Hyperfine Interactions

, Volume 226, Issue 1–3, pp 601–612 | Cite as

Mössbauer spectroscopy of samples from the 2010 Fimmvörðuháls/Eyjafjallajökull eruption

  • H. P. GunnlaugssonEmail author
  • Á. Höskuldsson
  • S. Steinthorsson
  • N. Óskarsson
  • M. B. Madsen
  • P. Nørnberg
  • J. Merrison
  • G. Larsen


Mössbauer spectra of samples from the 2010 Fimmvörðuháls/Eyjafjallajökull eruption are presented with determinations of the Fe3 + /FeTot ratios. Mössbauer spectra of time series of samples from the Eyjafjallajökull eruption show a change in the characteristics of the erupted material mid-way in the eruption, suggesting changing access of water to the eruption.


Mössbauer spectroscopy Volcanic ash Eyjafjallajökull eruption 2010 Fimmvörðuháls eruption 2010 


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© Springer Science+Business Media Dordrecht 2013

Authors and Affiliations

  • H. P. Gunnlaugsson
    • 1
    Email author
  • Á. Höskuldsson
    • 2
  • S. Steinthorsson
    • 2
  • N. Óskarsson
    • 2
  • M. B. Madsen
    • 3
  • P. Nørnberg
    • 4
  • J. Merrison
    • 1
  • G. Larsen
    • 2
  1. 1.Department of Physics and AstronomyAarhus UniversityAarhus CDenmark
  2. 2.NORDVULK, Institute of Earth Sciences, AskjaUniversity of IcelandReykjavikIceland
  3. 3.Niels Bohr InstituteUniversity of CopenhagenCopenhagen ØDenmark
  4. 4.Department of Earth SciencesAarhus UniversityAarhus CDenmark

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