrogen production in the subseafloor basaltic aquifer

Hydrogen (H<sub>2</sub>) is produced in geological settings by dissociation of water due to radiation from radioactive decay of naturally occurring uranium (<sup>238</sup>U, <sup>235</sup>U), thorium (<sup>232</sup>Th) and potassium (<sup>40</...

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Bibliographic Details
Main Authors: Mary E Dzaugis, Arthur J Spivack, Ann G Dunlea, Richard W Murray, Steven eD'Hondt
Format: Article
Language:English
Published: Frontiers Media S.A. 2016-02-01
Series:Frontiers in Microbiology
Subjects:
Online Access:http://journal.frontiersin.org/Journal/10.3389/fmicb.2016.00076/full