Hydrogen from Radiolysis of Aqueous Fluid Inclusions during Diagenesis

John Parnell* (Corresponding Author), Nigel Blamey

*Corresponding author for this work

Research output: Contribution to journalArticle

2 Citations (Scopus)
4 Downloads (Pure)

Abstract

A suite of Permian sylvite samples from Boulby potash mine, Yorkshire, UK, consistently yield traces of hydrogen upon analysis by a cold crush technique for liberating volatiles from entrapped fluid inclusions. In contrast, accompanying halite samples do not yield hydrogen. These data suggest the formation of hydrogen by radiolysis of water due to irradiation from potassium in the sylvite. The data indicate radiolysis as a mechanism for subsurface hydrogen generation, where it is available as an electron donor for a deep biosphere.

Original languageEnglish
Article number130
Pages (from-to)1-8
Number of pages8
JournalMinerals
Volume7
Issue number8
DOIs
Publication statusPublished - 25 Jul 2017

Fingerprint

Radiolysis
fluid inclusion
diagenesis
hydrogen
sylvite
Hydrogen
Fluids
Potash mines
potash
halite
Sodium chloride
biosphere
Potassium
irradiation
Permian
potassium
Irradiation
electron
Electrons
Water

Keywords

  • Boulby mine
  • Deep biosphere
  • Fluid inclusions
  • Halite
  • Hydrogen
  • Radiolysis
  • Sylvite

ASJC Scopus subject areas

  • Geotechnical Engineering and Engineering Geology
  • Geology

Cite this

Hydrogen from Radiolysis of Aqueous Fluid Inclusions during Diagenesis. / Parnell, John (Corresponding Author); Blamey, Nigel.

In: Minerals, Vol. 7, No. 8, 130, 25.07.2017, p. 1-8.

Research output: Contribution to journalArticle

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