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Hekla cold springs (Iceland): groundwater mixing with magmatic gases
Stockholm University, Faculty of Science, Department of Geological Sciences.
Stockholm University, Faculty of Science, Department of Geological Sciences.
2010 (English)In: Isotopes in environmental and health studies, ISSN 1025-6016, E-ISSN 1477-2639, Vol. 46, no 2, 180-189 p.Article in journal (Refereed) Published
Abstract [en]

We have analysed the chemical and stable isotope compositions of four springwaters situated just northwest of the Hekla volcano, where cold water emerges from the base of the lava flows. The stable isotope ratios of water (H, O), dissolved inorganic carbon (C) and sulphate (S) were used to determine whether magmatic gases are mixing with the groundwater. The waters can be characterised as Na-HCO3 type. The results show that deep-seated gases mix with groundwater, substantially affecting the concentration of solutes and the isotopic composition of dissolved carbon and sulphate.

Place, publisher, year, edition, pages
2010. Vol. 46, no 2, 180-189 p.
Keyword [en]
Hekla volcano, Iceland, groundwater, magmatic inputs, carbon-13, isotope ecology, hydrogen-2, oxygen-18, sulphur-34
National Category
Earth and Related Environmental Sciences
Identifiers
URN: urn:nbn:se:su:diva-50652DOI: 10.1080/10256016.2010.488814ISI: 000279219100005OAI: oai:DiVA.org:su-50652DiVA: diva2:383249
Note
authorCount :4Available from: 2011-01-04 Created: 2010-12-30 Last updated: 2017-12-11Bibliographically approved

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